The Corps of Royal Engineers just called the Royal Engineers, known as the Sappers, is one of the corps of the British Army. It provides military engineering and other technical support to the British Armed Forces and is headed by the Chief Royal Engineer; the Regimental Headquarters and the Royal School of Military Engineering are in Chatham in Kent, England. The corps is divided into several regiments, barracked at various places in the United Kingdom and around the world; the Royal Engineers trace their origins back to the military engineers brought to England by William the Conqueror Bishop Gundulf of Rochester Cathedral, claim over 900 years of unbroken service to the crown. Engineers have always served in the armies of the Crown. In Woolwich in 1716, the Board formed the Royal Regiment of Artillery and established a Corps of Engineers, consisting of commissioned officers; the manual work was done by the Artificer Companies, made up of contracted civilian artisans and labourers. In 1772, a Soldier Artificer Company was established for service in Gibraltar, the first instance of non-commissioned military engineers.
In 1787, the Corps of Engineers was granted the Royal prefix and adopted its current name and in the same year a Corps of Royal Military Artificers was formed, consisting of non-commissioned officers and privates, to be led by the RE. Ten years the Gibraltar company, which had remained separate, was absorbed and in 1812 the name was changed to the Corps of Royal Sappers and Miners; the Corps has no battle honours. In 1832, the regimental motto, Ubique' &'Quo Fas Et Gloria Ducunt, was granted; the motto signified that the Corps had seen action in all the major conflicts of the British Army and all of the minor ones as well. In 1855 the Board of Ordnance was abolished and authority over the Royal Engineers, Royal Sappers and Miners and Royal Artillery was transferred to the Commander-in-Chief of the Forces, thus uniting them with the rest of the Army; the following year, the Royal Engineers and Royal Sappers and Miners became a unified corps as the Corps of Royal Engineers and their headquarters were moved from the Royal Arsenal, Woolwich, to Chatham, Kent.
The re-organisation of the British military that began in the mid-Nineteenth Century and stretched over several decades included the reconstitution of the Militia, the raising of the Volunteer Force, the ever-closer organisation of the part-time forces with the regular army. The old Militia had been an infantry force, other than the occasional employment of Militiamen to man artillery defences and other roles on an emergency basis; this changed with the conversion of some units to artillery roles. Militia and Volunteer Engineering companies were created, beginning with the conversion of the militia of Anglesey and Monmouthshire to engineers in 1877; the Militia and Volunteer Force engineers supported the regular Royal Engineers in a variety of roles, including operating the boats required to tend the submarine mine defences that protected harbours in Britain and its empire. These included a submarine mining militia company, authorised for Bermuda in 1892, but never raised, the Bermuda Volunteer Engineers that wore Royal Engineers uniforms and replaced the regular Royal Engineers companies withdrawn from the Bermuda Garrison in 1928.
The various part-time reserve forces were amalgamated into the Territorial Force in 1908, retitled the Territorial Army after the First World War, the Army Reserve in 2014. In 1911 the Corps formed the first flying unit of the British Armed Forces; the Air Battalion was the forerunner of the Royal Flying Royal Air Force. In 1915, in response to German mining of British trenches under the static siege conditions of the First World War, the corps formed its own tunnelling companies. Manned by experienced coal miners from across the country, they operated with great success until 1917, when after the fixed positions broke, they built deep dugouts such as the Vampire dugout to protect troops from heavy shelling. Before the Second World War, Royal Engineers recruits were required to be at least 5 feet 4 inches tall, they enlisted for six years with the colours and a further six years with the reserve or four years and eight years. Unlike most corps and regiments, in which the upper age limit was 25, men could enlist in the Royal Engineers up to 35 years of age.
They trained at the Royal Engineers Depot in the RE Mounted Depot at Aldershot. During the 1980s, the Royal Engineers formed the vital component of at least three Engineer Brigades - 12 Engineer Brigade. After the Falklands War, 37 Engineer Regiment was active from August 1982 until 14 March 1985; the Royal Engineers Museum is in Gillingham in Kent. Britain having acquired an Empire, it fell to the Royal Engineers to conduct some of the most significant "civil" engineering schemes around the world; some examples of great works of the era of empire can be found in A. J. Smithers's book Honourable Conquests; the Royal Engineers, Columbia Detachment, commanded by Richard Clement Moody, was responsible for the foundation and settlement of British Columbia as the Colony of British Columbia. The Royal Albert Hall is one of the UK's most treasured and distinctive buildings, recognisable the world over. Since its opening by Queen Victoria in 1871, the world's leading artists from every kind of performance genre have appeared on its stage.
Each year it
A sea cave known as a littoral cave, is a type of cave formed by the wave action of the sea. The primary process involved is erosion. Sea caves are found throughout the world forming along present coastlines and as relict sea caves on former coastlines; some of the largest wave-cut caves in the world are found on the coast of Norway, but are now 100 feet or more above present sea level. These would still be classified as littoral caves. By contrast, in places like Thailand's Phang Nga Bay, solutionally formed caves in limestone have been flooded by the rising sea and are now subject to littoral erosion, representing a new phase of their enlargement; some of the best-known sea caves are European. Fingal's Cave, on the Scottish island of Staffa, is a spacious cave some 70 m long, formed in columnar basalt; the Blue Grotto of Capri, although smaller, is famous for the apparent luminescent quality of its water, imparted by light passing through underwater openings. The Romans built a stairway in a now-collapsed tunnel to the surface.
The Greek islands are noted for the variety and beauty of their sea caves. Numerous sea caves have been surveyed in England, in France on the Normandy coast; until 2013, the largest known sea caves were found along the west coast of the United States, the Hawaiian islands, the Shetland Islands. In 2013 the discovery and survey of the world's largest sea cave was announced. Matainaka Cave - located on the Otago coast of New Zealand's South Island - has proven to be the world's most extensive at 1.5 km in length. In 2013, Crossley reported a newly surveyed complex reaching just over a kilometer in survey at Bethells Beach on New Zealand's North Island. Littoral caves may be found in a wide variety of host rocks, ranging from sedimentary to metamorphic to igneous, but caves in the latter tend to be larger due to the greater strength of the host rock. However, there are some notable exceptions as discussed below. In order to form a sea cave, the host rock must first contain a weak zone. In metamorphic or igneous rock, this is either a fault as in the caves of the Channel Islands of California, or a dike as in the large sea caves of Kauai, Hawaii’s Na Pali Coast.
In sedimentary rocks, this may be a bedding-plane parting or a contact between layers of different hardness. The latter may occur in igneous rocks, such as in the caves on Santa Cruz Island, where waves have attacked the contact between the andesitic basalt and the agglomerate; the driving force in littoral cave development is wave action. Erosion is ongoing anywhere that waves batter rocky coasts, but where sea cliffs contain zones of weakness, rock is removed at a greater rate along these zones; as the sea reaches into the fissures thus formed, they begin to widen and deepen due to the tremendous force exerted within a confined space, not only by direct action of the surf and any rock particles that it bears, but by compression of air within. Blowholes attest to this process. Adding to the hydraulic power of the waves is the abrasive force of suspended sand and rock. Most sea-cave walls are irregular and chunky, reflecting an erosional process where the rock is fractured piece by piece. However, some caves have portions where the walls are rounded and smoothed floored with cobbles, result from the swirling motion of these cobbles in the surf zone.
True littoral caves should not be confused with inland caves that have been intersected and revealed when a sea cliff line is eroded back, or with dissolutional voids formed in the littoral zone on tropical islands. In some regions, such as Halong Bay, caves in carbonate rocks are found in littoral zones, being enlarged by littoral processes but were formed by dissolution; such caves have been termed as hybrid caves. Rainwater may influence sea-cave formation. Carbonic and organic acids leached from the soil may assist in weakening rock within fissures; as in solutional caves, small speleothems may develop in sea caves. Sea cave chambers sometimes collapse leaving a “littoral sinkhole”; these may be quite large, such as Oregon’s Devil’s Punchbowl or the Queen’s Bath on the Na Pali coast. Small peninsulas or headlands have caves that cut through them, since they are subject to attack from both sides, the collapse of a sea cave tunnel can leave a free-standing “sea stack” along the coast; the Californian island of Anacapa is thought to have been split into three islets by such a process.
Life within sea caves may assist in their enlargement as well. For example, sea urchins drill their way into the rock, over successive generations may remove considerable bedrock from the floors and lower walls. Most sea caves are small in relation to other types. A compilation of sea-cave surveys as of July 2014 shows 2 over 1000 meters, 6 over 400 meters, nine over 300 meters, 25 over 200 meters, 108 over 100 meters in length. In Norway, several relict sea caves exceed 300 meters in length. There is no doubt that many other large sea caves exist but have not been investigated due to their remote locations and/or hostile sea conditions. Several factors contribute to the development of large sea caves; the nature of the zone of weakness itself is a factor, although difficult to quantify. A more observed factor is the situation of the cave’s entrance relative to prevailing sea conditions. At Santa Cruz Island, the largest caves face into the prevailing northwest swell conditions—a factor which makes them more difficult to survey.
Caves in well-protected bays sheltered from prevailing seas and wi
Limestone is a carbonate sedimentary rock, composed of the skeletal fragments of marine organisms such as coral and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate. A related rock is dolostone, which contains a high percentage of the mineral dolomite, CaMg2. In fact, in old USGS publications, dolostone was referred to as magnesian limestone, a term now reserved for magnesium-deficient dolostones or magnesium-rich limestones. About 10% of sedimentary rocks are limestones; the solubility of limestone in water and weak acid solutions leads to karst landscapes, in which water erodes the limestone over thousands to millions of years. Most cave systems are through limestone bedrock. Limestone has numerous uses: as a building material, an essential component of concrete, as aggregate for the base of roads, as white pigment or filler in products such as toothpaste or paints, as a chemical feedstock for the production of lime, as a soil conditioner, or as a popular decorative addition to rock gardens.
Like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of marine organisms such as foraminifera; these organisms secrete shells made of aragonite or calcite, leave these shells behind when they die. Other carbonate grains composing limestones are ooids, peloids and extraclasts. Limestone contains variable amounts of silica in the form of chert or siliceous skeletal fragment, varying amounts of clay and sand carried in by rivers; some limestones do not consist of grains, are formed by the chemical precipitation of calcite or aragonite, i.e. travertine. Secondary calcite may be deposited by supersaturated meteoric waters; this produces speleothems, such as stalactites. Another form taken by calcite is oolitic limestone, which can be recognized by its granular appearance; the primary source of the calcite in limestone is most marine organisms. Some of these organisms can construct mounds of rock building upon past generations. Below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone does not form in deeper waters.
Limestones may form in lacustrine and evaporite depositional environments. Calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, dissolved ion concentrations. Calcite exhibits an unusual characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors with weathered surfaces. Limestone may be crystalline, granular, or massive, depending on the method of formation. Crystals of calcite, dolomite or barite may line small cavities in the rock; when conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together, or it can fill fractures. Travertine is a banded, compact variety of limestone formed along streams where there are waterfalls and around hot or cold springs. Calcium carbonate is deposited where evaporation of the water leaves a solution supersaturated with the chemical constituents of calcite.
Tufa, a porous or cellular variety of travertine, is found near waterfalls. Coquina is a poorly consolidated limestone composed of pieces of coral or shells. During regional metamorphism that occurs during the mountain building process, limestone recrystallizes into marble. Limestone is a parent material of Mollisol soil group. Two major classification schemes, the Folk and the Dunham, are used for identifying the types of carbonate rocks collectively known as limestone. Robert L. Folk developed a classification system that places primary emphasis on the detailed composition of grains and interstitial material in carbonate rocks. Based on composition, there are three main components: allochems and cement; the Folk system uses two-part names. It is helpful to have a petrographic microscope when using the Folk scheme, because it is easier to determine the components present in each sample; the Dunham scheme focuses on depositional textures. Each name is based upon the texture of the grains. Robert J. Dunham published his system for limestone in 1962.
Dunham divides the rocks into four main groups based on relative proportions of coarser clastic particles. Dunham names are for rock families, his efforts deal with the question of whether or not the grains were in mutual contact, therefore self-supporting, or whether the rock is characterized by the presence of frame builders and algal mats. Unlike the Folk scheme, Dunham deals with the original porosity of the rock; the Dunham scheme is more useful for hand samples because it is based on texture, not the grains in the sample. A revised classification was proposed by Wright, it adds some diagenetic patterns and can be summarized as follows: See: Carbonate platform About 10% of all sedimentary rocks are limestones. Limestone is soluble in acid, therefore forms many erosional landforms; these include limestone pavements, pot holes, cenotes and gorges. Such erosion landscapes are known
A stone tool is, in the most general sense, any tool made either or out of stone. Although stone tool-dependent societies and cultures still exist today, most stone tools are associated with prehistoric cultures that have become extinct. Archaeologists study such prehistoric societies, refer to the study of stone tools as lithic analysis. Ethnoarchaeology has been a valuable research field in order to further the understanding and cultural implications of stone tool use and manufacture. Stone has been used to make a wide variety of different tools throughout history, including arrow heads and querns. Stone tools may be made of either ground stone or chipped stone, a person who creates tools out of the latter is known as a flintknapper. Chipped stone tools are made from cryptocrystalline materials such as chert or flint, chalcedony, obsidian and quartzite via a process known as lithic reduction. One simple form of reduction is to strike stone flakes from a nucleus of material using a hammerstone or similar hard hammer fabricator.
If the goal of the reduction strategy is to produce flakes, the remnant lithic core may be discarded once it has become too small to use. In some strategies, however, a flintknapper reduces the core to a rough unifacial or bifacial preform, further reduced using soft hammer flaking techniques or by pressure flaking the edges. More complex forms of reduction include the production of standardized blades, which can be fashioned into a variety of tools such as scrapers, knives and microliths. In general terms, chipped stone tools are nearly ubiquitous in all pre-metal-using societies because they are manufactured, the tool stone is plentiful, they are easy to transport and sharpen. Archaeologists classify stone tools into industries that share distinctive technological or morphological characteristics. In 1969 in the 2nd edition of World Prehistory, Grahame Clark proposed an evolutionary progression of flint-knapping in which the "dominant lithic technologies" occurred in a fixed sequence from Mode 1 through Mode 5.
He assigned to them relative dates: Modes 1 and 2 to the Lower Palaeolithic, 3 to the Middle Palaeolithic, 4 to the Advanced and 5 to the Mesolithic. They were not to be conceived, however, as either universal—that is, they did not account for all lithic technology. Mode 1, for example, was in use in Europe. Clark's scheme was adopted enthusiastically by the archaeological community. One of its advantages was the simplicity of terminology; the transitions are of greatest interest. In the literature the stone tools used in the period of the Palaeolithic are divided into four "modes", each of which designate a different form of complexity, which in most cases followed a rough chronological order. KenyaStone tools found from 2011 to 2014 at Lake Turkana in Kenya, are dated to be 3.3 million years old, predate the genus Homo by half million years. The oldest known Homo fossil is 2.8 million years old compared to the 3.3 million year old stone tools. The stone tools may have been made by Australopithecus afarensis —also called Kenyanthropus platyops— the species whose best fossil example is Lucy, which inhabited East Africa at the same time as the date of the oldest stone tools.
Dating of the tools was by dating volcanic ash layers in which the tools were found and dating the magnetic signature of the rock at the site. EthiopiaGrooved and fractured animal bone fossils, made by using stone tools, were found in Dikika, Ethiopia near the remains of Selam, a young Australopithecus afarensis girl who lived about 3.3 million years ago. The earliest stone tools in the life span of the genus Homo are Mode 1 tools, come from what has been termed the Oldowan Industry, named after the type of site found in Olduvai Gorge, where they were discovered in large quantities. Oldowan tools were characterised by their simple construction; these cores were river pebbles, or rocks similar to them, struck by a spherical hammerstone to cause conchoidal fractures removing flakes from one surface, creating an edge and a sharp tip. The blunt end is the proximal surface. Oldowan is a percussion technology. Grasping the proximal surface, the hominid brought the distal surface down hard on an object he wished to detach or shatter, such as a bone or tuber.
The earliest known Oldowan tools yet found date from 2.6 million years ago, during the Lower Palaeolithic period, have been uncovered at Gona in Ethiopia. After this date, the Oldowan Industry subsequently spread throughout much of Africa, although archaeologists are unsure which Hominan species first developed them, with some speculating that it was Australopithecus garhi, others believing that it was in fact Homo habilis. Homo habilis was the hominin who used the tools for most of the Oldowan in Africa, but at about 1.9-1.8 million years ago Homo erectus inherited them. The Industry flourished in southern and eastern Africa between 2.6 and 1.7 million years ago, but was spread out of Africa and into Eurasia by travelling bands of H. erectus, who took it as far east as Java by 1.8 million years ago and Northern China by 1.6 million years ago. More complex, Mode 2 tools began to be developed through the Acheulean Industry, named after the site
Pottery is the process of forming vessels and other objects with clay and other ceramic materials, which are fired to give them a hard, durable form. Major types include earthenware and porcelain; the place where such wares are made by a potter is called a pottery. The definition of pottery used by the American Society for Testing and Materials, is "all fired ceramic wares that contain clay when formed, except technical and refractory products." In archaeology of ancient and prehistoric periods, "pottery" means vessels only, figures etc. of the same material are called "terracottas". Clay as a part of the materials used is required by some definitions of pottery, but this is dubious. Pottery is one of the oldest human inventions, originating before the Neolithic period, with ceramic objects like the Gravettian culture Venus of Dolní Věstonice figurine discovered in the Czech Republic dating back to 29,000–25,000 BC, pottery vessels that were discovered in Jiangxi, which date back to 18,000 BC.
Early Neolithic pottery artefacts have been found in places such as Jōmon Japan, the Russian Far East, Sub-Saharan Africa and South America. Pottery is made by forming a ceramic body into objects of a desired shape and heating them to high temperatures in a kiln and induces reactions that lead to permanent changes including increasing the strength and solidity of the object's shape. Much pottery is purely utilitarian, but much can be regarded as ceramic art. A clay body can be decorated after firing. Clay-based pottery can divided in three main groups: earthenware and porcelain; these require more specific clay material, higher firing temperatures. All three are made for different purposes. All may be decorated by various techniques. In many examples the group a piece belongs to is visually apparent, but this is not always the case; the fritware of the Islamic world does not use clay, so technically falls outside these groups. Historic pottery of all these types is grouped as either "fine" wares expensive and well-made, following the aesthetic taste of the culture concerned, or alternatively "coarse", "popular" "folk" or "village" wares undecorated, or so, less well-made.
All the earliest forms of pottery were made from clays that were fired at low temperatures in pit-fires or in open bonfires. They were hand undecorated. Earthenware can be fired as low as 600°C, is fired below 1200°C; because unglazed biscuit earthenware is porous, it has limited utility for the storage of liquids, eating off. However, earthenware has a continuous history from the Neolithic period to today, it can be made from a wide variety of clays, some of which fire to a buff, brown or black colour, with iron in the constituent minerals resulting in a reddish-brown. Reddish coloured varieties are called terracotta when unglazed or used for sculpture; the development of ceramic glaze which makes it impermeable makes it a popular and practical form of pottery. The addition of decoration has evolved throughout its history. Stoneware is pottery, fired in a kiln at a high temperature, from about 1,100°C to 1,200°C, is stronger and non-porous to liquids; the Chinese, who developed stoneware early on, classify this together with porcelain as high-fired wares.
In contrast, stoneware could only be produced in Europe from the late Middle Ages, as European kilns were less efficient, the right sorts of clay less common. It remained a speciality of Germany until the Renaissance. Stoneware is tough and practical, much of it has always been utilitarian, for the kitchen or storage rather than the table, but "fine" stoneware has been important in China and the West, continues to be made. Many utilitarian types have come to be appreciated as art. Porcelain is made by heating materials including kaolin, in a kiln to temperatures between 1,200 and 1,400 °C; this is higher than used for the other types, achieving these temperatures was a long struggle, as well as realizing what materials were needed. The toughness and translucence of porcelain, relative to other types of pottery, arises from vitrification and the formation of the mineral mullite within the body at these high temperatures. Although porcelain was first made in China, the Chinese traditionally do not recognise it as a distinct category, grouping it with stoneware as "high-fired" ware, opposed to "low-fired" earthenware.
This confuses the issue of. A degree of translucency and whiteness was achieved by the Tang Dynasty, considerable quantities were being exported; the modern level of whiteness was not reached until much in the 14th century. Porcelain was made in Korea and in Japan from the end of the 16th century, after suitable kaolin was located in those countries, it was not made outside East Asia until the 18th century. Before being shaped, clay must be prepared. Kneading helps to ensure an moisture content throughout the body. Air trapped within the clay body needs to be removed; this is called de-airing and can be accomplished either by a machine called a vacuum pug or manually by wedging. Wedging can help produce an moisture content. Once a clay body has been kneaded and de-aired or wedged, it is shaped by a variety of techniques. After it has been shaped, it is dried and fired. Greenware refers to unfired objects. At sufficient moisture content, bodies at this stage are in their most plastic form (as they are soft and mal
The Neolithic, the final division of the Stone Age, began about 12,000 years ago when the first development of farming appeared in the Epipalaeolithic Near East, in other parts of the world. The division lasted until the transitional period of the Chalcolithic from about 6,500 years ago, marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In Northern Europe, the Neolithic lasted until about 1700 BC, while in China it extended until 1200 BC. Other parts of the world remained broadly in the Neolithic stage of development, although this term may not be used, until European contact; the Neolithic comprises a progression of behavioral and cultural characteristics and changes, including the use of wild and domestic crops and of domesticated animals. The term Neolithic derives from the Greek νέος néos, "new" and λίθος líthos, "stone" meaning "New Stone Age"; the term was coined by Sir John Lubbock in 1865 as a refinement of the three-age system. Following the ASPRO chronology, the Neolithic started in around 10,200 BC in the Levant, arising from the Natufian culture, when pioneering use of wild cereals evolved into early farming.
The Natufian period or "proto-Neolithic" lasted from 12,500 to 9,500 BC, is taken to overlap with the Pre-Pottery Neolithic of 10,200–8800 BC. As the Natufians had become dependent on wild cereals in their diet, a sedentary way of life had begun among them, the climatic changes associated with the Younger Dryas are thought to have forced people to develop farming. By 10,200–8800 BC farming communities had arisen in the Levant and spread to Asia Minor, North Africa and North Mesopotamia. Mesopotamia is the site of the earliest developments of the Neolithic Revolution from around 10,000 BC. Early Neolithic farming was limited to a narrow range of plants, both wild and domesticated, which included einkorn wheat and spelt, the keeping of dogs and goats. By about 6900–6400 BC, it included domesticated cattle and pigs, the establishment of permanently or seasonally inhabited settlements, the use of pottery. Not all of these cultural elements characteristic of the Neolithic appeared everywhere in the same order: the earliest farming societies in the Near East did not use pottery.
In other parts of the world, such as Africa, South Asia and Southeast Asia, independent domestication events led to their own regionally distinctive Neolithic cultures, which arose independently of those in Europe and Southwest Asia. Early Japanese societies and other East Asian cultures used pottery before developing agriculture. In the Middle East, cultures identified as Neolithic began appearing in the 10th millennium BC. Early development occurred from there spread eastwards and westwards. Neolithic cultures are attested in southeastern Anatolia and northern Mesopotamia by around 8000 BC; the prehistoric Beifudi site near Yixian in Hebei Province, contains relics of a culture contemporaneous with the Cishan and Xinglongwa cultures of about 6000–5000 BC, neolithic cultures east of the Taihang Mountains, filling in an archaeological gap between the two Northern Chinese cultures. The total excavated area is more than 1,200 square yards, the collection of neolithic findings at the site encompasses two phases.
The Neolithic 1 period began around 10,000 BC in the Levant. A temple area in southeastern Turkey at Göbekli Tepe, dated to around 9500 BC, may be regarded as the beginning of the period; this site was developed by nomadic hunter-gatherer tribes, as evidenced by the lack of permanent housing in the vicinity, may be the oldest known human-made place of worship. At least seven stone circles, covering 25 acres, contain limestone pillars carved with animals and birds. Stone tools were used by as many as hundreds of people to create the pillars, which might have supported roofs. Other early PPNA sites dating to around 9500–9000 BC have been found in Jericho, West Bank, Gilgal in the Jordan Valley, Byblos, Lebanon; the start of Neolithic 1 overlaps the Heavy Neolithic periods to some degree. The major advance of Neolithic 1 was true farming. In the proto-Neolithic Natufian cultures, wild cereals were harvested, early seed selection and re-seeding occurred; the grain was ground into flour. Emmer wheat was domesticated, animals were herded and domesticated.
In 2006, remains of figs were discovered in a house in Jericho dated to 9400 BC. The figs are of a mutant variety that cannot be pollinated by insects, therefore the trees can only reproduce from cuttings; this evidence suggests that figs were the first cultivated crop and mark the invention of the technology of farming. This occurred centuries before the first cultivation of grains. Settlements became more permanent, with circular houses, much like those of the Natufians, with single rooms. However, these houses were for the first time made of mudbrick; the settlement had a surrounding stone wall and a stone tower. The wall served as protection from nearby groups, as protection from floods, or to keep animals penned; some of the enclosures suggest grain and meat storage. The Neolithic 2 began around 8800 BC according to the ASPRO chronology in the Levant; as with the PPNA dates, there are two versions from the same laboratories noted above. This system of terminology, however, is not convenient for southeast Anatolia and settlements of the middle Anatolia basin.
A settlement of 3,000 inhabitants was found in th