Man and the Glacial PeriodKegan Paul, 1892 - 385 pagina's |
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Pagina xii
... débris extending from the Alps into the plains of the Po . 134 148 42. Section of the Cefn Cave 43. Map showing moraine between Speeton and Flamborough 156 44 , Diagram - section near Cromer · 166 45. Section through the westerly chalk ...
... débris extending from the Alps into the plains of the Po . 134 148 42. Section of the Cefn Cave 43. Map showing moraine between Speeton and Flamborough 156 44 , Diagram - section near Cromer · 166 45. Section through the westerly chalk ...
Pagina 5
... débris of all grades of fineness ; but , owing to the different consistencies of ice and water , there are great differences in the mode and result of transportation by them . While water can hold in suspension only the very finest ...
... débris of all grades of fineness ; but , owing to the different consistencies of ice and water , there are great differences in the mode and result of transportation by them . While water can hold in suspension only the very finest ...
Pagina 6
... débris are called medial moraines . These are characteristic of all extensive glaciers formed by the union of tributaries . There is no limit to the number of medial moraines , except in the number of tributaries . A medial moraine ...
... débris are called medial moraines . These are characteristic of all extensive glaciers formed by the union of tributaries . There is no limit to the number of medial moraines , except in the number of tributaries . A medial moraine ...
Pagina 7
... débris , this settles down in a very irregular manner , leaving enclosed depres- sions to which there is no natural outlet . These depres- sions , from their resemblance to a familiar domestic uten- sil , are technically known as kettle ...
... débris , this settles down in a very irregular manner , leaving enclosed depres- sions to which there is no natural outlet . These depres- sions , from their resemblance to a familiar domestic uten- sil , are technically known as kettle ...
Pagina 24
... débris , it has piled up a terminal moraine which rises from two hundred to three hundred feet in height , and is now cov- ered with evergreen trees of considerable size . From Chilkat , at the head of Lynn Canal , to the sources of the ...
... débris , it has piled up a terminal moraine which rises from two hundred to three hundred feet in height , and is now cov- ered with evergreen trees of considerable size . From Chilkat , at the head of Lynn Canal , to the sources of 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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