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Eastern Border Fault, an inactive Mesozoic rift, formed the Connecticut River Valley and runs along the eastern side of it. The fault can be traced from New Haven, CT to Keene, NH. [20] Sporadic earthquakes along this fault lowered the valley and raised the eastern hills. [21] Merrimack Terrane Ware belt; Gardner belt; Wachusett Mountain belt
The fault is visible along I-495 just east of Westborough and further east, the Bloody Bluff-Lake Char fault splits into smaller branches. One of these faults, tentatively named the Weston fault, may extend into the Boston Basin. Where the Bloody Bluff fault ends in the northeast, at the terminus of the Burlington mylonite zone, it may ...
Firth – Scottish word used for various coastal inlets and straits; Fjard – Glacially formed, broad, shallow inlet; Fjord – Long, narrow inlet with steep sides or cliffs, created by glacial activity; Geo – Inlet, a gully or a narrow and deep cleft in the face of a cliff; Gulf – Large inlet from the ocean into the landmass List of gulfs
Jun. 28—FRANCONIA NOTCH Artists' Bluff, whose sublime views once enticed 19th-century painters, today is one of the most Instagrammed spots in the White Mountains. A magnet from late May through ...
Most of the bluff is displaced approximately 40 metres (131 ft) upwards relative to the adjoining bedrock along the Red Wing Fault, which transects the bluff near its south face. It is composed of early Paleozoic rocks, including Ordovician dolomite and sandstone atop Cambrian shale , siltstone and greensand at its base, deposited by early ...
The Marion Art Center has three February School vacation workshops for children led by Benares Angeley. The cost for each workshop is $35 for MAC members and $40 for nonmembers. More information ...
Three units of the Ice Age National Scientific Reserve are located within or adjacent to the Driftless Area: Devil's Lake State Park, Mill Bluff State Park, and Cross Plains State Park. In addition, the Ice Age Trail follows the Terminal moraine of the maximum glacial extent from the last ice age and enters the Driftless Area in several locations.
Gosses Bluff (or Gosse's Bluff) is thought to be the eroded remnant of an impact crater. [2] [3] [4] Known as Tnorala to the Western Arrernte people of the surrounding region, it is located in the southern Northern Territory, near the centre of Australia, about 175 km (109 mi) west of Alice Springs and about 212 km (132 mi) to the northeast of Uluru (Ayers Rock).