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
Northampton makes an excellent base for many drives that will gratify
the lover of scenery, of rocks, or of minerals. The drives range from
ten to one hundred miles in length, and any one of them may be extended
or shortened at the whim of the driver. To the east the hard surface of
Route 9 leads through Amherst, Pelham, and Belchertown; and to the west,
as the Berkshire Trail, it rises to the western upland via Williamsburg
and Goshen. Side roads go to Ashfield and Conway, and permit a return by
way of South Deerfield; or, via Cummington and West Chesterfield, one
may come back by way of Huntington and Westhampton. Federal Highway 5
follows the Valley north to Greenfield, whence optional return routes
are available through Shelburne Falls, Conway and South Deerfield in the
western upland; or through Orange, Pelham and Amherst in the eastern
upland. Each of these routes offers arresting views of the broad
Connecticut Valley, the picturesque gorges along its margins, and the
even-crested highlands with distant peaks of greater elevation. Indeed,
the choice of attractive drives is bewildering, even for those who are
hesitant about wandering off the surfaced highways.
In the following pages only a few of the possibilities which are
available to the motorist are described. And for each one chosen, the
striking views and the significant geological features are indicated, in
the hope and belief that the traveler may turn explorer and, in
following other byways, may reconstruct for himself many additional
details of the region’s geologic past.
_Northampton, Amherst, Pelham_
The route leaves from the Court House corner on Highway 5 and the
excursion follows Route 9 eastward across the Coolidge Memorial Bridge
(1.3),[1] where a panorama of the floodplain with its many channel scars
and terrace levels is spread out below (see pp. 1-3). Beyond Hadley
(3.0) the road tops the highest river floodplain at a conspicuous
terrace (4.9) and rolls gently over the ancient bed of Lake Hadley. The
shore line of this glacial lake appears as a broad flat between Orchard
Street and Lincoln Avenue in Amherst (6-9). (See pp. 5-7.)
Public-domain text, read in full here on John Shaqi.
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