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Prehistoric Indian Culture

Pinto Culture

As the Pleistocene Epoch drew to a close ten thousand years ago, and the rivers of glacial ice melted, people lived in an environment dramatically different from today—both cooler and wetter. Lakes and swamps existed where no water remains now. Lush grasslands covered the plains, supporting mammoths, mastodons, horses, camels, and, in some areas, bison.

Projectile points found along an extinct water channel in the Pinto Basin represent the earliest known human occupation of this area. Dated from four to eight thousand years ago, this Pinto culture was first described by amateur archeologists, William and Elizabeth Campbell in the 1930s.

The Campbells believed that there had been a river flowing through Pinto Basin but more recent research by geologists dispels the notion that there was either a river or a lake in Pinto Basin by the time humans occupied the area. The points collected by the Cambells are thick and triangular in shape, with notched shoulders and a broad stem. Pinto hunters attached the points to a wooden spear shaft and used a spear thrower, or atlatl, to propel the spear. Based on the relatively large number of Pinto points—as well as cutting and scraping tools—compared with the few seed-processing implements found at these early sites, it is believed that Pinto Culture was a mobile population dependent upon large game hunting and seasonal plant gathering.

The period of Pinto Culture occupation was an era of decreasing moisture, and by the end the environment was probably close to what we have today. As the Pleistocene water sources dried up, only desert adapted plants and animals survived. The archeological evidence suggests that the human population gradually adapted as well, by hunting smaller game and processing small seeds.

Little evidence links the Pinto Culture with today’s tribal groups. The Cahuilla, Chemehuevi, and Serrano who followed the Pinto period had a more diversified strategy of hunting and collecting food items that included distinct changes in stone tools and increasing numbers of hard-seed milling stones.


Pinto Basin - Joshua Tree National Park


Ecology

Pinto Basin & Mountains

Steep mountains, moderately steep hills; very gently to moderately sloping pediments and alluvial fans; and nearly level basin floor. Dry lake bed and dune sand are not extensive. The general orientation of the hills is not clear, except the north-south aligned Coxcomb Mountains.

Death Valley Prehistoric Culture

Pinto Period, 5000–2000 B.C. -- Dramatic environmental changes came to the Mojave Desert with the end of the Pleistocene Era, characterized by harsh climatic conditions with higher temperatures and lower precipitation. Lakes and rivers dried up, and resources available were much reduced.
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