1.
Terrain cartography
–
Terrain or relief is an essential aspect of physical geography, and as such its portrayal presents a central problem in cartography, and more recently GIS and geovisualization. The most obvious way to depict relief is to imitate it at scale, as in molded or sculpted solid terrain models, because of the disparity between the horizontal and vertical scales of maps, raised relief is typically exaggerated. On flat paper maps and computer screens, terrain can be depicted in a variety of ways, the most ancient form of relief depiction in cartography, hill profiles are simply illustrations of mountains and hills in profile, placed as appropriate on generally small-scale maps. They are seldom used today except as part of an antique styling, hachures are also an older mode of representing relief. They are a form of shading, although different from the one used in shaded maps and they show the orientation of slope, and by their thickness and overall density they provide a general sense of steepness. Being non-numeric, they are useful to a scientific survey than contours. Hachure representation of relief was standardized by the Austrian topographer Johann Georg Lehmann in 1799, contour lines are isolines showing equal elevation. This is the most common way of numerically showing elevation, and is familiar from topographic maps, most 18th and early 19th century national surveys did not record relief across the entire area of coverage, calculating only spot elevations at survey points. Hypsometric tints are used to indicate elevation, usually together with contour lines. They can be used to depict ranges of elevation as bands of color, usually in a graduated scheme, a typical scheme progresses from dark greens for lower elevations up through yellows/browns, and on to grays and white at the highest elevations. Shaded relief, or hill-shading, simulates the cast shadow thrown upon a raised relief map, the shadows normally follow the English convention of top-left lighting in which the light source is placed near the upper-left corner of the map. If the map is oriented with north at the top, the result is that the light appears to come from the north-west. Many people have pointed out that this is unrealistic for maps of the hemisphere, because the sun does not shine from that direction. However, the convention is followed to avoid multistable perception illusions. Much work has been done in recreating the work of Swiss master Eduard Imhof, widely regarded as the master of manual hill-shading technique. Imhofs contributions included an approach to shading, with purples in valleys. The use of illumination and shadow to produce an appearance of space on a flat-surfaced map closely parallels the painting technique known as chiaroscuro. Shaded relief today can be created digitally, using a digital elevation model as its basis, the DEM may be converted to shaded relief using software such as Photoshop, QGIS, GRASS GIS or ArcMaps Spatial Analyst extension
Terrain cartography
–
From a 1639 map of
Hispaniola by Joan Vinckenboons, showing use of hill profiles
Terrain cartography
–
USGS topographic map of
Stowe, Vermont with contour lines at 20-foot intervals
Terrain cartography
–
Dufour map of
Bern (1907); this is a shaded hachure map.
Terrain cartography
–
Siegfried map of
Bernina Pass (1877) with black, blue and brown contour lines at 30-meter intervals
2.
Shaded relief
–
Terrain or relief is an essential aspect of physical geography, and as such its portrayal presents a central problem in cartography, and more recently GIS and geovisualization. The most obvious way to depict relief is to imitate it at scale, as in molded or sculpted solid terrain models, because of the disparity between the horizontal and vertical scales of maps, raised relief is typically exaggerated. On flat paper maps and computer screens, terrain can be depicted in a variety of ways, the most ancient form of relief depiction in cartography, hill profiles are simply illustrations of mountains and hills in profile, placed as appropriate on generally small-scale maps. They are seldom used today except as part of an antique styling, hachures are also an older mode of representing relief. They are a form of shading, although different from the one used in shaded maps and they show the orientation of slope, and by their thickness and overall density they provide a general sense of steepness. Being non-numeric, they are useful to a scientific survey than contours. Hachure representation of relief was standardized by the Austrian topographer Johann Georg Lehmann in 1799, contour lines are isolines showing equal elevation. This is the most common way of numerically showing elevation, and is familiar from topographic maps, most 18th and early 19th century national surveys did not record relief across the entire area of coverage, calculating only spot elevations at survey points. Hypsometric tints are used to indicate elevation, usually together with contour lines. They can be used to depict ranges of elevation as bands of color, usually in a graduated scheme, a typical scheme progresses from dark greens for lower elevations up through yellows/browns, and on to grays and white at the highest elevations. Shaded relief, or hill-shading, simulates the cast shadow thrown upon a raised relief map, the shadows normally follow the English convention of top-left lighting in which the light source is placed near the upper-left corner of the map. If the map is oriented with north at the top, the result is that the light appears to come from the north-west. Many people have pointed out that this is unrealistic for maps of the hemisphere, because the sun does not shine from that direction. However, the convention is followed to avoid multistable perception illusions. Much work has been done in recreating the work of Swiss master Eduard Imhof, widely regarded as the master of manual hill-shading technique. Imhofs contributions included an approach to shading, with purples in valleys. The use of illumination and shadow to produce an appearance of space on a flat-surfaced map closely parallels the painting technique known as chiaroscuro. Shaded relief today can be created digitally, using a digital elevation model as its basis, the DEM may be converted to shaded relief using software such as Photoshop, QGIS, GRASS GIS or ArcMaps Spatial Analyst extension
Shaded relief
–
From a 1639 map of
Hispaniola by Joan Vinckenboons, showing use of hill profiles
Shaded relief
–
USGS topographic map of
Stowe, Vermont with contour lines at 20-foot intervals
Shaded relief
–
Dufour map of
Bern (1907); this is a shaded hachure map.
Shaded relief
–
Siegfried map of
Bernina Pass (1877) with black, blue and brown contour lines at 30-meter intervals
3.
Nablus
–
Nablus is a city in the northern West Bank, approximately 49 kilometers north of Jerusalem, with a population of 126,132. The city was named by the Roman Emperor Vespasian in 72 CE as Flavia Neapolis, since then, Nablus has been ruled by many empires over the course of its almost 2, 000-year-long history. In 636, Neapolis, along with most of Palestine, came under the rule of the Islamic Arab Caliphate of Umar ibn al-Khattab, its name Arabicized to Nablus. In 1099, the Crusaders took control of the city for less than a century, leaving its mixed Muslim, after Saladins Ayyubid forces took control of the interior of Palestine in 1187, Islamic rule was reestablished, and continued under the Mamluk and Ottoman empires to follow. Following its incorporation into the Ottoman Empire in 1517, Nablus was designated capital of the Jabal Nablus district, when Ottoman rule was firmly reestablished in 1841, Nablus prospered as a center of trade. After the city was captured by British forces during World War I, during the 1948 Arab–Israeli War, the city was captured and occupied by Transjordan, which subsequently annexed it unilaterally, until its occupation by Israel during the 1967 Six-Day War. Today, the population is predominantly Muslim, with small Christian and Samaritan minorities, since 1995, the city has been governed by the Palestinian National Authority. In the Old City, there are a number of sites of archaeological significance, culturally, the city is known for its kanafeh, a popular sweet throughout the Middle East, and its soap industry. Flavia Neapolis was named in 72 CE by the Roman emperor Vespasian and applied to an older Samaritan village, variously called Mabartha or Mamorpha. Located between Mount Ebal and Mount Gerizim, the new city lay 2 kilometers west of the Biblical city of Shechem which was destroyed by the Romans that same year during the First Jewish-Roman War, holy places at the site of the citys founding include Josephs Tomb and Jacobs Well. Due to the citys strategic position and the abundance of water from nearby springs, Neapolis prospered, accumulating extensive territory. Insofar as the topography of the site would allow, the city was built on a Roman grid plan and settled with veterans who fought in the victorious legions. In the 2nd century CE, Emperor Hadrian built a theater in Neapolis that could seat up to 7,000 people. Coins found in Nablus dating to this period depict Roman military emblems and gods and goddesses of the Greek pantheon such as Zeus, Artemis, Serapis, Neapolis was entirely pagan at this time. Justin Martyr who was born in the city c.100 CE, came into contact with Platonism, the city flourished until the civil war between Septimius Severus and Pescennius Niger in 198–9 CE. Having sided with Niger, who was defeated, the city was stripped of its legal privileges by Severus. In 244 CE, Philip the Arab transformed Flavius Neapolis into a Roman colony named Julia Neapolis and it retained this status until the rule of Trebonianus Gallus in 251 CE. The Encyclopaedia Judaica speculates that Christianity was dominant in the 2nd or 3rd century and it is known for certain that a bishop from Nablus participated in the Council of Nicaea in 325 CE
Nablus
–
Nablus, 2014
Nablus
–
Municipal Seal of Nablus
Nablus
–
Ruins from antiquity in a residential area in Nablus, 2008
Nablus
–
Minaret and entrance of 10th century Great Mosque of Nablus, 1908
4.
West Bank
–
The West Bank shares boundaries to the west, north, and south with Israel, and to the east, across the Jordan River, with Jordan. The West Bank also contains a significant section of the western Dead Sea shore, the West Bank, including East Jerusalem, has a land area of 5,640 km2 plus a water area of 220 km2, consisting of the northwest quarter of the Dead Sea. As of July 2015 it has an population of 2,785,366 Palestinians, and approximately 371,000 Israeli settlers. The international community considers Israeli settlements in the West Bank, including East Jerusalem, illegal under international law and this annexation was recognized only by Britain, Iraq and Pakistan. The term was chosen to differentiate the west bank of the River Jordan from the east bank of this river, the neo-Latin name Cisjordan or Cis-Jordan is the usual name for the territory in the Romance languages and Hungarian. The name West Bank, however, has become the standard usage for this entity in English. The analogous Transjordan has historically used to designate the region now roughly comprising the state of Jordan. From 1517 through 1917, the now known as the West Bank was under Ottoman rule as part of the provinces of Syria. At the 1920 San Remo conference, the victorious Allied powers allocated the area to the British Mandate of Palestine, the San Remo Resolution adopted on 25 April 1920 incorporated the Balfour Declaration of 1917. It and Article 22 of the Covenant of the League of Nations were the basic documents upon which the British Mandate for Palestine was constructed. Faced with the determination of Emir Abdullah to unify Arab lands under the Hashemite banner, the West Bank area, was conquered by Jordan during the 1948 war with the new state of Israel. In 1947, it was designated as part of a proposed Arab state by the United Nations partition plan for Palestine. 1949 Armistice Agreements defined the boundary between Israel and Jordan. In 1950, Transjordan annexed the area west of the Jordan River, naming it West Bank or Cisjordan, Jordan ruled over the West Bank from 1948 until 1967. Jordans annexation was never recognized by the international community, with the exception of the United Kingdom. King Abdullah of Jordan had been crowned King of Jerusalem by the Coptic Bishop on 15 November 1948. and granted Palestinian Arabs in the West Bank, in June 1967, the West Bank and East Jerusalem were captured by Israel as a result of the Six-Day War. With the exception of East Jerusalem and the former Israeli-Jordanian no mans land, the Israeli settlements were, on the other hand, administered subsequently as Judea and Samaria Area directly by Israel. Since the 1993 Oslo Accords, the Palestinian Authority officially controls a geographically non-contiguous territory comprising approx, 11% of the West Bank which remains subject to Israeli incursions
West Bank
–
City of
Salfit, West Bank
West Bank
–
City of
Bethlehem, West Bank
West Bank
–
The Cave of the Patriarchs is one of the most famous holy sites in the region.
West Bank
–
City of
Jericho, West Bank
5.
Map
–
A map is a symbolic depiction emphasizing relationships between elements of some space, such as objects, regions, or themes. Many maps are static, fixed to paper or some other durable medium, although the earliest maps known are of the heavens, geographic maps of territory have a very long tradition and exist from ancient times. The word map comes from the medieval Latin Mappa mundi, wherein mappa meant napkin or cloth, thus, map became the shortened term referring to a two-dimensional representation of the surface of the world. Cartography or map-making is the study and practice of crafting representations of the Earth upon a flat surface, in addition to location information maps may also be used to portray contour lines indicating constant values of elevation, temperature, rainfall, etc. The orientation of a map is the relationship between the directions on the map and the compass directions in reality. The word orient is derived from Latin oriens, meaning East, in the Middle Ages many maps, including the T and O maps, were drawn with East at the top. Today, the most common – but far from universal – cartographic convention is that North is at the top of a map, several kinds of maps are often traditionally not oriented with North at the top, Maps from non-Western traditions are oriented a variety of ways. Old maps of Edo show the Japanese imperial palace as the top, labels on the map are oriented in such a way that you cannot read them properly unless you put the imperial palace above your head. Medieval European T and O maps such as the Hereford Mappa Mundi were centred on Jerusalem with East at the top, indeed, prior to the reintroduction of Ptolemys Geography to Europe around 1400, there was no single convention in the West. Portolan charts, for example, are oriented to the shores they describe, Maps of cities bordering a sea are often conventionally oriented with the sea at the top. Route and channel maps have traditionally been oriented to the road or waterway they describe, polar maps of the Arctic or Antarctic regions are conventionally centred on the pole, the direction North would be towards or away from the centre of the map, respectively. Typical maps of the Arctic have 0° meridian towards the bottom of the page, reversed maps, also known as Upside-Down maps or South-Up maps, reverse the North is up convention and have south at the top. Buckminster Fullers Dymaxion maps are based on a projection of the Earths sphere onto an icosahedron, the resulting triangular pieces may be arranged in any order or orientation. Modern digital GIS maps such as ArcMap typically project north at the top of the map, compass decimal degrees can be converted to math degrees by subtracting them from 450, if the answer is greater than 360, subtract 360. The scale statement may be taken as exact when the region mapped is small enough for the curvature of the Earth to be neglected, over larger regions where the curvature cannot be ignored we must use map projections from the curved surface of the Earth to the plane. Thus for map projections we must introduce the concept of point scale, which is a function of position, although the scale statement is nominal it is usually accurate enough for all but the most precise of measurements. Large scale maps, say 1,10,000, cover relatively small regions in detail and small scale maps, say 1,10,000,000, cover large regions such as nations, continents. The large/small terminology arose from the practice of writing scales as numerical fractions, there is no exact dividing line between large and small but 1/100,000 might well be considered as a medium scale
Map
–
World map (2004,
CIA World Factbook)
Map
–
World map (1689,
Amsterdam)
Map
–
A celestial map from the 17th century, by the cartographer
Frederik de Wit
Map
–
The
Hereford Mappa Mundi from about 1300,
Hereford Cathedral, England, is a classic "T-O" map with Jerusalem at centre, east toward the top, Europe the bottom left and Africa on the right.
6.
Scale (map)
–
The scale of a map is the ratio of a distance on the map to the corresponding distance on the ground. This simple concept is complicated by the curvature of the Earths surface, because of this variation, the concept of scale becomes meaningful in two distinct ways. The first way is the ratio of the size of the globe to the size of the Earth. The generating globe is a model to which the Earth is shrunk. The ratio of the Earths size to the generating globes size is called the nominal scale, many maps state the nominal scale and may even display a bar scale to represent it. The second distinct concept of scale applies to the variation in scale across a map and it is the ratio of the mapped points scale to the nominal scale. In this case means the scale factor. If the region of the map is small enough to ignore Earths curvature—a town plan, in maps covering larger areas, or the whole Earth, the maps scale may be less useful or even useless in measuring distances. The map projection becomes critical in understanding how scale varies throughout the map, when scale varies noticeably, it can be accounted for as the scale factor. Tissots indicatrix is often used to illustrate the variation of point scale across a map, map scales may be expressed in words, as a ratio, or as a fraction. Examples are, one centimetre to one hundred metres or 1,10,000 or 1/10,000 one inch to one mile or 1,63,360 or 1/63,360 one centimetre to one thousand kilometres or 1,100,000,000 or 1/100,000,000. In addition to the many maps carry one or more bar scales. For example, some modern British maps have three bar scales, one each for kilometres, miles and nautical miles, a lexical scale may cause problems if it expressed in a language that the user does not understand or in obsolete or ill-defined units. For example, a scale of one inch to a furlong will be understood by older people in countries where Imperial units used to be taught in schools. A map is classified as small scale or large scale or sometimes medium scale, small scale refers to world maps or maps of large regions such as continents or large nations. In other words, they show areas of land on a small space. They are called small scale because the fraction is relatively small. Large scale maps show areas in more detail, such as county maps or town plans might
Scale (map)
–
The Winkel tripel projection with
Tissot's indicatrix of deformation
7.
Terrain
–
Terrain or relief is the vertical and horizontal dimension of the land surface. When relief is described underwater, the term bathymetry is used, the Latin Word Terra, is Earth. Terrain is used as a term in physical geography, referring to the lay of the land. This is usually expressed in terms of the elevation, slope, terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns, complex arrays of relief data are used as input parameters for hydrology transport models to allow prediction of river water quality. Understanding terrain also supports soil conservation, especially in agriculture, contour ploughing is an established practice enabling sustainable agriculture on sloping land, it is the practice of ploughing along lines of equal elevation instead of up and down a slope. Terrain is militarily critical because it determines the ability of armed forces to take and hold areas, an understanding of terrain is basic to both defensive and offensive strategy. Terrain is important in determining weather patterns, two areas geographically close to each other may differ radically in precipitation levels or timing because of elevation differences or a rain shadow effect. Precise knowledge of terrain is vital in aviation, especially for low-flying routes and maneuvers, terrain will also affect range and performance of radars and terrestrial radio navigation systems. Furthermore, a hilly or mountainous terrain can strongly impact the implementation of a new aerodrome, relief refers specifically to the quantitative measurement of vertical elevation change in a landscape. It is the difference between maximum and minimum elevations within an area, usually of limited extent. The relief of a landscape can change with the size of the area over which it is measured, making the definition of the scale over which it is measured very important. Because it is related to the slope of surfaces within the area of interest and to the gradient of any streams present, the relief of a landscape is a useful metric in the study of the Earths surface. Relief energy, which may be defined inter alia as the height range in a regular grid, is essentially an indication of the ruggedness or relative height of the terrain. Geomorphology is in part the study of the formation of terrain or topography. Terrain is formed by intersecting processes, Geological processes, Migration of tectonic plates, faulting and folding, volcanic eruptions, erosional processes, water and wind erosion, landslides. Tectonic processes such as orogenies cause land to be elevated, land surface parameters are quantitative measures of various morphometric properties of a surface. The most common examples are used to derive slope or aspect of a terrain or curvatures at each location and these measures can also be used to derive hydrological parameters that reflect flow/erosion processes
Terrain
–
A shaded and colored image (i.e. terrain is enhanced) of varied terrain from the
Shuttle Radar Topography Mission. This shows
elevation model of New Zealand's
Alpine Fault running about 500 km (300 mi) long. The
escarpment is flanked by a vast chain of hills between the
fault and the
mountains of
New Zealand 's
Southern Alps. Northeast is towards the top.
Terrain
–
Present-day
Earth altimetry and
bathymetry. Data from the
National Geophysical Data Center 's TerrainBase Digital Terrain Model.
8.
Contour line
–
A contour line of a function of two variables is a curve along which the function has a constant value. It is a cross-section of the graph of the function f parallel to the x, y plane. In cartography, a contour line joins points of elevation above a given level. A contour map is a map illustrated with contour lines, for example a map, which thus shows valleys and hills. The contour interval of a map is the difference in elevation between successive contour lines. More generally, a line for a function of two variables is a curve connecting points where the function has the same particular value. The gradient of the function is always perpendicular to the contour lines, when the lines are close together the magnitude of the gradient is large, the variation is steep. A level set is a generalization of a line for functions of any number of variables. Contour lines are curved, straight or a mixture of lines on a map describing the intersection of a real or hypothetical surface with one or more horizontal planes. The configuration of these contours allows map readers to infer relative gradient of a parameter, in the latter case, the method of interpolation affects the reliability of individual isolines and their portrayal of slope, pits and peaks. Contour lines are given specific names beginning iso- according to the nature of the variable being mapped. Specific names are most common in meteorology, where multiple maps with different variables may be viewed simultaneously, the prefix iso- can be replaced with isallo- to specify a contour line connecting points where a variable changes at the same rate during a given time period. The words isoline and isarithm are general terms covering all types of contour line, an isogon is a contour line for a variable which measures direction. In meteorology and in geomagnetics, the term isogon has specific meanings which are described below, an isocline is a line joining points with equal slope. In population dynamics and in geomagnetics, the terms isocline and isoclinic line have specific meanings which are described below, equidistant is a line of equal distance from a given point, line, polyline. In geography, the word isopleth is used for lines that depict a variable which cannot be measured at a point. An example is population density, which can be calculated by dividing the population of a district by the surface area of that district. Each calculated value is presumed to be the value of the variable at the centre of the area, the idea of an isopleth map can be compared with that of a choropleth map
Contour line
–
A three-dimensional surface, whose contour graph is below.
Contour line
–
The bottom part of the diagram shows some contour lines with a straight line running through the location of the maximum value. The curve at the top represents the values along that straight line.
Contour line
–
Contour map labeled aesthetically in an "elevation up" manner.
9.
Cartographic relief depiction
–
Terrain or relief is an essential aspect of physical geography, and as such its portrayal presents a central problem in cartography, and more recently GIS and geovisualization. The most obvious way to depict relief is to imitate it at scale, as in molded or sculpted solid terrain models, because of the disparity between the horizontal and vertical scales of maps, raised relief is typically exaggerated. On flat paper maps and computer screens, terrain can be depicted in a variety of ways, the most ancient form of relief depiction in cartography, hill profiles are simply illustrations of mountains and hills in profile, placed as appropriate on generally small-scale maps. They are seldom used today except as part of an antique styling, hachures are also an older mode of representing relief. They are a form of shading, although different from the one used in shaded maps and they show the orientation of slope, and by their thickness and overall density they provide a general sense of steepness. Being non-numeric, they are useful to a scientific survey than contours. Hachure representation of relief was standardized by the Austrian topographer Johann Georg Lehmann in 1799, contour lines are isolines showing equal elevation. This is the most common way of numerically showing elevation, and is familiar from topographic maps, most 18th and early 19th century national surveys did not record relief across the entire area of coverage, calculating only spot elevations at survey points. Hypsometric tints are used to indicate elevation, usually together with contour lines. They can be used to depict ranges of elevation as bands of color, usually in a graduated scheme, a typical scheme progresses from dark greens for lower elevations up through yellows/browns, and on to grays and white at the highest elevations. Shaded relief, or hill-shading, simulates the cast shadow thrown upon a raised relief map, the shadows normally follow the English convention of top-left lighting in which the light source is placed near the upper-left corner of the map. If the map is oriented with north at the top, the result is that the light appears to come from the north-west. Many people have pointed out that this is unrealistic for maps of the hemisphere, because the sun does not shine from that direction. However, the convention is followed to avoid multistable perception illusions. Much work has been done in recreating the work of Swiss master Eduard Imhof, widely regarded as the master of manual hill-shading technique. Imhofs contributions included an approach to shading, with purples in valleys. The use of illumination and shadow to produce an appearance of space on a flat-surfaced map closely parallels the painting technique known as chiaroscuro. Shaded relief today can be created digitally, using a digital elevation model as its basis, the DEM may be converted to shaded relief using software such as Photoshop, QGIS, GRASS GIS or ArcMaps Spatial Analyst extension
Cartographic relief depiction
–
From a 1639 map of
Hispaniola by Joan Vinckenboons, showing use of hill profiles
Cartographic relief depiction
–
USGS topographic map of
Stowe, Vermont with contour lines at 20-foot intervals
Cartographic relief depiction
–
Dufour map of
Bern (1907); this is a shaded hachure map.
Cartographic relief depiction
–
Siegfried map of
Bernina Pass (1877) with black, blue and brown contour lines at 30-meter intervals
10.
Map series
–
Map series occur when an area is to be covered by a map that, due to its scale, must be spread over several sheets. Nevertheless, the sheets of a map series can also be used quite independently, as they generally have full map surround details. If a publisher produces several map series at different scales, then these series are called scale series, in everyday use, individual maps and atlases are sometimes described as being part of a map series. The scope of a map series can range from as few as two sheets to at least tens of thousands of sheets, obsolete maps, especially of the 19th century, are often named Topographic Atlases, because their small-sized sheets were also bound into atlases. An example of such a map series is the Topographic Atlas of the Kingdom of Hanover and the Duchy of Brunswick. It is technically difficult, and it would be highly impractical, to print. For that reason, map series are issued and preserved in loose-leaf form, in extreme cases, a map series can include thousands of sheets. Probably the greatest map series ever created is the 1,25,000 topographic map of the Soviet Union, with about 300,000 sheets, completed in 1987. Occasionally, smaller map series will be compiled by the buyer into a bound volume, the sheets of a map series can also be glued by the buyer to their neighbouring sheets, especially as a wall decoration. So, for example, the National Map of Switzerland, which consists of 22 sheets, can be seen as a decoration in the Federal Palace of Switzerland. Map series are divided into systems of single sheets named and numbered according to common principles. Thus, the characteristics of a sheet in a map series apply equally to all the other sheets of the map series. So, for example, all normally have the same cartographic projections, scale. Theoretically, almost any sheet network design can be used, in practice, variants of the mercator projection are the most widely used today, frequently in conjunction with the UTM coordinate system. All sheets of a map series are created in the same way, an individual sheets title and number identifies and locates that sheets place in the map series. The sheets are divided from each other either square to the map grid, or along the meridians, in the first case, the sheets will all be the same size. In the second case, the size will decrease towards the north or the south. To determine whether a map sheet forms part of a map series
Map series
–
Mairie de
Loevenich (
Germany), from the Topographic Survey of the Rhineland by Tranchot/Müffling, sheet 57 (published 1806/07).
Map series
–
Bochum (Germany), in the Prussian original survey, 1840.
11.
Natural Resources Canada
–
It was created in 1995 by amalgamating the now-defunct Departments of Energy, Mines and Resources and Forestry. Natural Resources Canada works to ensure the development of Canadas natural resources, including energy, forests. NRCan also uses its expertise in earth sciences to build and maintain a knowledge base of our landmass. To promote internal collaboration, NRCan has implemented a departmental wide wiki based on MediaWiki, under the Canadian constitution, responsibility for natural resources belongs to the provinces, not the federal government. However, the government has jurisdiction over off-shore resources, trade and commerce in natural resources, statistics, international relations. The current Minister of Natural Resources is Jim Carr as of November 4,2015, the department is governed by the Resources and Technical Surveys Act, R. S. C. C. R-7 and the Department of Natural Resources Act, S. C, structured along business lines according to types of natural resources and areas of interest
Natural Resources Canada
–
Department of Natural Resource Funding
12.
Chorography
–
Chorography is the art of describing or mapping a region or district, and by extension such a description or map. This term derives from the writings of the ancient geographer Pomponius Mela and Ptolemy, however, its resonances of meaning have varied at different times. Richard Helgerson states that chorography defines itself by opposition to chronicle and it is the genre devoted to place, and chronicle is the genre devoted to time. Darrell Rohl prefers a broad definition of the representation of space or place, in his text of the Geographia, Ptolemy defined geography as the study of the entire world, but chorography as the study of its smaller parts—provinces, regions, cities, or ports. Its goal was an impression of a part, as one makes an image of just an ear or an eye. Ptolemys most recent English translators, however, render the term as regional cartography, ptolemys text was rediscovered in the west at the beginning of the fifteenth century, and the term chorography was revived by humanist scholars. An early instance is a map of Britain in an early fifteenth-century manuscript. John Dee in 1570 regarded the practice as an underling, the term also came to be used, however, for written descriptions of regions. These regions were extensively visited by the writer, who then combined local topographical description, summaries of the historical sources, the most influential example was probably William Camdens Britannia, which described itself on its title page as a Chorographica descriptio. William Harrison in 1587 similarly described his own Description of Britaine as an exercise in chorography, a late example was William Greys Chorographia, a survey of the antiquities of the city of Newcastle upon Tyne. Even before Camdens work appeared, Andrew Melville in 1574 had referred to chorography, however, the term also continued to be used for maps and map-making, particularly of sub-national or county areas. By the beginning of the century the term had largely fallen out of use in all these contexts. In practice, however, the term is rarely found in English by this date. However, its use was revived for a time in the late nineteenth century by the geographer Ferdinand von Richthofen. He regarded chorography as a specialization within geography, comprising the description through field observation of the traits of a given area. The term is now widely used by historians and literary scholars to refer to the early modern genre of topographical. Antiquarianism Cartography Khôra Chorology English county histories Regional geography Brayshay, Mark, no Historie So Meete, gentry culture and the development of local history in Elizabethan and early Stuart England. Forms of Nationhood, the Elizabethan Writing of England, speculum Britanniae, regional study, antiquarianism and science in Britain to 1700
Chorography
–
Ptolemy as imagined by a 16th-century artist
Chorography
–
William Camden
Chorography
–
Example of
Christopher Saxton 's cartography.
Chorography
–
Ferdinand von Richthofen
13.
Thematic map
–
A thematic map is a type of map specifically designed to show a particular theme connected with a specific geographic area. A thematic map is a map that focuses on a theme or subject area. This is in contrast to general maps, which regularly show the variety of phenomena—geological, geographical. The contrast between them lies in the fact that thematic maps use the data, such as coastlines, boundaries and places. General maps portray the base data, such as landforms, lines of transportation, settlements, thematic maps emphasize spatial variation of one or a small number of geographic distributions. These distributions may be physical phenomena such as climate or human characteristics such as population density, barbara Petchenik described the difference as in place, about space. While general reference maps show where something is in space, thematic maps tell a story about that place, thematic maps are sometimes referred to as graphic essays that portray spatial variations and interrelationships of geographical distributions. Location, of course, is important to provide a base of where selected phenomena are occurring. An important cartographic element preceding thematic mapping was the development of base maps. Improvements in accuracy proceeded at a pace, and even until the mid-17th century. Still, base maps around this time were good enough to display appropriate information and his first significant cartographic contribution was a star chart of the constellation of the Southern Hemisphere, made during his stay on St. Helena and published on 1686. In that same year he published his first terrestrial map in an article about trade winds. In 1701 he published the New and Correct Chart Shewing the Variations of the Compass, see first image, another example of early thematic mapping comes from London physician John Snow. Though disease had been mapped thematically, Snow’s cholera map in 1854 is the best known example of using maps for analysis. Essentially, his technique and methodology anticipate principles of an information system. Starting with a base map of a London neighborhood which included streets and water pump locations. The emerging pattern centered around one particular pump on Broad Street, at Snow’s request, the handle of the pump was removed, and new cholera cases ceased almost at once. Further investigation of the area revealed the Broad Street pump was near a cesspit under the home of the outbreaks first cholera victim, another 19th century example of thematic maps, according to Friendly, was the earliest known choropleth map in 1826 created by Charles Dupin
Thematic map
–
Edmond Halley 's New and Correct Chart Shewing the Variations of the Compass (1701), the first chart to show lines of equal
magnetic variation.
Thematic map
–
John Snow 's cholera map about the cholera deaths in London in the 1840s, published 1854.
Thematic map
–
Map of climate and plant
hardiness zones.
14.
Topography
–
Topography is the study of the shape and features of the surface of the Earth and other observable astronomical objects including planets, moons, and asteroids. The topography of an area could refer to the shapes and features themselves. This field of geoscience and planetary science is concerned with detail in general, including not only relief but also natural and artificial features. This meaning is common in the United States, where topographic maps with elevation contours have made topography synonymous with relief. The older sense of topography as the study of place still has currency in Europe, topography in a narrow sense involves the recording of relief or terrain, the three-dimensional quality of the surface, and the identification of specific landforms. This is also known as geomorphometry, in modern usage, this involves generation of elevation data in digital form. It is often considered to include the representation of the landform on a map by a variety of techniques, including contour lines, hypsometric tints. The term topography originated in ancient Greece and continued in ancient Rome, the word comes from the Greek τόπος and -γραφία. In classical literature this refers to writing about a place or places, in Britain and in Europe in general, the word topography is still sometimes used in its original sense. Detailed military surveys in Britain were called Ordnance Surveys, and this term was used into the 20th century as generic for topographic surveys, the earliest scientific surveys in France were called the Cassini maps after the family who produced them over four generations. The term topographic surveys appears to be American in origin, the earliest detailed surveys in the United States were made by the “Topographical Bureau of the Army, ” formed during the War of 1812, which became the Corps of Topographical Engineers in 1838. In the 20th century, the term started to be used to describe surface description in other fields where mapping in a broader sense is used. An objective of topography is to determine the position of any feature or more generally any point in terms of both a horizontal coordinate system such as latitude, longitude, and altitude, identifying features, and recognizing typical landform patterns are also part of the field. There are a variety of approaches to studying topography, which method to use depend on the scale and size of the area under study, its accessibility, and the quality of existing surveys. Work on one of the first topographic maps was begun in France by Giovanni Domenico Cassini, in areas where there has been an extensive direct survey and mapping program, the compiled data forms the basis of basic digital elevation datasets such as USGS DEM data. This data must often be cleaned to eliminate discrepancies between surveys, but it forms a valuable set of information for large-scale analysis. The original American topographic surveys involved not only recording of relief, remote sensing is a general term for geodata collection at a distance from the subject area. Besides their role in photogrammetry, aerial and satellite imagery can be used to identify and delineate terrain features, certainly they have become more and more a part of geovisualization, whether maps or GIS systems
Topography
–
A surveying point in
Germany
Topography
–
A topographic map with
contour intervals
15.
Cadastre
–
A cadastre, using a cadastral survey or cadastral map, is a comprehensive register of the real estate or real propertys metes-and-bounds of a country. In most countries, legal systems have developed around the administrative systems and use the cadastre to define the dimensions. The cadastre is a source of data in disputes and lawsuits between landowners. In the United States, Cadastral Survey within the Bureau of Land Management maintains records of all public lands, such surveys often require detailed investigation of the history of land use, legal accounts, and other documents. A cadastre commonly includes details of the ownership, the tenure, the location, the dimensions, the cultivations if rural. Cadastres are used by nations around the world, some in conjunction with other records. The International Federation of Surveyors defines cadastre as follows, A Cadastre is normally a parcel based, the word forms the adjective cadastral, used in public administration, primarily for ownership and taxation purposes. The terminology for cadastral divisions may include counties, parishes, ridings, hundreds, sections, lots, blocks, other languages have kept the original t sound in the second syllable. In modern Greek, though, it has replaced by κτηματολόγιο /ktimatologio/. Some of the earliest cadasters were ordered by Roman Emperors to recover state owned lands that had appropriated by private individuals. In this way Vespasian was able to reimpose taxation formerly uncollected on these lands, with the fall of Rome the use of cadastral maps effectively discontinued. Medieval practice used written descriptions of the extent of land rather than using more precise surveys, only in the sixteenth and early seventeenth centuries did the use of cadastral maps resume, beginning in the Netherlands. With the emergence of capitalism in Renaissance Europe the need for cadastral maps reemerged as a tool to determine and this took place first privately in land disputes and later spread to governmental practice as a means of more precise tax assessment. Cadastral surveys document the boundaries of land ownership, by the production of documents, diagrams, sketches, plans, charts and they were originally used to ensure reliable facts for land valuation and taxation. An example from early England is the Domesday Book in 1086, napoleon established a comprehensive cadastral system for France that is regarded as the forerunner of most modern versions. The Public Lands Survey System is a survey of the United States originating in legislation from 1785. The Dominion Land Survey is a cadastral survey conducted in Western Canada begun in 1871 after the creation of the Dominion of Canada in 1867. Both cadastral surveys are made relative to principal meridian and baselines and these cadastral surveys divided the surveyed areas into townships, square land areas of approximately 36 square miles
Cadastre
–
Cadastral map of the village of
Pielnia, 1852,
Austrian Empire.
Cadastre
–
BLM cadastral survey marker from 1992 in
San Xavier, Arizona.
16.
Cartography
–
Cartography is the study and practice of making maps. Combining science, aesthetics, and technique, cartography builds on the premise that reality can be modeled in ways that communicate spatial information effectively, the fundamental problems of traditional cartography are to, Set the maps agenda and select traits of the object to be mapped. This is the concern of map editing, traits may be physical, such as roads or land masses, or may be abstract, such as toponyms or political boundaries. Represent the terrain of the object on flat media. This is the concern of map projections, eliminate characteristics of the mapped object that are not relevant to the maps purpose. This is the concern of generalization, reduce the complexity of the characteristics that will be mapped. This is also the concern of generalization, orchestrate the elements of the map to best convey its message to its audience. This is the concern of map design, modern cartography constitutes many theoretical and practical foundations of geographic information systems. The earliest known map is a matter of debate, both because the term map isnt well-defined and because some artifacts that might be maps might actually be something else. A wall painting that might depict the ancient Anatolian city of Çatalhöyük has been dated to the late 7th millennium BCE, the oldest surviving world maps are from 9th century BCE Babylonia. One shows Babylon on the Euphrates, surrounded by Assyria, Urartu and several cities, all, in turn, another depicts Babylon as being north of the world center. The ancient Greeks and Romans created maps since Anaximander in the 6th century BCE, in the 2nd century AD, Ptolemy wrote his treatise on cartography, Geographia. This contained Ptolemys world map – the world known to Western society. As early as the 8th century, Arab scholars were translating the works of the Greek geographers into Arabic, in ancient China, geographical literature dates to the 5th century BCE. The oldest extant Chinese maps come from the State of Qin, dated back to the 4th century BCE, in the book of the Xin Yi Xiang Fa Yao, published in 1092 by the Chinese scientist Su Song, a star map on the equidistant cylindrical projection. Early forms of cartography of India included depictions of the pole star and these charts may have been used for navigation. Mappa mundi are the Medieval European maps of the world, approximately 1,100 mappae mundi are known to have survived from the Middle Ages. Of these, some 900 are found illustrating manuscripts and the remainder exist as stand-alone documents, the Arab geographer Muhammad al-Idrisi produced his medieval atlas Tabula Rogeriana in 1154
Cartography
–
A medieval depiction of the
Ecumene (1482, Johannes Schnitzer, engraver), constructed after the coordinates in Ptolemy's
Geography and using his second map projection. The translation into Latin and dissemination of Geography in Europe, in the beginning of the 15th century, marked the rebirth of scientific cartography, after more than a millennium of stagnation.
Cartography
–
Valcamonica rock art (I), Paspardo r. 29, topographic composition, 4th millennium BC
Cartography
–
The
Bedolina Map and its tracing, 6th–4th century BC
Cartography
–
Copy (1472) of
St. Isidore's TO map of the world.
17.
Topography as the study of place
–
Topography is the study of the shape and features of the surface of the Earth and other observable astronomical objects including planets, moons, and asteroids. The topography of an area could refer to the shapes and features themselves. This field of geoscience and planetary science is concerned with detail in general, including not only relief but also natural and artificial features. This meaning is common in the United States, where topographic maps with elevation contours have made topography synonymous with relief. The older sense of topography as the study of place still has currency in Europe, topography in a narrow sense involves the recording of relief or terrain, the three-dimensional quality of the surface, and the identification of specific landforms. This is also known as geomorphometry, in modern usage, this involves generation of elevation data in digital form. It is often considered to include the representation of the landform on a map by a variety of techniques, including contour lines, hypsometric tints. The term topography originated in ancient Greece and continued in ancient Rome, the word comes from the Greek τόπος and -γραφία. In classical literature this refers to writing about a place or places, in Britain and in Europe in general, the word topography is still sometimes used in its original sense. Detailed military surveys in Britain were called Ordnance Surveys, and this term was used into the 20th century as generic for topographic surveys, the earliest scientific surveys in France were called the Cassini maps after the family who produced them over four generations. The term topographic surveys appears to be American in origin, the earliest detailed surveys in the United States were made by the “Topographical Bureau of the Army, ” formed during the War of 1812, which became the Corps of Topographical Engineers in 1838. In the 20th century, the term started to be used to describe surface description in other fields where mapping in a broader sense is used. An objective of topography is to determine the position of any feature or more generally any point in terms of both a horizontal coordinate system such as latitude, longitude, and altitude, identifying features, and recognizing typical landform patterns are also part of the field. There are a variety of approaches to studying topography, which method to use depend on the scale and size of the area under study, its accessibility, and the quality of existing surveys. Work on one of the first topographic maps was begun in France by Giovanni Domenico Cassini, in areas where there has been an extensive direct survey and mapping program, the compiled data forms the basis of basic digital elevation datasets such as USGS DEM data. This data must often be cleaned to eliminate discrepancies between surveys, but it forms a valuable set of information for large-scale analysis. The original American topographic surveys involved not only recording of relief, remote sensing is a general term for geodata collection at a distance from the subject area. Besides their role in photogrammetry, aerial and satellite imagery can be used to identify and delineate terrain features, certainly they have become more and more a part of geovisualization, whether maps or GIS systems
Topography as the study of place
–
A surveying point in
Germany
Topography as the study of place
–
A topographic map with
contour intervals
18.
Cadastral survey
–
A cadastre, using a cadastral survey or cadastral map, is a comprehensive register of the real estate or real propertys metes-and-bounds of a country. In most countries, legal systems have developed around the administrative systems and use the cadastre to define the dimensions. The cadastre is a source of data in disputes and lawsuits between landowners. In the United States, Cadastral Survey within the Bureau of Land Management maintains records of all public lands, such surveys often require detailed investigation of the history of land use, legal accounts, and other documents. A cadastre commonly includes details of the ownership, the tenure, the location, the dimensions, the cultivations if rural. Cadastres are used by nations around the world, some in conjunction with other records. The International Federation of Surveyors defines cadastre as follows, A Cadastre is normally a parcel based, the word forms the adjective cadastral, used in public administration, primarily for ownership and taxation purposes. The terminology for cadastral divisions may include counties, parishes, ridings, hundreds, sections, lots, blocks, other languages have kept the original t sound in the second syllable. In modern Greek, though, it has replaced by κτηματολόγιο /ktimatologio/. Some of the earliest cadasters were ordered by Roman Emperors to recover state owned lands that had appropriated by private individuals. In this way Vespasian was able to reimpose taxation formerly uncollected on these lands, with the fall of Rome the use of cadastral maps effectively discontinued. Medieval practice used written descriptions of the extent of land rather than using more precise surveys, only in the sixteenth and early seventeenth centuries did the use of cadastral maps resume, beginning in the Netherlands. With the emergence of capitalism in Renaissance Europe the need for cadastral maps reemerged as a tool to determine and this took place first privately in land disputes and later spread to governmental practice as a means of more precise tax assessment. Cadastral surveys document the boundaries of land ownership, by the production of documents, diagrams, sketches, plans, charts and they were originally used to ensure reliable facts for land valuation and taxation. An example from early England is the Domesday Book in 1086, napoleon established a comprehensive cadastral system for France that is regarded as the forerunner of most modern versions. The Public Lands Survey System is a survey of the United States originating in legislation from 1785. The Dominion Land Survey is a cadastral survey conducted in Western Canada begun in 1871 after the creation of the Dominion of Canada in 1867. Both cadastral surveys are made relative to principal meridian and baselines and these cadastral surveys divided the surveyed areas into townships, square land areas of approximately 36 square miles
Cadastral survey
–
Cadastral map of the village of
Pielnia, 1852,
Austrian Empire.
Cadastral survey
–
BLM cadastral survey marker from 1992 in
San Xavier, Arizona.
19.
Great Trigonometric Survey
–
The Great Trigonometrical Survey was a project which aimed to measure the entire Indian subcontinent with scientific precision. It was begun in 1802 by the infantry officer William Lambton, under the leadership of his successor, George Everest, the project was made a responsibility of the Survey of India. Everest was succeeded by Andrew Scott Waugh and after 1861 the project was led by James Walker, among the many accomplishments of the Survey were the demarcation of the British territories in India and the measurement of the height of the Himalayan giants, Everest, K2, and Kanchenjunga. From its inception in 1600 to the beginning of the nineteenth century, with the acquisition of new territory, it employed several explorers and cartographers to provide maps and other information on its territories, most notably James Rennell, from 1767 in Bengal. As Rennell proceeded making maps, some flaws in them surfaced, based on a lack of precise measurements. The Great Trigonometrical Survey of India started on 10 April 1802 with the measurement of a baseline near Madras, major Lambton selected the flat plains with St. Thomas Mount at the north end and Perumbauk hill at the southern end. The baseline was 7.5 miles long, lieutenant Kater was despatched to find high vantage points on the hills of the west so that the coastal points of Tellicherry and Cannanore could be connected. The high hills chosen were Mount Delly and Tadiandamol, the distance from coast to coast was 360 miles and this survey line was completed in 1806. The East India Company thought that this project would take about 5 years but eventually it took nearly 70 years well past the Indian Rebellion of 1857, at times the survey party numbered 700 people. The Trigonometrical Survey was conducted independent of other surveys, notably the topographical, in 1875 the decision was taken that the Survey budget should be reduced from 240,000 to 200,000 pounds. This resulted in a reorganization under Surveyor-General Colonel J. T. Walker to amalgamate the Great Trigonometrical, Topographical, triangulation surveys were based on a few carefully measured baselines and a series of angles. The initial baseline was measured with accuracy, since the accuracy of the subsequent survey was critically dependent upon it. Various corrections were applied, principally temperature, an especially accurate folding chain was used, laid on horizontal tables, all shaded from the sun and with a constant tension. The early surveys made use of large and bulky theodolites made by William Carey, later surveys used more compact theodolites. Accurate instruments could not always be purchased through the system of government contract. He had a maker, Henry Barrow, set up an instrument company in Calcutta, for a while Barrow was succeeded by Syed Mohsin from Arcot and after his death the instruments were supplied by Cooke from York. The Great Trigonometrical Survey of India in a Historical Perspective by Rama Deb Roy
Great Trigonometric Survey
–
A map showing the triangles and transects used in the survey, produced in 1870
Great Trigonometric Survey
–
Colonel Thomas Tupper Carter-Campbell of Possil, a surveyor in the Great Trigonometrical Survey of the 3rd Grade.
20.
East India Company
–
The company also ruled the beginnings of the British Empire in India. The company received a Royal Charter from Queen Elizabeth I on 31 December 1600, wealthy merchants and aristocrats owned the Companys shares. Initially the government owned no shares and had only indirect control, during its first century of operation the focus of the Company was trade, not the building of an empire in India. The company eventually came to rule large areas of India with its own armies, exercising military power. Despite frequent government intervention, the company had recurring problems with its finances, the official government machinery of British India had assumed its governmental functions and absorbed its armies. Soon after the defeat of the Spanish Armada in 1588, London merchants presented a petition to Queen Elizabeth I for permission to sail to the Indian Ocean, one of them, Edward Bonventure, then sailed around Cape Comorin to the Malay Peninsula and returned to England in 1594. In 1596, three ships sailed east, however, these were all lost at sea. Two days later, on 24 September, the Adventurers reconvened and resolved to apply to the Queen for support of the project, the Adventurers convened again a year later. For a period of fifteen years the charter awarded the newly formed company a monopoly on trade with all countries east of the Cape of Good Hope and west of the Straits of Magellan. Anybody who traded in breach of the charter without a licence from the Company was liable to forfeiture of their ships and cargo, the governance of the company was in the hands of one governor and 24 directors or committees, who made up the Court of Directors. They, in turn, reported to the Court of Proprietors, ten committees reported to the Court of Directors. According to tradition, business was transacted at the Nags Head Inn, opposite St Botolphs church in Bishopsgate. Sir James Lancaster commanded the first East India Company voyage in 1601, in March 1604 Sir Henry Middleton commanded the second voyage. Early in 1608 Alexander Sharpeigh was appointed captain of the Companys Ascension, thereafter two ships, Ascension and Union sailed from Woolwich on 14 March 1607–8. Initially, the company struggled in the trade because of the competition from the already well-established Dutch East India Company. The company opened a factory in Bantam on the first voyage, the factory in Bantam was closed in 1683. During this time belonging to the company arriving in India docked at Surat. In the next two years, the company established its first factory in south India in the town of Machilipatnam on the Coromandel Coast of the Bay of Bengal
East India Company
–
Imperial entities of India
East India Company
–
Company flag after 1801
East India Company
–
James Lancaster commanded the first East India Company voyage in 1601
East India Company
–
Red Dragon fought the Portuguese at the
Battle of Swally in 1612, and made several voyages to the
East Indies.
21.
British Raj
–
The British Raj was the rule by the British Crown in the Indian subcontinent between 1858 and 1947. The rule is also called Crown rule in India, or direct rule in India, the resulting political union was also called the Indian Empire and after 1876 issued passports under that name. It lasted until 1947, when the British Indian Empire was partitioned into two sovereign states, the Dominion of India and the Dominion of Pakistan. The British Raj extended over almost all present-day India, Pakistan and this area is very diverse, containing the Himalayan mountains, fertile floodplains, the Indo-Gangetic Plain, a long coastline, tropical dry forests, arid uplands, and the Thar desert. In addition, at times, it included Aden, Lower Burma, Upper Burma, British Somaliland. Burma was separated from India and directly administered by the British Crown from 1937 until its independence in 1948, among other countries in the region, Ceylon was ceded to Britain in 1802 under the Treaty of Amiens. Ceylon was part of Madras Presidency between 1793 and 1798, the kingdoms of Nepal and Bhutan, having fought wars with the British, subsequently signed treaties with them and were recognised by the British as independent states. The Kingdom of Sikkim was established as a state after the Anglo-Sikkimese Treaty of 1861, however. The Maldive Islands were a British protectorate from 1887 to 1965, India during the British Raj was made up of two types of territory, British India and the Native States. In general, the term British India had been used to also to the regions under the rule of the British East India Company in India from 1600 to 1858. The term has also used to refer to the British in India. The terms Indian Empire and Empire of India were not used in legislation, the monarch was known as Empress or Emperor of India and the term was often used in Queen Victorias Queens Speeches and Prorogation Speeches. The passports issued by the British Indian government had the words Indian Empire on the cover, in addition, an order of knighthood, the Most Eminent Order of the Indian Empire, was set up in 1878. At the turn of the 20th century, British India consisted of eight provinces that were administered either by a Governor or a Lieutenant-Governor, during the partition of Bengal the new provinces of Assam and East Bengal were created as a Lieutenant-Governorship. In 1911, East Bengal was reunited with Bengal, and the new provinces in the east became, Assam, Bengal, Bihar, there were 565 princely states when India and Pakistan became independent from Britain in August 1947. The princely states did not form a part of British India, the larger ones had treaties with Britain that specified which rights the princes had, in the smaller ones the princes had few rights. Within the princely states external affairs, defence and most communications were under British control, the British also exercised a general influence over the states internal politics, in part through the granting or withholding of recognition of individual rulers. Although there were nearly 600 princely states, the majority were very small
British Raj
–
An 1909 map of the British Indian Empire
British Raj
–
Flag
British Raj
–
British Raj coins during
Edward VII and
George V,
Indian Museum
British Raj
–
Imperial entities of India
22.
United Kingdom
–
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom or Britain, is a sovereign country in western Europe. Lying off the north-western coast of the European mainland, the United Kingdom includes the island of Great Britain, Northern Ireland is the only part of the United Kingdom that shares a land border with another sovereign state—the Republic of Ireland. The Irish Sea lies between Great Britain and Ireland, with an area of 242,500 square kilometres, the United Kingdom is the 78th-largest sovereign state in the world and the 11th-largest in Europe. It is also the 21st-most populous country, with an estimated 65.1 million inhabitants, together, this makes it the fourth-most densely populated country in the European Union. The United Kingdom is a monarchy with a parliamentary system of governance. The monarch is Queen Elizabeth II, who has reigned since 6 February 1952, other major urban areas in the United Kingdom include the regions of Birmingham, Leeds, Glasgow, Liverpool and Manchester. The United Kingdom consists of four countries—England, Scotland, Wales, the last three have devolved administrations, each with varying powers, based in their capitals, Edinburgh, Cardiff and Belfast, respectively. The relationships among the countries of the UK have changed over time, Wales was annexed by the Kingdom of England under the Laws in Wales Acts 1535 and 1542. A treaty between England and Scotland resulted in 1707 in a unified Kingdom of Great Britain, which merged in 1801 with the Kingdom of Ireland to form the United Kingdom of Great Britain and Ireland. Five-sixths of Ireland seceded from the UK in 1922, leaving the present formulation of the United Kingdom of Great Britain, there are fourteen British Overseas Territories. These are the remnants of the British Empire which, at its height in the 1920s, British influence can be observed in the language, culture and legal systems of many of its former colonies. The United Kingdom is a country and has the worlds fifth-largest economy by nominal GDP. The UK is considered to have an economy and is categorised as very high in the Human Development Index. It was the worlds first industrialised country and the worlds foremost power during the 19th, the UK remains a great power with considerable economic, cultural, military, scientific and political influence internationally. It is a nuclear weapons state and its military expenditure ranks fourth or fifth in the world. The UK has been a permanent member of the United Nations Security Council since its first session in 1946 and it has been a leading member state of the EU and its predecessor, the European Economic Community, since 1973. However, on 23 June 2016, a referendum on the UKs membership of the EU resulted in a decision to leave. The Acts of Union 1800 united the Kingdom of Great Britain, Scotland, Wales and Northern Ireland have devolved self-government
United Kingdom
–
Stonehenge, in
Wiltshire, was erected around 2500 BC.
United Kingdom
–
Flag
United Kingdom
–
The
Bayeux Tapestry depicts the
Battle of Hastings, 1066, and the events leading to it.
United Kingdom
–
The
Treaty of Union led to a single united kingdom encompassing all Great Britain.
23.
Ordnance Survey
–
Ordnance Survey is a non-ministerial government department which acts as the national mapping agency for Great Britain and is one of the worlds largest producers of maps. Since 1 April 2015 it has operated as Ordnance Survey Ltd, the Ordnance Survey Board remain accountable to the Secretary of State for Business, Energy and Industrial Strategy. It is also a member of the Public Data Group, the agencys name indicates its original military purpose, mapping Scotland in the wake of the Jacobite rebellion in 1745. There was also a general and nationwide need in light of the potential threat of invasion during the Napoleonic Wars. Ordnance Survey mapping is usually classified as either large-scale or small-scale, the Surveys large-scale mapping comprises maps at six inches to the mile or more and was available as sheets until the 1980s, when it was digitised. Small-scale mapping comprises maps at less than six inches to the mile, such as the one inch to the mile leisure maps. These are still available in sheet form. Ordnance Survey maps remain in copyright for fifty years after their publication, some of the Copyright Libraries hold complete or near-complete collections of pre-digital OS mapping. The origins of the Ordnance Survey lie in the aftermath of the last Jacobite rising which was defeated by forces loyal to the government at the Battle of Culloden in 1746. In 1747, Lieutenant-colonel David Watson proposed the compilation of a map of the Highlands to facilitate the subjugation of clans, in response, King George II charged Watson with making a military survey of the Highlands under the command of the Duke of Cumberland. Among Watsons assistants were William Roy, Paul Sandby and John Manson, the survey was produced at a scale of 1 inch to 1000 yards and included the Duke of Cumberlands Map now held in the British Library. This work was the point of the Principal Triangulation of Great Britain. Roys technical skills and leadership set the standard for which Ordnance Survey became known. Work was begun in earnest in 1790 under Roys supervision, when the Board of Ordnance began a military survey starting with the south coast of England. A set of stamps, featuring maps of the Kentish village of Hamstreet, was issued in 1991 to mark the bicentenary. In 1801, the first one-inch-to-the-mile map was published, detailing the county of Kent, during the next twenty years, roughly a third of England and Wales was mapped at the same scale under the direction of William Mudge, as other military matters took precedence. It took until 1823 to re-establish a relationship with the French survey made by Roy in 1787, by 1810, one inch to the mile maps of most of the south of England were completed, but were withdrawn from sale between 1811 and 1816 because of security fears. It was gruelling work, major Thomas Colby, later the longest serving director general of Ordnance Survey, in 1824, Colby and most of his staff moved to Ireland to work on a six-inches-to-the-mile valuation survey
Ordnance Survey
–
Grid square TF from the
Ordnance Survey National Grid, shown at a scale of 1:250,000. The map shows
the Wash and the
North Sea, as well as places within the counties of
Lincolnshire, Cambridgeshire and
Norfolk.
Ordnance Survey
–
Part of an Ordnance Survey map, at the scale of one inch to the mile, from a New Popular Edition map published in 1946.
Ordnance Survey
–
The
original draftsman's drawings for the area around
St. Columb Major in
Cornwall, made in 1810.
Ordnance Survey
–
The
old site of Ordnance Survey, London Road,
Southampton City Centre, in 2005.
24.
United States Army Corps of Engineers
–
The United States Army Corps of Engineers, also sometimes shortened to CoE is a U. S. Although generally associated with dams, canals and flood protection in the United States, the Corps of Engineers provides outdoor recreation opportunities to the public, and provides 24% of U. S. hydropower capacity. The corps mission is to Deliver vital public and military engineering services, partnering in peace and war to strengthen our Nations security, energize the economy and their most visible missions include, Planning, designing, building, and operating locks and dams. Other civil engineering projects include flood control, beach nourishment, design and construction of flood protection systems through various federal mandates. Design and construction management of military facilities for the Army, Air Force, Army Reserve and Air Force Reserve and other Defense and Federal agencies. The history of United States Army Corps of Engineers can be traced back to 16 June 1775, colonel Richard Gridley became General George Washingtons first chief engineer, however, it was not until 1779 that Congress created a separate Corps of Engineers. One of its first tasks was to build fortifications near Boston at Bunker Hill, the first Corps of Engineers was mostly composed of French subjects who had been hired by General Washington from the service of Louis XVI. that the said Corps. Shall be stationed at West Point in the State of New York, until 1866, the superintendent of the United States Military Academy was always an officer of engineer. During the first half of the 19th century, West Point was the major and, for a while, the General Survey Act of 1824 authorized the use of Army engineers to survey road and canal routes. Separately authorized on 4 July 1838, the U. S and it was merged with the Corps of Engineers on 31 March 1863, at which point the Corps of Engineers also assumed the Lakes Survey District mission for the Great Lakes. In 1841, Congress created the Lake Survey, the survey, based in Detroit, Mich. was charged with conducting a hydrographical survey of the Northern and Northwestern Lakes and preparing and publishing nautical charts and other navigation aids. The Lake Survey published its first charts in 1852, in the mid-19th century, Corps of Engineers officers ran Lighthouse Districts in tandem with U. S. Naval officers. The Army Corps of Engineers played a significant role in the American Civil War, many of the men who would serve in the top leadership in this institution were West Point graduates who rose to military fame and power during the Civil War. Some of these men were Union Generals George McClellan, Henry Halleck, George Meade, and Confederate generals Robert E. Lee, Joseph Johnston, the versatility of officers in the Army Corps of Engineers contributed to the success of numerous missions throughout the Civil War. They were responsible for building pontoon and railroad bridges, forts and batteries, the destruction of supply lines. The Army Corps of Engineers served as a function in making the war effort logistically feasible. This method of building trenches was known as the zigzag pattern, from the beginning, many politicians wanted the Corps of Engineers to contribute to both military construction and works of a civil nature. During World War II the mission grew to more than 27,000 military, included were aircraft, tank assembly, and ammunition plants, camps for 5.3 million soldiers, depots, ports, and hospitals, as well as the Manhattan Project, and the Pentagon
United States Army Corps of Engineers
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Colonel Debra Lewis, the Gulf Region Division Central District commander with Sheik O'rhaman Hama Raheem, an Iraqi councilman, celebrate the opening of a new women's center in Assriya Village that the Corps helped construct in 2006.
United States Army Corps of Engineers
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USACE Logo
United States Army Corps of Engineers
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U.S. Army Corps of Engineers Dredge Tauracavor 3 in New York Harbor.
United States Army Corps of Engineers
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Mississippi River Improvement, 1890.
25.
United States Department of the Interior
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The United States Department of the Interior is the United States federal executive department of the U. S. About 75% of federal land is managed by the department. The Department is administered by the United States Secretary of the Interior, the current Secretary is Ryan Zinke. The Inspector General position is vacant, with Mary Kendall serving as acting Inspector General. Despite its name, the Department of the Interior has a different role from that of the ministries of other nations. In the United States, national security and immigration functions are performed by the Department of Homeland Security primarily, the Department of the Interior has often been humorously called The Department of Everything Else because of its broad range of responsibilities. A department for domestic concern was first considered by the 1st United States Congress in 1789, the idea of a separate domestic department continued to percolate for a half-century and was supported by Presidents from James Madison to James Polk. The 1846–48 Mexican–American War gave the new steam as the responsibilities of federal government grew. Polks Secretary of the Treasury, Robert J. Walker, became a champion of creating the new department. In 1849, Walker stated in his report that several federal offices were placed in departments with which they had little to do. Walker argued that these and other bureaus should be together in a new Department of the Interior. A bill authorizing its creation of the Department passed the House of Representatives on February 15,1849, the Department was established on March 3,1849, the eve of President Zachary Taylors inauguration, when the Senate voted 31 to 25 to create the Department. Its passage was delayed by Democrats in Congress who were reluctant to create more patronage posts for the incoming Whig administration to fill, the first Secretary of the Interior was Thomas Ewing. Many of the concerns the Department originally dealt with were gradually transferred to other Departments. Other agencies became separate Departments, such as the Bureau of Agriculture, however, land and natural resource management, American Indian affairs, wildlife conservation, and territorial affairs remain the responsibilities of the Department of the Interior. As of mid-2004, the Department managed 507 million acres of surface land, energy projects on federally managed lands and offshore areas supply about 28% of the nations energy production. Within the Interior Department, the Bureau of Indian Affairs handles some federal relations with Native Americans, the current acting Assistant Secretary for Indian Affairs is Lawrence S. Roberts, an enrolled member of the Oneida Tribe in Wisconsin. Several cases have sought accounting of such funds from the departments of Interior, in addition, some Native American nations have sued the government over water-rights issues and their treaties with the US
United States Department of the Interior
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Main Interior Building 1849 C Street
NW Washington, D.C., U.S. 38°53′37.11″N 77°2′33.33″W / 38.8936417°N 77.0425917°W / 38.8936417; -77.0425917
United States Department of the Interior
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Seal of the U.S. Department of the Interior
United States Department of the Interior
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The
hierarchy of the U.S. Department of the Interior.
26.
United States Geological Survey
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The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its resources. The organization has four science disciplines, concerning biology, geography, geology. The USGS is a research organization with no regulatory responsibility. The USGS is a bureau of the United States Department of the Interior, the USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, the current motto of the USGS, in use since August 1997, is science for a changing world. The agencys previous slogan, adopted on the occasion of its anniversary, was Earth Science in the Public Service. Prompted by a report from the National Academy of Sciences, the USGS was created, by a last-minute amendment and it was charged with the classification of the public lands, and examination of the geological structure, mineral resources, and products of the national domain. This task was driven by the need to inventory the vast lands added to the United States by the Louisiana Purchase in 1803, the legislation also provided that the Hayden, Powell, and Wheeler surveys be discontinued as of June 30,1879. Clarence King, the first director of USGS, assembled the new organization from disparate regional survey agencies, after a short tenure, King was succeeded in the directors chair by John Wesley Powell. Administratively, it is divided into a Headquarters unit and six Regional Units, Other specific programs include, Earthquake Hazards Program monitors earthquake activity worldwide. The National Earthquake Information Center in Golden, Colorado on the campus of the Colorado School of Mines detects the location, the USGS also runs or supports several regional monitoring networks in the United States under the umbrella of the Advanced National Seismic System. The USGS informs authorities, emergency responders, the media, and it also maintains long-term archives of earthquake data for scientific and engineering research. It also conducts and supports research on long-term seismic hazards, USGS has released the UCERF California earthquake forecast. The USGS National Geomagnetism Program monitors the magnetic field at magnetic observatories and distributes magnetometer data in real time, the USGS operates the streamgaging network for the United States, with over 7400 streamgages. Real-time streamflow data are available online, since 1962, the Astrogeology Research Program has been involved in global, lunar, and planetary exploration and mapping. USGS operates a number of related programs, notably the National Streamflow Information Program. USGS Water data is available from their National Water Information System database
United States Geological Survey
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Clarence King, founder of the USGS
United States Geological Survey
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Seal of the United States Geological Survey
United States Geological Survey
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The USGS headquarters in
Reston, Virginia
United States Geological Survey
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USGS gauging station 03221000 on the
Scioto River below
O'Shaughnessy Dam near
Dublin, Ohio
27.
International Map of the World
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The International Map of the World was a project begun in 1913 to create a complete map of the world according to internationally agreed standards. Roads were depicted in red, towns and railways were depicted in black, the map was the brainchild of Albrecht Penck, a German geographer who first proposed it in 1891. The Central Bureau of the Map of the World was established at the Ordnance Survey in London, after the Second World War, the United Nations took over the project. In 1964, Arthur H. Robinson dismissed the IMW as cartographic wallpaper of no practical use, there were few updates thereafter, and in 1989, UNESCO declared the project was no longer feasible and stopped monitoring it. A map indexing system was developed for dividing the globe into sections spanning six degrees of longitude by four degrees latitude, longitudinal slices are numbered 1 through 60. Latitudinal slices are named NA through NV and SA through SV, for example Map NJ-10 covers 36-40°N, 120-126°W including San Francisco at 37°47′N 122°25′W. SG-35 covers 24-28°S, 24-30°E including Johannesburg at 26°12′S 28°03′E, nL-38 covers 44-48N, 48-54E including Astrakhan at 46°19′N 48°2′E. NI-54 covers 32-36°N, 138-144°E including Tokyo at 35°42′N 139°43′E, due to shortening of longitudinal distances with increasing latitude, longitudinal span beyond 60 degrees latitude doubles to twelve degrees. Beyond 76 degrees it doubles again to 24 degrees and this indexing system outlived the international project and is still used in national and international mapping programs by Australia, Russia and the United States. World Aeronautical Chart, another world map Pearson, Alastair, Taylor, D. R. Fraser, Kline, Karen D. Heffernan. Cartographic ideals and geopolitical realities, international maps of the world from the 1890s to the present, the International Map of the World, the International Geographical Union, and the United Nations. International Map of the World 1,1,000,000 index to scans at the Perry-Castañeda Library Map Collection
International Map of the World
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Map NL 39
International Map of the World
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Map index of northern and central Asia. Since it lies entirely north of the equator, prefix map index numbers with N. Note longitudinal span increasing to 12° at 60°N, then to 24° at 76°N.
28.
Federal government of the United States
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The Federal Government of the United States is the national government of the United States, a republic in North America, composed of 50 states, one district, Washington, D. C. and several territories. The federal government is composed of three branches, legislative, executive, and judicial, whose powers are vested by the U. S. Constitution in the Congress, the President, and the courts, including the Supreme Court. The powers and duties of these branches are defined by acts of Congress. The full name of the republic is United States of America, no other name appears in the Constitution, and this is the name that appears on money, in treaties, and in legal cases to which it is a party. The terms Government of the United States of America or United States Government are often used in documents to represent the federal government as distinct from the states collectively. In casual conversation or writing, the term Federal Government is often used, the terms Federal and National in government agency or program names generally indicate affiliation with the federal government. Because the seat of government is in Washington, D. C, Washington is commonly used as a metonym for the federal government. The outline of the government of the United States is laid out in the Constitution, the government was formed in 1789, making the United States one of the worlds first, if not the first, modern national constitutional republics. The United States government is based on the principles of federalism and republicanism, some make the case for expansive federal powers while others argue for a more limited role for the central government in relation to individuals, the states or other recognized entities. For example, while the legislative has the power to create law, the President nominates judges to the nations highest judiciary authority, but those nominees must be approved by Congress. The Supreme Court, in its turn, has the power to invalidate as unconstitutional any law passed by the Congress and these and other examples are examined in more detail in the text below. The United States Congress is the branch of the federal government. It is bicameral, comprising the House of Representatives and the Senate, the House currently consists of 435 voting members, each of whom represents a congressional district. The number of each state has in the House is based on each states population as determined in the most recent United States Census. All 435 representatives serve a two-year term, each state receives a minimum of one representative in the House. There is no limit on the number of terms a representative may serve, in addition to the 435 voting members, there are six non-voting members, consisting of five delegates and one resident commissioner. In contrast, the Senate is made up of two senators from each state, regardless of population, there are currently 100 senators, who each serve six-year terms
Federal government of the United States
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The
United States Capitol is the
seat of government for Congress.
Federal government of the United States
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Great Seal of the United States
Federal government of the United States
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Diagram of the Federal Government and American Union, 1862.
29.
TIGER
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The tiger is the largest cat species, most recognisable for their pattern of dark vertical stripes on reddish-orange fur with a lighter underside. The species is classified in the genus Panthera with the lion, leopard, jaguar, Tigers are apex predators, primarily preying on ungulates such as deer and bovids. They are territorial and generally solitary but social animals, often requiring large contiguous areas of habitat that support their prey requirements and this, coupled with the fact that they are indigenous to some of the more densely populated places on Earth, has caused significant conflicts with humans. Tigers once ranged widely across eastern Eurasia, from the Black Sea in the west, to the Indian Ocean in the south, today, they range from the Siberian taiga to open grasslands and tropical mangrove swamps. The remaining six tiger subspecies have been classified as endangered by the International Union for Conservation of Nature, a 2016 global census estimated the population of wild tigers at approximately 3,890 individuals. Major reasons for decline include habitat destruction, habitat fragmentation. The extent of area occupied by tigers is estimated at less than 1,184,911 km2, in 2016, wildlife conservation group at WWF declared that worlds count of wild tigers has risen for the first time in a century. Tigers are among the most recognisable and popular of the charismatic megafauna. They have featured prominently in ancient mythology and folklore, and continue to be depicted in modern films and they appear on many flags, coats of arms, and as mascots for sporting teams. The tiger is the animal of Bangladesh, India, Malaysia. In 1758, Linnaeus described the tiger in his work Systema Naturae, in 1929, the British taxonomist Reginald Innes Pocock subordinated the species under the genus Panthera using the scientific name Panthera tigris. The derivation from Greek pan- and ther may be folk etymology, the specific epithet, tigris, as well as the common name, tiger, come from the Middle English tigre and the Old English tigras, both used for the animal. These derive from the Old French tigre, itself a derivative of the Latin word tigris and the Greek word tigris. The original source may have been the Persian tigra meaning pointed or sharp, the tigers closest living relatives were previously thought to be the lion, leopard and jaguar, all of which are classified under the genus Panthera. The oldest remains of an extinct relative, called Panthera zdanskyi or the Longdan tiger, have been found in the Gansu province of northwestern China. This species is considered to be a taxon to the extant tiger and lived about 2 million years ago. It was smaller than the tiger, being the size of a jaguar. Despite being considered more primitive, the Longdan tiger was functionally and possibly ecologically similar to its modern cousin, as Panthera zdanskyi lived in northwestern China, that may have been where the tiger lineage originated
TIGER
TIGER
TIGER
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Bengal tiger (P. t. tigris), also called the Indian tiger
TIGER
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Indochinese tiger (P. t. corbetti), also called
Corbett's tiger
