Drainage Modifications and Glaciation in the Danbury Region Connecticut: State of Connecticut State Geological and Natural History Survey Bulletin No. 30Harvey, Ruth Sawyer
Science
Drainage Modifications and Glaciation in the Danbury Region Connecticut: State of Connecticut State Geological and Natural History Survey Bulletin No. 30
Harvey, Ruth Sawyer
Geology -- Connecticut; Glacial epoch
Between Danbury and New Milford no moraine crosses either the Rocky or
the Still valley, but the abundance of till which overspreads the
whole country indicates a slowly retreating glacier well loaded with
rock debris. The mounds of stratified drift scattered along the valley
doubtless represent the deltas of streams issuing from the ice front.
The waters of Rocky River were ponded until the outlet near Jerusalem
was uncovered and the disappearance of ice from the ravine below
allowed an escape to the Housatonic. Stratified drift is present in
greatest amount along the valleys of Still River and the west fork of
Rocky River, indicating that these were the two chief lines of
drainage. The uplands are practically without stratified drift.
Along the valley of the Housatonic, glacial material is chiefly in the
form of gravel terraces; they extend from Gaylordsville to New
Milford, in some places on one side only, in others on both sides of
the river. Part of these gravel benches are kame terraces, as shown by
their rolling tops and the ravine which separates the terrace from the
hillside; others may have been made by the river cutting through the
mantle of drift which was laid down in the period of land depression
at the time of glacial retreat,[15] or they may be a combination of the
two forms. In many places by swinging in its flood plain, the river
has cut into the terraces and left steep bluffs of gravel. The valley
of Womenshenuck Brook above Merwinsville contains heavy deposits of
stratified drift, indicating that this broad valley which extends from
Kent on the Housatonic to Merwinsville was an important channel for
the water which flowed from the melting ice.
[Footnote 14: Rice, W. N. and Gregory, H. E., Manual of the Geology of
Connecticut: Conn. Geol. and Nat. Hist. Survey Bull. 6, pp. 34-35,
1906.]
[Footnote 15: Hobbs, W. H., op. cit.]
* * * * *
Transcriber's Notes:
With the following exceptions, the text presented here is that
obtained through scanned images from an original copy of the
manuscript.
Possible Typographic Errors Corrected
occuying => occupying
PLATE II A. "of" repeated
Emphasis Notation:
_text_ - italicized
=text= - bold
~text~ - small caps
Public-domain text, read in full here on John Shaqi.
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