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Isunngua

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Isunngua (old spelling: Isúngua ) is a highland in the Qeqqata municipality in central-western Greenland , located immediately west of the Greenland Ice Sheet edge. In large part it is covered by the tundra , although in the immediate vicinity of the Sermersuaq ice sheet it gradually becomes exposed, barren, and largely devoid of life. The climate is polar continental , with the area receiving very little rainfall. Isunngua is a calving site for reindeer .

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27-538: Isunngua is notable for a gravel road which leads through it towards the edge of the Greenland Ice Sheet, located 40 km (25 mi) east of Kangerlussuaq , and due to trivial approach it remains a popular tourist target, although very few hikers make the journey on foot, or explore the neighboring glaciers. The highland is bounded from the north by the Isunnguata Sermia glacier , from

54-426: A few tens of kilometers of their source outcrops. Gravel is deposited as gravel blankets or bars in stream channels; in alluvial fans ; in near-shore marine settings, where the gravel is supplied by streams or erosion along the coast; and in the deltas of swift-flowing streams. The upper Mississippi embayment contains extensive chert gravels thought to have their origin less than 100 miles (160 km) from

81-644: A high hydraulic conductivity , sometimes reaching above 1 cm/s. Most gravel is derived from disintegration of bedrock as it weathers . Quartz is the most common mineral found in gravel, as it is hard, chemically inert, and lacks cleavage planes along which the rock easily splits. Most gravel particles consist of multiple mineral grains, since few rocks have mineral grains coarser than about 8 millimeters (0.31 in) in size. Exceptions include quartz veins , pegmatites , deep intrusions , and high-grade metamorphic rock . The rock fragments are rapidly rounded as they are transported by rivers , often within

108-529: A minor component, making up less than 1% of all sedimentary rock. Alluvial fans likely contain the largest accumulations of gravel in the geologic record. These include conglomerates of the Triassic basins of eastern North America and the New Red Sandstone of south Devon . [REDACTED] Media related to Gravel at Wikimedia Commons Crushed stone Crushed stone or angular rock

135-434: Is a form of construction aggregate , typically produced by mining a suitable rock deposit and breaking the removed rock down to the desired size using crushers . It is distinct from naturally occurring gravel , which is produced by natural processes of weathering and erosion and typically has a more rounded shape. Crushed stone is a major basic raw material used by construction , agriculture, and other industries. Despite

162-409: Is a high-volume, low-value commodity . The industry is highly competitive and is characterized by many operations serving local or regional markets. Production costs are determined mainly by the cost of labor, equipment, energy, and water, in addition to the costs of compliance with environmental and safety regulations. These costs vary depending on geographic location, the nature of the deposit, and

189-882: Is a loose aggregation of rock fragments . Gravel occurs naturally on Earth as a result of sedimentary and erosive geological processes; it is also produced in large quantities commercially as crushed stone . Gravel is classified by particle size range and includes size classes from granule - to boulder -sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel (2–4 mm or 0.079–0.157 in) and pebble gravel (4–64 mm or 0.2–2.5 in). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm (0.079–0.248 in) for fine and 20–63 mm (0.79–2.48 in) for coarse. One cubic metre of gravel typically weighs about 1,800 kg (4,000 lb), or one cubic yard weighs about 3,000 lb (1,400 kg). Gravel

216-414: Is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete . Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a high hydraulic conductivity , making them important aquifers . Colloquially,

243-416: Is responsible for the wide dispersion of quarries, usually located near highly populated areas. However, increasing land values combined with local environmental concerns are moving crushed stone quarries farther from the end-use locations, increasing the price of delivered material. Economies of scale , which might be realized if fewer, larger operations served larger marketing areas, would probably not offset

270-537: Is sometimes distinguished from rubble, which is loose rock particles in the same size range but angular in shape. The Udden-Wentworth scale , widely used by geologists in the US, defines granular gravel as particles with a size from 2 to 4 mm (0.079 to 0.157 in) and pebble gravel as particles with a size from 4 to 64 mm (0.16 to 2.52 in). This corresponds to all particles with sizes between coarse sand and cobbles . The U.S. Department of Agriculture and

297-405: Is widely and plentifully distributed, mostly as river deposits, river flood plains, and glacial deposits, so that environmental considerations and quality dictate whether alternatives, such as crushed stone , are more economical. Crushed stone is already displacing natural gravel in the eastern United States, and recycled gravel is also becoming increasingly important. The word gravel comes from

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324-708: The Old French gravele or gravelle . Different varieties of gravel are distinguished by their composition, origin, and use cases. Types of gravel include: In locales where gravelly soil is predominant, plant life is generally more sparse. This is due to the inferior ability of gravels to retain moisture, as well as the corresponding paucity of mineral nutrients, since finer soils that contain such minerals are present in smaller amounts. Sediments containing over 30% gravel that become lithified into solid rock are termed conglomerate . Conglomerates are widely distributed in sedimentary rock of all ages, but usually as

351-830: The Soil Science Society of America define gravel as particles from 2 to 80 mm (0.079 to 3.150 in) in size, while the German scale (Atterburg) defines gravel as particles from 2 to 200 mm (0.079 to 7.874 in) in size. The U.S. Army Corps of Engineers defines gravel as particles under 3 in (76 mm) in size that are retained by a number 4 mesh, which has a mesh spacing of 4.76 mm (0.187 in). ISO 14688 for soil engineering grades gravels as fine, medium, and coarse with ranges 2 mm to 6.3 mm to 20 mm to 63 mm. The bulk density of gravel varies from 1,460 to 1,920 kg/m (2,460 to 3,240 lb/cu yd). Natural gravel has

378-490: The U.S., with a total value of about $ 12.6 billion. Some 960 million tons of construction sand and gravel were produced. This greatly exceeds production of industrial sand and gravel (68 million tons), which is mostly sand rather than gravel. It is estimated that almost half of construction sand and gravel is used as aggregate for concrete . Other important uses include in road construction, as road base or in blacktop ; as construction fill; and in myriad minor uses. Gravel

405-499: The increased transportation costs. According to the United States Geological Survey , 1.72 billion tons of crushed stone worth $ 13.8 billion was sold or used in 2006, of which 1.44 billion tons was used as construction aggregate , 74.9 million tons used for cement manufacture, and 18.1 million tons used to make lime . Crushed marble sold or used totaled 11.8 million tons,

432-731: The low value of its basic products, the crushed stone industry is a major contributor to and an indicator of the economic well-being of a nation . The demand for crushed stone is determined mostly by the level of construction activity, and, therefore, the demand for construction materials. Stone resources of the world are very large. High-purity limestone and dolomite suitable for specialty uses are limited in many geographic areas. Crushed stone substitutes for roadbuilding include sand and gravel , and slag . Substitutes for crushed stone used as construction aggregates include sand and gravel, iron and steel slag, sintered or expanded clay or shale , and perlite or vermiculite . Crushed stone

459-433: The majority of which was ground very fine and used as calcium carbonate . In 2006, 9.40 million tons of crushed stone (almost all limestone or dolomite) was used for soil treatment, primarily to reduce soil acidity . Soils tend to become acidic from heavy use of nitrogen-containing fertilizers, unless a soil conditioner is used. Using aglime or agricultural lime , a finely-ground limestone or dolomite, to change

486-459: The much denser molten metal (i.e., iron). The slag cools to become a stone-like material that is commonly crushed and recycled as construction aggregate. In addition, 4.53 million tons of crushed stone was used for fillers and extenders (including asphalt fillers or extenders), 2.71 million tons for sulfur oxide removal-mine dusting-acid water treatment, and 1.45 million tons sold or used for poultry grit or mineral food. Crushed stone

513-459: The number and type of products produced. Crushed stone has one of the lowest average by weight values of all mineral commodities. The average unit price increased from US$ 1.58 per metric ton, f.o.b. plant, in 1970 to US$ 4.39 in 1990. However, the unit price in constant 1982 dollars fluctuated between US$ 3.48 and US$ 3.91 per metric ton for the same period. Increased productivity achieved through increased use of automation and more efficient equipment

540-488: The periphery of the embayment. It has been suggested that wind-formed ( aeolian ) gravel "megaripples" in Argentina have counterparts on the planet Mars . Gravel is a major basic raw material in construction . Sand is not usually distinguished from gravel in official statistics, but crushed stone is treated as a separate category. In 2020, sand and gravel together made up 23% of all industrial mineral production in

567-629: The proving grounds after last-minute checks. This project was abandoned and from 2006 the road leading to the edge of the ice cap is maintained for tourist purposes only, though access to the last segment of the road is limited and requires a key to open the padlocked gate. Ice activity has demolished the inland ice segment of the road, and it now ends in Isunngua, on the edge of the ice sheet. 67°08′40″N 50°10′00″W  /  67.14444°N 50.16667°W  / 67.14444; -50.16667 Gravel Gravel ( / ˈ ɡ r æ v əl / )

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594-522: The soil from acidic to nearly neutral particularly benefits crops by maximizing availability of plant nutrients, and also by reducing aluminum or manganese toxicity, promoting soil microbe activity, and improving the soil structure. In 2006, 5.29 million tons of crushed stone (mostly limestone or dolomite) was used as a flux in blast furnaces and in certain steel furnaces to react with gangue minerals (i.e. silica and silicate impurities) to produce liquid slag that floats and can be poured off from

621-420: The south by Russell Glacier and Aajuitsup Tasia lake, and from the west by Sanningasoq twin lake. Both glaciers flow to the west from the ice sheet, which constrains Isunngua from the east. The average height of the highland hills is approximately 500–530 metres (1,640–1,740 ft). The highland is dotted with freshwater lakes, kettles , and meltwater outflow lakes saturated with glacial silt . In

648-487: The spring of 2000 the Swedish construction group Skanska 's Greenlandic subsidiary completed six months' work in establishing a 30 kilometres (19 mi) road for the testing company Nausta, which operates a testing site in northern Sweden. The road runs through the glacial valley of Akuliarusiarsuup Kuua , from Kangerlussuaq to the edge of the permanent inland ice in Isunngua. A road stretching 150 km (93 mi)

675-536: The term gravel is often used to describe a mixture of different size pieces of stone mixed with sand and possibly some clay. The American construction industry distinguishes between gravel (a natural material) and crushed stone (produced artificially by mechanical crushing of rock.) The technical definition of gravel varies by region and by area of application. Many geologists define gravel simply as loose rounded rock particles over 2 mm (0.079 in) in diameter, without specifying an upper size limit. Gravel

702-432: Was laid on the inland ice. Nausta built the facility to complement the winter testing done by Volkswagen in northern Sweden and Finland . The site at Kangerlussuaq was primarily used in the summer half of the year, from April through October. The entire testing ground was used to test cars' performance in extreme cold and conditions of near-zero friction. The cars were flown from Europe to Kangerlussuaq, and then driven to

729-456: Was mainly responsible for maintaining the prices at this level. Transportation is a major factor in the delivered price of crushed stone. The cost of moving crushed stone from the plant to the market often equals or exceeds the sale price of the product at the plant. Because of the high cost of transportation and the large quantities of bulk material that have to be shipped, crushed stone is usually marketed locally. The high cost of transportation

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