Glaciation of the Uinta Mountains ..
Glaciation of the Uinta Mountains ..
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In our eReader you can find the full English version of the book. Read Glaciation of the Uinta Mountains .. Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Glaciation of the Uinta Mountains ..
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A few miles farther south the valley slopes become somewhat irregular in form and at places have a hum- mocky topography. There is nothing, however, in this topography, or in the material, that demonstrates glaciation, and it is believed that the forms may all ^junuv artft have been produced by landslides in the Tertiary conglomerates.
At the upstream margin of the outer terrace the moraines have the characteristic forms and posi- tions of such deposits. They mask the lower slopes of the valley..., ap- pear as irregular heaps in the midst of the valley, and continue upstream to the younger terminal moraines in the different tributaries. In fact, these older moraines extend still farther upstream and stand higher on canyon walls than the younger lateral moraines. (See fig. 2.) The glacial deposits crossing the valleys w r here the upper alluvial terraces end upstream are interpreted as terminal moraines of the later ice advajice, representing the position of that ice at its maximum extension.
What to read after Glaciation of the Uinta Mountains ..?
You can find similar books in the "Read Also" column, or choose other free books by Wallace Walter Atwood to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
A few miles farther south the valley slopes become somewhat irregular in form and at places have a hum- mocky topography. There is nothing, however, in this topography, or in the material, that demonstrates glaciation, and it is believed that the forms may all ^junuv artft have been produced by landslides in the Tertiary conglomerates.
At the upstream margin of the outer terrace the moraines have the characteristic forms and posi- tions of such deposits. They mask the lower slopes of the valley..., ap- pear as irregular heaps in the midst of the valley, and continue upstream to the younger terminal moraines in the different tributaries. In fact, these older moraines extend still farther upstream and stand higher on canyon walls than the younger lateral moraines. (See fig. 2.) The glacial deposits crossing the valleys w r here the upper alluvial terraces end upstream are interpreted as terminal moraines of the later ice advajice, representing the position of that ice at its maximum extension.
What to read after Glaciation of the Uinta Mountains ..?
You can find similar books in the "Read Also" column, or choose other free books by Wallace Walter Atwood to read onlineMoreLess
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