 The canons in general are deepest to the westward and gradually run out to the Sacramento river in the newer deposits which fill the valley. It is evident that since the baselevel was formed, it has been affected by differential elevation in the uplifting...  Proceedings of the American Academy of Arts and Sciences - 170 ページAmerican Academy of Arts and Sciences 著 - 1899全文表示 - この書籍について
 | Joseph Silas Diller - 1893 - 454 ページ
...deposits which fill the valley. It is evident that since the baselevel was formed, it has been affected by differential elevation in the uplifting of the Coast...fortieth parallel, to the extent of over 2,000 feet, and if we may judge from the traces of the baselevel seen at Shower's pass and South Fork Mountain,... | |
 | Geological Survey (U.S.) - 1894 - 818 ページ
...deposits which fill the valley. It is evident that since the baselevel was formed it has been affected by differential elevation in the uplifting of the Coast...fortieth parallel to the extent of over 2,000 feet, and if we may judge from the traces of the baselevel 'Geological Survey of California, Geology, Vol.... | |
 | 1899 - 870 ページ
...Geol., 1804, H 32-54 ; 14th Ann. USGS, 18S2-93. Ft. II. 423; VV. Lindgren, Bull. GSA, 1893, IV. 257-298. differential elevation in the uplifting of the Coast...and sixty miles. As one stands upon the peneplain in the western part of Massachusetts, he may look to the southeast across an almost even surface of... | |
 | 1894 - 904 ページ
...deposits which fill the valley. It is evident that since the baselevel was formed, it has been affected by differential elevation in the uplifting of the Coast...fortieth parallel, to the extent of over 2,000 feet, and if we may judge from the traces of the baselevel seen at Shower's pass and South Fork Mountain,... | |
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