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Cobequid Fault
The Cobequid Fault is a fault that is the extension of the Chedabucto Fault. This fault runs from Truro to Cape Chignecto south of the Cobequid Hills. Both the Cobequid fault and the Chedabucto Fault form the Minas Fault zone splitting Nova Scotia into the Avalon Zone and the Meguma Zone. Movement on the Cobequid Fault started before 400 million years ago and end around 40 million years ago. Between that time around 350 million years violent volcanic eruptions at Spicers Cove north Cape Chignecto Provincial Park and 50 million years after grey sandstone rich in fossil plants were deposited. At Five Islands Provincial Park 5 is a number, numeral, and glyph. 5, five or number 5 may also refer to: * AD 5, the fifth year of the AD era * 5 BC, the fifth year before the AD era Literature * 5 (visual novel), ''5'' (visual novel), a 2008 visual novel by Ram * 5 (comic ... there are red rocks formed by the large accumulation of mud, sand and gravel around 210 million years ago. Ref ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cobequid Fault Zone Near Clarke Head
The old name Cobequid was derived from the Mi'kmaq word "Wagobagitk" meaning "the bay runs far up", in reference to the area surrounding the easternmost inlet of the Minas Basin, a body of water called Cobequid Bay. Cobequid was granted in 1689 to Mathieu Martin. He was said to be the first Acadian born in Acadia. In 1705, the Acadians first settled in this area near Cobequid Bay. The Acadian culture consisted primarily of farming. Their advanced farming systems of dykes permitted them to recuperate valuable farmland from the marshlands that cover the entire coast of the community. The community, which is now called Masstown, is located 10 minutes west of Truro on Highway 2 or Exit 12 off Highway 104. In 1714 many inhabitants of Minas signed to a resolution, dated 9 September 1714, to go to Cape Breton. Many came from Cobequid, Grand-Pré, Riviere des Gasparots (Gaspareaux), Riviere de Pessequid, Riviere des Habitants, and Riviere de la Vieille Habitation. In August 1744, a cert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chedabucto Fault
The Chedabucto Fault is a Fault (geology), fault that divides Mainland Nova Scotia from the Minas Basin in the west to Chedabucto Bay in the east into the Avalonia, Avalon zone in the north and the Meguma Zone in the south. The Avalon and Meguma terrane, Meguma Zones are different because they belonged to different land masses that were widely separated from one another. The Avalon Zone was a part of Laurasia, while the Meguma Zone was a part of Gondwana. It marks the southern margin of the Cobequid Mountains. The Cobequid fault, Cobequid-Chedabucto Fault Zone is the most prominent geological feature of Nova Scotia. ReferencesCobequid-Chedabucto Fault at Cape Chignecto, Nova Scotia *[https://notyourgrandfathersmining.ca/geo-cc-fault-system Cobequid-Chedabucto Fault System] [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Truro, Nova Scotia
Truro (Mi'kmaq: ''Wagobagitik''; Scottish Gaelic: ''Truru'') is a town in central Nova Scotia, Canada. Truro is the shire town of Colchester County and is located on the south side of the Salmon River floodplain, close to the river's mouth at the eastern end of Cobequid Bay. History The area has been home to the Mi'kmaq people for several centuries. The Mi'kmaq name for the Truro area, "Wagobagitik" means "end of the water's flow". Mi'kmaq people continue to live in the area at the Millbrook and Truro reserves of the Millbrook – We’kopekwitk band. Acadian settlers came to this area in the early 1700s. The Mi'kmaq name for the Truro area was shortened by the settlers to "Cobequid", and the bay to the west of the town is still named Cobequid Bay. By 1727, the settlers had established a small village near the present downtown site of Truro known as "Vil Bois Brule" (Village in the burnt wood). Many Acadians in this region left in the Acadian Exodus which preceded the Expulsi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Chignecto
Cape Chignecto is a headland located on the Bay of Fundy coast of the Canadian province of Nova Scotia. Cape Chignecto is located at the westernmost tip of Cumberland County and is the western limit of the Cobequid Hills, a low mountain range that is part of the Appalachian Mountains and extends across the northern part of the Nova Scotia peninsula. The cape bifurcates the Bay of Fundy into Chignecto Bay to the north and the Minas Channel, leading to the Minas Basin to the east. Since 1998 the cape has been located within Cape Chignecto Provincial Park, the largest provincial park in the province and a renowned wilderness reserve. The cape features a rugged topography with reportedly the highest cliffs on the Nova Scotia peninsula, created by the upthrusting Cobequid fault. The cape is mostly uninhabited. It includes the ghost towns of Eatonville and New Yarmouth. The nearest inhabited village is Advocate, Nova Scotia. The name "Chignecto" derives from the Mi'kmaw name Siknikt, m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cobequid Hills
The Cobequid Mountains, also sometimes referred to as the Cobequid Hills, is a Canadian mountain range located in Nova Scotia in the mainland portion of the province. Geologic history Geologically, the Cobequid Mountains are considered part of the Appalachians. The range stretches from Cape Chignecto in Cumberland County in the west through to Pictou County in the east. The Cobequid Mountains trace their geologic history to the Precambrian and Devonian ages; consequently the mountains are composed of a combination of sediments, granites, and volcanic rock all of which has been crushed and folded by continental drift when this part of Nova Scotia was located at the centre of the Pangea supercontinent. Subsequent erosion over millions of years has resulted in the present-day low range of mountains and rolling hills. The part of northern Nova Scotia which contains the Cobequid Mountains is believed to have been linked with what is now northern Europe. Its collision with a section ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nova Scotia
Nova Scotia ( ; ; ) is one of the thirteen provinces and territories of Canada. It is one of the three Maritime provinces and one of the four Atlantic provinces. Nova Scotia is Latin for "New Scotland". Most of the population are native English-speakers, and the province's population is 969,383 according to the 2021 Census. It is the most populous of Canada's Atlantic provinces. It is the country's second-most densely populated province and second-smallest province by area, both after Prince Edward Island. Its area of includes Cape Breton Island and 3,800 other coastal islands. The Nova Scotia peninsula is connected to the rest of North America by the Isthmus of Chignecto, on which the province's land border with New Brunswick is located. The province borders the Bay of Fundy and Gulf of Maine to the west and the Atlantic Ocean to the south and east, and is separated from Prince Edward Island and the island of Newfoundland by the Northumberland and Cabot straits, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Chignecto Provincial Park
Cape Chignecto Provincial Park is a Canadian provincial park located in Nova Scotia. A wilderness park, it derives its name from Cape Chignecto, a prominent headland which divides the Bay of Fundy with Chignecto Bay to the north and the Minas Channel leading to the Minas Basin to the east. The park, which opened in 1998, is the largest provincial park in Nova Scotia. It also anchors one end of the UNESCO Cliffs of Fundy Global Geopark. Landscape The park's landscape is renowned for spectacular shoreline with extensive backpacking trails and scenic day hikes. The highest cliffs in Mainland Nova Scotia are located along the park's southern coast, measuring 200 metres (600 ft). The park occupies and has of wilderness coastline with unique geological features such as raised beaches, caves and sea stacks. The complex geology was created by continental collision along the Cobequid fault. The spectacular coastal landscapes of the park make it popular for hikers and kayakers. It a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Five Islands Provincial Park
5 is a number, numeral, and glyph. 5, five or number 5 may also refer to: * AD 5, the fifth year of the AD era * 5 BC, the fifth year before the AD era Literature * ''5'' (visual novel), a 2008 visual novel by Ram * ''5'' (comics), an award-winning comics anthology * ''No. 5'' (manga), a Japanese manga by Taiyō Matsumoto * The Famous Five (novel series), a series of children's adventure novels written by English author Enid Blyton Films * ''Five'' (1951 film), a post-apocalyptic film * ''Five'' (2003 film), an Iranian documentary by Abbas Kiarostami * ''Five'' (2011 film), a comedy-drama television film * ''Five'' (2016 film), a French comedy film * Number 5, the protagonist in the film ''Short Circuit'' (1986 film) Television and radio * 5 (TV channel), a television network in the Philippines (currently known as TV5 from 2008 to 2018 and again since 2020), owned by TV5 Network, Inc. * Channel 5 (British TV channel), British free-to-air television network sometime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of Nova Scotia
The Nova Scotia peninsula is a peninsula on the Atlantic Ocean, Atlantic coast of North America. Location The Nova Scotia peninsula is part of the province of Nova Scotia, Canada and is connected to the neighbouring province of New Brunswick through the Isthmus of Chignecto. It fronts the open Atlantic Ocean on the south and southeast, the Gulf of Maine to the west, the Bay of Fundy and its sub-basins to the northwest, the Northumberland Strait to the north, and the Strait of Canso to the east. The narrow and deep waters of the Strait of Canso separate the peninsula from Cape Breton Island, the second largest land mass constituting the province of Nova Scotia. In addition to Cape Breton Island, other much smaller islands are geologically associated with the Nova Scotia peninsula, including Boularderie Island, Brier Island, Long Island (Nova Scotia), Long Island, Pictou Island, Big Tancook Island, Tancook Island and various smaller islands along the Atlantic coast. Geology Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Nova Scotia
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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