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Hingham (/ ˈ h ɪ ŋ ə m / HING-əm) is a town in northern Plymouth County in the U.S. state of Massachusetts. Part of the Greater Boston region, it is located on the South Shore of Massachusetts. At the 2020 census, the population was 24,284. [5] Hingham is known for its colonial history and location on Boston Harbor.
Route 3A is a 97-mile-long (156 km) state highway in eastern Massachusetts, which parallels Route 3 and U.S. Route 3 (US 3) from Cedarville in southern Plymouth to Tyngsborough at the New Hampshire state line. Route 3A has two major posted segments, separated by a lengthy concurrency with Route 3 and US 3.
It encompasses the earliest streets laid out in Hingham at the time of its founding in 1635, covering more than 300 years of development and a cross section of Hingham's architectural history. It includes some of the town's oldest buildings, including most notably the Old Ship Church and the General Benjamin Lincoln House , both National ...
The Greenbush Line is a branch of the MBTA Commuter Rail system which serves the South Shore region of Massachusetts. The 27.6-mile (44.4 km) line runs from downtown Boston, Massachusetts through the cities and towns of Quincy, Braintree, Weymouth, Hingham, Cohasset, and Scituate to the Greenbush neighborhood in southern Scituate.
For a period of time, from at least the early 1930s through 1967, a mile of what is now Route 53, between Derby Street and Main Street (Route 228), was also coextensive with Route 128. In 1967 that route was cut back to the Braintree Split , and again in 1997 it was officially cut back to the I-95 / I-93 junction in Canton .
Nantasket Avenue begins in Hingham and Cohasset, at a four-way junction with Rockland Street (west), Jerusalem Road (east), and Hull Street (south).Hull Street and Nantasket Avenue are designated Massachusetts Route 228, and the road forms the town line between Hingham and Cohasset until it crosses Straits Pond Dam into Hull just north of the junction.
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Boston Harbor and its smaller sections such as Hingham Bay are characterized by geography created through Quaternary glaciations.During the last 100,000 years two glacial periods shaped the typical topography of the area through creation of drumlins and moraines followed by marine incursion flooding the low levels as the glaciers receded. [8]
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