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
The Mohawk Trail (State Highway 2) heads west from the center of
Greenfield and crosses the Green River (0.6) before climbing out of the
valley. A lookout (2.1) affords an excellent view of the north end of
the Connecticut Lowland, and the observation tower on Shelburne Summit
(3.2), situated on a shelf cut out of black Ordovician slate (see pp. 35
-37), provides a broader sweep of central New England scenery. Beyond,
the upland is gently rolling, trenched by one deep valley at Shelburne
Center (6.8). The descent into this valley (5.6) offers a glimpse to the
south across the Deerfield River gorge, but the road soon rises again,
hovering 300 feet above the sharply incised stream. The Sweetheart
Teahouse (9.9) makes use of one of the ideal sites overlooking the gorge
and river. The highway to Colrain (10.2) continues straight ahead, but
the Trail turns left across the Deerfield River (10.6) and then right in
Shelburne Falls. The road left leads to Conway and South Deerfield.
Thick, almost horizontal bands of gray granite gneiss are exposed in the
road cuts (11.6) along the south bank of the Deerfield River, but the
entrenched stream has left so little room for the highway that the
latter soon crosses to the relatively low and more hospitable north bank
(11.9). For many miles the road follows the stream so closely that
spring floods occasionally cover its surface with ice cakes. The drive
along this stretch to the next bridge (21.0) contains the most restful
scenery on the trip, though the flat open valley is hemmed in by abrupt
slopes which rise for 800 feet. Nor does the flatness of the valley
harmonize with the mountain-structure of the platy Goshen schist, which
stands on edge all along the roadside. Davis Brook (18.7) crosses the
route, and the road beside it leads up to the Davis Mine, which once did
a thriving business extracting iron pyrites for the manufacture of
sulphuric acid.
Once more the highway crosses the Deerfield River (21.0) and enters
Mohawk Park, which invites the motorist to linger. A mile farther on
(22.0) the road leaves the Deerfield River (22.0) and follows the narrow
gorge of Cold River, which seems scarcely wide enough to accommodate it.
A shady picnic ground and auto camp (23.6) lie just below the narrowest
and deepest part of the gorge (24.5), where the crowding summits seem to
tower high above the puny cars.
The road crosses to the north bank of Cold River (25.8) and climbs a
shelf cut into green volcanic schists (25.8 to 27.6). Leaving the gorge
(26.6), it ascends to the upland (29.0), while in view below is the
laborious route of the Boston and Maine Railroad along the Deerfield and
thence through the east portal of the Hoosac Tunnel near Zoar.
Public-domain text, read in full here on John Shaqi.
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