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Gulmarg Wildlife Sanctuary
The Gulmarg Wildlife Sanctuary spread over is a protected area in Gulmarg, Baramulla district of Jammu and Kashmir, India. The sanctuary lies on the north-eastern side of the Pir Panjal mountain range and falls under the northwest Biogeographic Zone 2A. It lies south-west of Srinagar and from Baramulla. The sanctuary was first declared as a game reserve in 1981 and later upgraded to a sanctuary in 1987. Geography The Gulmarg Wildlife Sanctuary lies in the Pir Panjal Range of the Western Himalayas. The Gulmarg tourist resort including the Gulmarg Golf Club and the long Gulmarg Gondola are surrounded by the sanctuary. The elevation of the sanctuary ranges from to . It is surrounded by the forests of the Gulmarg basin and the upper catchment area of the Ferozpur stream. The sanctuary is bordered by the forest divisions of Jehlum Valley to the north and west, Poonch and Pir Panjal to the south and the Drang village to the east. The highly steep terrain of the upper reaches of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulmarg
Gulmarg (), known as Gulmarag (; ) in Kashmiri, is a town, hill station, popular skiing destination, and notified area committee in the Baramulla district of Jammu and Kashmir, India. It is located at a distance of from Baramulla and from Srinagar. The town is situated in the Pir Panjal Range in the Western Himalayas and lies within the boundaries of Gulmarg Wildlife Sanctuary. Etymology Originally called Gauri Marg (meaning "the path of Devi Gauri"), its name was changed to 'Gulmarg' in the 1500s by Yousuf Shah of the Chak dynasty. Gulmarg is now interpreted as 'meadow of flowers'. History Yousuf Shah Chak, who ruled Kashmir from 1579 to 1586, frequented the place with his queen Habba Khatoon and renamed it 'Gulmarg' ("meadow of flowers"). Wild flowers of 21 different varieties were collected by the Mughal emperor Jahangir for his gardens in Gulmarg. In the 19th century, British civil servants started using Gulmarg as a retreat to escape summers in North Indian ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Flows
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Tundra
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra. The high elevation causes an adverse climate, which is too cold and windy to support tree growth. Alpine tundra transitions to sub-alpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone are known as '' Krummholz''. With increasing elevation it ends at the snow line where snow and ice persist through summer. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the alpine tundra is caused by adiabatic cooling of air, and is similar to polar climate. Geography Alpine tundra occurs at high enough altitude at any latitude. Por ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Acer Cappadocicum
''Acer cappadocicum'', the Cappadocian maple, is a maple native to Asia, from central Turkey (ancient Cappadocia) east along the Caucasus, the Himalayas, to southwestern China.Mitchell, A. F. (1974). ''A Field Guide to the Trees of Britain and Northern Europe''. Collins Mitchell, A. F. (1982). ''The Trees of Britain and Northern Europe''. Collins Bean, W. J. (1976). ''Trees and Shrubs Hardy in the British Isles'' 8th ed., vol. 1. John Murray .Huxley, A., ed. (1992). ''New RHS Dictionary of Gardening''. Macmillan .Rushforth, K. (1999). ''Trees of Britain and Europe''. Collins . Description It is a medium-sized deciduous tree growing to 20–30 m tall with a broad, rounded crown. The leaves are opposite, palmately lobed with 5-7 lobes, 6–15 cm across. The leaf stems bleed a milky latex when broken. The flowers are in corymbs of 15-30 together, yellow-green with five petals 3–4 mm long; flowering occurs in early spring. The fruit is a double samara with two winged see ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Picea Smithiana
''Picea smithiana'' is a species of evergreen tree in the family Pinaceae family It is referred to by the common names morinda spruce and West Himalayan spruce, and is a spruce native to the western Himalaya and adjacent mountains, from northeast Afghanistan, northern Pakistan, India to central Nepal. It grows at altitudes of 2,400-3,600 m in forests together with deodar cedar, blue pine and pindrow fir. Description ''Picea smithiana'' is a large evergreen tree growing to 40–55 m tall (exceptionally to 60 m), and with a trunk diameter of up to 1–2 m. It has a conical crown with level branches and usually pendulous branchlets. The shoots are pale buff-brown, and glabrous (hairless). The leaves are needle-like, the longest of any spruce, 3–5 cm long, rhombic in cross-section, mid-green with inconspicuous stomatal lines. The cones are broad cylindric-conic, 9–16 cm long and 3 cm broad, green when young, maturing buff-brown and opening to 5–6 cm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taxus Wallichiana
''Taxus wallichiana'', the Himalayan yew, is a species of yew, native to the Himalaya and parts of south-east Asia. The species has a variety of uses in traditional medicine. It is currently classified as endangered by the IUCN. Distribution and habitat The species favours a reasonably wide range of habitats, growing in montane, temperate, warm temperate, and tropical submontane to high montane forests which may be deciduous, evergreen, or of mixed character. In forests, it tends to present as a low canopy tree; in open situations it usually forms a large, broadly spreading shrub. Elevation ranges from 900 m to 3,700 m. Growth It is a medium-sized evergreen coniferous tree growing to 10 m tall, similar to ''Taxus baccata'' and sometimes treated as a subspecies of it. The shoots are green at first, becoming brown after three or four years. The leaves are thin, flat, slightly falcate (sickle-shaped), 1.5–2.7 cm long and 2 mm broad, with a softly mucronate apex; th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinus Griffithii
''Pinus wallichiana'' is a coniferous evergreen tree native to the Himalaya, Karakoram and Hindu Kush mountains, from eastern Afghanistan east across northern Pakistan and north west India to Yunnan in southwest China. It grows in mountain valleys at altitudes of 1800–4300 m (rarely as low as 1200 m), reaching in height. It favours a temperate climate with dry winters and wet summers. In Pashto, it is known as ''Nishtar''. This tree is often known as Bhutan pine, (not to be confused with the recently described Bhutan white pine, ''Pinus bhutanica'', a closely related species). Other names include blue pine, Himalayan pine and Himalayan white pine. Description The leaves ("needles") are in fascicles (bundles) of five and are 12–18 cm long. They are noted for being flexible along their length, and often droop gracefully. The cones are long and slender, 16–32 cm, yellow-buff when mature, with thin scales; the seeds are 5–6 mm long with a 20–30&nb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Pine
''Pinus wallichiana'' is a coniferous evergreen tree native to the Himalaya, Karakoram and Hindu Kush mountains, from eastern Afghanistan east across northern Pakistan and north west India to Yunnan in southwest China. It grows in mountain valleys at altitudes of 1800–4300 m (rarely as low as 1200 m), reaching in height. It favours a temperate climate with dry winters and wet summers. In Pashto, it is known as ''Nishtar''. This tree is often known as Bhutan pine, (not to be confused with the recently described Bhutan white pine, ''Pinus bhutanica'', a closely related species). Other names include blue pine, Himalayan pine and Himalayan white pine. Description The leaves ("needles") are in fascicles (bundles) of five and are 12–18 cm long. They are noted for being flexible along their length, and often droop gracefully. The cones are long and slender, 16–32 cm, yellow-buff when mature, with thin scales; the seeds are 5–6 mm long with a 20–30&nb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silver Birch
''Betula pendula'', commonly known as silver birch, warty birch, European white birch, or East Asian white birch, is a species of tree in the family Betulaceae, native to Europe and parts of Asia, though in southern Europe, it is only found at higher altitudes. Its range extends into Siberia, China, and southwest Asia in the mountains of northern Turkey, the Caucasus, and northern Iran. It has been introduced into North America, where it is known as the European white birch or weeping birch and is considered invasive in some states in the United States and parts of Canada. The tree can also be found in more temperate regions of Australia. The silver birch is a medium-sized deciduous tree that owes its common name to the white peeling bark on the trunk. The twigs are slender and often pendulous and the leaves are roughly triangular with doubly serrate margins and turn yellow and brown in autumn before they fall. The flowers are catkins and the light, winged seeds get widely ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abies Pindrow
''Abies pindrow'', the pindrow fir or west Himalayan fir, is a fir native to the western Himalaya and adjacent mountains, from northeast Afghanistan east through northern Pakistan and India to central Nepal. Description It is a large evergreen tree growing to tall, and with a trunk diameter of up to . It has a conical crown with level branches. The shoots are greyish-pink to buff-brown, smooth and glabrous (hairless). The leaves are needle-like, among the longest of any fir, long, flattened in cross-section, glossy dark green above, with two whitish stomatal bands on the underside; they are arranged spirally on the shoots, but twisted at the base to lie in a flat plane either side of the shoot. The cones are broad cylindric-conic, long and broad, dark purple when young, disintegrating when mature to release the seeds 5–7 months after pollination. The closely related Gamble's fir occurs in the same area but on somewhat drier sites; it differs in shorter leaves 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Temperate Climate
In geography, the temperate climates of Earth occur in the middle latitudes (23.5° to 66.5° N/S of Equator), which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation changes. In temperate climates, not only do latitudinal positions influence temperature changes, but sea currents, prevailing wind direction, continentality (how large a landmass is) and altitude also shape temperate climates. The Köppen climate classification defines a climate as "temperate" C, when the mean temperature is above but below in the coldest month to account for the persistency of frost. However, other climate classifications set the minimum at . Zones and climates The north temperate zone extends from the Tropic of Cancer (approximately 23.5° north latitude) to the Arct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called " slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
