UNESCO Biosphere Reserves are environment-protected scientific-research institutions of international status that are created with the intent for conservation in a natural state the most typical natural complexes of biosphere, conducting background ecological monitoring, studying of the surrounding natural environment, its changes under the activity of anthropogenic factors.
Waterton Lakes National Park is in the southwest corner of Alberta, Canada. The national park borders Glacier National Park in Montana, United States. Waterton was the fourth Canadian national park, formed in 1895 as Kootenay Lakes Forest Reserve. It is named after Waterton Lake, in turn after the Victorian naturalist and conservationist Charles Waterton. Its range is between the Rocky Mountains and prairies. This park contains 505 km2 (195 sq mi) of rugged mountains and wilderness. It has a diverse ecosystem.
The San Francisco Peaks are a volcanic mountain range in the San Francisco volcanic field in north central Arizona, just north of Flagstaff and a remnant of the former San Francisco Mountain. The highest summit in the range, Humphreys Peak, is the highest point in the state of Arizona at 12,637 feet (3,852 m) in elevation. The San Francisco Peaks are the remains of an eroded stratovolcano. An aquifer within the caldera supplies much of Flagstaff's water while the mountain itself is in the Coconino National Forest, a popular recreation site. The Arizona Snowbowl ski area is on the western slopes of Humphreys Peak, and has been the subject of major controversy involving several tribes and environmental groups.
The Rocky Mountains subalpine zone is the biotic zone immediately below tree line in the Rocky Mountains of North America. In northern New Mexico, the subalpine zone occupies elevations approximately from 9,000 to 12,000 feet ; while in northern Alberta, the subalpine zone extends from 1,350 to 2,300 metres.
Waterton Lake is a mountain lake in southern Alberta, Canada, and northern Montana, United States. The lake is composed of two bodies of water, connected by a shallow channel known locally as the Bosporus. The two parts are referred to as Middle Waterton Lake, and Upper Waterton Lake, the latter of which is divided by the Canada–United States border with Canada containing about two thirds of the lake while the southern third falls in the United States. The Boundary Commission Trail ends at the lake as the last border marker was placed there on 8 August 1874. The United States Geological Survey gives the geocoordinates of 49°03′00″N113°54′03″W for Upper Waterton Lake. Lower Waterton Lake is north of Middle Waterton Lake and is separated by a channel known as the Dardanelles.
Krummholz — also called knieholz — is a type of stunted, deformed vegetation encountered in the subarctic and subalpine tree line landscapes, shaped by continual exposure to fierce, freezing winds. Under these conditions, trees can only survive where they are sheltered by rock formations or snow cover. As the lower portion of these trees continues to grow, the coverage becomes extremely dense near the ground. In Newfoundland and Labrador, the formation is known as tuckamore. Krummholz trees are also found on beaches such as the Oregon coast, where trees can become much taller than their subalpine cousins.
The wildlife of Canada or biodiversity of Canada consist of over 80,000 classified species, and an equal number thought yet to be recognized. Known fauna and flora have been identified from five kingdoms: protozoa represent approximately 1% of recorded species; chromist ; fungis ; plants ; and animals. Insects account for nearly 70 percent of documented animal species in Canada. More than 300 species are found exclusively in Canada.
The biogeoclimatic zones of British Columbia are units of a classification system used by the British Columbia Ministry of Forests for the Canadian province's fourteen different broad, climatic ecosystems. The classification system, termed Biogeoclimatic Ecosystem Classification, exists independently of other ecoregion systems, one created by the World Wildlife Fund and the other in use by Environment Canada, which is based on one created by the Commission for Environmental Cooperation (CEC) and also in use by the US Environmental Protection Agency (EPA). The system of biogeoclimatic ecosystem classification was partly created for the purpose of managing forestry resources, but is also in use by the British Columbia Ministry of Environment and Climate Change Strategy and other provincial agencies. A biogeoclimatic zone is defined as "a geographic area having similar patterns of energy flow, vegetation and soils as a result of a broadly homogenous macroclimate."
The ecology of the Rocky Mountains is diverse due to the effects of a variety of environmental factors. The Rocky Mountains are the major mountain range in western North America, running from the far north of British Columbia in Canada to New Mexico in the southwestern United States, climbing from the Great Plains at or below 1,800 feet (550 m) to peaks of over 14,000 feet (4,300 m). Temperature and rainfall varies greatly also and thus the Rockies are home to a mixture of habitats including the alpine, subalpine and boreal habitats of the Northern Rocky Mountains in British Columbia and Alberta, the coniferous forests of Montana and Idaho, the wetlands and prairie where the Rockies meet the plains, a different mix of conifers on the Yellowstone Plateau in Wyoming, the montane forests of Utah, and in the high Rockies of Colorado and New Mexico, and finally the alpine tundra of the highest elevations.
The Colorado Rockies forests is a temperate coniferous forest ecoregion of the United States. This ecoregion is located in the highest ranges of the Rocky Mountains, in central and western Colorado, northern New Mexico and southeastern Wyoming, and experiences a dry continental climate.
The North Central Rockies forests is a temperate coniferous forest ecoregion of Canada and the United States. This region overlaps in large part with the North American inland temperate rainforest and gets more rain on average than the South Central Rockies forests and is notable for containing the only inland populations of many species from the Pacific coast.
The Great Basin montane forests is an ecoregion of the Temperate coniferous forests biome, as designated by the World Wildlife Fund (WWF).
South Chilcotin Mountains Provincial Park is a provincial park in British Columbia, Canada, located on Highway 40 northwest of Lillooet, British Columbia. The park, which is 56,796 ha. in size, was established on April 18, 2001, and It was created out of a portion of the Spruce Lake Protected Area. The park is located on three Indigenous Nations: The Tsilhqot’in, St’at’imc, and Secwepemc.
Bogd Khan Uul Biosphere Reserve is a nature reserve situated to the south of Ulaanbaatar in Mongolia. It is in the southern part of the forest steppe zone and is in the Khentii Mountains area. It includes Bogd Khan Mountain, and was designated as a UNESCO Biosphere Reserve in 1996. It claims to be the oldest National Park in the world.
The Bryansk Forest Nature Reserve, also known as Bryansky Les, is a nature reserve in Bryansk Oblast, Russia, along the Nerussa River near the Russian border with Ukraine.
Visim Nature Reserve is a Russian 'zapovednik' protecting an area of southern taiga in the low Middle Ural Mountains. In 2001, it was named a UNESCO MAB Biosphere Reserve. It is named for the ancient village of Visim, which was home to the Russian writer Dmitry Mamin-Sibiryak, who wrote about rural life in the Urals. Most of the reserve is located on its western slope in the headwaters of the Sulёm River, a right tributary of the Chusovoi River, part of the vast Volga-Kama basin. Part, however is on the eastern slope in the Ob River watershed. The reserve thus straddles the Europe-Asia continental divide: water from the reserve flows into both the Caspian Sea through the Volga River, and the Kara Sea through the Ob River. The reserve is situated in the Kirovgrad District of Sverdlovsk Oblast, about 100 km northwest of Yekaterinburg.
Niwot Ridge is an alpine ecology research station located 65 km northwest of Denver in north-central Colorado. It is on the Front Range of the southern Rocky Mountains and lies within the Roosevelt National Forest. Niwot Ridge is 2,900 metres (9,500 ft) high.
The Fraser Experimental Forest is an outdoor research laboratory to study timber, water, wildlife management, and their integration in the high elevation subalpine coniferous forests. The experimental forest was established in 1937, and encompasses 9,328 hectares (36.02 sq mi). It is situated on the west side of the Continental Divide in north-central Colorado and includes the entire watershed of main Saint Louis Creek, a tributary of the Fraser River.
Los Volcanes Biosphere Reserve is a UNESCO Biosphere Reserve located within the Trans-Mexican Volcanic Belt of south-central Mexico. The 171,774.4 hectares (663.225 sq mi) reserve surrounds the volcanoes of Popocatépetl and Ixtaccíhuatl and marks the biogeographical boundary between the Nearctic and Neotropical realms. The reserve is managed by Iztaccíhuatl Popocatépetl Zoquiapan National Park.
The Lake Manyara Biosphere Reserve is a UNESCO Biosphere Reserve in the depression of the East African Rift Valley in the Lake Manyara Basin in Arusha Region of northern Tanzania. The reserve is managed by Tanzanian Lake Manyara National Park.
