
Light-colored lake beds. Photo by Ray Nordeen, NPS.
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An Ancient Lake
Walking up Golden Canyon involves traveling through an ancient, changing
landscape. It's time to again look closely at the rocks exposed in the canyon walls. Youll
notice that the conglomerate layers composed of large
boulders have given way to a different kind of rock. In contrast, these
light-colored deposits
are comprised of very small particles of silt and mud.
Such fine-grained sediment is typical of debris that is deposited at
the bottom of a calm
lake.
These mudstones are thought to be of similar age to
the lower conglomerate. So the boundary between these
different rock layers represents a change in the
ancient landscape rather than a change in time
or climate-you have walked across the alluvial fan
and into a lake!

Ripplemarks preserved in an ancient lake bed of Golden Canyon. Click for close-up.
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Ripples in Time
Look closely at the surface of the tilted rock layers in this area.
Rather than being perfectly flat, some of the surfaces have an undulating
pattern. If you are familiar with a lake or sea shore environment, perhaps
you have observed similar ripples shaped in the sand.
The ripple marks that you see here are further evidence
of the ancient lake that once occupied this area;
they were created by the movement of water over the loose sediment deposited
at the bottom
of the lake. The preservation of their delicate pattern
required rapid burial beneath another layer of sediment. In other places
in Death Valley,
fascinating fossil footprints of large mammals have
been found in lake deposits of similar age.
Continue hiking up Golden Canyon
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