Matthews-Winters Park: Stop 5 -
Geologic Map |
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FOUNTAIN
Exposure: No
significant surface exposures along trail.
Age:
Pennsylvanian and early Permian
Lithology: Red arkoses, sandy mudstones and conglomerates,
crossbedding common
Depositional Environment: a complex of shallow braided channels
deposited on alluvial fans |
LYONS
Exposure: Forms a
fairly prominent ridge bisecting park
Age: Permian
Lithology: "..light gray conglomerate arkose...overlain by cross-
stratified conglomerate tat grads upward into fine- to
medium-grained feldspathic sandstone."*
Depositional Environment: Braided stream deposits grading
upward into eolian deposits and dunes |
LYKINS
Exposure: Less
resistant than the Lyons, but more than the
Fountain. Some low exposures.
Age: Permian
Lithology: "...brick-red, thinly bedded siltstone and shales.
Two
crinkly laminated carbonates layers .. are present in the
lower 100 feet..."*
Depositional Environment: "a nonmarine aqueous deposit, either
related to widespread supersaline restricted marine, or
to saline freshwater lake conditions."* |
Note: The
stratigraphic boundaries are only approximated and are based on surface
exposures visible in the aerial photo. No interpretation of faults or
other structures is attempted. |
*Weimer, R. J., 1996, Guide
to the Petroleum Geology and Laramide Orogeny, Denver Basin and Front Range,
Colorado: Colorado Geological Survey, Bulletin 51, 127p. |