This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1920 edition. Excerpt: ...(74). PVillsboro quadrangle. The profile levels along the west side of the lake rise from about 615 to 660 feet. The lower plains of the Bouquet delta are conspicuous on the map, north and south of Villsboro. The coarser detritus of the river was dropped at the junction with the high-level waters far inland, that of the south branch at Elizabethtown, as already noted, and that of the north branch on the Ausable quadrangle 3 miles north of Towers Forge. The hill 2 miles south of Willsboro carries elegant inferior bars on the summit and east face, from 300 feet down. Northwest of East Bouquet mountain clear evidence of standing water was seen along two roads up to a height of 620 feet. The theoretic height is about 625 feet. Examination of the area will locate many evidences of summit wave action. Plattsburg and Damzemora qmuirangles. On this area the summit shore features lie inland, with handsome display. The Plattsburg sheet shows the low ground built by the Ausable, Little Ausable, Salmon and Saranac rivers. But the south edge of this sheet covers the north part of the Trembleau mountain, which carries on its northwest slope a fine series of gravel bars below the summit of the marine flood. W'oodworth maps these bars in his plate 21. The Trembleau gravel bars lie one and one-half miles southwest of Port Kent, and 2 miles east of Keeseville. An east and west road crosses the plateau which carries the higher good bars. The highest bars, at about 590 feet, lie in weak form close to the steep northwest face of the mountain. This is 70 feet short of the summit plane, but the steep rock face shows its rinsing. On the road bars appear at about 575, 560, 545 and 530 feet. The northwest end of the hill is encircled by a series of bars to a lower...