000928976 000__ 04047cam\a2200469Ii\4500 000928976 001__ 928976 000928976 005__ 20230306151326.0 000928976 006__ m\\\\\o\\d\\\\\\\\ 000928976 007__ cr\nn\nnnunnun 000928976 008__ 200227s2020\\\\sz\a\\\\o\\\\\000\0\eng\d 000928976 019__ $$a1141215828$$a1141510417$$a1142996362 000928976 020__ $$a9783030351373$$q(electronic book) 000928976 020__ $$a3030351378$$q(electronic book) 000928976 020__ $$z9783030351359 000928976 020__ $$z3030351351 000928976 0248_ $$a10.1007/978-3-030-35 000928976 035__ $$aSP(OCoLC)on1142371323 000928976 035__ $$aSP(OCoLC)1142371323$$z(OCoLC)1141215828$$z(OCoLC)1141510417$$z(OCoLC)1142996362 000928976 040__ $$aLQU$$beng$$cLQU$$dGW5XE$$dYDX$$dEBLCP 000928976 043__ $$an-cn--- 000928976 049__ $$aISEA 000928976 050_4 $$aGB428.5.C2 000928976 08204 $$a551.41 000928976 24500 $$aLandscapes and landforms of Eastern Canada /$$cOlav Slaymaker, Norm Catto, editors. 000928976 264_1 $$aCham :$$bSpringer,$$c2020. 000928976 300__ $$a1 online resource (xvi, 596 pages) :$$billustrations. 000928976 336__ $$atext$$btxt$$2rdacontent 000928976 337__ $$acomputer$$bc$$2rdamedia 000928976 338__ $$aonline resource$$bcr$$2rdacarrier 000928976 4901_ $$aWorld Geomorphological Landscapes Ser. 000928976 5050_ $$aGeomorphological landscapes of Eastern Canada: general overview -- Case studies, with at least one outstanding example from each of the major physiographic regions -- Geomorphological landscapes as heritage. 000928976 506__ $$aAccess limited to authorized users. 000928976 520__ $$aThis is the only book to focus on the geomorphological landscapes of eastern Canada and provides a companion volume to "Landscapes and Landforms of Western Canada" (2017). There are a number of unique characteristics of eastern Canadas landscapes, notably its magnificent coastlines, the extraordinary variety and extent of wetlands, the huge Great Lakes-St. Lawrence basin, the high incidence of meteorite craters , the spectacular Niagara Falls, urban karst in Montreal and Ottawa, youthful, glaciated karst in Ontario, Newfoundland, Quebec and Nova Scotia, the ubiquitous permafrost terrain of Nunavut, Labrador and northern Quebec and the magnificent arctic fjords and glaciers. Looking at coastlines, the tidal extremes of the Bay of Fundy are world renowned; the structural complexity of the island of Newfoundland is less well known, but produces an astounding variety of coastlines in close succession; the arctic fjordlands of Baffin and Ellesmere islands and the extravagant raised beaches of Hudson Bay bear comparison with the classic fjords of Norway and the Baltic Sea raised beaches. As for wetlands there are distinctive Arctic, Subarctic, Boreal, Eastern Temperate and Atlantic wetlands and their extent is second only to those of Russia. In the Hudson and James bay regions between 75-100% of the terrestrial surface is comprised of wetlands. One of North Americas largest river basins, the Great Lakes-St. Lawrence basin, has its source in Minnesota, straddles the USA-Canada border and debouches into Quebec as the St. Lawrence River and evolves through its estuary into the Gulf of St. Lawrence, a journey of almost 5,000 km. As far as meteorite craters are concerned, 10% of the worlds total are located in eastern Canada, including some of the largest and most complex. They are preserved preferentially in the ancient Shield terrain of Quebec. Finally, the three million kmĀ² of permafrost controlled relief in eastern Canada serves as a reminder of the vulnerabi lity of eastern Canadas landscapes to climate change. Effects of warming are expressed through thaw]ing of the permafrost, disruption of transportation corridors and urban construction problems, ever-present geomorphic hazards. 000928976 650_0 $$aGeomorphology$$zCanada. 000928976 7001_ $$aSlaymaker, Olav,$$d1939- 000928976 7001_ $$aCatto, Norm,$$d1956- 000928976 77608 $$iPrint version: $$z3030351351$$z9783030351359$$w(OCoLC)1123181870 000928976 830_0 $$aWorld Geomorphological Landscapes Ser. 000928976 852__ $$bebk 000928976 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-030-35137-3$$zOnline Access$$91397441.1 000928976 909CO $$ooai:library.usi.edu:928976$$pGLOBAL_SET 000928976 980__ $$aEBOOK 000928976 980__ $$aBIB 000928976 982__ $$aEbook 000928976 983__ $$aOnline 000928976 994__ $$a92$$bISE