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Geology: Walk Through Time

Stirling Quartzite

sample of Stirling quartzite, Death Valley 2,000 foot thick, 540+ million years old. Crossbedded sandstone was formed in a near-shore environment and then partially metamorphosed into impure quartzite.

Phanerzoic eon > Paleozoic era > Cambrian period > Series 1 epoch > Stage 1 age

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ecology: wildlife - plants - geography: places - MAPS - map/sat - roads & trails: route 66 - old west - communities - weather - book store
ghost towns - gold mines - parks & public lands: wilderness - native culture - history - geology: natural features - glossary - comments
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