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Economy Of Jammu And Kashmir
Jammu and Kashmir's economy is primarily services-based and agriculture-oriented. The gross domestic product of Jammu and Kashmir was estimated at in 2020–21. In the fiscal year 2023–2024, it is expected that Jammu and Kashmir's Gross Domestic Product (GDP) will exceed Rs 2.30 lakh crore, with a growth rate of 10 per cent. Along with horticulture and agriculture, tourism is an important industry for Jammu and Kashmir, accounting for about 7% to its economy. The Kashmir Valley is known for its sericulture and cold-water fisheries. Wood from Kashmir is used to make high-quality cricket bats, popularly known as Kashmir Willow. Major agricultural exports from Jammu and Kashmir include apples, pears, cherries, plums, saffron and walnuts. The traditional Kashmiri handicrafts industry employs a large workforce of around 340 thousand artisans and has potential for producing export goods. Small-scale cottage industries include carpet weaving, silks, shawls, basketry, pottery, copper a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Indian States And Union Territories By GDP
These are lists of Indian states and union territories by their nominal gross state domestic product (GSDP). GSDP is the sum of all value added by industries within each state or union territory and serves as a counterpart to the national gross domestic product (GDP). , the Government accounted for about 21% of the GDP followed by agriculture with 21% and corporate sector at 12%. The remaining 48% is sourced from small proprietorship and partnership companies, unorganized sector and households. List Zonal contribution Historical data See also * List of Indian metropolitan areas by GDP * Comparison between Indian states and countries by GDP (PPP) * Economy of India * Foreign-exchange reserves of India * Income in India * List of country subdivisions by GDP over 200 billion US dollars * List of countries by GDP (nominal) Gross domestic product (GDP) is the market value of all final goods and services from a nation in a given year. Countries ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nigella Sativa
''Nigella sativa'' (common names, black caraway, black cumin, nigella or kalonji) is an annual flowering plant in the family Ranunculaceae, native to western Asia (Arabia, the Levant, Cyprus, Turkey, Iran and Iraq), and eastern Europe (Bulgaria and Romania). It is naturalized over parts of Europe, northern Africa, and east to Myanmar. It is used as a spice in various food preparations, especially in Arab and Halal cuisines. Etymology The genus name ''Nigella'' is a diminutive of the Latin "black", referring to the seed color. The specific epithet ''sativa'' means "cultivated". Common names In food preparation, ''Nigella sativa'' and its seeds are variously called black caraway, black seed, black cumin, fennel flower, nigella, nutmeg flower, Roman coriander, or black onion seed. Black seed and black caraway may also refer to '' Elwendia persica'', which is also known as ''Bunium persicum''. Description ''N. sativa'' grows to tall, with finely divided, linear (but not thread ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
India Brand Equity Foundation
India Brand Equity Foundation (IBEF) is a Trust established by the Department of Commerce, Ministry of Commerce and Industry, Government of India. IBEF's primary objective is to promote and create international awareness of the Made in India label in markets overseas and to facilitate the dissemination of knowledge of Indian products and services. Towards this objective, IBEF works closely with stakeholders across government and industry. IBEF works as the branding and communication partner for India's participation at various global trade exhibitions. IBEF also manages onsite branding, media advertisements, public relations, Digital marketing, publishing reports and knowledge kits. History India Brand Equity Foundation (IBEF) was established as a Trust in 1996 by the Department of Commerce, Ministry of Commerce and Industry, Government of India. Through its core promotional and branding activities, IBEF has contributed to creating awareness of the Made in India label and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (mineral)
Dolomite () is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite (see Dolomite (rock)). An alternative name sometimes used for the dolomitic rock type is dolostone. History As stated by Nicolas-Théodore de Saussure the mineral dolomite was probably first described by Carl Linnaeus in 1768. In 1791, it was described as a rock by the French natural history, naturalist and geologist Déodat Gratet de Dolomieu (1750–1801), first in buildings of the old city of Rome, and later as samples collected in the County_of_Tyrol, Tyrolean Alps. Nicolas-Théodore de Saussure first named the mineral (after Dolomieu) in March 1792. Properties The mineral dolomite crystallizes in the trigonal, trigonal-rhombohedral system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magnetite
Magnetite is a mineral and one of the main iron ores, with the chemical formula . It is one of the iron oxide, oxides of iron, and is ferrimagnetism, ferrimagnetic; it is attracted to a magnet and can be magnetization, magnetized to become a permanent magnet itself. With the exception of extremely rare native iron deposits, it is the most magnetic of all the naturally occurring minerals on Earth. Naturally magnetized pieces of magnetite, called lodestone, will attract small pieces of iron, which is how ancient peoples first discovered the property of magnetism. Magnetite is black or brownish-black with a metallic luster, has a Mohs scale of mineral hardness, Mohs hardness of 5–6 and leaves a black streak (mineralogy), streak. Small grains of magnetite are very common in igneous rocks, igneous and metamorphic rocks. The chemical IUPAC name is iron(II,III) oxide and the common chemical name is ''ferrous-ferric oxide''. Properties In addition to igneous rocks, magnetite als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ministry Of Mines (India)
The Ministry of Mines is the ministry in the Government of India. The ministry functions as the primary body for the formulation and administration of laws relating to mines in India. The head of the ministry is G. Kishan Reddy, who has been serving since June 2024. Functions The Ministry of Mines is responsible for surveying and exploring for minerals (other than natural gas and petroleum) that are used in mining and metallurgy. It searches for non-ferrous metals including: aluminium, copper, zinc, lead, gold, nickel, etc. for administration of Mines and Minerals (Development and Regulation) Act, 1957 (MMDR Act) in respect of all mines and minerals other than coal and lignite. There is one attached office, one subordinate office, three public sector undertakings (PSUs), three autonomous bodies, and additional agencies working under the support of the Ministry of Mines. Attached office * Geological Survey of India; headquarters at Kolkata Subordinate office * Indian Bure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diaspore
Diaspore ()also called diasporite, empholite, kayserite, or tanatariteis an aluminium hydroxide oxide mineral, α-AlO(OH), crystallizing in the orthorhombic system and isomorphous with goethite. It occurs sometimes as flattened crystals, but usually as lamellar or scaly masses, the flattened surface being a direction of perfect cleavage on which the lustre is markedly pearly in character. It is colorless or greyish-white, yellowish, sometimes violet in color, and varies from translucent to transparent. It may be readily distinguished from other colorless transparent minerals with a perfect cleavage and pearly luster (e.g. mica, talc, brucite, and gypsum) by its greater hardness of 6.5–7. Its specific gravity is 3.4. When heated before the blowpipe, it decrepitates violently, breaking up into white pearly scales. The mineral occurs as an alteration product of corundum or emery and is found in granular limestone and other crystalline rocks. Well-developed crystals a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bentonite
Bentonite ( ) is an Absorption (chemistry), absorbent swelling clay consisting mostly of montmorillonite (a type of smectite) which can either be Na-montmorillonite or Ca-montmorillonite. Na-montmorillonite has a considerably greater swelling capacity than Ca-montmorillonite. Bentonite usually forms from the weathering of volcanic ash in seawater, or by hydrothermal circulation through the porosity of volcanic ash beds, which converts (devitrification) the volcanic glass (obsidian, rhyolite, dacite) present in the ash into clay minerals. In the mineral alteration process, a large fraction (up to 40–50 wt.%) of amorphous silica is dissolution (chemistry), dissolved and leaching (agriculture), leached away, leaving the bentonite deposit in place. Bentonite beds are white or pale blue or green (traces of redox, reduced ) in fresh exposures, turning to a cream color and then yellow, red, or brown (traces of oxidation, oxidized ) as the exposure is weathered further. As a swel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaolinite
Kaolinite ( ; also called kaolin) is a clay mineral, with the chemical composition Al2 Si2 O5( OH)4. It is a layered silicate mineral, with one tetrahedral sheet of silica () linked through oxygen atoms to one octahedral sheet of alumina (). Kaolinite is a soft, earthy, usually white, mineral (dioctahedral phyllosilicate clay), produced by the chemical weathering of aluminium silicate minerals like feldspar. It has a low shrink–swell capacity and a low cation-exchange capacity (1–15 meq/100 g). Rocks that are rich in kaolinite, and halloysite, are known as kaolin () or china clay. In many parts of the world kaolin is colored pink-orange-red by iron oxide, giving it a distinct rust hue. Lower concentrations of iron oxide yield the white, yellow, or light orange colors of kaolin. Alternating lighter and darker layers are sometimes found, as at Providence Canyon State Park in Georgia, United States. Kaolin is an important raw material in many industries and app ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ball Clay
Ball clays are kaolinitic sedimentary clays that commonly consist of 20–80% kaolinite, 10–25% mica and 6–65% quartz, along with small amounts of organic matter (such as lignite) and trace amounts of other minerals such as pyrite and siderite. They are a common raw material for various types of ceramics, where their primary roles are to impart unfired strength, plasticity or to aid rheological stability during the shaping processes. Most ball clays impart colours ranging from buff to cream to off-white when fired in an oxidising atmosphere.'Industrial Minerals & Rocks - Commodities, Markets And Uses' J. E. Kogel. Society For Mining, Metallurgy And Exploration, 2006 The name "ball clay" is derived from the form of the extracted material when dug by spade as cubes, which then became rounded during subsequent transport, in Dorset and Devon, England during the early days of the industry during the 18th century. In 2008, UK production of ball clay was reported to be worth £82 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bauxite
Bauxite () is a sedimentary rock with a relatively high aluminium content. It is the world's main source of aluminium and gallium. Bauxite consists mostly of the aluminium minerals gibbsite (), boehmite (γ-AlO(OH)), and diaspore (α-AlO(OH)), Mixture, mixed with the two iron oxides goethite (FeO(OH)) and haematite (), the aluminium Clay minerals, clay mineral kaolinite () and small amounts of anatase () and ilmenite ( or ). Bauxite appears dull in Lustre (mineralogy), luster and is reddish-brown, white, or tan. In 1821, the French people, French geologist Pierre Berthier discovered bauxite near the village of Les Baux-de-Provence, Les Baux in Provence, southern France. Formation Numerous classification schemes have been proposed for bauxite but, , there was no consensus. Vadász (1951) distinguished Laterite, lateritic bauxites (silicate bauxites) from karst bauxite ores (carbonate bauxites): * The carbonate bauxites occur predominantly in Europe, Guyana, Suriname, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magnesite
Magnesite is a mineral with the chemical formula ( magnesium carbonate). Iron, manganese, cobalt, and nickel may occur as admixtures, but only in small amounts. Occurrence Magnesite occurs as veins in and an alteration product of ultramafic rocks, serpentinite and other magnesium rich rock types in both contact and regional metamorphic terrains. These magnesites are often cryptocrystalline and contain silica in the form of opal or chert. Magnesite is also present within the regolith above ultramafic rocks as a secondary carbonate within soil and subsoil, where it is deposited as a consequence of dissolution of magnesium-bearing minerals by carbon dioxide in groundwaters. Formation Magnesite can be formed via talc carbonate metasomatism of peridotite and other ultramafic rocks. Magnesite is formed via carbonation of olivine in the presence of water and carbon dioxide at elevated temperatures and high pressures typical of the greenschist facies. Magnesite can also be f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
