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Xibun
Xibun is an alternate Mayan spelling of Sibun that appears on some Spanish colonial-period maps of the region, and is sometimes used to refer to: *the Sibun River located in central Belize *ancient or historic Maya settlers in the Sibun River valley Xibun Maya Xibun may denote the ancient and historic Maya inhabitants of the Sibun River valley. The Sibun River meanders through a Karst topography containing countless Maya cave sites. A significant contribution of archaeological research in the area has been the documentation of the ritual use of caves by the Xibun Maya. Of particular note, a pattern of speleothem A speleothem (; ) is a geological formation by mineral deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending ... (cave formation) breakage was documented in caves that was explained by their incorporation into public architecture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Xibun River
The Sibun River (Xibun River, formerly Sheboon River) is a river in Belize which drains a large central portion of the country. The Sibun (Xibun) were ancient Maya people who inhabited the region. The headwaters of the Sibun River are located within the Maya Mountains, at approximately 800 meters above sea level, where it is known as the Caves Branch River. The river then flows through a gorge until it reaches an alluvial floodplain, where citrus and cacao plantations exist. Here the river valley is flanked by karst topography featuring Maya cave sites. Before the river reaches the village of Freetown Sibun, river figs and spiny bamboo (''Guadua longifolia'') are common along its banks; along the stretch of river between the coast and the village, mangroves are predominant. It empties into the Caribbean Sea, south of Belize City. The Sibun River Watershed features several vegetation types, including tropical evergreen seasonal mixed needle forest, broadleaf forest, mangrove ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sibun River
The Sibun River (Xibun River, formerly Sheboon River) is a river in Belize which drains a large central portion of the country. The Sibun ( Xibun) were ancient Maya people who inhabited the region. The headwaters of the Sibun River are located within the Maya Mountains, at approximately 800 meters above sea level, where it is known as the Caves Branch River. The river then flows through a gorge until it reaches an alluvial floodplain, where citrus and cacao plantations exist. Here the river valley is flanked by karst topography featuring Maya cave sites. Before the river reaches the village of Freetown Sibun, river figs and spiny bamboo (''Guadua longifolia'') are common along its banks; along the stretch of river between the coast and the village, mangroves are predominant. It empties into the Caribbean Sea, south of Belize City. The Sibun River Watershed features several vegetation types, including tropical evergreen seasonal mixed needle forest, broadleaf forest, mangroves, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maya Cave Sites
Mayan cave sites are associated with the Mayan civilization of pre-Columbian Mesoamerica. Beliefs and observances connected with these cave sites persist among some contemporary Mayan communities. Many of the Mayan caves served religious purposes. For this reason, the artifacts found there, alongside the Epigraphy, epigraphic, Iconology, iconographic, and Ethnography, ethnographic studies, help build the modern-day understanding of the Mayan religion and society. Mayan cave sites have also attracted thieves and invaders. Consequently, some of them have been walled shut to stop any damage to the sites. The immured Dos Pilas#Caves, caves of Dos Pilas and Naj Tunich have been sealed. Study In works compiled for the fight against idolatry, 16th-century Spanish Empire, Spanish sources mentioned 17 Maya peoples, Maya caves and cenotes - nine of which have been found. In his book ''Relación de las cosas de Yucatán'', friar Diego de Landa described the Sacred Cenote. Underground Maya a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belize
Belize (; bzj, Bileez) is a Caribbean and Central American country on the northeastern coast of Central America. It is bordered by Mexico to the north, the Caribbean Sea to the east, and Guatemala to the west and south. It also shares a water boundary with Honduras to the southeast. It has an area of and a population of 441,471 (2022). Its mainland is about long and wide. It is the least populated and least densely populated country in Central America. Its population growth rate of 1.87% per year (2018 estimate) is the second-highest in the region and one of the highest in the Western Hemisphere. Its capital is Belmopan, and its largest city is the namesake city of Belize City. Belize is often thought of as a Caribbean country in Central America because it has a history similar to that of English-speaking Caribbean nations. Indeed, Belize’s institutions and official language reflect its history as a British colony. The Maya civilization spread into the area of Beli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maya Civilization
The Maya civilization () of the Mesoamerican people is known by its ancient temples and glyphs. Its Maya script is the most sophisticated and highly developed writing system in the pre-Columbian Americas. It is also noted for its art, architecture, mathematics, calendar, and astronomical system. The Maya civilization developed in the Maya Region, an area that today comprises southeastern Mexico, all of Guatemala and Belize, and the western portions of Honduras and El Salvador. It includes the northern lowlands of the Yucatán Peninsula and the highlands of the Sierra Madre, the Mexican state of Chiapas, southern Guatemala, El Salvador, and the southern lowlands of the Pacific littoral plain. Today, their descendants, known collectively as the Maya, number well over 6 million individuals, speak more than twenty-eight surviving Mayan languages, and reside in nearly the same area as their ancestors. The Archaic period, before 2000 BC, saw the first developments in agricul ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Topography
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. 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. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Speleothem
A speleothem (; ) is a geological formation by mineral deposits that accumulate over time in natural caves. Speleothems most commonly form in calcareous caves due to carbonate dissolution reactions. They can take a variety of forms, depending on their depositional history and environment. Their chemical composition, gradual growth, and preservation in caves make them useful paleoclimatic proxies. Chemical and physical characteristics More than 300 variations of cave mineral deposits have been identified. The vast majority of speleothems are calcareous, composed of calcium carbonate (CaCO3) minerals (calcite or aragonite). Less commonly, speleothems are made of calcium sulfate (gypsum or mirabilite) or opal. Speleothems of pure calcium carbonate or calcium sulfate are translucent and colorless. The presence of iron oxide or copper provides a reddish brown color. The presence of manganese oxide can create darker colors such as black or dark brown. Speleothems can also be brown d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Mesoamerica
The geography of Mesoamerica describes the geographic features of Mesoamerica, a culture area in the Americas inhabited by complex indigenous pre-Columbian cultures exhibiting a suite of shared and common cultural characteristics. Several well-known Mesoamerican cultures include the Olmec, Teotihuacan, the Maya, the Aztec and the Purépecha. Mesoamerica is often subdivided in a number of ways. One common method, albeit a broad and general classification, is to distinguish between the highlands and lowlands. Another way is to subdivide the region into sub-areas that generally correlate to either culture areas or specific physiographic regions. Geographic location Mesoamerica – meaning "middle of America" – is located in the mid-latitudes (between 10° and 22° N) of the Americas in the southern portion of North America, encompassing much of the isthmus that joins it with South America. Situated within the wider region known as Middle America, Mesoamerica extends from south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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