1.
Maya civilization
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The Maya civilization developed in an area that encompasses southeastern Mexico, all of Guatemala and Belize, and the western portions of Honduras and El Salvador. The Archaic period, prior to 2000 BC, saw the first developments in agriculture, the first Maya cities developed around 750 BC, and by 500 BC these cities possessed monumental architecture, including large temples with elaborate stucco façades. Hieroglyphic writing was being used in the Maya region by the 3rd century BC, in the Late Preclassic a number of large cities developed in the Petén Basin, and Kaminaljuyu rose to prominence in the Guatemalan Highlands. Beginning around 250 AD, the Classic period is defined as when the Maya were raising sculpted monuments with Long Count dates. This period saw the Maya civilization develop a number of city-states linked by a complex trade network. In the Maya Lowlands two great rivals, Tikal and Calakmul, became powerful, the Classic period also saw the intrusive intervention of the central Mexican city of Teotihuacan in Maya dynastic politics. In the 9th century, there was a political collapse in the central Maya region, resulting in internecine warfare, the abandonment of cities. The Postclassic period saw the rise of Chichen Itza in the north, in the 16th century, the Spanish Empire colonized the Mesoamerican region, and a lengthy series of campaigns saw the fall of Nojpetén, the last Maya city in 1697. Classic period rule was centred on the concept of the divine king, kingship was patrilineal, and power would normally pass to the eldest son. A prospective king was expected to be a successful war leader. Maya politics was dominated by a system of patronage, although the exact political make-up of a kingdom varied from city-state to city-state. By the Late Classic, the aristocracy had greatly increased, resulting in the reduction in the exclusive power of the divine king. Maya cities tended to expand haphazardly, and the city centre would be occupied by ceremonial and administrative complexes, different parts of a city would often be linked by causeways. The principal architecture of the city consisted of palaces, pyramid-temples, ceremonial ballcourts, the Maya elite were literate, and developed a complex system of hieroglyphic writing that was the most advanced in the pre-Columbian Americas. The Maya recorded their history and ritual knowledge in screenfold books, there are also a great many examples of Maya text found on stelae and ceramics. The Maya developed a complex series of interlocking ritual calendars. As a part of their religion, the Maya practised human sacrifice, the Maya civilization developed within the Mesoamerican cultural area, which covers a region that spreads from northern Mexico southwards into Central America. Mesoamerica was one of six cradles of civilization worldwide, the Mesoamerican area gave rise to a series of cultural developments that included complex societies, agriculture, cities, monumental architecture, writing, and calendrical systems
2.
Mexico
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Mexico, officially the United Mexican States, is a federal republic in the southern half of North America. It is bordered to the north by the United States, to the south and west by the Pacific Ocean, to the southeast by Guatemala, Belize, and the Caribbean Sea, and to the east by the Gulf of Mexico. Covering almost two million square kilometers, Mexico is the sixth largest country in the Americas by total area, Mexico is a federation comprising 31 states and a federal district that is also its capital and most populous city. Other metropolises include Guadalajara, Monterrey, Puebla, Toluca, Tijuana, pre-Columbian Mexico was home to many advanced Mesoamerican civilizations, such as the Olmec, Toltec, Teotihuacan, Zapotec, Maya and Aztec before first contact with Europeans. In 1521, the Spanish Empire conquered and colonized the territory from its base in Mexico-Tenochtitlan, Three centuries later, this territory became Mexico following recognition in 1821 after the colonys Mexican War of Independence. The tumultuous post-independence period was characterized by instability and many political changes. The Mexican–American War led to the cession of the extensive northern borderlands, one-third of its territory. The Pastry War, the Franco-Mexican War, a civil war, the dictatorship was overthrown in the Mexican Revolution of 1910, which culminated with the promulgation of the 1917 Constitution and the emergence of the countrys current political system. Mexico has the fifteenth largest nominal GDP and the eleventh largest by purchasing power parity, the Mexican economy is strongly linked to those of its North American Free Trade Agreement partners, especially the United States. Mexico was the first Latin American member of the Organisation for Economic Co-operation and Development and it is classified as an upper-middle income country by the World Bank and a newly industrialized country by several analysts. By 2050, Mexico could become the fifth or seventh largest economy. The country is considered both a power and middle power, and is often identified as an emerging global power. Due to its culture and history, Mexico ranks first in the Americas. Mexico is a country, ranking fourth in the world by biodiversity. In 2015 it was the 9th most visited country in the world, Mexico is a member of the United Nations, the World Trade Organization, the G8+5, the G20, the Uniting for Consensus and the Pacific Alliance. Mēxihco is the Nahuatl term for the heartland of the Aztec Empire, namely, the Valley of Mexico, and its people, the Mexica and this became the future State of Mexico as a division of New Spain prior to independence. It is generally considered to be a toponym for the valley became the primary ethnonym for the Aztec Triple Alliance as a result. After New Spain won independence from Spain, representatives decided to name the new country after its capital and this was founded in 1524 on top of the ancient Mexica capital of Mexico-Tenochtitlan
3.
Puuc
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Puuc is the name of either a region in the Mexican state of Yucatán or a Maya architectural style prevalent in that region. The word puuc is derived from the Maya term for hill, since the Yucatán is relatively flat, this term was extended to encompass the large karstic range of hills in the southern portion of the state, hence, the terms Puuc region or Puuc hills. The Puuc hills extend into northern Campeche and western Quintana Roo, the term Puuc is also used to designate the architectural style of ancient Maya sites located within the Puuc hills, hence, the term Puuc architecture. This architectural style began at the end of the Late Classic period, in the florescence of Puuc architecture buildings were decorated with carefully cut veneer stones set into a concrete core. Long-nosed masks are found on many Puuc buildings, the concrete core-veneer masonry allowed for slightly larger and more stable interior rooms. Many corbelled vaults in the Puuc style remain standing, even when most of the stones have fallen away. The most famous of the Maya sites exhibiting the Puuc architectural style is Uxmal, other major Puuc-style sites in the region include Labna, Kabah, Sayil, the architectural style is also seen at Kiuic, Bolonchen, Chunhuhub, Xculoc, and many smaller ruins. The transition from earlier Classic Period architecture to Puuc style core-veneer masonry is well documented at the site of Oxkintok, to the south, the style can be found in Edzná, and to the east at Chichen Itza. As stated by the Maya explorer Teobert Maler, who explored this zone intensively, the recently completed Chunhuaymil project compiled data of the remaining Puuc architecture of 19 archaeological sites located in a 100 square kilometers area. Andrews, George F. Pyramids, Palaces, Monsters and Masks, carmean, Kelli, Nicholas Dunning and Jeff K. Kowalski. 2004 High times in the country, a perspective from the Terminal Classic Puuc region. In, The Terminal Classic in the Maya Lowlands, Collapse, Transition, arthur A. Demarest, Prudence M. Rice, and Don S. Rice, eds. pp. 424–449. Dunning, Nicholas P.1992 Lords of the Hills, Ancient Maya Settlement in the Puuc Region, Yucatán, centre dEtudes Mexicaines et Centraméricaines, Mexico. Dunning, Nicholas P. and Jeff K. Kowalski,1994 Lord of the Hills, Classic Maya settlement patterns and political iconography in the Puuc Region, Mexico. Gendrop, Paul 1998 Rio Bec, Chenes, and Puuc Styles in Maya Architecture, merk, Stephan 2011 The Long Silence. Sabana Piletas and Its Neighbours, An Architectural Survey of Maya Ruins in Northeastern Campeche, markt Schwaben, Germany, Verlag Anton Saurwein. Mills, Lawrence,1979 The Puuc, New Perspectives, Papers Presented at the Puuc Symposium, Central College, pollock, Harry E. D.1980 Puuc, An Architectural Survey of the Hill Country of Yucatan and Northern Campeche, Mexico. Harvard University, Peabody Museum of Archaeology and Ethnology, Prem, Hanns J.1994 Hidden Among the Hills, Maya Archaeology of the Northwest Yucatan Península
4.
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
5.
Limestone
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Limestone is a sedimentary rock, composed mainly of skeletal fragments of marine organisms such as coral, forams and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate, about 10% of sedimentary rocks are limestones. The solubility of limestone in water and weak acid solutions leads to karst landscapes, most cave systems are through limestone bedrock. The first geologist to distinguish limestone from dolomite was Belsazar Hacquet in 1778, like most other sedimentary rocks, most limestone is composed of grains. Most grains in limestone are skeletal fragments of organisms such as coral or foraminifera. Other carbonate grains comprising limestones are ooids, peloids, intraclasts and these organisms secrete shells made of aragonite or calcite, and leave these shells behind when they die. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragment, some limestones do not consist of grains at all, and are formed completely by the chemical precipitation of calcite or aragonite, i. e. travertine. Secondary calcite may be deposited by supersaturated meteoric waters and this produces speleothems, such as stalagmites and 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 commonly marine organisms. Some of these organisms can construct mounds of rock known as reefs, below about 3,000 meters, water pressure and temperature conditions cause the dissolution of calcite to increase nonlinearly, so limestone typically does not form in deeper waters. Limestones may also form in lacustrine and evaporite depositional environments, calcite can be dissolved or precipitated by groundwater, depending on several factors, including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits a characteristic called retrograde solubility, in which it becomes less soluble in water as the temperature increases. Impurities will cause limestones to exhibit different colors, especially with weathered surfaces, Limestone may be crystalline, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, 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, particularly there are waterfalls. Calcium carbonate is deposited where evaporation of the 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 building process, limestone recrystallizes into marble
6.
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
7.
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
8.
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
9.
Belize
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Belize, formerly British Honduras, is an independent country on the eastern coast of Central America. Belize is bordered on the north by Mexico, on the south and west by Guatemala and its mainland is about 290 km long and 110 km wide. Belize has an area of 22,800 square kilometres and a population of 368,310 and it has the lowest population density in Central America. The countrys population growth rate of 1. 87% per year is the second highest in the region, Belizes abundance of terrestrial and marine species and its diversity of ecosystems gives it a key place in the globally significant Mesoamerican Biological Corridor. Belize has a society, composed of many cultures and languages that reflect its rich history. English is the language of Belize, with Belizean Kriol being the unofficial language. Over half the population is multilingual, with Spanish being the second most common spoken language, Belize is considered a Central American and Caribbean nation with strong ties to both the Latin American and Caribbean regions. Belize is a Commonwealth realm, with Queen Elizabeth II as its monarch, Belize is known for its September Celebrations, its extensive coral reefs, and punta music. The origin of the name Belize remains unclear, the earliest known record of the name appears in the journal of the Dominican priest Fray José Delgado, dating to 1677. Delgado recorded the names of three rivers that he crossed while travelling north along the Caribbean coast, Rio Soyte, Rio Xibum. The names of these waterways, which correspond to the Sittee River, Sibun River and it is likely that Delgados Balis was actually the Mayan word belix, meaning muddy-watered. Others have suggested that the name derives from a Spanish pronunciation of the name of the Scottish buccaneer Peter Wallace, there is no proof that Wallace settled in this area and some scholars have characterized this claim as a myth. Writers and historians have suggested other possible etymologies, including postulated French. Many aspects of this culture persist in the area despite nearly 500 years of European domination, prior to about 2500 BC, some hunting and foraging bands settled in small farming villages, they later domesticated crops such as corn, beans, squash, and chili peppers. A profusion of languages and subcultures developed within the Maya core culture, between about 2500 BC and 250 AD, the basic institutions of Maya civilisation emerged. The peak of this occurred during the classic period, which began about 250 AD. The Maya civilisation spread across what is now Belize around 1500 BC, the recorded history of the middle and southern regions is dominated by Caracol, an urban political centre that may have supported over 140,000 people. North of the Maya Mountains, the most important political centre was Lamanai, in the late Classic Era of Maya civilisation, as many as 1 million people may have lived in the area that is now Belize
10.
Cahal Pech
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Cahal Pech is a Maya site located near the town of San Ignacio in the Cayo District of Belize. The site rests high above the banks of the Macal River and is located to overlook the confluence of the Macal River. The site is a collection of 34 structures, with the tallest temple being about 25 meters in height, the site was abandoned in the 9th century CE for unknown reasons. The earliest pottery in western Belize is found here, emerging information from western Belize suggests that ceramic-using populations may have been in place as early as ca.1200 B. C. at Cahal Pech and perhaps elsewhere. It is now a reserve, and houses a small museum with artifacts from various ongoing excavations. The primary excavation of the began in 1988. Restoration was completed in 2000 under the leadership of Dr. Jaime Awe, Director of the National Institute of Archaeology, other nearby Mayan sites include Chaa Creek, Xunantunich, Baking Pot, and Lower Dover
