The flow of time in the Connecticut valley : $b geological imprintsBain, George W. (George William)
Science
The flow of time in the Connecticut valley : $b geological imprints
Bain, George W. (George William)
Geology -- Connecticut River Valley
This tour also leaves Northampton by the Coolidge Memorial Bridge, but
at Hadley (3.0) it turns north on State Highway 63 and follows the river
to Sunderland. Here the route recrosses the river, joining Federal
Highway 5 at South Deerfield, and from this point south to Northampton
the road lies almost literally in the shadow of the western upland.
In Hadley (3.0) the road turns north along Center Street and then swings
right at the curve in the Connecticut (3.5). The river bank is lined
with riprap to resist the current and to prevent the river from washing
away a substantial section of the town. Across the stream in Hatfield
the Connecticut very nearly achieved the type of destruction which the
residents of Hadley are trying to escape, and the flood-channel, or
“washout,” which was gouged by the swollen stream in the spring of 1936,
may be seen (4.3) on the way to North Hadley. The road approaches Mount
Warner, whose crystalline rocks appear at the south end of a long, low
spur (4.8) on the edge of the river floodplain. Elsewhere along the base
of the eminence, which scarcely merits the name “Mount,” the crystalline
rocks are hidden by a terrace, but they crop out on the higher slopes.
The younger red Triassic sandstones are present, too, and they may be
seen dipping steeply westward in the brook bed between the bridge (5.9)
and the dam (6.1) at North Hadley.
Sand dunes appear near the river on the outskirts of North Hadley (6.3)
and extend north beyond Mount Warner (7.0) to the point where the road
drops from the terrace to the floodplain (8.2). Here the former bed of
the river is occupied by a puny brook, which enters the mainstream on
the left. The terrace marking the edge of the floodplain lies close to
the east side of the road for a long distance (8.2 to 9.8) and then
swings a half mile eastward. The road follows a high area between two
abandoned channels formerly used by the river (11.3), until it joins the
Amherst-Sunderland road (11.8) at the southern edge of Sunderland. The
route turns left in the center of town (12.4), crossing the river
beneath Mount Sugarloaf, and it continues on to Federal Highway 5 at the
traffic light in South Deerfield (14.2).
On the trip south from the junction, sand dunes appear east of the
railroad between the Boston & Maine (14.6) and the New Haven crossings
(14.9). The highway is situated on the flat bed of Lake Hadley from this
point to Hatfield. The road to Whately, which turns west at 16.7, offers
some attractions. It forks two miles beyond Whately, and the right
branch leads to the Northampton reservoir and to Haydenville (see
p. 89). The left branch follows West Fork Brook and comes back to
Federal Highway 5 at North Hatfield (19.1). Either route provides a
scenic drive over little-frequented gravel roads.
Public-domain text, read in full here on John Shaqi.
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