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Yamnuska Mountain
Mount John Laurie is a mountain in the Canadian Rockies, in Alberta's Municipal District of Bighorn No. 8. Various names Officially named Mount John Laurie in 1961, it is also known as Mount Laurie, or by its original Stoney Nakoda name ''Îyâmnathka'', borrowed into English as Mount Yamnuska or simply Yamnuska. is a compound that includes root words meaning "mountain" and "flat", however it is usually translated more figuratively as "flat-faced mountain". John Lee Laurie, 1899–1959, was a founder of the Indian Association of Alberta. The mountain's 1961 renaming came at the request of the Stoney Nakoda First Nation. Laurie, an educator and political activist, served as secretary of the Indian Association of Alberta from 1944 to 1956, promoting the causes of First Nations in Alberta. Peak and climbing Standing at approximately above sea level, Mount John Laurie is the last mountain on the north side of the Bow River valley (Bow Valley) as it exits the mountains for t ...
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Canadian Rockies
The Canadian Rockies () or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part of the Canadian Cordillera, which is the northern segment of the North American Cordillera, the expansive system of interconnected mountain ranges between the Interior Plains and the Pacific Coast that runs northwest–southeast from central Alaska to the Isthmus of Tehuantepec in Mexico. Canada officially defines the Rocky Mountains system as the mountain chains east of the Rocky Mountain Trench extending from the Liard River valley in northern British Columbia to the Albuquerque Basin in New Mexico, not including the Mackenzie, Richardson and British Mountains/ Brooks Range in Yukon and Alaska (which are all included as the "Arctic Rockies" in the United States' definition of the Rocky Mountains system). The Canadian Rockies, being the northern segment of ...
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Rock Climbing
Rock climbing is a climbing sports discipline that involves ascending climbing routes, routes consisting of natural rock in an outdoor environment, or on artificial resin climbing walls in a mostly indoor environment. Routes are documented in climbing guidebook, guidebooks, and on online databases, detailing how to climb the route (called the beta (climbing), beta), and who made the first ascent (or FA) and the coveted First ascent#In rock climbing, first free ascent (or FFA). Climbers will try to ascend a route onsight, however, a climber can spend years projecting (climbing), projecting a route before they make a redpoint (climbing), redpoint ascent. Routes range from a few metres to over a in height, and traverse (climbing), traverses can reach in length. They include slab climbing, slabs, face climbing, faces, crack climbing, cracks and overhang (climbing), overhangs/roofs. Popular rock types are granite (e.g. El Capitan), limestone (e.g. Verdon Gorge), and sandstone (e ...
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Scrambles In The Canadian Rockies
''Scrambles in the Canadian Rockies'' is a climbing guidebook by Alan Kane describing scrambling routes of mountains in the Canadian Rockies. It is published by Rocky Mountain Books, located in Calgary, Alberta Alberta is a Provinces and territories of Canada, province in Canada. It is a part of Western Canada and is one of the three Canadian Prairies, prairie provinces. Alberta is bordered by British Columbia to its west, Saskatchewan to its east, t .... The third edition , released in May 2016, has been updated and contains route descriptions for 175 peaks. The peaks are rated from easy to difficult and information on trail heads and the standard routes are covered. '' Backpacker'' magazine has twice featured the book as an expedition guide. The '' Canadian Alpine Journal'' referred to it as a "scree gospel". The book is solely responsible for creating a widespread interest in scrambling up mountain peaks, whether the peaks are in USA or Western Canada. Since first publishe ...
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Pyramids Of Chichen Itza
Chichén Itzá , , often with the emphasis reversed in English to ; from () "at the mouth of the well of the Itza people" (often spelled ''Chichen Itza'' in English and traditional Yucatec Maya) was a large pre-Columbian city built by the Maya people of the Terminal Classic period. The archeological site is located in Tinúm Municipality, Yucatán State, Mexico. Chichén Itzá was a major focal point in the Northern Maya Lowlands from the Late Classic ( AD 600–900) through the Terminal Classic ( AD 800–900) and into the early portion of the Postclassic period ( AD 900–1200). The site exhibits a multitude of architectural styles, reminiscent of styles seen in central Mexico and of the Puuc and Chenes styles of the Northern Maya lowlands. The presence of central Mexican styles was once thought to have been representative of direct migration or even conquest from central Mexico, but most contemporary interpretations view the presence of these non-Maya styles more a ...
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Uluru
Uluru (; ), also known as Ayers Rock ( ) and officially gazetted as UluruAyers Rock, is a large sandstone monolith. It outcrop, crops out near the centre of Australia in the southern part of the Northern Territory, south-west of Alice Springs. Uluru is sacred to the Pitjantjatjara, the Aboriginal Australians, Aboriginal people of the area, known as the Aṉangu. The area around the formation is home to an abundance of springs, depression (geology), waterholes, rock caves and cave painting, ancient paintings. Uluru is listed as a UNESCO World Heritage Site. Uluru and Kata Tjuta (Also known as the Olgas) are the two major features of the Uluṟu-Kata Tjuṯa National Park. Uluru is one of Australia's most recognisable natural landmarks and has been a popular destination for tourists since the late 1930s. It is also one of the most important indigenous sites in Australia. Name The local Aṉangu, the Pitjantjatjara people, call the landmark ''Uluṟu'' (). This word is a pro ...
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Machu Picchu
Machu Picchu is a 15th-century Inca citadel located in the Eastern Cordillera of southern Peru on a mountain ridge at . Often referred to as the "Lost City of the Incas", it is the most familiar icon of the Inca Empire. It is located in the Machupicchu District within the Urubamba Province above the Sacred Valley, which is northwest of the city of Cusco. The Urubamba River flows past it, cutting through the Cordillera and creating a canyon with a subtropical mountain climate. The Inca civilization had no written language and following the first encounter by the Spanish soldier Baltasar Ocampo, no Europeans are recorded to have visited the site from the late 16th century until the 19th century. As far as historical knowledge extends, there are no existing written records detailing the site during its period of active use. The leading theory is that Machu Picchu was a private city for Incan royalty. The names of the buildings, their supposed uses, and their inhabitants, ...
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Mount Shasta
Mount Shasta ( ; Shasta people, Shasta: ''Waka-nunee-Tuki-wuki''; Karuk language, Karuk: ''Úytaahkoo'') is a Volcano#Volcanic activity, potentially active stratovolcano at the southern end of the Cascade Range in Siskiyou County, California. At an elevation of , it is the second-highest peak in the Cascades and the List of California fourteeners, fifth-highest in the state. Mount Shasta has an estimated volume of , which makes it the most voluminous stratovolcano in the Cascade Volcanoes, Cascade Volcanic Arc. The mountain and surrounding area are part of the Shasta–Trinity National Forest. Description The origin of the name "Shasta people#Origin of name, Shasta" is vague, either derived from a Shasta people, people of a name like it or otherwise garbled by early Westerners. Mount Shasta is connected to its satellite cone of Shastina, and together they dominate the landscape. Shasta rises abruptly to tower nearly above its surroundings. On a clear winter day, the mountain ...
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Stonehenge
Stonehenge is a prehistoric Megalith, megalithic structure on Salisbury Plain in Wiltshire, England, west of Amesbury. It consists of an outer ring of vertical sarsen standing stones, each around high, wide, and weighing around 25 tons, topped by connecting horizontal lintel stones, held in place with mortise and tenon joints, a feature unique among contemporary monuments. Inside is a ring of smaller bluestones. Inside these are free-standing trilithons, two bulkier vertical sarsens joined by one lintel. The whole monument, now ruinous, is aligned towards the sunrise on the summer solstice and sunset on the winter solstice. The stones are set within Earthwork (archaeology), earthworks in the middle of the densest complex of Neolithic British Isles, Neolithic and Bronze Age Britain, Bronze Age monuments in England, including several hundred ''tumuli'' (burial mounds). Stonehenge was constructed in several phases beginning about 3100 BC and continuing until about 1600 B ...
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Mount Fuji
is an active stratovolcano located on the Japanese island of Honshu, with a summit elevation of . It is the highest mountain in Japan, the second-highest volcano on any Asian island (after Mount Kerinci on the Indonesian island of Sumatra), and List of islands by highest point, seventh-highest peak of an island on Earth. Mount Fuji Hōei eruption, last erupted from 1707 to 1708. It is located about southwest of Tokyo, from where it is visible on clear days. Its exceptionally symmetrical cone, which is snow field, covered in snow for about five months of the year, is a Japanese cultural icon and is frequently depicted in art and photography, as well as visited by sightseers, hikers and mountain climbers. Mount Fuji is one of Japan's along with Mount Tate and Mount Haku. It is a List of Special Places of Scenic Beauty, Special Historic Sites and Special Natural Monuments, Special Place of Scenic Beauty and one of Japan's Monuments of Japan, Historic Sites. It was added to th ...
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Belly River Formation
The Belly River Group is a stratigraphic unit of Late Cretaceous age in the Western Canadian Sedimentary Basin. It takes the name from the Belly River, a tributary of the Oldman River in southern Alberta, and was first described in outcrop on the banks of the Oldman River (at the time considered part of the Belly River) and Bow River by George Mercer Dawson in 1883.Dawson, G.M., 1883. Preliminary report on the geology of the Bow and Belly river region, Northwest Territory, with special reference to the coal deposits. Geological Survey of Canada, Report of Progress for 1880-81-82, Part B. Lithology The Belly River Group is composed of very fine grained sandstone with coarse grained beds and minor bentonite, coal, green shale, and concretionary beds. Hydrocarbon production Gas is produced from the Belly River Group in the Deep Basin, in west-central Alberta and in the Canadian Rockies foothills. Paleofauna Dinosaur remains are among the fossils that have been recovered from ...
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Clastic
Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus,Essentials of Geology, 3rd Ed, Stephen Marshak, p. G-3 chunks, and smaller grains of rock broken off other rocks by physical weathering.Essentials of Geology, 3rd Ed, Stephen Marshak, p. G-5 Geologists use the term clastic to refer to sedimentary rocks and particles in sediment transport, whether in Suspension (chemistry), suspension or as bed load, and in sediment deposits. Sedimentary clastic rocks Clastic sedimentary rocks are rocks composed predominantly of broken pieces or ''clasts'' of older weathering, weathered and erosion, eroded rocks. Clastic sediments or sedimentary rocks are classified based on grain size, clast and cementing material (Matrix (geology), matrix) composition, and texture. The classification factors are often useful in determining a sample's Sedimentary depositional environment, environment of deposition. An example of cla ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ...
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