Man and the Glacial PeriodKegan Paul, 1892 - 385 pagina's |
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Pagina 98
... loess . " Loess is very abundant in the whole valley of the Missouri River below Yankton , South Dakota , being for a long distance in the vicinity of the river a hundred feet or more in depth . Over north- ern Missouri and southern ...
... loess . " Loess is very abundant in the whole valley of the Missouri River below Yankton , South Dakota , being for a long distance in the vicinity of the river a hundred feet or more in depth . Over north- ern Missouri and southern ...
Pagina 101
... loess referred to ) and extending nearly to the latitude of St. Louis . West of Wisconsin President Chamberlin's " terminal moraine of the second Glacial epoch " bends southward through eastern Minnesota , and , sweeping down through ...
... loess referred to ) and extending nearly to the latitude of St. Louis . West of Wisconsin President Chamberlin's " terminal moraine of the second Glacial epoch " bends southward through eastern Minnesota , and , sweeping down through ...
Pagina 110
... rational way of reconciling the conflicting statements concerning it . * Bulletin of the Geological Society of America , vol . i , pp . 287- " 2. Peat or Soil under Loess . - This 310 . 110 MAN AND THE GLACIAL PERIOD .
... rational way of reconciling the conflicting statements concerning it . * Bulletin of the Geological Society of America , vol . i , pp . 287- " 2. Peat or Soil under Loess . - This 310 . 110 MAN AND THE GLACIAL PERIOD .
Pagina 111
George Frederick Wright. " 2. Peat or Soil under Loess . - This does not signify much if the loess was formed in a lake subject to oro- graphic oscillations , or if , as I am coming to believe , it is a fluviatile deposit of an ...
George Frederick Wright. " 2. Peat or Soil under Loess . - This does not signify much if the loess was formed in a lake subject to oro- graphic oscillations , or if , as I am coming to believe , it is a fluviatile deposit of an ...
Pagina 120
... loess , or loam , is so extensive that it is perhaps necessary to sup- pose that the central portions of the Mississippi Valley were subjected to a subsidence amounting to about five hundred feet ; so that the glacial streams from the ...
... loess , or loam , is so extensive that it is perhaps necessary to sup- pose that the central portions of the Mississippi Valley were subjected to a subsidence amounting to about five hundred feet ; so that the glacial streams from the ...
Overige edities - Alles bekijken
Veelvoorkomende woorden en zinsdelen
8vo Parchment Library A. E. WAITE accumulation Alps America animals basin boulder-clay boulders cave channel clay coast containing County Crown 8vo débris depth drainage drift east elevation Elzevir 8vo Parchment England erosion Europe evidence extending Fcap Fifth Edition flints Fort Snelling Fourth Edition Frontispiece Geological glacial deposits Glacial epoch glacial ice glacial motion Glacial period glaciated area glaciated region glaciers Grammar gravel Greenland height hills hundred feet Ice age ice-sheet Illustrations implements Irish Sea Island Lake Lake Agassiz land latitude loess mass miles Mountains névé northern northward numerous Ohio Parchment or cloth Pliocene portion Post 8vo preglacial present Professor Rhône Glacier ridges River rocks Rocky sand Sanskrit Second Edition shells side southern southward species strata streams subsidence surface terminal moraine terraces Tertiary Thenay theory Third Edition thousand feet tion Translated tributary Trübner's Oriental Series valley Vellum vicinity vols western
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