Report On the Geology of Vermont Descriptive Theoretical Economical And Scen
Report On the Geology of Vermont Descriptive Theoretical Economical And Scen
Vermont State Geologist
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H. H. C. H. H. C. H. H. C. B. A. C. B. A. C. B. A. C. B. A. C. B. A. C. H. H. An inspection of this list shows that in the southern part of the formation, the prevailing dip is to the east; that in the part north of Colchester Point, the usual dip is to the northeast and north; while in Bridport and Addison, a westerly dip prevails. These variations in the two first instances, depend upon the direction of the whole formation; and in the latter case it depends upon its position upon the west sid...e of an anticlinal axis. The magnitude of the dip, in many cases, is due to local causes, or the cleavage planes may have been mistaken for the true inclination. Rock Dunder is a naked mass of slate, lying nearly midway between Pottier's Point, in Shelburne and Juniper Island. Its circumference, at the surface of the water, on the 28th of July, 1846, was 310 feet, and its height above the water 36 feet; but as there is considerable space around the base of the rock, near the water level, the circumference will vary with the amount of water in the lake.
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