Brady Glacier is known for its beauty in the Fairweather Range of Alaska. Many people every year during the summer months visit the glaciers surrounding the gulf coast of Alaska to see their statuesque landforms. Brady Glacier is that of a serene landscape, but one of many glaciers that are retreating and becoming victim to ice calving. Geographers have been studying the interesting glaciations of Brady for centuries now. Three geographers, especially, are taking notice to the change in advance and retreat of the glacier. The location of Brady Glacier is significant to tourism because it is around other glaciers in Alaska and once one glacier starts to retreat, soon others will follow. Brady Glacier in the region of the North pacific Coast of Alaska is becoming a figure to ice calving and possible flooding in the surrounding land leading to the risk in tourism.
Landsat Project Science Officeat NASA’s Goddard Space Flight Center. Landsat Glacier Bay. 2003. USA. Visible Earth NASA. Web. 16. Mar. 2014.
The physical geography of the North Pacific Coast is not the greatest attraction to tourists in some cases, but the land itself is the winning prize that attracts many to its coast. Much of the North Pacific coast is covered in mountainous terrains that give the land its beauty. The land is very rugged when approaching the mountains and, “is a land of dramatic coastal mountains cut by glacially eroded fiords and islands,” (Birdsall). The rough terrain gives transportation in and around the region in the north difficulties resulting in the limitation of accessibility to only “air and water,” (Birdsall). “Brady Glacier is the largest glacier in the Fairweather Range of the St. Elias Mountain in southeast Alaska,” (Drendochology to the ...
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...Clague, John J., Luckman, Brian H., Wiles, Gregory C. “Tree-Ring Dating of the Nineteenth-Century Advance of Brady Glacier and the Evolution of Two Ice- Marginal Lakes, Alaska.” The Holocene 21.4 (2001): 641-649. Sage Journals. Web. 9. Feb. 2014.
Capps, D., Clague, J.J., Pelto, B., Pelto, M. “Rising ELA and Expanding Proglacial Lakes Lead to Initiation of Rapid Retreat of Brady Glacier, Alaska.” 69th Eastern Snow Conference. Nichols, 2012. Web. 9. Feb. 2014.
Derksen, Stephan J. Glacial Geology of the Brady Glacier Region, Alaska. Report No. 60. Ohio: Institute of Polar Studies and Department of Geology and Minerology, 1976. Print.
“Glacier Bay Flightseeing & Tours.” Fjord Flying Service. 2014. Web. 20. Feb. 2014.
“How Dangerous are Glaciers?: Glaciers Have Their Own Warning Signs.” Alaska Satellite Facility. University of Alaska Fairbanks, 2014. Web. 17. Feb. 2014.
This is a report based on three days of observations and testing in the region known as the Peterborough drumlin field. It will address a variety of regional elements, such as climate, soil, vegetation, hydrology, geomorphology, and geology. A variety of sites located on the Canadian Shield, the zone of thick glacial deposits to the south, and the transition between them will be the focus of the report. It is supplemented with previous research on the region. September 8, 1999, day one of the field study involved an area of largely granite bedrock that is part of the Canadian Shield and is the most northern point of study (see Map 2). September 9, 1999, day two, involved three main areas of study: the Bridgenorth esker (Map 3), Mark S. Burnham Park (Map 4), and the Rice Lake drumlin (Map 6). These sites are in areas of thick glacial deposits. September 10, 1999, day three, involved studying the Warsaw Caves (see Map 5) as a transition zone between Precambrian Shield rock to the north and Paleozoic rock to the south. A general map of the entire study region is provided by Map 1.
Before Lake Coeur d’Alene existed, the St. Joe River ran through the present lakebed northward and up through the Rathdrum Prairie before turning west and into the Spokane Valley. About 15,000 years ago, during the peak of the last glacial period, huge glaciers covered much of British Columbia. This ice, which was almost 4,000 feet thick, unimaginably covered all but the highest mountain peaks. The glacier slowly crept down into North Idaho, stopping just north of Coeur d’Alene (Wuerthner, 30, 32).
Glaciers are an integral part of the world’s climate. In fact, as Richard Armstrong of the University of Colorado says, “Glaciers are key indicators in monitoring and detecting climate change” (Univ. of Colorado, Boulder, 2003, p. 1). Not only are they an important part of monitoring current climate, they can hold many keys to the past. Glaciers are in fact, “a source of paleoclimate data…” (Meier and Dyurgerov, 1980, p. 37). This paleoclimate data can give geologists information on the conditions that were present at the time of the glaciers birth, as well as the approximate age. This has an important role in the geologic time scale of the Colorado Rocky Mountains. These Glaciers played a role in the carving of the present day Rocky Mountains in Colorado, which will be the primary focus of this paper. In addition, glacial formations will be discussed to give the reader background information and the future of the Glaciers in Colorado will close this paper.
About fifty miles long, along the coast of southern Alaska lay a scenic destination. A bay filled with glaciers that tell
Lake effect snow was not a quick discovery compared to other forms of weather. In the 1800’s when there was no satellites or weather radar to track a storm, early day forecasters would have to get observations from spotters across the country and provide a one and two day forecast on the type of weather that may ...
Americas by 14,000 ago” (O’Brien 12), after large portions of North America encountered the last ice age, which
...e Palaeo-Eskimo Prehistory of the North Devon Lowlands'. Arctic, vol. 44(no. 4), pp. 301-317 [Online]. Available at: http://pubs.aina.ucalgary.ca/arctic/Arctic44-4-301.pdf [Accessed 10 December 2013].
Glaciers flow through three different mechanisms: (1) by internal deformation; (2) by basal sliding; and (3) by subglacial deformation.
Schultz, Cathy. "Cold Mountain." University of St. Francis - Joliet, Il. Web. 10 Jan. 2012. http://www.stfrancis.edu/content/historyinthemovies/coldmountain.htm
One of the most striking features in Glacier National Park is the color banding. This feature can be seen in nearly every mountain within the park as they are composed of different layers of rocks and colors. The rock strata are mainly composed of sedimentary rocks limestones, shales, sandstones, and lightly metamorphosed rocks (Dyson,1957). These rocks all belong to a single large unit known as the Belt series. The rocks are very unusual in that they were deposited in late in the Precambrian between 1600 and 800 million years ago and are relatively undeformed and only lightly metamorphosed (Alt, 1983). The rocks can be spotted throughout the large area of western Montana, northern Idaho, and southern British Columbia. The formation of the Belt Supergroup started during the Proterozoic era as a long narrow section of North America extending from the Arctic Ocean southward which slowly sank to form a large sea-filled trough also known as a geosyncline (Dyson, 1957). Streams from nearby lands carried muds and sands into the sea almost completely filling it. These muds were eventually compressed into shales, some limestones, and sands into sandstones. Many of the rocks in this series have very distinct features that give a clue about their origin, features suc...
"What to Do at Denali - National Geographic." Travel & Cultures -- National Geographic. N.p., n.d. Web. 28 Feb. 2012. .
Both Allen (2008) and Hoffman (1998) then thought that the glaciation ended fast due to very high levels of carbon dioxide. According to Hoffman (1998) the carbon dioxide levels got higher because of release ...
The foundation of the Great Lakes began around three billion years ago, which is known as the Precambrian Era. The Precambrian Era contains numerous ecological events, which consists of volcanic activity to erosion to the mountains and hills seen today being formed. Then during the Pleistocene Epoch or known as the “Ice Age, occurred between 1.6 million and 10,000 years ago. At least four times during the Pleistocene Epoch, large masses of ice advanced and retreated over the surface of what is now North America. As the glaciers advanced, giant sheets of ice flowed across the land, leveling mountains and carving out massive ...
Glaciers have disappeared due to increasing in global temperatures because of which the water level had drastically increased and its causing flood all over the world