Pennsylvania Glaciation First Phase Materials for a Discussion of the Attenuat
Pennsylvania Glaciation First Phase Materials for a Discussion of the Attenuat
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There is, however, no " attenuation" here, as the drift is the usual sandy clayless body including abundant various sandstones and conglomerate masses. The exposure just east of Locust Summit is especially fine. From Locust Summit (1340) to Locust Gap is a fall along a ponded and filled valley draining northward 52 PENNSYLVANIA GLACIATION. FIRST PHASE into Shamokin Creek, and cuttings in a thick drift-sheet are numerous. It carries large boulders and rests of a glaciated rock floor.
Shamokin Ba...sin. The outer (Pocono) border of this is Little Moun- tain, which is an extension of Nescopeck Mountain, which, in turn, ex- tends the Moosic-Pocono barrier across the ridge at Bear Creek Summit (2000) and sweeps S. 50 W. For 36 miles to Susquehanna River as the gradually rising border of the Mauch Chunk valley of Nescopeck Creek, and, beyond the saddle therein, of Scotch Creek. At the Nescopeck Creek Gap it rises 900 feet above that stream. At the Susquehanna, near Catawissa it turns sharply S.
What to read after Pennsylvania Glaciation First Phase Materials for a Discussion of the Attenuat?
You can find similar books in the "Read Also" column, or choose other free books by Edward Higginson Williams to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
There is, however, no " attenuation" here, as the drift is the usual sandy clayless body including abundant various sandstones and conglomerate masses. The exposure just east of Locust Summit is especially fine. From Locust Summit (1340) to Locust Gap is a fall along a ponded and filled valley draining northward 52 PENNSYLVANIA GLACIATION. FIRST PHASE into Shamokin Creek, and cuttings in a thick drift-sheet are numerous. It carries large boulders and rests of a glaciated rock floor.
Shamokin Ba...sin. The outer (Pocono) border of this is Little Moun- tain, which is an extension of Nescopeck Mountain, which, in turn, ex- tends the Moosic-Pocono barrier across the ridge at Bear Creek Summit (2000) and sweeps S. 50 W. For 36 miles to Susquehanna River as the gradually rising border of the Mauch Chunk valley of Nescopeck Creek, and, beyond the saddle therein, of Scotch Creek. At the Nescopeck Creek Gap it rises 900 feet above that stream. At the Susquehanna, near Catawissa it turns sharply S.
What to read after Pennsylvania Glaciation First Phase Materials for a Discussion of the Attenuat?
You can find similar books in the "Read Also" column, or choose other free books by Edward Higginson Williams to read onlineMoreLess
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