id	author	title	date	pages	extension	mime	words	sentences	flesch	summary	cache	txt
33050	Harvey, Ruth Sawyer	Drainage Modifications and Glaciation in the Danbury Region Connecticut State of Connecticut State Geological and Natural History Survey Bulletin No. 30			.txt	text/plain	17825	1061	74	[Illustration: ~Fig. 2.~ Geological map of Still River Valley.] and for the broad drift-filled valley at the mouth of Rocky River. feet from the east bank of Rocky River and about 1-3/4 miles north of [Illustration: ~Fig. 5.~ Rocky River Valley. the barrier which choked the Rocky River valley near its mouth and If Still River occupies the valley of a reversed stream, the following Drift forms the divide at the western end of Still River valley beyond valley to the west indicates that glacial deposits forced the river the Still River valley joins the Housatonic, and it indicates normal 2-1/4 miles north of Bethel, Still River crosses rock at a level of FEATURES OF STILL RIVER VALLEY WEST OF DANBURY FEATURES OF STILL RIVER VALLEY WEST OF DANBURY B. Till ridges on the western border of Still River Valley, south damming of river valleys by glacial deposits and (2) rock basins	./cache/33050.txt	./txt/33050.txt