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Mojave River Valley Museum
Furnace Creek Lake
Millions of years prior to the actual sinking and widening of Death Valley and the existence of Lake Manly,
another lake covered a large portion of Death Valley including the area around Zabriskie Point. This ancient
lake was here approximately nine million years ago. During the several million years of the lake's existence,
sediments were collecting at the bottom in the form of saline muds, gravels from nearby mountains, and ashfalls
from the then active Black Mountain volcanic field. These sediments combined to form what we today call the
Furnace Creek formation. The climate along Furnace Creek Lake was dry but not nearly as dry as today's. Camels,
mastadons, horses, carnivores, and birds left tracks in the lakeshore muds along with fossilized grass and reeds.
Borates which made up a large degree of Death Valley's historical past were concentrated in the lakebeds from hot spring
waters and alteration of rhyolite in the nearby volcanic field. Weathering and alteration by thermal waters are
also responsible for the variety of colors represented here.
Christian Brevoort Zabriskie"Being an active young man, one job was not enough to keep him occupied and he soon branched out into other ventures, one of which was a partnership with a local cabinetmaker to establish a mortuary. ..."
*Source - National Park Service
Clickable Map of Furnace Creek Area
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