DEPOSITS BETWEEN BEAVER BROOK MOUNTAIN AND MOUTH OF STILL RIVER

About a mile beyond Beaver Brook Mountain, the railroad cuts through

the edge of a hill 80 feet in height exposing a section consisting of

distinctly stratified layers of fine white quartz sand, coarser

yellowish sand, and small round pebbles. The quartz sand was used at

one time in making glass. Farther east where the two tracks of the New

York and New England railroads converge, a cut shows a section of at

least 40 feet of boulder clay. Near the river, limestone boulders are

common, indicating that the valley to the north was degraded to some

extent by the glacier.

[Illustration: ~State Geol. Nat. Hist. Survey Bull. 30. Plate V.~

A. Kames in Still River Valley west of Brookfield Junction.

B. Till ridges on the western border of Still River Valley, south

of Brookfield.]

In the valley at Brookfield Junction and on its western side, are

thick deposits of clean sand. One mile north of Brookfield Junction,

along the western border of the valley, an esker follows an irregular

course for several hundred yards approximately parallel to the river

and terminates at its southern end in a group of kames (Pl. V, A and

B). Opposite the point where these accumulations occur, is a

terrace-like deposit of till. Between the gorge at Brookfield and the

mouth of Still River, swampy areas, flat meadows, and small hills of

drift occur.

In comparison with the Still River lowland, the flat land east of

Green Mountain may be called a plateau. The step between the two is

made by an east-facing rocky slope, the outline of which has been

softened by a lateral moraine separated from the plateau edge by a

small ravine. On the lowland below the moraine is a group of kames.

Near Lanesville (fig. 6), are thick deposits of water-laid material,

including a hill of gravel near the river having a large bowl-shaped

depression on one side formed by the melting of an ice block. Two and

a half miles south of Lanesville on the west side of the lowland, a

wooded esker extends for about one-quarter mile parallel to the valley

axis and then merges into the rocky hillside.

Drainage modifications and glaciation in the Danbury region, Connecticut · 第 60 / 62 题