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Bottle Cove, Newfoundland And Labrador
Bottle Cove is located on the west coast of Newfoundland. It opens directly onto the Gulf of Saint Lawrence, although it is typically included in the regional descriptor, "Bay of Islands," which lies at the mouth of the Humber Arm. Bottle Cove is also referred to as Bottle Cove Provincial Park and as Bottle Cove Day Park (no amenities) in official Parks documentation. Bottle Cove lies in the Newfoundland Time Zone (UTC−3.5) and observes daylight saving time. Newfoundland is considered to have a humid continental climate. Winter day temperatures in the area of Bottle Cove tend to average 0 degrees C (32 degrees Fahrenheit). Summer has an average day temperature of around 16 °C (61°Fahrenheit). Bottle Cove is a popular spot with locals and tourists alike, and it is renowned for its rugged, pristine beauty. History There is little specific written documentation available regarding the history of Bottle Cove. Small evidence of possible use by members of the Little Passage ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newfoundland (island)
Newfoundland (, ; french: link=no, Terre-Neuve, ; ) is a large island off the east coast of the North American mainland and the most populous part of the Canadian province of Newfoundland and Labrador. It has 29 percent of the province's land area. The island is separated from the Labrador Peninsula by the Strait of Belle Isle and from Cape Breton Island by the Cabot Strait. It blocks the mouth of the Saint Lawrence River, creating the Gulf of Saint Lawrence, the world's largest estuary. Newfoundland's nearest neighbour is the French overseas collectivity of Saint Pierre and Miquelon. With an area of , Newfoundland is the world's 16th-largest island, Canada's fourth-largest island, and the largest Canadian island outside the North. The provincial capital, St. John's, is located on the southeastern coast of the island; Cape Spear, just south of the capital, is the easternmost point of North America, excluding Greenland. It is common to consider all directly neighbouring i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newfoundland Outport
An outport is the term given for a small coastal community in the Canadian province of Newfoundland and Labrador other than the chief port of St. John's. Originally, the term was used for coastal communities on the island of Newfoundland, but the term has now been adopted for those on the mainland area of Labrador as well. History Outports are some of the oldest European settlements in Canada. Giovanni Caboto (known by his English sponsors as John Cabot) visited Newfoundland or Cape Breton Island in 1497; and news spread quickly that Cabot had caught cod by simply lowering and lifting a weighted basket. Gaspar Corte-Real of Portugal visited Newfoundland in 1500, and by 1506 the catch from the Grand Banks of Newfoundland encouraged the King of Portugal to impose a ten percent import tariff to protect local fishermen. The first recorded French fishing boat on the Grand Banks was in 1504, Basque whalers arrived in 1527, and Spanish fishermen followed by 1540. A lot of fishin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Head, Bay Of Islands
South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz'' ("south"), possibly related to the same Proto-Indo-European root that the word ''sun'' derived from. Some languages describe south in the same way, from the fact that it is the direction of the sun at noon (in the Northern Hemisphere), like Latin meridies 'noon, south' (from medius 'middle' + dies 'day', cf English meridional), while others describe south as the right-hand side of the rising sun, like Biblical Hebrew תֵּימָן teiman 'south' from יָמִין yamin 'right', Aramaic תַּימנַא taymna from יָמִין yamin 'right' and Syriac ܬܰܝܡܢܳܐ taymna from ܝܰܡܝܺܢܳܐ yamina (hence the name of Yemen, the land to the south/right of the Levant). Navigation By convention, the ''bottom or down-facing side'' of a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Resources Canada
Natural Resources Canada (NRCan; french: Ressources naturelles Canada; french: RNCan, label=none)Natural Resources Canada is the applied title under the Federal Identity Program; the legal title is Department of Natural Resources (). is the department of the Government of Canada responsible for natural resources, energy, minerals and metals, forests, earth sciences, mapping, and remote sensing. It was formed in 1994 by amalgamating the Department of Energy, Mines and Resources with the Department of Forestry. Under the ''Constitution Act, 1867'', primary responsibility for natural resources falls to provincial governments, however, the federal government has jurisdiction over off-shore resources, trade and commerce in natural resources, statistics, international relations, and boundaries. The department administers federal legislation relating to natural resources, including energy, forests, minerals and metals. The department also collaborates with American and Mexican governme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wave Cut Platform
A wave-cut platform, shore platform, coastal bench, or wave-cut cliff is the narrow flat area often found at the base of a sea cliff or along the shoreline of a lake, bay, or sea that was created by erosion. Wave-cut platforms are often most obvious at low tide when they become visible as huge areas of flat rock. Sometimes the landward side of the platform is covered by sand, forming the beach, and then the platform can only be identified at low tides or when storms move the sand. __TOC__ Formation Wave-cut platforms form when destructive waves hit against the cliff face, causing an undercut between the high and low water marks, mainly as a result of abrasion, corrosion and hydraulic action, creating a wave-cut notch. This notch then enlarges into a cave. The waves undermine this portion until the roof of the cave cannot hold due to the pressure and freeze-thaw or biological weathering acting on it, and collapses, resulting in the cliff retreating landward. The base of the cav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pillow Lava
Pillow lavas are lavas that contain characteristic pillow-shaped structures that are attributed to the extrusion of the lava underwater, or ''subaqueous extrusion''. Pillow lavas in volcanic rock are characterized by thick sequences of discontinuous pillow-shaped masses, commonly up to one meter in diameter. They form the upper part of Layer 2 of normal oceanic crust. Composition Pillow lavas are commonly of basaltic composition, although pillows formed of komatiite, picrite, boninite, basaltic andesite, andesite, dacite or even rhyolite are known. In general, the more felsic the composition (richer in silica - resulting in an Intermediate composition), the larger the pillows, due to the increase in viscosity of the erupting lava. Occurrence They occur wherever lava is extruded underwater, such as along marine hotspot volcano chains and the constructive plate boundaries of mid-ocean ridges. As new oceanic crust is formed, thick sequences of pillow lavas are erupted at the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ophiolite
An ophiolite is a section of Earth's oceanic crust and the underlying upper mantle that has been uplifted and exposed above sea level and often emplaced onto continental crustal rocks. The Greek word ὄφις, ''ophis'' (''snake'') is found in the name of ophiolites, because of the superficial texture of some of them. Serpentinite especially evokes a snakeskin. The suffix ''lite'' from the Greek ''lithos'' means "stone". Some ophiolites have a green color. The origin of these rocks, present in many mountainous massifs, remained uncertain until the advent of plate tectonic theory. Their great significance relates to their occurrence within mountain belts such as the Alps and the Himalayas, where they document the existence of former ocean basins that have now been consumed by subduction. This insight was one of the founding pillars of plate tectonics, and ophiolites have always played a central role in plate tectonic theory and the interpretation of ancient mountain belts. Pse ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allochthon
upright=1.6, Schematic overview of a thrust system. The hanging wall block is (when it has reasonable proportions) called a nappe. If an erosional hole is created in the nappe that is called a window (geology)">window. A klippe is a solitary outcrop of the nappe in the middle of autochthonous material. An allochthon, or an allochthonous block, is a large block of rock which has been moved from its original site of formation, usually by low angle thrust faulting. An allochthon which is isolated from the rock that pushed it into position is called a klippe. If an allochthon has a "hole" in it so that one can view the autochthon (geology), autochthon beneath the allochthon, the hole is called a "window" (or Fenster). Etymology: Greek; 'allo' = other, and 'chthon' = earth. In generalized terms, the term is applied to any geologic units that originated at a distance from their present location For comparison, see also Autochthon. In the United States there are three notable al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Appalachian Mountains
The Appalachian Mountains, often called the Appalachians, (french: Appalaches), are a system of mountains in eastern to northeastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period. They once reached elevations similar to those of the Alps and the Rocky Mountains before experiencing natural erosion. The Appalachian chain is a barrier to east–west travel, as it forms a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. Definitions vary on the precise boundaries of the Appalachians. The United States Geological Survey (USGS) defines the ''Appalachian Highlands'' physiographic division as consisting of 13 provinces: the Atlantic Coast Uplands, Eastern Newfoundland Atlantic, Maritime Acadian Highlands, Maritime Plain, Notre Dame and Mégantic Mountains, Western Newfoundland Mountains, Piedmont, Blue Ridge, Valley and Ridge, St. Lawrence Valley, Appalac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corner Brook
Corner Brook ( 2021 population: 19,333 CA 29,762) is a city located on the west coast of the island of Newfoundland in the province of Newfoundland and Labrador, Canada. Corner Brook is the fifth largest settlement in Newfoundland and Labrador. Located on the Bay of Islands at the mouth of the Humber River, the city is the second-largest population centre in the province behind St. John's, and smallest of three cities behind St. John's and Mount Pearl. As such, Corner Brook functions as a service centre for western and northern Newfoundland. It is located on the same latitude as Gaspé, Quebec, a city of similar size and landscape on the other side of the Gulf of St. Lawrence. Corner Brook is the most northern city in Atlantic Canada. It is the administrative headquarters of the Qalipu Mi'kmaq First Nations band government. The Mi'kmaq name for the nearby Humber River is "Maqtukwek". History The area was surveyed by Captain James Cook in 1767. The Captain James Cook Hist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Newfoundland And Labrador Route 450
Route 450 (also known as Captain Cook's Trail) is a highway in the Canadian province of Newfoundland and Labrador. The highway starts at an interchange at Route 1 (Trans-Canada Highway) in Corner Brook. When approaching O'Connell Drive, motorists can turn left to continue their journey along the route. The route terminates at a cul-de-sac in Lark Harbour. Route 450 made headlines in Newfoundland in January 2018 when massive rainfall caused flooding on January 13 and created a huge crater causing a large portion in the highway to collapse, thus separating residents in Lark Harbour and York Harbour from the remainder of the island. The impacted portion of the road was reopened to traffic on January 17, 2018. Route description Route 450 begins in Corner Brook at an interchange with Route 1 (Trans-Canada Highway, Exit 4), with the road continuing northeast as Massey Drive to the town of the same name. It heads west along the southern edge of the city to have an intersection ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
