Penobscot Bay in the context of Stonington, Maine


Penobscot Bay in the context of Stonington, Maine

⭐ Core Definition: Penobscot Bay

Penobscot Bay (French: Baie de Penobscot) is an inlet of the Gulf of Maine and Atlantic Ocean in south central Maine, a stretch known as Midcoast Maine, in a broader Atlantic region known as Down East. The bay originates from the mouth of Maine's Penobscot River, downriver from Belfast. Penobscot Bay has many working waterfronts including Rockland, Rockport, Stonington, and Belfast. Penobscot Bay is between Muscongus Bay and Blue Hill Bay, just west of Acadia National Park.

At the beginning of the Holocene epoch 11,000 years ago, the Gulf of Maine's sea level fell as low as 180 feet (55 m) below its present height. Penobscot Bay was then a continuation of Penobscot River that meandered through a broad lowland extending past present day Matinicus Island.

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Penobscot Bay in the context of Gulf of Maine

The Gulf of Maine is a large gulf of the Atlantic Ocean on the east coast of North America. It is bounded by Cape Cod at the eastern tip of Massachusetts in the southwest and by Cape Sable Island at the southern tip of Nova Scotia in the northeast. The gulf includes the entire coastlines of the U.S. states of New Hampshire and Maine, as well as Massachusetts north of Cape Cod, and the southern and western coastlines of the Canadian provinces of New Brunswick and Nova Scotia, respectively.

The gulf was named for the adjoining English colonial Province of Maine, which was in turn likely named by early explorers after the province of Maine in France. Massachusetts Bay, Penobscot Bay, Passamaquoddy Bay, and the Bay of Fundy are all arms of the Gulf of Maine.

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Penobscot Bay in the context of Bay mud

Bay mud consists of thick deposits of soft, unconsolidated silty clay, which is saturated with water; these soil layers are situated at the bottom of certain estuaries, which are normally in temperate regions that have experienced cyclical glacial cycles.

Example locations are Cape Cod Bay, Chongming Dongtan Reserve in Shanghai, China, Banc d'Arguinpreserve in Mauritania, The Bristol Channel in the United Kingdom, Mandø Island in the Wadden Sea in Denmark, Florida Bay, San Francisco Bay, Bay of Fundy, Casco Bay, Penobscot Bay, and Morro Bay.

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Penobscot Bay in the context of Dominion of New England

The Dominion of New England in America (1686–1689) was a short-lived administrative union of English colonies covering all of New England and the Mid-Atlantic Colonies, with the exception of the Delaware Colony and the Province of Pennsylvania. The region's political structure was one of centralized control similar to the model used by the Spanish monarchy under the Viceroyalty of New Spain. The dominion was unacceptable to most colonists because they deeply resented being stripped of their rights and having their colonial charters revoked. Governor Edmund Andros tried to make legal and structural changes, but most of these were undone and the Dominion was overthrown as soon as word was received that King James II had vacated the throne in England. One notable change was the forced introduction of the Church of England into Massachusetts, whose Puritan leaders had previously refused to allow it any foothold.

The Dominion encompassed a very large area from the Delaware River in the south to Penobscot Bay in the north, composed of the Province of New Hampshire, Massachusetts Bay Colony, Plymouth Colony, Colony of Rhode Island and Providence Plantations, Connecticut Colony, Province of New York, the provinces of East Jersey and West Jersey, and a small portion of Maine. It was too large for a single governor to manage. Governor Andros was highly unpopular and was seen as a threat by most political factions. News of the Glorious Revolution in England reached Boston in 1689, and the Puritans launched the 1689 Boston revolt against Andros, arresting him and his officers.

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