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Concept
Xunantunich
Summary
Xunantunich (ʃunanˈtunitʃ) is an Ancient Maya archaeological site in western Belize, about 70 miles (110 km) west of Belize City, in the Cayo District. Xunantunich is located atop a ridge above the Mopan River, well within sight of the Guatemala border – which is to the west. It served as a Maya civic ceremonial centre to the Belize Valley region in the Late and Terminal Classic periods. At that time, when the region was at its peak, nearly 200,000 people lived in the Belize Valley.
Xunantunich's name means "Maiden of the Rock" in the Maya language (Mopan and Yucatec combination name Xunaan (Noble lady) Tuunich (stone for sculpture)), and, like many names given to Maya archaeological sites, is a modern name; the ancient name is unknown. The "Stone Woman" refers to the ghost of a woman claimed by several people to inhabit the site, beginning in 1892. She is dressed completely in white, and has fire-red glowing eyes. She generally appears in front of "El Castillo", ascends the stone stairs, and disappears into a stone wall.
The first modern explorations of the site were conducted by Thomas Gann in the mid-1890s. Gann moved from Britain and served as the district surgeon and district commissioner of Cayo, British Honduras, starting in 1892. He chose this area to settle in because he had an interest in Mayan archaeology, and he wished to be able to explore what were at the time the unknown wonders of the indigenous people. Gann's successor, Sir J. Eric S. Thompson, implemented a more methodical approach, and was able to establish the region's first ceramic chronology. The main recent archaeological teams to work at Xunantunich and the surrounding region are the Xunantunich Archaeological Project (XAP), the Xunantunich Settlement Survey (XSS), and the Belize Valley Archaeological Reconnaissance Project (BVAR).
In 1959–60, the Cambridge Expedition to British Honduras arrived in the colony, and its archaeologist member, Euan MacKie, carried out several months of excavation at Xunantunich.
Official source
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