| 1. |
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Joaquin Rocks, formed by massive sandstone of the Panoche formation, looking north from point near summit of Joaquin Ridge. Fresno County, California. 1910. Plate 4-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 146 anr00146 |
| 2. |
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Joaquin Rocks, formed by massive sandstone of the Panoche formation, looking north from point near summit of Joaquin Ridge. Fresno County, California. 1910. Plate 4-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 147 anr00147 |
| 3. |
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Hills formed by northeastward-dipping Cretaceous and Tertiary strata north of Coalinga district, looking south along the central part of Ragged Valley from the north bank of Salt Creek. Note the subdued topography characteristic of the two shale zones and the large landslip in the foreground to the right. Joaquin Rocks are shown on the skyline to the right. Fresno County, California. 1910. Plate 2 in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 160 anr00160 |
| 4. |
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Hills formed by northeastward-dipping Cretaceous and Tertiary strata north of Coalinga district, looking south along the central part of Ragged Valley from the north bank of Salt Creek. Note the subdued topography characteristic of the two shale zones and the large landslip in the foreground to the right. Joaquin Rocks are shown on the sky line to the right. Fresno County, California. 1910. Plate 2 in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 161 anr00161 |
| 5. |
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Typical cliffs of white quartzose sandstone of the Tejon formation, in the Cantua region, looking south from the divide between the Cantua and Salt Creeks; the Tejon here is formed almost wholly of sandstone and contains but little of the carbonaceous shale which becomes so abundant about The Vallecitos. Fresno County, California. 1910. Plate 7 in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 166 anr00166 |
| 6. |
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Typical cliffs of white quartzose sandstone of the Tejon formation, in the Cantua region, looking south from the divide between the Cantua and Salt Creeks; the Tejon here is formed almost wholly of sandstone and contains but little of the carbonaceous shale which becomes so abundant about The Vallecitos. Fresno County, California. C. 1910. Plate 7 in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 167 anr00167 |
| 7. |
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Typical exposure of the siliceous Kreyenhagen shale on Domengine Creek: showing characteristic surface crumpling. Fresno County, California. C. 1910. Plate 8-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 172 anr00172 |
| 8. |
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Unconformity of sandstone of the Vaqueros formation on Kreyhagen shale along the east face of the Ciervo Hills, looking north one mile south of Arroyo Hondo. Fresno County, California. C. 1910. Plate 9-B in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 175 anr00175 |
| 9. |
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Characteristic outcrop of the Big Blue serpentinous member of the Vaqueros formation near Cantu Creek, looking east at outcrop about half a mile south of Arroyo Hondo. The central outcrop is formed of indurated green and brown shale compose of comminuted fragments of serpentine derived from the serpentine area near New Idria. The freedom from fragments of quartzose rock is remarkable. Fresno County, California. C. 1910. Plate 11-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 185 anr00185 |
| 10. |
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Huge serpentine boulders in the Big Blue member on Martinez Creek. Fresno County, California. C. 1910. Plate 11-B in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 189 anr00189 |
| 11. |
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Terrace deposits of the Tulare (?) formation at he crest of the Panoche Hills, looking north from a point near the south end of the hills. The flat topped hill in the foreground and at the left are formed by steeply tilted beds of the Panoche formation capped by flat lying clay and gravel of the Tulare (?). Fresno County, California. C. 1910. Plate 12-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 210 anr00210 |
| 12. |
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Terrace deposits of the Tulare (?) formation at he crest of the Panoche Hills, looking north from a point near the south end of the hills. The flat topped hill in the foreground and at the left are formed by steeply tilted beds of the Panoche formation capped by flat lying clay and gravel of the Tulare (?). Fresno County, California. C. 1910. Plate 12-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 211 anr00211 |
| 13. |
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Terrace deposits of the Tulare (?) formation at he crest of the Panoche Hills, looking north from a point near the south end of the hills. The flat topped hill in the foreground and at the left are formed by steeply tilted beds of the Panoche formation capped by flat lying clay and gravel of the Tulare (?). Fresno County, California. C. 1910. Plate 12-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 212 anr00212 |
| 14. |
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Zion National Park, Utah. Ice fall on Zion Canyon wall 10 or more miles above Virgin River. A small water fall dropping from the top of the cliff at this point freezes on the wall, and blocks of ice drop at intervals with a loud roar. 1910.
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ID. Anderson, R. 247 anr00247 |
| 15. |
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Characteristic out crops of conglomerate in the Panoche formation north of Panoche Pass, looking north across the Ortigalito Creek near schoolhouse. Merced County, California. C. 1910. Plate 4-B in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 268 anr00268 |
| 16. |
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Characteristic out crops of conglomerate in the Panoche formation north of Panoche Pass, looking north across the Ortigalito Creek near schoolhouse. Merced County, California. C. 1910. Plate 4-B in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 269 anr00269 |
| 17. |
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Unconformity of the oil sands of the Vaqueros formation on oily Kreyenhagen shale along Silver Creek, looking north at bank of creek below New Bedford well. Fresno County, California. C. 1910. Plate 9-A in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 284 anr00284 |
| 18. |
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Sandstone dikes in the Moreno formation in the Panoche Hills, looking north across Moreno Gulch. The lateral ridges are approximately determined by siliceous shale. The clastic dikes are almost exactly normal to the bedding of the shale. Fresno County, California. C. 1910. Plate 5 in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 292 anr00292 |
| 19. |
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Sandstone dikes in the Moreno formation in the Panoche Hills, looking north across Moreno Gulch. The lateral ridges are approximately determined by siliceous shale. The clastic dikes are almost exactly normal to the bedding of the shale. Fresno County, California. C. 1910. Plate 5 in U.S. Geological Survey. Bulletin 603. 1915.
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ID. Anderson, R. 293 anr00293 |