1974
DOI: 10.1086/201454
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The Prehistory of the Southeastern Maya Periphery

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Cited by 31 publications
(24 citation statements)
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“…The decimation of human populations in central E1 Salvador has been clearly documented (Sheets 1971(Sheets , 1979(Sheets , 1981(Sheets , 1983a people in the immediate vicinity of the vent during the eruption include: lahars, earthquakes, acid burns, carbon dioxide, carbon monoxide and flourine poisoning, and coastal tsunamis along the Pacific coast (Blong 1984;Scarth 1999;Thorarinsson 1979).9 Although there is little doubt that central E1 Salvador was completely devastated by the TBJ eruption and void of human life immediately following it, the post-TBJ demography of western E1 Salvador has been the subject of some debate; one side arguing for the virtually complete and prolonged depopulation of the upper Rio Paz drainage basin (Sharer 1974(Sharer , 1978bSheets 1984), and the other for demographic and cultural continuity-suggesting only temporary local displacement of human populations following the TBJ event (Demarest 1986, 1988). Demarest (1986:179-180) speculates that the denizens of Chalchuapa must have remained in western E1 Salvador, moving "up out of ash-buried basins," or that they retreated west to the nearby highlands and coastal plain of southeastern Guatemala.…”
Section: Reevaluating the Archaeological Record: The Tbj Tephra In Cumentioning
confidence: 99%
“…The decimation of human populations in central E1 Salvador has been clearly documented (Sheets 1971(Sheets , 1979(Sheets , 1981(Sheets , 1983a people in the immediate vicinity of the vent during the eruption include: lahars, earthquakes, acid burns, carbon dioxide, carbon monoxide and flourine poisoning, and coastal tsunamis along the Pacific coast (Blong 1984;Scarth 1999;Thorarinsson 1979).9 Although there is little doubt that central E1 Salvador was completely devastated by the TBJ eruption and void of human life immediately following it, the post-TBJ demography of western E1 Salvador has been the subject of some debate; one side arguing for the virtually complete and prolonged depopulation of the upper Rio Paz drainage basin (Sharer 1974(Sharer , 1978bSheets 1984), and the other for demographic and cultural continuity-suggesting only temporary local displacement of human populations following the TBJ event (Demarest 1986, 1988). Demarest (1986:179-180) speculates that the denizens of Chalchuapa must have remained in western E1 Salvador, moving "up out of ash-buried basins," or that they retreated west to the nearby highlands and coastal plain of southeastern Guatemala.…”
Section: Reevaluating the Archaeological Record: The Tbj Tephra In Cumentioning
confidence: 99%
“…The Rio Paz Valley in western El Salvador may have been one of the first interior valleys in El Salvador to be permanently settled by farmers, with archaeological data pointing to settlement sometime before 1200 cal yr BC (Sharer, 1974(Sharer, , 1978. A pollen record from Laguna Cuzcachapa largely corroborates the archaeological sequence, and confirms human occupation back to at least ca.…”
Section: The Late Holocene-agricultural Revolution and Anthropogenic mentioning
confidence: 99%
“…Although the altitudinal gradient (which runs largely north to south) may create a natural stimulus to local trade, major long-distance trade routes ran east to west (Parsons and Price 1971;Sharer 1974). There may have been several such routes: a highland route, passing over the rough terrain separating montane valleys; a piedmont route, linking the numerous sculpture-rich sites; and a coastal trade route, including an ''inland waterway'' of estuaries and streams (Arroyo 1991(Arroyo , 1994 Hatch have become a point of reference for archaeological study within the Guatemalan highlands and Pacific Coast because they help to define both regions and long-standing traditions of material culture.…”
Section: The Cultural Geography Of Southern Pacific Mesoamericamentioning
confidence: 99%