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Geography Of Nova Scotia
Nova Scotia is a province located in Eastern Canada fronting the Atlantic Ocean. One of the Maritimes, Maritime Provinces, Nova Scotia's geography is complex, despite its relatively small size in comparison to other Canadian provinces. Physical geography The mainland portion of the Nova Scotia peninsula is attached to North America through the Isthmus of Chignecto. Various offshore islands, the largest of which is Cape Breton Island, form the bulk of the eastern part of the province. The geology, geological history of the province spans more than 1.2 billion year Continental drift led to the southern half of the province's mainland portion, the Meguma terrane, once being attached to Africa whereas the Avalon terrane comprising the northern half, including Cape Breton Island, was once attached to Scandinavia and Scotland. The Meguma terrane became joined to the present North American landmass as part of the Appalachian orogeny. Composed largely of Cambrian to Ordovician sedim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Joggins Cliffs, Nova Scotia
Joggins is a rural community located in western Cumberland County, Nova Scotia, Canada. On July 7, 2008 a 15-km length of the coast constituting the Joggins Fossil Cliffs was officially inscribed on the World Heritage List.UNESCO portal History The area was known to the as "Chegoggins" meaning place of the large fish weir, a name modified by French and English settlers to Joggins. Situated on the Cumberland Basin, a sub-basin of the |
Minas Fault Zone
Minas or MINAS may refer to: People with the given name Minas * Menas of Ethiopia (died 1563) * Saint Menas (Minas, 285–309) * Minias of Florence (Minas, Miniato, died 250) * Minas Alozidis (born 1984), Greek hurdler * Minas Avetisyan (1928–1975) * Minas Hantzidis (born 1966), Greek footballer * Minas Hadjimichael (born 1956), Permanent Representative to the United Nations for Cyprus * Minas Hatzisavvas (1948–2015), Greek actor * Minas of Aksum, 6th-century bishop People with the surname Minas * Iskouhi Minas (1884–1951), French poet and writer of Armenian descent. Places * Minas Gerais, Brazil * Minas, Uruguay * Minas Department, Córdoba, Argentina * Minas Department, Neuquén, Argentina * Minas, Cuba, a municipality in Cuba * Minas, Iran, a village in West Azerbaijan Province, Iran * Minas Basin in Nova Scotia * Les Mines, a former Acadian community on the shores of the Minas Basin (called Minas or Mines in English) Other uses * Minas (band), an American bos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Minas Basin
The Minas Basin () is an inlet of the Bay of Fundy and a sub-basin of the Fundy Basin located in Nova Scotia, Canada. It is known for its extremely high tides. Geography The Minas Basin forms the eastern part of the Bay of Fundy which splits at Cape Chignecto and is delineated by the massive basalt headlands of Cape Split and Cape d'Or. The Minas Basin is divided into four sections: (1) the Minas Channel, from the shortest line between Cape Chignecto and the Annapolis Valley Shore to Minas Passage, between Parrsboro and Cape Blomidon; (2) Central Minas Basin, from Minas Passage to the mouth of Cobequid Bay, the shortest line point between Economy and the Noel Shore; (3) Cobequid Bay which extends to the mouth of the Salmon River; and (4) the Southern Bight, from the mouth of the Avon River to the shortest line between Cape Blomidon and the Noel Shore. Several large rivers drain into the Minas Basin: the Shubenacadie River, Cornwallis River, Avon River, Gaspereau Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cumberland Basin (Canada)
Cumberland Basin is an inlet and northeasternmost part of the Bay of Fundy, located on the border between the Canada, Canadian provinces of Nova Scotia and New Brunswick. It is the eastern branch of Chignecto Bay, which in turn is the western arm of the upper Bay of Fundy. In geology, the Cumberland Basin (geology), Cumberland Basin is a sedimentary basin which underlies most of Cumberland County, Nova Scotia, west of Chignecto Bay and north of the Cobequid Mountains. It is a one of eleven sub-basins of the Maritimes Basin. The geological Cumberland Basin is west of, and extends beneath, the maritime Cumberland Basin. Along the Nova Scotia shore of the lower Cumberland Basin at Joggins, Nova Scotia, Joggins are seaside cliffs known for fossil formations. Several coal seams are also exposed. These were mined commercially for Bituminous coal for nearly 140 years (1819–1958). The upper Cumberland loops clockwise, north of a flatland called Elysian Fields and southeast to Amherst Po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Fundy
The Bay of Fundy () is a bay between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state of Maine. It is an arm of the Gulf of Maine. Its tidal range is the highest in the world. The bay was named ''Bakudabakek'' by the indigenous Mi'kmaq and Passamaquoddy groups, meaning "open way". The Wolastoqiyik peoples named it ''Wekwabegituk'', meaning "waves at the head of the bay". The name "Fundy" has been speculated to have derived from the French word ("split") or ("head of the bay"). Some individuals have disputed this, including William Francis Ganong, who suggested that the name likely derived from Portuguese origin instead, specifically regarding João Álvares Fagundes, who may have referred to the bay as ("Great Bay") and nearby waters as ("deep river"). Hydrology Tides The tidal range in the Bay of Fundy is about ; the average tidal range worldwide is only . Some tides are higher than others, depending on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cabot Strait
Cabot Strait (; , ) is in Atlantic Canada between Cape Ray, Newfoundland, and Cape North, Cape Breton Island. The strait, approximately 110 kilometres wide, is the widest of the three outlets for the Gulf of Saint Lawrence into the Atlantic Ocean, the others being the Strait of Belle Isle and Strait of Canso. It is named for the Italian explorer Giovanni Caboto. Geography and geology Bathymetry The strait's bathymetry is varied, with the Laurentian Channel creating a deep trench through its centre, and comparatively shallow coastal waters closer to Newfoundland and Cape Breton Island. These bathymetric conditions have been known by mariners to cause rogue waves. The steep slope of the Laurentian Channel was the site of a disastrous submarine landslide at the southeastern end of the strait, triggered by the 1929 Grand Banks earthquake and leading to a tsunami that devastated communities along Newfoundland's south coast and parts of Cape Breton Island. St. Paul Islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumberland Strait
The Northumberland Strait (French: ''détroit de Northumberland'') is a strait in the southern part of the Gulf of Saint Lawrence in eastern Canada. The strait is formed by Prince Edward Island and the gulf's eastern, southern, and western shores. Boundaries The western boundary of the strait is delineated by a line running between North Cape, Prince Edward Island and Point Escuminac, New Brunswick while the eastern boundary is delineated by a line running between East Point, Prince Edward Island and Inverness, Nova Scotia. Hydrography The Northumberland Strait varies in depth between 17 and 65 metres, with the deepest waters at either end. The tidal patterns are complex; the eastern end has the usual two tides per day, with a tidal range of 1.2 to 1.8 metres, while the western end effectively has only one tide per day. The strait's shallow depths lend to warm water temperatures in summer months, with some areas reaching 25° C, or 77° F. Consequently, the strait is re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of St
A gulf is a large inlet from an ocean or their seas into a landmass, larger and typically (though not always) with a narrower opening than a bay (geography), bay. The term was used traditionally for large, highly indented navigable bodies of salt water that are enclosed by the coastline. Many gulfs are major shipping areas, such as the Persian Gulf, Gulf of Mexico, Gulf of Finland, and Gulf of Aden. See also * References External links * {{Geography-stub Gulfs, Bodies of water Coastal and oceanic landforms Coastal geography Oceanographical terminology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Appalachian Mountains
The Appalachian Mountains, often called the Appalachians, are a mountain range in eastern to northeastern North America. The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the Geological Survey of Canada to describe the respective countries' Physiographic region, physiographic regions. The U.S. uses the term Appalachian Highlands and Canada uses the term Appalachian Uplands; the Appalachian Mountains are not synonymous with the Appalachian Plateau, which is one of the provinces of the Appalachian Highlands. The Appalachian range runs from the Newfoundland (island), Island of Newfoundland in Canada, southwestward to Central Alabama in the United States; south of Newfoundland, it crosses the 96-square-mile (248.6 km2) archipelago of Saint Pierre and Miquelon, an overseas collectivity of France, meaning it is technica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary Period
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS), as well as the current and most recent of the twelve periods of the Phanerozoic eon. It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today); a proposed third epoch, the Anthropocene, was rejected in 2024 by IUGS, the governing body of the ICS. The Quaternary is typically defined by the Quaternary glaciation, the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Changes in atmospheric and associated radiative forcing were among the primary drivers of globally cold glacial and warm interglacial climates, with changes in ocean physical circulation, biological productivity and seawater acid-base chemistry likely causing most of the recorded changes Penultimate Glacial Period The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
