|
Tobeatic Wilderness Area
The Tobeatic Wilderness Area is the largest protected area in the Canadian Maritimes, located in southwestern Nova Scotia. It contains nearly 120,000 hectares of land and spans parts of five counties, Annapolis, Digby, Queens, Shelburne and Yarmouth.Tobeatic Wilderness Area Government of Nova Scotia Located adjacent to , it was formerly known as the Tobeatic Wildlife Management Area, and the Tobeatic Game Reserve. History The name Tobeatic is derived from "Place of the Alder" in the Mi'kmaq language.[...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] |
Esker
An esker, eskar, eschar, or os, sometimes called an ''asar'', ''osar'', or ''serpent kame'', is a long, winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions of Europe and North America. Eskers are frequently several kilometres long and, because of their uniform shape, look like railway embankments. Etymology The term ''esker'' is derived from the Irish word ''eiscir'' ( Old Irish: ''escir''), which means "ridge or elevation, especially one separating two plains or depressed surfaces". The Irish word was and is used particularly to describe long sinuous ridges, which are now known to be deposits of fluvio-glacial material. The best-known example of such an ''eiscir'' is the '' Eiscir Riada'', which runs nearly the whole width of Ireland from Dublin to Galway, a distance of , and is still closely followed by the main Dublin-Galway road The synonym ''os'' comes from the Swedish word ''ås'', "ridge". Geology Most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shelburne River
The Shelburne River is a 53 km long river in Nova Scotia, Canada. It is a wilderness river and is a tributary of Mersey River. It starts in the Tobeatic Wilderness Area. The Shelburne River was designated a Canadian Heritage River The Canadian Heritage Rivers System (CHRS; french: Le réseau de rivières du patrimoine canadien) is a joint program administered by the federal, provincial and territorial governments to conserve and protect the best examples of Canada's river he ... in 1997. See also * List of rivers of Nova Scotia References Canadian Heritage Rivers SystemGovernment of Nova Scotia Rivers of Nova Scotia Canadian Heritage Rivers {{NovaScotia-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White-tailed Deer
The white-tailed deer (''Odocoileus virginianus''), also known as the whitetail or Virginia deer, is a medium-sized deer native to North America, Central America, and South America as far south as Peru and Bolivia. It has also been introduced to New Zealand, all the Greater Antilles in the Caribbean (Cuba, Jamaica, Hispaniola, and Puerto Rico), and some countries in Europe, such as the Czech Republic, Finland, France, Germany, Romania and Serbia. In the Americas, it is the most widely distributed wild ungulate. In North America, the species is widely distributed east of the Rocky Mountains as well as in southwestern Arizona and most of Mexico, except Lower California. It is mostly displaced by the black-tailed or mule deer (''Odocoileus hemionus'') from that point west except for mixed deciduous riparian corridors, river valley bottomlands, and lower foothills of the northern Rocky Mountain region from Wyoming west to eastern Washington and eastern Oregon and north to nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Moose
The eastern moose (''Alces alces americana'') is a subspecies of moose that currently ranges throughout Eastern Canada, New England and northern New York State. It inhabits boreal forests and mixed deciduous forests. It is the third largest North American subspecies, after the western moose and the Alaskan moose. Males are aggressive during mating season and will attack anything that provokes them. Distribution The eastern moose's range spans a broad swath of northeastern North America, which includes New Brunswick, Newfoundland and Labrador (while it is native to Labrador, it was introduced to Gander Bay, Newfoundland in 1878 and to Howley, NF in 1904), Nova Scotia, Quebec, Eastern Ontario, Maine, New Hampshire, Vermont, Massachusetts, Connecticut, and northern New York. The moose that roam in Cape Breton Highlands National Park are descended from the western moose that originated from Alberta's Elk Island National Park. The population and range of the eastern moose increa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monzogranite
Monzogranites are biotite granite rocks that are considered to be the final fractionation product of magma. Monzogranites are characteristically felsic (SiO2 > 73%, and FeO + MgO + TiO2 < 2.4), weakly peraluminous (Al2O3/ (CaO + Na2O + K2O) = 0.98–1.11), and contain , sphene, and as accessory s. Although the com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biotite
Biotite is a common group of phyllosilicate minerals within the mica group, with the approximate chemical formula . It is primarily a solid-solution series between the iron- endmember annite, and the magnesium-endmember phlogopite; more aluminous end-members include siderophyllite and eastonite. Biotite was regarded as a mineral ''species'' by the International Mineralogical Association until 1998, when its status was changed to a mineral ''group''. The term ''biotite'' is still used to describe unanalysed dark micas in the field. Biotite was named by J.F.L. Hausmann in 1847 in honor of the French physicist Jean-Baptiste Biot, who performed early research into the many optical properties of mica. Members of the biotite group are sheet silicates. Iron, magnesium, aluminium, silicon, oxygen, and hydrogen form sheets that are weakly bound together by potassium ions. The term "iron mica" is sometimes used for iron-rich biotite, but the term also refers to a flaky mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halifax Formation
Halifax commonly refers to: *Halifax, Nova Scotia, Canada *Halifax, West Yorkshire, England * Halifax (bank), a British bank Halifax may also refer to: Places Australia *Halifax, Queensland, a coastal town in the Shire of Hinchinbrook *Halifax Bay, a bay south of the town of Halifax Canada Nova Scotia *Halifax, Nova Scotia, the capital city of the province **Downtown Halifax **Halifax Peninsula, part of the core of the municipality **Mainland Halifax, a region of the municipality *Halifax (electoral district), a federal electoral district *Halifax (provincial electoral district), a provincial electoral district **Halifax County, Nova Scotia, the county dissolved into the regional municipality in 1996 * Halifax Harbour, a saltwater harbour * Halifax West, a federal electoral district since 1979 Prince Edward Island *Halifax Parish, Prince Edward Island British Columbia * Halifax Range, a mountain range United Kingdom *Halifax, West Yorkshire, England **Halifax (UK Parliament ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goldenville Formation
Goldenville is a small community located near to Sherbrooke, Nova Scotia in the Municipality of the District of St. Mary's. The community is mainly a forestry community but also has a gold mining museum. History Nelson Nickerson found gold in the Goldenville area in August, 1861 and Zeba Hewitt built one of the first houses in the village that fall. By July, 1862, several houses had been erected in Goldenville and mining was begun. Two wharves were built the following spring and a road was constructed to the diggings. In 1867 the Templars erected a hall that was also used as a church. An Orange Order Lodge Hall was built in 1869 and the lower part was used as a schoolroom. A Masonic Lodge Hall was also built in 1869. A Roman Catholic chapel was built in Goldenville in 1871, but was moved to Sherbrooke in 1907. A Presbyterian church was opened in Goldenville on January 12, 1902. Gold production in Goldenville from 1862 to 1941 is reported to have been 209,383.3 oz., the best pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kettle (landform)
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluvi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
