An Introduction to the Geology of Dayton And Vicinity With Special Reference to
An Introduction to the Geology of Dayton And Vicinity With Special Reference to
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The Eastview and Sunset ridges are united at several points hy short transverse ridges, the most con- spicuous of which is at the Tip Top knob, at the southern end of the Old Orchard hollow, on the Moraine farm. Connecting ridges are seen also in the Delco Dell area. One of these is followed by the main road entering the grounds. It is probable that the spurs projecting westward from the Delco ridge, in the Delco Dell area, represent similar transverse channels connecting with a north and south... ridge farther westward, of which only partial remnants remain. Short lateral spurs occur also on the western side of the Sunset ridge, northwest of the Summer camp, on the Moraine farm. Larger spurs occur on the Grand View Hill farm, southwest of the Delco Dell area.
The presence of these transverse ridges and short spurs suggests that the front of the ice sheet must have been very stagnant at the time of their formation. Moving ice would have shifted these lateral channels and would have spread their deposits over a wider territory.
What to read after An Introduction to the Geology of Dayton And Vicinity With Special Reference to?
You can find similar books in the "Read Also" column, or choose other free books by August Frederic Foerste to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The Eastview and Sunset ridges are united at several points hy short transverse ridges, the most con- spicuous of which is at the Tip Top knob, at the southern end of the Old Orchard hollow, on the Moraine farm. Connecting ridges are seen also in the Delco Dell area. One of these is followed by the main road entering the grounds. It is probable that the spurs projecting westward from the Delco ridge, in the Delco Dell area, represent similar transverse channels connecting with a north and south... ridge farther westward, of which only partial remnants remain. Short lateral spurs occur also on the western side of the Sunset ridge, northwest of the Summer camp, on the Moraine farm. Larger spurs occur on the Grand View Hill farm, southwest of the Delco Dell area.
The presence of these transverse ridges and short spurs suggests that the front of the ice sheet must have been very stagnant at the time of their formation. Moving ice would have shifted these lateral channels and would have spread their deposits over a wider territory.
What to read after An Introduction to the Geology of Dayton And Vicinity With Special Reference to?
You can find similar books in the "Read Also" column, or choose other free books by August Frederic Foerste to read onlineMoreLess
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