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The complex was first identified by Malcolm J. Rogers in 1919 at site SDI-W-240 in Escondido in San Diego County, California. [1] He assigned the Paleo-Indian designation of 'Scraper Makers' to the prehistoric producers of the complex, based on the common occurrence of unifacially flaked lithic (stone) tools at their sites.
Coso Rock Art District is a rock art site containing over 100,000 Petroglyphs by Paleo-Indians and/or Native Americans. [1] The district is located near the towns of China Lake and Ridgecrest, California. Big and Little Petroglyph Canyons were declared a National Historic Landmark in 1964.
The Paleo-Indians, also known as the Lithic peoples, are the earliest known settlers of the Americas; the period's name, the Lithic stage, derives from the appearance of lithic flaked stone tools. Paleo-Indians were the first peoples who entered and subsequently inhabited the Americas towards the end of the Late Pleistocene period.
Arlington Springs Man [nb 1] was an ancient Paleoindian, [1] most likely a man, [2] whose remains were found in 1959 on Santa Rosa Island, one of the Channel Islands located off the coast of Southern California.
Big and Little Petroglyph Canyons are two principal landforms within which are found major accumulations of Paleo-Indian and/or Native American Petroglyphs, or rock art, by the Coso People located in the Coso Range Mountains of the northern Mojave Desert, and now within the Naval Air Weapons Station China Lake, near the towns of China Lake and Ridgecrest, California. [3]
Historian and author Benjamin Madley observes that between 1845 and 1870, California’s Native American population “plunged from perhaps 150,000 to 30,000. By 1880 census takers recorded just ...
Which Southern California native plants survived climate change and mass extinctions 13,000 years ago and still live today? La Brea Tar Pits researchers compiled a list.
The stone tools of these industries, along with preforms, lithic core, technical flakes, and pieces of angular debitage, mainly of chalcedony, are found on and in late middle Pleistocene-age fanglomerates and younger inset alluvial terraces in the Calico Hills (also known as the Yermo Hills) east of the Calico Peaks and the Calico Mountains.