Himalayan Salt
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Himalayan Salt
Himalayan salt is rock salt (halite) mined from the Punjab region of Pakistan. The salt, which often has a pinkish tint due to trace minerals, is primarily used as a food additive to replace refined table salt but is also used for cooking and food presentation, decorative lamps and spa treatments. The product is often promoted with unsupported claims that it has health benefits. Geology Himalayan salt is mined from the Salt Range mountains, the southern edge of a fold-and-thrust belt that underlies the Pothohar Plateau south of the Himalayas in Pakistan. Himalayan salt comes from a thick layer of Ediacaran to early Cambrian evaporites of the ''Salt Range Formation''. This geological formation consists of crystalline halite intercalated with potash salts, overlain by gypsiferous marl and interlayered with beds of gypsum and dolomite with infrequent seams of oil shale that accumulated between 600 and 540 million years ago. These strata and the overlying Cambrian to Eocene sedim ...
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Himalayan Salt (coarse)
Himalayan salt is rock salt (halite) mined from the Punjab region of Pakistan. The salt, which often has a pinkish tint due to trace minerals, is primarily used as a food additive to replace refined table salt but is also used for cooking and food presentation, decorative lamps and spa treatments. The product is often promoted with unsupported claims that it has health benefits. Geology Himalayan salt is mined from the Salt Range mountains, the southern edge of a fold-and-thrust belt that underlies the Pothohar Plateau south of the Himalayas in Pakistan. Himalayan salt comes from a thick layer of Ediacaran to early Cambrian evaporites of the ''Salt Range Formation''. This geological formation consists of crystalline halite intercalated with potash salts, overlain by gypsiferous marl and interlayered with beds of gypsum and dolomite with infrequent seams of oil shale that accumulated between 600 and 540 million years ago. These strata and the overlying Cambrian to Eocene se ...
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Gypsum
Gypsum is a soft sulfate mineral composed of calcium sulfate dihydrate, with the chemical formula . It is widely mined and is used as a fertilizer and as the main constituent in many forms of plaster, blackboard or sidewalk chalk, and drywall. Alabaster, a fine-grained white or lightly tinted variety of gypsum, has been used for sculpture by many cultures including Ancient Egypt, Mesopotamia, Ancient Rome, the Byzantine Empire, and the Nottingham alabasters of Medieval England. Gypsum also crystallizes as translucent crystals of selenite. It forms as an evaporite mineral and as a hydration product of anhydrite. The Mohs scale of mineral hardness defines gypsum as hardness value 2 based on scratch hardness comparison. Etymology and history The word ''gypsum'' is derived from the Greek word (), "plaster". Because the quarries of the Montmartre district of Paris have long furnished burnt gypsum (calcined gypsum) used for various purposes, this dehydrated gypsum became known ...
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Sodium Chloride
Sodium chloride , commonly known as salt (although sea salt also contains other chemical salts), is an ionic compound with the chemical formula NaCl, representing a 1:1 ratio of sodium and chloride ions. With molar masses of 22.99 and 35.45 g/mol respectively, 100 g of NaCl contains 39.34 g Na and 60.66 g Cl. Sodium chloride is the salt most responsible for the salinity of seawater and of the extracellular fluid of many multicellular organisms. In its edible form, salt (also known as ''table salt'') is commonly used as a condiment and food preservative. Large quantities of sodium chloride are used in many industrial processes, and it is a major source of sodium and chlorine compounds used as feedstocks for further chemical syntheses. Another major application of sodium chloride is de-icing of roadways in sub-freezing weather. Uses In addition to the familiar domestic uses of salt, more dominant applications of the approximately 250 million tonnes per year production (2008 ...
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Table Salt
Salt is a mineral composed primarily of sodium chloride (NaCl), a chemical compound belonging to the larger class of salts; salt in the form of a natural crystalline mineral is known as rock salt or halite. Salt is present in vast quantities in seawater. The open ocean has about of solids per liter of sea water, a salinity of 3.5%. Salt is essential for life in general, and saltiness is one of the basic human tastes. Salt is one of the oldest and most ubiquitous food seasonings, and is known to uniformly improve the taste perception of food, including otherwise unpalatable food. Salting, brining, and pickling are also ancient and important methods of food preservation. Some of the earliest evidence of salt processing dates to around 6,000 BC, when people living in the area of present-day Romania boiled spring water to extract salts; a salt-works in China dates to approximately the same period. Salt was also prized by the ancient Hebrews, Greeks, Romans, Byzantines, Hi ...
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Himalayan Rock Salt
Himalayan may refer to: * Himalayas mountain range ** Transhimalaya, a subrange (some species found there are referred to as "Himalayan" not "Transhimalayan") * ''Himalayan'' (album), an album by the band Band of Skulls * Himalayan cat, the breed of domesticated cat * Himalayan guinea pig, a coloration pattern in the domesticated guinea pig (cavy) * Himalayan rabbit, the breed of rabbit * The Himalayans (band), a Nepali band * The Himalayans (American band) See also * Himalaya (other) The Himalayas or Himalaya are a mountain range in Asia. Himalaya may also refer to: People * Andy Himalaya (born 1959), Mexican Alpine skier * Prince Himalaya of Nepal (1921–1980) Entertainment * Himalaya (book), ''Himalaya'' (book), a 2004 tr ...
{{Disambiguation, geo ...
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Punjab Plain
The Punjab Plain is a large alluvial plain in Eastern Pakistan and Northwestern India. The plain includes the Pakistani province of Punjab and the Indian states of Punjab and Haryana, and parts of Rajasthan. This plain is around 200–300 meters above mean sea level. The plain is extensively farmed for cereals and cotton. The plain is the western part of the North Indian River Plain, formed by the Indus River and its tributaries - the Jhelum, the Chenab, the Ravi, the Beas and the Sutlej. The land formed of alluvium in between two rivers known as ''Doab ''Doab'' () is a term used in South Asia Quote: "Originally and chiefly in South Asia: (the name of) a strip or narrow tract of land between two rivers; spec. (with) the area between the rivers Ganges and Jumna in northern India." for the tract ...'' is found here. Bhangar : The flood plains formed due to deposition of older alluvium is known as ''Bhangar''. Bet : The flood plains seen here which are formed due to re ...
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Indus River
The Indus ( ) is a transboundary river of Asia and a trans-Himalayan river of South and Central Asia. The river rises in mountain springs northeast of Mount Kailash in Western Tibet, flows northwest through the disputed region of Kashmir, Quote: "Kashmir, region of the northwestern Indian subcontinent. It is bounded by the Uygur Autonomous Region of Xinjiang to the northeast and the Tibet Autonomous Region to the east (both parts of China), by the Indian states of Himachal Pradesh and Punjab to the south, by Pakistan to the west, and by Afghanistan to the northwest. The northern and western portions are administered by Pakistan and comprise three areas: Azad Kashmir, Gilgit, and Baltistan, ... The southern and southeastern portions constitute the Indian state of Jammu and Kashmir. The Indian- and Pakistani-administered portions are divided by a "line of control" agreed to in 1972, although neither country recognizes it as an international boundary. In addition, China became ...
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Jhelum District
Jhelum District (Urdu and pnb, ), is partially in Pothohar Plateau, and partially in Punjab Plain of the Punjab province of Pakistan. Jhelum is one of the oldest districts of Punjab. It was established on 23 March 1849. According to the 1998 census, the district had a population of 936,957, of which 31.48% were urban. Jhelum District has a diverse population of 1,103,000 (2006). Jhelum is known for providing many soldiers to the British and later to the Pakistan armed forces due to which it is also known as 'city of soldiers' or 'land of martyrs and warriors'. The district of Jhelum stretches from the river Jhelum almost to the Indus. Salt is quarried at the Mayo mine in the Salt Range. There are two coal mines in the district from which the North-Western railway obtains parts of its supply. These are the only coal mines in Punjab province which are in working condition. The chief center of the salt trade is Pind Dadan Khan. The district is crossed by the main line of the North ...
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Khewra Salt Mine
The Khewra Salt Mine (or Mayo Salt Mine) is in Khewra, north of Pind Dadan Khan, an administrative subdivision of Jhelum District, Punjab Region, Pakistan. The mine is in the Salt Range, Potohar plateau, which rises from the Indo-Gangetic Plain, and is the second largest in the world. The mine is famous for its production of pink Khewra salt, often marketed as Himalayan salt, and is a major tourist attraction, drawing up to 250,000 visitors a year. Its history dates back to its discovery by Alexander's troops in 320 BC, but it started trading in the Mughal era. The main tunnel at ground level was developed by H. Warth, a mining engineer, in 1872 during British rule. After independence, the BMR took possession until 1956 and then PIDC owned the mines till 1965. After India-Pakistan war in 1965, the WPIDC took over the administration of salt mines and in 1974, the Pakistan Mineral Development Corporation took over the mine, which still remains the largest source of salt in the ...
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Janjua
The Janjua (also spelt janjua'', Junjua, Janjuah'') is a Rajput clan found predominantly in Pakistan's Punjab Pothohar Plateau. History Connection with the Hindu Shahis The 10th century Arab historian Masudi mentioned that in his time the kings of Gandhara were all called "" (which has been variously read ''Hajaj'', ''J.haj'' or ''Ch'hach''), while the area of Gandhara itself was called "country of the ''Rahbūt''" (Rajputs). Elliot transliterated the character to "Hahaj" and Cunningham had it equated to the Janjua tribe/clan, who were held to be descendants of Juan-Juan Khaganate. Rahman doubts this theory and instead transliterates to "J.haj", an Arabicised form of ''Chhachh'', which is even today the name of the region around the Hindu Shahi capital of Hund. Delhi Sultanate Period The Janjuas were allies of the Mongols during the reign of Balban, who launched a punitive expedition to the region, capturing a large number of horses. The author of the Tarikh-i Mubarak Shahi ...
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Alexander The Great
Alexander III of Macedon ( grc, wikt:Ἀλέξανδρος, Ἀλέξανδρος, Alexandros; 20/21 July 356 BC – 10/11 June 323 BC), commonly known as Alexander the Great, was a king of the Ancient Greece, ancient Greek kingdom of Macedonia (ancient kingdom), Macedon. He succeeded his father Philip II of Macedon, Philip II to the throne in 336 BC at the age of 20, and spent most of his ruling years conducting a lengthy military campaign throughout Western Asia and ancient Egypt, Egypt. By the age of thirty, he had created one of the List of largest empires, largest empires in history, stretching from Greece to northwestern Historical India, India. He was undefeated in battle and is widely considered to be one of history's greatest and most successful military commanders. Until the age of 16, Alexander was tutored by Aristotle. In 335 BC, shortly after his assumption of kingship over Macedon, he Alexander's Balkan campaign, campaigned in the Balkans and reasserted control ...
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Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ...
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