1.
Campeche
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Campeche, officially the Free and Sovereign State of Campeche, is one of the 31 states which, with the Federal District, comprise the 32 Federal Entities of Mexico. It has a coastline to the west with the Gulf of Mexico, the state capital, also called Campeche, was declared a World Heritage Site in 1997. The formation of the state began with the city, which was founded in 1540 as the Spanish began the conquest of the Yucatán Peninsula, during the colonial period, the city was a rich and important port, but declined after Mexico’s Independence. Campeche was part of the province of Yucatán but split off in the mid-19th century, today, much of the state’s economic comeback is due to the finding of petroleum offshore in the 1970s, which has made the coastal cities of Campeche and Ciudad del Carmen important economic centers. The state has important Mayan and colonial sites but they are not as well known or visited as others in the Yucatán. The states executive power rests in the governor of Campeche and the legislative power rests in the Congress of Campeche which is a legislature composed of 35 deputies. The state of Campeche is located in southeast Mexico, on the west side of the Yucatan Peninsula, the territory is 56,858. 84km2, which is 2. 6% of Mexico’s total. It borders the states of Yucatán, Quintana Roo and Tabasco, with the country of Belize to the east, Guatemala to the south and the Gulf of Mexico to the west. Politically, it is divided into municipalities, Calkiní, Calakmul, Campeche, Candelaria, Champotón, Ciudad del Carmen, Escárcega, Hecelchakán, Hopelchén, Palizada. Campeche is a flat area of Mexico with 523 km of shoreline on the Gulf of Mexico. Most of the surface is of sedimentary rock much of which is from marine origin, the area with the highest elevations is near the borders with Guatemala and Quintana Roo. Notable elevations include Cerro Champerico, Cerro los Chinos, Cerro El Ramonal, Cerro El Doce, however, these hills are separated by large expanses of lower flat land. In the south of the municipality of Champotón begin a series of rolling hills known as the Sierra Alta or Puuc and these have only an average altitude of between forty and sixty meters with some reaching 100 meters. There other areas of rolling hills, near the city of Campeche with main ones known as Maxtum, Boxol. Another set is called the Sierra Seybaplaya in the center of the state, away from the coast, these rainforests are interspersed with savannah areas and along the coast are accompanied by areas with sand dunes, mangrove wetlands and estuaries. Species that can be found in the various rainforests include huapaque, cedar, pukte, sapote, dyewood, dzalam and it also includes a number of precious tropical hardwoods such as red cedar, mahogany, ciricote and guayacán. Along the coastal areas, palms such as the coconut. The main wildlife species in the state are the jaguar, ocelot, puma, deer, wild boar, raccoon, hare, ring-tailed cat, there are many bird species including the chachalaca, ducks, quail, pelican, toucan, buzzard and many more
2.
Kabah (Maya site)
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Kabah is a Maya archaeological site in the Puuc region of western Yucatan, south of Mérida. Kabah is south of Uxmal, connected to that site by a grand 18 kilometres long raised pedestrian causeway 5 metres wide with monumental arches at each end, Kabah is the second largest ruin of the Puuc region after Uxmal. The name Kabah or Kabaah is usually taken to be archaic Maya language for strong hand and this is a pre-Columbian name for the site, mentioned in Maya chronicles. An alternative name is Kabahaucan or royal snake in the hand, the area was inhabited by the mid 3rd century BCE. Most of the now visible was built between the 7th century and 11th centuries CE. A sculpted date on a doorjamb of one of the buildings gives the date 879, another inscribed date is one of the latest carved in the Maya Classic style, in 987. Kabaah was abandoned or at least no new ceremonial architecture built for centuries before the Spanish conquest of Yucatán. This massive repetition of a set of elements is unusual in Maya art. Masks of the rain god abound on other structures throughout the site, copal incense has been discovered in some of the stone noses of the raingods. The emphasis placed on Chaac, the Protector of the Harvest, there are no cenotes in this dryer, northern part of the Yucatán, so the Maya here had to depend solely on rain. The site also has a number of palaces, low stone buildings. While most is in the Puuc Maya style, some show Chenes elements, the site had a number of sculpted panels, lintels, and doorjambs, most of which have been removed to museums elsewhere. The sculptures mostly depict the rulers and scenes of warfare. The first detailed account of the ruin was published by John Lloyd Stephens, the site is on Mexican highway 261, some 140 kilometres south from Mérida, Yucatán, towards Campeche, Campeche, and is a popular tourism destination. Ruins extend for a distance on both sides of the highway, many of the more distant structures are little visited. As of 2003, a program is ongoing to clear and restore more buildings, microbial biofilms have been found degrading stone buildings at Uxmal and Kabah. Phototrophs such as Xenococcus are found more often on interior walls, however stone degrading Gloeocapsa and Synechocystis were also present in large numbers. Kabah was declared a Yucatán state park in 1993, Kabah on MayaInfo. org with photos Kabáh on sci. mus. mn. us more photos Kabáh, The Mayan Kingdom A photographic web-book on the Maya Kabah web site at Reed College
3.
Uxmal
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Uxmal is an ancient Maya city of the classical period in present-day Mexico. It is considered one of the most important archaeological sites of Maya culture, along with Palenque, Chichén, and Calakmul in Mexico, Caracol and Xunantunich in Belize, and Tikal in Guatemala. It is located in the Puuc region and is considered one of the Maya cities most representative of the dominant architectural style. It has been designated a UNESCO World Heritage Site in recognition of its significance and it is located 62 km south of Mérida, capital of Yucatán state in Mexico. Its buildings are noted for their size and decoration and its buildings are typical of the Puuc style, with smooth low walls that open on ornate friezes based on representations of typical Maya huts. These are represented by columns and trapezoidal shapes, entwined snakes and, in many cases two-headed snakes are used for masks of the rain god, Chaac, its big noses represent the rays of the storms. Feathered serpents with open fangs are shown leaving from the human beings. Also seen in cities are the influences of the Nahua. These were integrated with the elements of the Puuc tradition. The present name seems to derive from Oxmal, meaning three times built and this seems to refer to the sites antiquity and the times it had to rebuild. The etymology is disputed, another possibility is Uchmal which means what is to come, by tradition, this was supposed to be an invisible city, built in one night by the magic of the dwarf king. While much work has been done at the popular tourist destination of Uxmal to consolidate and restore buildings, little in the way of serious archeological excavation, the citys dates of occupation are unknown and the estimated population is a rough guess. Most of the major construction took place while Uxmal was the capital of a Late Classic Maya state around 850-925 AD. After about 1000 AD, Toltec invaders took over, and most building ceased by 1100 AD, Maya chronicles say that Uxmal was founded about 500 A. D. by Hun Uitzil Chac Tutul Xiu. For generations Uxmal was ruled over by the Xiu family and it was the most powerful site in western Yucatán, and for a while, in alliance with Chichen Itza, dominated all of the northern Maya area. Sometime after about 1200, no new major construction seems to have made at Uxmal, possibly related to the fall of Uxmals ally Chichen Itza. The Xiu moved their capital to Maní, and the population of Uxmal declined, Uxmal was dominant from 875 to 900 CE. The site appears to have been the capital of a state in the Puuc region from 850-950 CE
4.
Maya architecture
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A unique and intricate style, the tradition of Maya architecture spans several thousands of years. Often, the buildings most dramatic and easily recognizable as Mayans are the stepped pyramids the Terminal Pre-classic period, being based on the general Mesoamerican architectural traditions, these pyramids relied on intricate carved stone in order to create a stairstep design. Each pyramid was dedicated to a deity whose shrine sat at its peak, during this height of Maya culture, the centers of their religious, commercial and bureaucratic power grew into large cities, namely Tikal, and Uxmal. Through observation of the numerous consistent elements and stylistic distinctions, remnants of Maya architecture have become an important key to understanding the evolution of their ancient temples, Maya architecture tends to integrate a great degree of natural features. However, some semblance of order, as required by any large city, at the onset of large-scale construction, a predetermined axis was typically established in congruence with the cardinal directions. Immediately outside of this center were the structures of lesser nobles, smaller temples, and individual shrines. Outside of the evolving urban core were the less permanent. Classic Era Maya urban design could easily be described as the division of space by great monuments, in this case, the open public plazas were the gathering places for the people and the focus of the urban design, while interior space was entirely secondary. Only in the Late Post-Classic era did the great Maya cities develop into more fortress-like defensive structures that lacked, for the most part, the large and numerous plazas of the Classic. A flight of steep stone steps split the large stepped platforms on at least one side. Depending on the prevalent stylistic tendencies of an area, these platforms most often were built of a stucco, as is the case with many other Maya reliefs, those on the platforms often were related to the intended purpose of the residing structure. Thus, as the platforms were completed, the grand residences and temples of the Maya were constructed on the solid foundations of the platforms. Commonly, these would continue uninterrupted around a structure and contain a variety of artwork pertaining to the inhabitants or purpose of a building. Though not the case in all Maya locations, broad use of painted stucco has been discovered as well and it has been suggested that, in conjunction to the Maya Long Count Calendar, every fifty-two years, or cycle, temples and pyramids were remodeled and rebuilt. It appears now that the process was often instigated by a new ruler or for political matters. However, the process of rebuilding on top of old structures is indeed a common one, most notably, the North Acropolis at Tikal seems to be the sum total of 1,500 years of architectural modifications. These were commonly limestone platforms of typically less than four meters in height where public ceremonies, large and often highly decorated, the palaces usually sat close to the center of a city and housed the populations elite. Every exceedingly large royal palace, or one consisting of many chambers on different levels might be referred to as an acropolis, archaeologists seem to agree that many palaces are home to various tombs
5.
Hill
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A hill is a landform that extends above the surrounding terrain. It often has a summit, although in areas with scarp/dip topography a hill may refer to a particular section of flat terrain without a massive summit. The distinction between a hill and a mountain is unclear and largely subjective, but a hill is considered to be less tall. The Great Soviet Encyclopedia defines hill as an upland with a height up to 200 m. Today, a mountain is usually defined in the UK and Ireland as any summit at least 2,000 feet high, some definitions include a topographical prominence requirement, typically 100 feet or 500 feet. In practice, mountains in Scotland are frequently referred to as no matter what their height, as reflected in names such as the Cuillin Hills. In Wales, the distinction is more a term of land use, for a while, the U. S. defined a mountain as being 1,000 feet or more tall. Any similar landform lower than this height was considered a hill, the United States Geological Survey, however, has concluded that these terms do not in fact have technical definitions in the U. S. A hillock is a small hill, other words include knoll and its variant, knowe. Artificial hills may be referred to by a variety of names, including mound. Various names used to describe types of hill, based on appearance and these include, Drumlin – an elongated whale-shaped hill formed by glacial action. Butte – an isolated hill with steep sides and a flat top. Kuppe – a rounded hill or low mountain, typical of central Europe Tor – a rock found on a hilltop, also used to refer to the hill. Puy – used especially in the Auvergne, France, to describe a conical volcanic hill, pingo – a mound of earth-covered ice found in the Arctic and Antarctica. For example, Ancient Rome was built on seven hills, protecting it from invaders, in northern Europe, many ancient monuments are sited in heaps. Some of these are structures, but others appear to have hardly any significance. In Britain, many churches at the tops of hills are thought to have built on the sites of earlier pagan holy places. The National Cathedral in Washington, DC has followed this tradition and was built on the highest hill in that city, Hills provide a major advantage to an army, giving them an elevated firing position and forcing an opposing army to charge uphill to attack them
6.
Karst
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Karst topography is a landscape formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves and it has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes, the English word karst was borrowed from German Karst in the late 19th century. The German word came into use before the 19th century, according to the prevalent interpretation, the term is derived from the German name for the Karst region, a limestone plateau above the city of Trieste in the northern Adriatic. Scholars disagree, however, on whether the German word was borrowed from Slovene, the Slovene common noun kras was first attested in the 18th century, and the adjective form kraški in the 16th century. The Slovene words arose through metathesis from the reconstructed form *korsъ, ultimately, the word is of Mediterranean origin, believed to derive from some Romanized Illyrian base. It has been suggested that the word may derive from the Proto-Indo-European root karra- rock, the name may also be connected to the oronym Karsádios oros cited by Ptolemy, and perhaps also to Latin Carusardius. The development of karst occurs whenever acidic water starts to break down the surface of bedrock near its cracks, as the bedrock continues to degrade, its cracks tend to get bigger. As time goes on, these fractures will become wider, if this underground drainage system does form, it will speed up the development of karst formations there because more water will be able to flow through the region, giving it more erosive power. The carbonic acid that causes karstic features is formed as rain passes through the atmosphere picking up carbon dioxide, once the rain reaches the ground, it may pass through soil that can provide much more CO2 to form a weak carbonic acid solution, which dissolves calcium carbonate. The oxidation of sulfides leading to the formation of acid can also be one of the corrosion factors in karst formation. As oxygen -rich surface waters seep into deep anoxic karst systems, they bring oxygen, sulfuric acid then reacts with calcium carbonate, causing increased erosion within the limestone formation. This chain of reactions is, This reaction chain forms gypsum, the karstification of a landscape may result in a variety of large- or small-scale features both on the surface and beneath. On exposed surfaces, small features may include solution flutes, runnels, limestone pavement, medium-sized surface features may include sinkholes or cenotes, vertical shafts, foibe, disappearing streams, and reappearing springs. Large-scale features may include limestone pavements, poljes, and karst valleys, mature karst landscapes, where more bedrock has been removed than remains, may result in karst towers, or haystack/eggbox landscapes. Beneath the surface, complex underground systems and extensive caves. Some of the most dramatic of these formations can be seen in Thailands Phangnga Bay, calcium carbonate dissolved into water may precipitate out where the water discharges some of its dissolved carbon dioxide. Rivers which emerge from springs may produce tufa terraces, consisting of layers of calcite deposited over extended periods of time, in caves, a variety of features collectively called speleothems are formed by deposition of calcium carbonate and other dissolved minerals
7.
Quintana Roo
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Quintana Roo, officially the Free and Sovereign State of Quintana Roo, is one of the 31 states which, with the Federal District, make up the 32 federal entities of Mexico. It is divided into ten municipalities and its capital city is Chetumal and it is located in Southeastern Mexico, on the eastern part of the Yucatán Peninsula. Quintana Roo has a coastline to the east with the Caribbean Sea and it also claims territory which gives it a small border with Guatemala in the southwest of the state, although this disputed area is also claimed by Campeche. The Sian Kaan biosphere reserve is located in the state. The statewide population is expanding at a rapid rate due to the construction of hotels, many immigrants come from Yucatán, Campeche, Tabasco, and Veracruz. On February 1,2015, Quintana Roo officially adopted a new zone, Southeastern, which is five hours behind Coordinated Universal Time. Reasons cited for the change include coordination of air travel, banking operations, and more daylight hours, the area that makes up modern Quintana Roo was long part of Yucatán, sharing its history. With the Caste War of Yucatán, which started in the 1840s, the independent Maya nation of Chan Santa Cruz was based on what is now the town of Felipe Carrillo Puerto. For decades it maintained independence, having separate trade and treaty relationships with British Honduras. Quintana Roo was made a territory of Mexico by decree of President Porfirio Díaz on November 24,1902 and it was named after an early patriot of the Mexican Republic, Andrés Quintana Roo. The Mexican army succeeded in defeating most of the Maya population of the region during the 1910s, in 1915 the area was again declared to be legally part of the state of Yucatán. Quintana Roo was granted statehood within the United Mexican States on October 8,1974 and it is the Mexican Republics youngest state. According to the Köppen climate classification, much of the state has a tropical wet, the mean annual temperature is 26 °C. The hottest months are April and August where the high is 33 °C while January is coldest month with an average low of 17 °C. Extreme temperatures can range from low of 10 °C in the coldest months to 36 °C in the hottest months, Quintana Roo averages 1,300 mm of precipitation per year, which falls throughout the year, though June to October are the wetter months. Hurricanes can occasionally hit the areas during the hurricane season. The State of Quintana Roo is divided into 11 municipalities, each headed by a municipal president, Quintana Roo ranks sixth among Mexican states according to the United Nations Human Development index. The Yucatán Peninsula is one of the most forested areas of the world in terms of mass per hectare
8.
Mesoamerican architecture
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The distinctive features of Mesoamerican architecture encompass a number of different regional and historical styles, which however are significantly interrelated. Mesoamerican architecture is noted for its pyramids which are the largest such structures. One interesting and widely researched topic is the relation between cosmovision, religion, geography, and architecture in Mesoamerica, much seems to suggest that many traits of Mesoamerican architecture were governed by religious and mythological ideas. For example, the layout of most Mesoamerican cities seem to be influenced by the directions and their mythological. Another part of Mesoamerican architecture is its iconography, the monumental architecture of Mesoamerica was decorated with images of religious and cultural significance, and also in many cases with writing in some of the Mesoamerican writing systems. Iconographic decorations and texts on buildings are important contributors to the current knowledge of pre-Columbian Mesoamerican society, history. An important part of the Mesoamerican religious system was replicating their beliefs in concrete tangible forms, the underworld was represented by the direction north and many structures and buildings related to the underworld, such as tombs, are often found in the citys northern half. Mesoamerican architecture is designed to align to specific celestial events. Pyramids, temples, and other structures were designed to achieve special lighting effects on the equinoxes or on other days important in the Mesoamerican cosmovision. A famous example is the El Castillo pyramid at Chichen Itza, much Mesoamerican architecture is also aligned to roughly 15° east of north. Vincent H Malmstrom has argued that this is because of a wish to align the pyramids to face the sunset on August 13. Often the most important religious temples sat atop the towering pyramids, while recent discoveries point toward the extensive use of pyramids as tombs, the temples themselves seem to rarely, if ever, contain burials. Residing atop the pyramids, some of over two-hundred feet, such as that at El Mirador, commonly topped with a roof comb, or superficial grandiose wall, these temples might have served as a type of propaganda. All but the earliest ball courts are masonry structures, the later vertical faces, such as those at Chichen Itza and El Tajin, are often covered with complex iconography and scenes of human sacrifice. Although the alleys in early ball courts were open-ended, later ball courts had enclosed end-zones, the playing alley may be at ground level, or the ball court may be sunken. Ball courts were no mean feats of engineering, one of the sandstone stones on El Tajins South Ball court is 11 m long and weighs more than 10 tons. Large and often decorated, the palaces usually sat close to the center of a city. Any exceedingly large royal palace, or one consisting of many chambers on different levels might be referred to as an acropolis, archaeologists seem to agree that many palaces are home to various tombs
9.
Mesoamerican chronology
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Mesoamerican chronology divides the history of pre-Columbian Mesoamerica into several periods, the Paleo-Indian, the Archaic, the Preclassic or Formative, the Classic, and the Postclassic. However, this applies to other pre-Columbian Mesoamerican civilizations as well. 3500-2000 BCE During the Archaic Era agriculture was developed in the region, Late in this era, use of pottery and loom weaving became common, and class divisions began to appear. Many of the technologies of Mesoamerica in terms of stone-grinding, drilling. 1800 BCE–200 CE During the Preclassic Era, or Formative Period, large-scale ceremonial architecture, writing, cities, the Olmec civilization developed and flourished at such sites as La Venta and San Lorenzo Tenochtitlán. 200–1000 CE The Classic Era was dominated by numerous independent city-states in the Maya region and also featured the beginnings of political unity in central Mexico, regional differences between cultures grew more manifest. The city-state of Monte Albán dominated the Valley of Oaxaca until the late Classic, highly sophisticated arts such as stuccowork, architecture, sculptural reliefs, mural painting, pottery, and lapidary developed and spread during the Classic era. In the Maya region, numerous city states such as Tikal, Calakmul, Copán, Palenque, Uxmal, Cobá, each of these polities was generally independent, although they often formed alliances and sometimes became vassal states of each other. The main conflict during this period was between Tikal and Calakmul, who fought a series of wars over the course of more than half a millennium, each of these states declined during the Terminal Classic and were eventually abandoned. This is sometimes seen as a period of increased chaos and warfare, the Postclassic is often viewed as a period of cultural decline. However, it was a time of technological advancement in architecture, engineering, metallurgy came into use for jewelry and some tools, with new alloys and techniques being developed in a few centuries. The Postclassic was a period of rapid movement and population growth — especially in Central Mexico post-1200 —, for instance, in Yucatán, dual rulership apparently replaced the more theocratic governments of Classic times, whilst oligarchic councils operated in much of Central Mexico. Likewise, it appears that the wealthy pochteca and military orders became more powerful than was apparently the case in Classic times and this afforded some Mesoamericans a degree of social mobility. The Toltec for a time dominated central Mexico in the 11th–13th century, the northern Maya were for a time united under Mayapan, and Oaxaca was briefly united by Mixtec rulers in the 11th–12th centuries. The Aztec Empire arose in the early 15th century and appeared to be on a path to asserting dominance over the Valley of Mexico region not seen since Teotihuacan. Spain was the first European power to contact Mesoamerica, however, and its conquistadores, by the 15th century, the Mayan revival in Yucatán and southern Guatemala and the flourishing of Aztec imperialism evidently enabled a renaissance of fine arts and science. Examples include the Pueblan-Mexica style in pottery, codex illumination, and goldwork, the flourishing of Nahua poetry, arguably, the Post-Classic continued until the conquest of the last independent native state of Mesoamerica, Tayasal, in 1697. Mesoamerican civilization was a network of different cultures
