for the market widely known as Halite Central Sofia Market Hall Infobox mineral name Halite category Halide mineral boxwidth boxbgcolor image Selpologne.jpg imagesize caption Halite from the Wieliczka ... ref name Webmin http webmineral.com data Halite.shtml Webmineral data ref Halite IPA en h la t pron , commonly known as rock salt , is the mineral form of sodium chloride sodium Na chlorine Cl . Halite ... File Halite 249324.jpg thumb upright left Halite cubes from the Stassfurt Potash deposit, Saxony Anhalt, Germany size 6.7 x 1.9 x 1.7 cm Halite occurs in vast beds of sedimentary evaporite minerals that result ... . The Khewra Salt Mines Khewra salt mine is a massive deposit of halite near Islamabad , Pakistan ... Winsford Halite Mine , Random fact appears on each page this is one example. ref Salt dome s are vertical ... , and native sulfur , in addition to halite and sylvite . They are common along the Gulf of Mexico ..., halite is said to be behaving in the manner of a rheid . Image SaltCrystalCasts.JPG thumb left Hopper crystal cast of halite in a Jurassic rock, Carmel Formation, Utah Unusual, purple, fibrous vein filling halite is found in France and a few other localities. Halite crystals termed hopper crystals ... grow faster than the centers. Halite crystals form very quickly in some rapidly evaporating lakes resulting in modern artifacts with a coating or encrustation of halite crystals. Halite flowers are rare stalactite s of curling fibers of halite that are found in certain arid caves of Australia s Nullarbor Plain . Halite stalactites and encrustations are also reported in the Quincy native copper mine of Hancock, Michigan . Uses Halite is often used both residentially and municipally for managing ice ... on ice will cause it to melt. Another effect of applying halite to an icy surface covered with water ... is able to replace. Therefore, the presence of halite in solution with water itself melts ice. It is common ... heights 200px perrow 3 Image Halite Egypt.jpg Unusual halite crystals from Fayum , Egypt Image halite09.jpg ... more details
orphan date December 2008 Abraum salts is the name given to a mixed deposit of salt s, including halite sodium chloride , carnallite , and kieserite magnesium sulfate , found in association with rock salt at Aschersleben Sta furt in Germany . The term comes from the German language German Abraum salze , salts to be removed. Abraum, which is red, is used to darken mahogany . ref http dictionary.reference.com browse abraum?qsrc 2446 Dictionary.com ref References reflist 1911 Category Salts Mineral stub pt Sais de Abraum ... more details
Unreferenced date November 2008 An isodesmic crystal is a crystal in which all the chemical bond bonds have the same electrostatic valency chemistry valency . This means that all the bonds are of the same strength. Diamond s and halite have isodesmic crystals. The opposite of an isodesmic crystal is an anisodesmic crystal , in which anion s more strongly bonded to central coordinating cation . Graphite is an example of an isodesmic crystal. Category Crystals ... more details
Unreferenced date June 2009 File MountSodom061607.jpg thumb Mount Sodom, Israel, showing the so called Lot s Wife pillar made of halite like the rest of the mountain. coord 31 4 19 N 35 23 49 E type landmark display title Mount Sodom lang ar , Jabal u ssud m lang he , Har Sdom is a hill along the southwestern part of the Dead Sea in Israel . It is most remarkable because it is made almost entirely of halite , or rock salt. It is approximately five miles 8 km long, three miles 5 km wide, convert 742 ft m above the Dead Sea water level, yet convert 557 ft m below sea level . Because of weathering, sometimes portions become separated. One of these separate pillars has been labeled Lot s Wife rock formation Lot s Wife , a reference to Lot s wife in the Biblical account of the destruction of Sodom and Gomorrah . References reflist DEFAULTSORT Sodom Category Hebrew Bible mountains Category Mountains of Israel Category Dead Sea Category Dry areas below sea level he pl Sodom wzg rze ru ... more details
Unreferenced date December 2009 Orphan date December 2009 An anisodesmic crystal sometimes anisodemic crystal is a crystal containing chemical bond bonds with differing electrostatic valencies. All other crystals are known as isodesmic crystal s or isodemic and examples include diamond and halite . These terms are of particular importance when discussing the structural chemistry of mineral s. The electrostatic valency is a measure of the strength of bonds, being the valence charge divided by the coordination number . Linus Pauling s second rule of ionic bonding, the Electrostatic Valence Principle states, An ionic structure will be stable to the extent that the sum of the strengths of the electrostatic bonds that reach an anion equals the charge on that anion. When there is more than one type of bonding in a crystal, strongly anisotropic physical properties can result such as those of graphite . Many other substances have anisotropic physical properties. Such properties are directly related to the atomic structures of the substances. Conversely, halite is an example of an isotropic crystal with equal hardness in all directions. DEFAULTSORT Anisodesmic Crystal Category Crystals ... more details
Trapped in a time capsule the same size as the diameter of a human hair, the ore forming liquid in this inclusion was so hot and contained so much dissolved solids that when it cooled, crystals of halite, sylvite, gypsum, and hematite formed. As the samples cooled, the fluid shrank more than the surrounding mineral, and created a vapor bubble. Heating the inclusion to the temperature at which the bubble is reabsorbed and daughter crystals dissolve gives an estimate of the minimum temperature at the moment of ore formation. Source http minerals.cr.usgs.gov gips 0fluid.htm http minerals.cr.usgs.gov gips 0fluid.htm PD USGov Interior USGS ... more details
File Sylvinite.jpg thumb Sylvinite is the most important ore for the production of potash in North America . It is a mechanical mixture of sylvite KCl, or potassium chloride and halite NaCl, or sodium chloride . ref Weiss N.L., SME Mineral Processing Handbook 1985, Page 22 2 ref Most Canadian operations mine sylvinite with proportions of about 31 KCl and 66 NaCl with the balance being insoluble clays, anhydrite and in some locations carnallite . References references Category Mining Category Sedimentary rocks petrology stub mining stub fr Sylvinite lt Silvinitas ru ... more details
Dicdef Mud weight http www.glossary.oilfield.slb.com Display.cfm?Term mud 20weight as described in the oil industry oilfield is the density weight of the drilling fluid and is normally measured in pounds per gallon lb sub m sub gal or ppg . In the field it is measured using a mud scale or mud balance . In conventional drilling fluid s, barite is used to incresase the density weight . Though other additives such as halite salt or calcium carbonate can also be used. Mud weight can be decreased by dilution or solids control equipment such as an industrial centrifuge . Petroleum stub Category Petroleum engineering Category Oilfield terminology ... more details
No footnotes date April 2010 Image HaliteEncrustedCobbleDeadSea.JPG thumb Cobble encrusted with halite evaporated from the Dead Sea , Israel. Evaporite pron en v p ra t is a name for a water soluble mineral sedimentary rock sediment that result from the evaporation from an aqueous solution and has been concentrated by evaporation. ref name Jackson Jackson, Julia A., 1997, Glossary of Geology 4 sup th sup edition, American Geologic Institute, Alexandria Virginia ref There are two types of evaporate deposits, marine which can also be described as ocean deposits, and non marine which are found in standing bodies of water such as lakes. Evaporites are considered sedimentary rock s. Formation of evaporite rocks Although all water bodies on the surface and in aquifers contain dissolved salts, the water ... the mineral gypsum begins to form, which is then followed by halite at 10 . ref name Boggs Excluding ..., halite, sylvite, carnellite, langbeinite, polyhalite, and kanite. Kieserite MgSO sub 4 sub may also ... may also contain halite, gypsum, and anhydrite, and may in some cases even be dominated by these minerals ... cast of halite in a Jurassic rock, Carmel Formation, southwestern Utah. Evaporite formations need not be composed entirely of halite salt. In fact, most evaporite formations do not contain more ... simply require recognition of halite pseudomorph s, sequences composed of some proportion of evaporite ... in the production on fertilizer and explosive s. Thick halite deposits are expected to become ... engineering and physical behaviour and imperviousness to groundwater. Halite formations are famous ... Halite Sylvite Carnallite Langbeinite Polyhalite Kainite NaCl KCl KMgCl sub 3 sub 6H sub 2 sub ... crystal Halide mineral Halides halite , sylvite KCl , and fluorite Sulfate mineral Sulfates such as gypsum ... CaSO sub 4 sub 2H sub 2 sub O and anhydrite CaSO sub 4 sub . Halite i.e. common salt, NaCl Potassium ... , which is more common than halite , which is more common than potassium and magnesium salts. Evaporites ... more details
In Metallurgy , Materials Science and Structural geology continuous sub grain rotation type dynamic recrystallization is recognized as an important mechanism for dynamic recrystallisation . It involves the rotation of initially low angle sub grain boundaries until the mismatch between the crystal lattice s across the boundary is sufficient for them to be regarded as grain boundaries . This mechanism has been recognized in many minerals, including quartz , calcite , olivine , pyroxene s, mica s, feldspar s, halite and garnet s, and in metals various magnesium , aluminium and nickel alloys . References Microtectonics by C.W.Passchier and R.A.J.Trouw, 2nd rev. and enlarged ed., 2005, XVI, 366 p., 322 illus., with CD Dynamic recrystallization of minerals J. L. Urai, W. D. Means & G. S. Lister http www.ged.rwth aachen.de Ww projects rexx Urai 86Recrystallization Urai 86Recrystallization5.htm Li, J.C.M. Possibility of subgrain rotation during recrystallization. J. Appl. Phys. 33, 2958 2965. 1962 . Category Metallurgy Category Structural geology ... more details
Langbeinite is a potassium magnesium sulfate mineral with formula potassium K sub 2 sub magnesium Mg sub 2 sub sulfur S oxygen O sub 4 sub sub 3 sub . Langbeinite crystallizes in the Cubic crystal system isometric tetartoidal system as transparent colorless or white with pale tints of yellow to green and violet crystalline masses. It has a vitreous lustre mineralogy luster . The Mohs hardness is 3.5 to 4 and the specific gravity is 2.83. The crystals are phosphorescent and piezoelectric . The mineral is an ore of potassium and occurs in marine evaporite deposits in association with carnallite , halite and sylvite . It was first described in 1891 and named for A. Langbein of Leopoldshall, Germany. References http rruff.geo.arizona.edu doclib hom langbeinite.pdf Mineral Data Publishing http www.mindat.org min 2320.html Mindat with location data http www.webmineral.com data Langbeinite.shtml Webmineral data Category Sulfate minerals it Langbeinite nl Langbeiniet uk ... more details
on laminate kilkennymusic.com spotlight on Laminate http irishmusicdb.com h halitehalite familytree.htm Immodium, Wilt, Halite and Laminate family tree http www.last.fm music Laminate Laminate on Last.fm ... more details
This is a list of minerals, both metallic and non metallic. Metallic Aluminium Antimony Arsenic Bauxite Chromite Coal Copper Dolomite Gold Iron ore Fire clay Fluorite Glass sand Garnet Granite Graphite Gypsum Lead Magnesite Manganese Tungsten Zinc Non Metallic Asbestos Barite Brine Calcite Cinnabar Kaolinite Kaolin Kyanite Lignite Limenite Limestone Marble Mica Rock phosphate Potash Pyrite Quartz Radioactive minerals Halite Rock salt Sand Silica sand Soapstone Sulphur Vermiculite Vesuvianite Zircon See also Pakistan Mineral Development Corporation PMDC References Encyclopedia of Pakistan by Zahid Hussain Anjum , Jahangir Book Depot, Pakistan 2005 2006 Category Pakistan related lists Minerals of Pakistann ... more details
Infobox mineral name Hydrohalite category Halide mineral boxwidth boxbgcolor image imagesize alt caption formula NaCl 2H sub 2 sub O strunz 03.BA.05 dana symmetry Z molweight colour colourless or white habit system Monoclinic crystal system Monoclinic twinning cleavage fracture tenacity mohs luster streak diaphaneity transparent gravity density polish opticalprop refractive birefringence pleochroism 2V dispersion extinction length fast slow fluorescence absorption melt fusibility diagnostic solubility other alteration references Hydrohalite is a mineral that occurs in saturated halite brines at cold temperatures &minus 5 C . It was first described in 1847 in Salzburg , Austria . References http www.mindat.org min 1975.html Hydrohalite mineral information and data http www.webmineral.com data Hydrohalite.shtml Hydrohalite Mineral Data Category Halide minerals Category Sodium minerals halide mineral stub ... more details
Image Death Valley Devil s Golf Course.jpg thumb Devil s Golf Course. Image DevilsGolfCourse031411.jpg thumb Devil s Golf Course. The Devil s Golf Course is a large salt pan geology salt pan on the floor of Death Valley , located in the Mojave Desert within Death Valley National Park in eastern California . It was named after a line in the 1934 National Park Service guide book to Death Valley National Monument, which stated that Only the devil could play golf on its surface, due to a rough texture from the large Halite Halite salt crystal formations. ref http www.nps.gov deva planyourvisit furnacecreekarea.htm ref Description Lake Manly once covered the valley to a depth of convert 30 ft m . The salt in the Devil s Golf Course consists of the minerals that were dissolved in the lake s water and left behind in the Badwater Basin as the lake evaporated. With an elevation several feet above the valley floor at Badwater , the Devil s Golf Course remains dry, allowing weathering processes to sculpt the salt there into complicated forms. Through exploratory holes drilled by the Pacific Coast Borax Company , prior to Death Valley becoming a national monument in 1934, it was discovered that the salt and gravel beds of the Devil s Golf Course extend to a depth of more than convert 1000 ft m . Later studies suggest that in places the depth ranges up to convert 9000 ft m . ref http www.uoregon.edu millerm DVSP.html ref Access Devil s Golf Course can be reached from Badwater Road via a convert 1.3 mi km sing on gravel drive, closed in wet weather. It should not be confused with an actual golf course in Furnace Creek, California Furnace Creek , also in Death Valley. See also Racetrack Playa Places of interest in the Death Valley area References Reflist External links http www.nps.gov deva planyourvisit furnacecreekarea.htm National Park Service Death Valley National Park the Furnace Creek Area Death Valley coord missing California Category Death Valley Category Death Valley Nati ... more details
Infobox mineral name Zabuyelite category Carbonate mineral boxwidth boxbgcolor image caption formula Li sub 2 sub CO sub 3 sub molweight 73.89 strunz 05.AA.05 dana color Colorless habit system Monoclinic 2 m , Space group C2 c lattice twinning cleavage 100 perfect 011 good fracture tenacity Brittle mohs 3 luster refractive n sub sub 1.4285, n sub sub 1.5672, n sub sub 1.5743 opticalprop Biaxial 2V 25 birefringence 0.1458 pleochroism none streak White gravity 2.09 density melt fusibility diagnostic solubility diaphaneity other references ref name Webmin http webmineral.com data Zabuyelite.shtml Zabuyelite at Webmineral ref ref name Mindat http www.mindat.org min 2166.html Zabuyelite at Mindat ref ref name HDM http www.handbookofmineralogy.org pdfs zabuyelite.pdf Zabuyelite at Handbook of Mineralogy ref Zabuyelite is the natural mineral form of lithium carbonate , with a chemical formula formula lithium Li sub 2 sub carbon C oxygen O sub 3 sub . It was discovered in 1987 at Lake Zabuye , Tibet , after which it is named. It forms colorless vitreous monoclinic crystals. It occurs as inclusions within halite in lithium rich evaporite s and as solid phase in fluid inclusions in the mineral spodumene . Associated minerals include halite, gaylussite and northupite in the Tibet locality. ref name HDM In addition to the Tibetan salt lake it has been reported from Bikita and Kamativi in Zimbabwe , from Kings Mountain, North Carolina Kings Mountain , Cleveland County, North Carolina , USA and the Tanco pegmatite , Bernic Lake , Manitoba , Canada. ref name HDM References reflist Category Lithium minerals Category Carbonate minerals Carbonate mineral stub it Zabuyelite ... more details
Image SaltGlaciers ZagrosMtns 20010810.jpg thumb Salt domes hills and salt glaciers dark areas in the Zagros Mountains of southern Iran . A salt glacier is a flow of salt typically halite that is created when a rising diapir in a salt dome breaches the surface. Gravity causes the salt to flow like glaciers into adjacent valleys. Most of the flow occurs during the winter, when the salt is wet, as the strength of salt is critically dependent on its water content. The resulting tongue shaped bodies can extend for kilometers, with repeating bow shaped ridges separated by crevasse like gullies and with steep sides and fronts. Clays may be brought up with the salt, turning it dark. The salt glaciers of Iran ref cite web url http earthobservatory.nasa.gov Newsroom NewImages images.php3?img id 16435 title Iran s Salt Glaciers work NASA Earth Observatory accessdate 2006 04 27 ref ref Talbot, C.J. and Rogers, E.A. 1980. Seasonal movements in a salt glacier in Iran . Science , 208 , 395 397. ref are halite while the salt glacier of L neburg Kalkberg , Germany is gypsum and other carbonate s. References references Urai, J.L., Spiers, C.J., Zwart, H.J. & Lister, G.S. 1986. Weakening of rock salt by water during long term creep. Nature, 324, 554 557 Category Sediments geology stub ca Glacera salina de Salzgletscher es Glaciar salino fa ja ... more details
are hand carved in the halite rock. Some marble sculptures are included. The Salt Cathedral is considered ... 14 9 46. ref History The halite mines were exploited already by the pre Columbian Muisca culture ... , No. 1, enero abril de 1978, p. 39 41 ref The traditional halite mining was described by Alexander ... this deposit as bigger than the main halite mines of the time, such as those in Spain , Switzerland ... the halite tunnels don t require Beam structure beams , lowering the costs. ref http www.epigrafe.com ... kneeling platforms carved into the halite structure. The Dome Located at the end of the main ... Axis A town square square with an halite hand carved cross 4.20 Meter s height The Salt ... from the halite. Also, exhibitions of the geological studies, engineering and architecture process ... more details
Polyhalite is an evaporite mineral, a hydrated sulfate of potassium , calcium and magnesium with formula K sub 2 sub Ca sub 2 sub Mg SO sub 4 sub sub 4 sub · 2 H sub 2 sub O . Polyhalite crystallizes in the triclinic system although crystals are very rare. The normal habit is massive to fibrous. It is typically colorless, white to gray, although it may be brick red due to iron oxide inclusions. It has a Mohs hardness of 3.5 and a specific gravity of 2.8. It occurs in sedimentary marine evaporites and is a major potassium ore mineral in the Carlsbad Deposits of New Mexico . Polyhalite was first described in 1818 for specimens from its type locality in Salzberg , Austria . The name is from the Greek language Greek polys hals for many salts . It has no connection to the sodium halide mineral halite other than that both are evaporite minerals. References http www.mindat.org min 3259.html Mindat with location data http webmineral.com data Polyhalite.shtml Webmineral http mineral.galleries.com minerals sulfates polyhali polyhali.htm Mineral galleries Category Magnesium minerals Category Calcium minerals Category Potassium minerals Category Sulfate minerals Category Triclinic minerals Sulfate mineral stub ca Polihalita de Polyhalit it Polihalite uk vi Polyhalit ... more details
expert subject Geology date April 2010 Keuper marl is the former name for a layer of mudstone s and siltstone s from the late Triassic period formerly known as the Keuper period . Typically red, or occasionally green or grey, it is featureless and contains few fossils. In basin formations, thick halite bearing layers, or rock salt deposits, are sometimes present at the base of the marl. In modern nomenclature, Keuper marl is included within the Mercia Mudstone Group . ref name BGS http www.bgs.ac.uk lexicon lexicon.cfm?pub MMG British Geological Survey Lexicon of Named Rock Units Mercia Mudstone Group accessed 10 April 2010 ref ref http www.jncc.gov.uk pdf gcrdb v24chap1.pdf Benton M, Cook E, Turner P. Permian and Triassic Red Beds and the Penarth Group of Great Britain , pp. 11, 19. Geological Conservation Review Series , No. 24 Joint Nature Conservation Committee 2002 ISBN 1 86107 493 X ref In England, Keuper marl is found in Cheshire , ref name BGS Nottinghamshire , ref name BGS Devon , eastern Worcestershire and northern Yorkshire . Citation needed date April 2010 References Reflist DEFAULTSORT Keuper Marl Category Sedimentary rocks Category Triassic geologic formations ... more details
her Mercury Music Prize Mercury Music Prize 2002 nominated album Night on My Side . Halite Hopkins then went on to record two albums with his own band Halite. Halite began as a solo project ... and Derren Dempsey if they would tour with him. Halite then grew into a fully formed band. They soon ... of a harder and frantic edge than the first album. Halite played numerous shows over the following two ... more details
Valley . It is associated with halite , borax , trona and aphthitalite in the Searles Lake area. ref ... Hanksite halite borax trona nahcolite tincalconite References Reflist Category Sodium minerals Category ... more details
Unreferenced date January 2008 image Bismuth crystal macro.jpg thumb 300px right Synthetic bismuth crystal A hopper crystal is a form of crystal , defined by its Gravity wagon hopper ed shape. The edges of hoppered crystals are fully developed, but the interior spaces are not filled in. This results in what appears to be a hollowed out step lattice mathematics lattice formation, as if someone had removed interior sections of the individual crystals. In fact, the removed sections never filled in, because the crystal was growing so rapidly that there was not enough time or material to fill in the gaps. The interior edges of a hoppered crystal still show the crystal form characteristic to the specific mineral , and so appear to be a series of smaller and smaller stepped down miniature versions of the original crystal. Hoppering occurs when electricity electrical attraction is higher along the edges of the crystal, causing faster growth at edges than near face centers. This attraction draws the mineral molecule s more strongly than the interior sections of the crystal, thus the edges develop more quickly. Hoppering is common in many minerals, including lab grown bismuth , galena , quartz called skeletal or fenster crystals , gold , calcite , halite salt , and water ice . References http www.wolframscience.com nksonline page 993c text Hopper crystals in A New Kind of Science by Stephen Wolfram , p. 993. External links http www.gc.maricopa.edu earthsci imagearchive bismuth.htm Pictures Category Crystals ... more details
For places in Schleswig Holstein in Germany Rheide disambiguation In geology , a rheid IPA en ri d is a solid material that deforms by viscosity viscous flow. The term has the same greek root as rheology , the science of viscoelasticity and nonlinear flow. Types of rheids Almost any type of rock geology rock can behave as a rheid under appropriate conditions of temperature and pressure . For example, the Earth s mantle geology mantle is believed to undergo convection over long time scales. Since the mantle is known to be solid it supports the propagation of seismic waves shear waves , it must be behaving as a rheid. Granite has a measured viscosity at Standard conditions for temperature and pressure standard temperature and pressure of about 4.5× 10 sup 19 sup Pa s ref cite journal last Kumagai first Naoichi coauthors Sadao Sasajima, Hidebumi Ito title Long term Creep of Rocks Results with Large Specimens Obtained in about 20 Years and Those with Small Specimens in about 3 Years journal Journal of the Society of Materials Science Japan volume 27 issue 293 pages 157 161 publisher Japan Energy Society url http translate.google.com translate?hl en&sl ja&u http ci.nii.ac.jp naid 110002299397 &sa X&oi translate&resnum 4&ct result&prev search 3Fq 3DIto 2BHidebumi 26hl 3Den date 15 February 1978 accessdate 2008 06 16 ref so it should be considered a rheid. Halite , the mineral form of sodium chloride salt , is a geological material that behaves as a rheid over relatively short time periods. As salt is buried by other types of sedimentary rock sediments , it will often flow laterally towards regions of less confining stress physics stress . Through this mechanism, salt dome s and other structures are formed. In some areas, such as the Gulf of Mexico , these structures often serve as traps for petroleum and natural gas . References reflist Category Structural geology geol stub it Reido geologia pt Rheid ... more details
Cleanup date July 2009 Image ImgSalt.jpg thumb 150px right Rock salt crystal Bahadur Khel is a village and Union Councils of Pakistan Union Council of Karak District in Khyber Pakhtunkhwa province of Pakistan . ref http www.nrb.gov.pk lg election union.asp?district 59&dn Karak Tehsils & Unions in the District of Karak Government of Pakistan ref It is located at 33 10 57N 70 57 15E with an altitude of 548 metres 1801 feet , ref http www.fallingrain.com world PK 3 Bahadur Khel.html Location of Bahadur Khel Falling Rain Genomics ref the village is the site of an extensive halite rock salt quarry. The quarry one mile long by half a mile broad produce high quality rock salt suitable for human consumption. The facility is managed by the Pakistan Mineral Development Corporation. History During British Raj British rule the area was part of the old Kohat Division Kohat District ref http dsal.uchicago.edu reference gazetteer pager.html?objectid DS405.1.I34 V03 194.gif Mines and Minerals Imperial Gazetteer of India, v. 3, p. 159. ref and the facility was under the control of the Northern India Salt Department, a government body of British India . Bahader Khel is union council which is 7 big villages Bahader Khel Darish Khel Ghol Banda Anar Banda Shaheedan Banda Charpara banda Shaheedan Darish Khel is the oldest village of this area. References Wikisource1911Enc Bahadur Khel Reflist coord 33 10 57 N 70 57 15 E region PK type city display title Category Populated places in Khyber Pakhtunkhwa NorthWestFrontier geo stub ... more details
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