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Geology:
Walk Through Time
Stirling Quartzite 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 Next > < Previous |
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| Intro:: Nature:: Map:: Points of Interest:: Roads & Trails:: People & History:: Ghosts & Gold:: Communities:: BLOG:: Weather:: :?:: glossary |
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Country Life Realty Wrightwood, Ca. |
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Canyon Cartography |
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Grizzly Cafe Family Dining |
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These items are historical in scope and are intended for educational purposes only; they are not meant as an aid for travel planning. Copyright ©Walter Feller. 1995-2023 - All rights reserved. |