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- W2147889406 abstract "The termination of Ridge Basin deposition early during the Pliocene Epoch is documented by the Hungry Valley Formation, a nonmarine alluvial fan and braided river deposit about 1400 m (4500 ft) thick that lies conformably on top of other units of the Ridge Basin Group. The alluvial fan facies consists of white cross-bedded sandstone and gray-green mudstone in fining upward sequences. The sandstone fluvial facies is interpreted as deposited by braided rivers at the distal ends of alluvial fans on fluvial plains. On the east, conglomerate and sandstone beds of the formation lap across the Liebre Fault, showing that this fault ceased activity before deposition of the formation. On the northwest beds lap across the San Gabriel Fault and can be traced westward into Lockwood Valley where they, are equivalent to the Quatal Formation. Much of the material constituting the Hungry Valley Formation came from the north and northeast from source areas within the Mojave Desert region but with a contribution from Frazier Mountain that had begun to rise. Hungry Valley beds are severely deformed near the San Andreas Fault and facies are truncated by it. Slip on the San Andreas Fault, beginning about 6 m. y. ago, has presumably displaced and offset source areas of the formation but these have not yet been identfied with confidence, nor have remnants of the formation, if they are still preserved, been matched with it." @default.
- W2147889406 created "2016-06-24" @default.
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- W2147889406 date "1982-01-01" @default.
- W2147889406 modified "2023-09-27" @default.
- W2147889406 title "Pliocene Hungry Valley Formation, Ridge Basin, Southern California" @default.
- W2147889406 hasPublicationYear "1982" @default.
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