Aravalli Range

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Aravalli Range
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{{about|the mountain range in western India|information about the district in Gujarat state|Aravali district}}{{short description|Mountain range in western India}}{{Use Indian English|date=January 2018}}{{Use dmy dates|date=January 2018}}

| range = 24337430type:mountain_region:INdisplay=inline}}2573.5type:mountain_region:INdisplay=inline,title}}| coordinates_ref =| length_km = 692| length_orientation = | width_km = | width_orientation =| area_km2 =| topo = | type = | age =| volcanic_arc = | volcanic_belt = | volcanic_field = | volcanic_arc/belt = | last_eruption = | first_ascent =| easiest_route = | normal_route = | access = | child = | embedded =India}}| state = Rajasthan| state1 = Haryana| state2 = Delhi| state3 = Gujarat| region = North India, Western India| border = | city = Delhi, Gurgaon, Mount Abu| part_type = RiversBanas River>BanasLuni River>Luni| part2 = SakhiSabarmati River>Sabarmati| geology = Fold mountains from Plate tectonics | orogeny = Aravalli-Delhi Orogen | period = Precambrian }}The Aravalli Range (Devanagari, also spelled Aravali range, is a range of mountains running approximately 692 km (430 mi) in a southwest direction, starting in North India from Delhi and passing through southern Haryana,WEB,weblink Aravalli Biodiversity Park, Gurgaon, yes,weblink" title="">weblink 2012-05-28, through to Western India across the states of Rajasthan and ending in Gujarat.{{citation|last=Kohli|first=M.S.|title=Mountains of India: Tourism, Adventure, Pilgrimage|url=|year=2004|publisher=Indus Publishing|isbn=978-81-7387-135-1|pages=29–}}BOOK,weblink Aravali Range, Students' Britannica India, Dale Hoiberg, Indu Ramchandani, Popular Prakashan, 2000, 978-0-85229-760-5, 92–93, Mount Abu is the highest peak in the mountain range at 5650 feet.


Aravalli, a composite Sanskrit word from "ara" and "vali", literally means the "line of peaks".BOOK, The Geography of British India, Political & Physical, George Smith, J. Murray, 1882, 23, WEB,weblink Aravali Range,,

Natural History


{{see also | Geology of India }}
(File:Indiahills.png|thumb|300px|Map of prominent mountain ranges in India, showing Aravalli in north-west India)The Aravalli Range, an eroded stub of ancient mountains, is the oldest range of fold mountains in India.Roy, A. B. (1990). Evolution of the Precambrian crust of the Aravalli Range. Developments in Precambrian Geology, 8, 327–347. The natural history of the Aravalli Range dates back to times when the Indian Plate was separated from the Eurasian Plate by an ocean. The Proterozoic Aravalli-Delhi orogenic belt in northwest India is similar to the younger Himalayan-type orogenic belts of the Mesozoic-Cenozoic era (of the Phanerozoic) in terms of component parts and appears to have passed through a near-orderly Wilson supercontinental cycle of events. The range rose in a Precambrian event called the Aravalli-Delhi Orogen. The Aravalli Range is a northeast-southwest trending orogenic belt that is located in the northwestern part of Indian Peninsula. It is part of the Indian Shield that was formed from a series of cratonic collisions.Mishra, D.C.; Kumar, M. Ravi. Proterozoic orogenic belts and rifting of Indian cratons: Geophysical constraints. Geoscience Frontiers. 2013 March. 5: 25–41. In ancient times, Aravalli were extremely high but since have worn down almost completely by millions of years of weathering, whereas the Himalayas being young fold mountains are still continuously rising. Aravalli, being the old fold mountains, have stopped growing higher due to the cessation of upward thrust caused by the stopping of movement of the tectonic plates in the Earth's crust below them. The Aravalli Range joins two of the ancient earth's crust segments that make up the greater Indian craton, the Aravalli Craton which is the Marwar segment of earth's crust to the northwest of the Aravalli Range, and the Bundelkand Craton segment of earth's crust to the southeast of the Aravalli Range. Cratons, generally found in the interiors of tectonic plates, are old and stable parts of the continental lithosphere that has remained relatively undeformed during the cycles of merging and rifting of continents.(File:Subduction-en.svg|thumb|240px|volcanic arc and geological process of undersea subduction during tactonic collusion)File:ConMarRJS.jpg|thumb|240px|global convergent boundary of plate margins ]]It consists of two main sequences formed in Proterozoic eon, metasedimentary rock (sedimentary rocks metamorphised under pressure and heat without melting) and metavolcanic rock (metamorphised volcanic rocks) sequences of the Aravalli Supergroup and Delhi Supergroup. These two supergroups rest over the Archean Bhilwara Gneissic Complex basement, which is a gneissic (high-grade metamorphism of sedimentary or igneous rocks) basement formed during the archean eon 4 Ga ago. It started as an inverted basin, that rifted and pulled apart into granitoid basement, initially during Aravalli passive rifting around 2.5 to 2.0 Ga years ago and then during Delhi active rifting around 1.9 to 1.6 Ga years ago. It started with rifting of a rigid Archaean continent banded gneissic complex around 2.2 Ga with the coexisting formation of the Bhilwara aulacogen in its eastern part and eventual rupturing and separation of the continent along a line parallel to the Rakhabdev (Rishabhdev) lineament to the west, simultaneous development of a passive continental margin with the undersea shelf rise sediments of the Aravalli-Jharol belts depositing on the attenuated crust on the eastern flank of the separated continent, subsequent destruction of the continental margin by accretion of the Delhi island arc (a type of archipelago composed of an arc-shaped chain of volcanoes closely situated parallel to a convergent boundary between two converging tectonic plates) from the west around 1.5 Ga. This tectonic plates collision event involved early thrusting with partial obduction (overthrusting of oceanic lithosphere onto continental lithosphere at a convergent plate boundary) of the oceanic crust along the Rakhabdev lineament, flattening and eventual wrenching (also called strike-slip plate fault, sideways horizontal movement of colliding plates with no vertical motion) parallel to the collision zone. Associated mafic igneous rocks show both continental and oceanic tholeiitic geochemistry (magnesium and iron-rich igneous rocks) from phanerozoic eon (541–0 million) with rift-related magmatic rock formations.P. K. VermaR. O. Greiling, December 1995, "Tectonic evolution of the Aravalli orogen (NW India): an inverted Proterozoic rift basin?", Geologische Rundschau, Volume 84, Issue 4, pp 683–696.The Aravalli-Delhi Orogen is an orogen event that led to a large structural deformation of the Earth's lithosphere (crust and uppermost mantle, such as Aravalli and Himalayas fold mountains) due to the interaction between tectonic plates when a continental plate is crumpled and is pushed upwards to form mountain ranges, and involve a great range of geological processes collectively called orogenesis.BOOK, Foundations of Engineering Geology, Tony Waltham, 20,weblink 978-0-415-46959-3, Taylor & Francis, 2009, 3rd, BOOK, Global Tectonics, Philip Kearey, Keith A. Klepeis, Frederick J. Vine,weblink 287, Chapter 10: Orogenic belts, 978-1-4051-0777-8, 2009, Wiley-Blackwell, 3rd,


The archean basement had served as a rigid indentor which controlled the overall wedge shaped geometry of the orogen. Lithology of area shows that the base rocks of Aravalli are of Mewar Gneiss formed by high-grade regional metamorphic processes from preexisting formations that were originally sedimentary rock with earliest life form that were formed during the archean eon, these contain fossils of unicellular organism such as green algae and cyanobacteria in stromatolitic carbonate ocean reefs formed during the paleoproterozoic era. Sedimentary exhalative deposits of base metal sulfide ores formed extensively along several, long, linear zones in the Bhilwara aulacogen or produced local concentration in the rifted Aravalli continental margin, where rich stromatolitic phosphorites also formed. Tectonic evolution of the Aravalli Mountains shows Mewar Geniss rocks are overlain by Delhi Supergroup type of rocks that also have post-Aravalli intrusions. Metal sulfide ores were formed in two different epocs, lead and zinc sulfide ores were formed in the sedimentary rocks around 1.8 Ga years ago during Paleoproterozoic phase. The tectonic setting of Zinc-lead-copper sulfides mineralization in Delhi supergroup rocks in Haryana-Delhi were formed in mantle plume volcanic action around 1 Ga years ago covering Haryana and Rajasthan during mesoproterozoic. In the southern part of Aravalli supergroup arc base metal sulfides were generated near the subduction zone on the western fringe and in zones of back-arc extension to the south-east. Continued subduction produced W-Sn (Tungsten-Tin) mineralisation in S-type (sedimentary unmetamorphosed rock) felsic (volcanic rock) plutons (underground crystallised solidified magma). This includes commercially viable quantities of minerals, such as rock phosphate, lead-zinc-silver mineral deposits at Zawar, Rikahbdev serpentinite, talc and pyrophyllite) and asbestos, apatite, kyanite and beryl.M. Deb and Wayne David Goodfellow, 2004, "Sediment Hosted Lead-Zinc Sulphide Deposits", Narosa Publishing, pp 260.Naveed Qamar, "Indian shield rocks".


Mining of copper and other metals in the Aravalli range dates back to at least the 5th century BCE, based on carbon dating.SM Gandhi (2000) Chapter 2 – Ancient Mining and Metallurgy in Rajasthan, Crustal Evolution and Metallogeny in the Northwestern Indian Shield: A Festschrift for Asoke Mookherjee, {{ISBN|978-1842650011}}Shrivastva, R. (1999). Mining of copper in ancient India. Indian Journal of History of Science, 34, 173–180 Recent research indicates that copper was already mined here during the Sothi-Siswal period going back to c. 4000 BCE. Ancient Kalibangan and Kunal, Haryana settlements obtained copper here.Jane McIntosh, The Ancient Indus Valley: New Perspectives. Understanding ancient civilizations. ABC-CLIO, 2008 {{ISBN|1576079074}} p77

Geographical features

{{See also|Tectonic evolution of the Aravalli Mountains#General formation}}File:Arbuda Mountains.JPG|thumb|upright=1.2|The Aravalli Range, seen from the range's highest point at Guru ShikharGuru ShikharThe Indian Craton includes five major cratons. Cratons are part of continental crust made up of upper layer called platforms and older bottom layer called basement rocks. sheilds are part of a craton where basement rock crops out at the surface and it is the relatively oldest and most stable part that are undeformed by the plate tectonics. The Aravalli Craton (Marwar-Mewar Craton or Western Indian Craton) covers Rajasthan as well as western and southern Haryana. It includes the Mewar Craton in the east and Marwar Craton in the west. It is limited by the Great Boundary Fault in the east, the Thar desert in the west, Indo-ganetic alluvium in the north, and the Son River-Narmada River-Tapti River basins in the south. It mainly has quartzite, marble, pelite, greywacke and extinct volcanos exposed in the Aravalli-Delhi Orogen. Malani Igneous Suite is the largest in India and third largest igneous suit in the world.Cratons of India.Cratons of India, The uniqueness of the geological feature of Malani Igneous Suite at Jodhpur prompted the Geological Survey of India to declare the site as a National Geological Monument.BOOK, National Geological Monuments, 2009-03-23, Jodhpur Group-Malani Igneous Suite Contact, 65–67, Geological Survey of India, 27 Jawaharlal Nehru Road, Kolkata,700016, 2001,weblink

Tatctonic-stratigraphic evolution

Tatctonic-stratigraphic evolution of the Aravalli Range:

Stratigrpahic classification

The Stratigraphic classification Aravalli Range can be divided into the following parts (north to south direction):
  • The Archean basement is a banded gneissic complex with schists (medium grade metamorphic rock), gneisses (high grade regional metamorphic rock), composite gneiss and quartzites. It forms the basement rock for both Delhi Supergroup and Aravalli Supergroup.
  • Aravalli Supergroup: The Aravalli supergroup passes through Rajasthan state, dividing it into two halves, with three-fifths of Rajasthan on the western side towards Thar Desert and two third on the eastern side consisting of the catchment area of Banas and Chambal rivers bordering the state of Madhya Pradesh. Guru Shikhar, the highest peak in the Aravalli Range at 5650 feet (1722 meters) in Mount Abu of Rajasthan, lies near the south-western extremity of the Central Aravalli range, close to the border with Gujarat state. The southern Aravalli Supergroup enters the northeast of Gujarat near Modasa where it lends its name to the Aravalli district, and ends at the center of the state at Palanpur near Ahmedabad.
    • Champaner Group is a rectangular outcrop composed of subgreywacke, siliceous phyllite, pelitic schist, quartzite and pertomict conglomerate.
    • Lunavada Group is a polygon area in the south of Aravali Orogen composed of greywacke-phyllite
    • Jharol Group is spread over 200 km2 area with average width of 40 km carbonate-free phyllite and arenite with turbidite facies and argillaceous rocks.
    • Udaipur Group is a thick accumulation of greywacke-phyllite basement overlain by dolomite.
    • Debari Group (Delbari Group) consists of carbonates, quartzite, and pelitic rocks which are overlain by the Delwara group.
    • Delwara Group is spread over 500 km2 area with average width of 500 m and includes basement orthoquartzite overlain by volcanic congolomerate.
    • Unconformities
      • Mangalwar/Sandmata Complex and Mewar Gneiss with enclaves of the Jagat group
  • Delhi Supergroup
Tosham Hill range basement rocks include quartzite with chiastolite, the upper layers of quartz porphyry ring dyke, felsite, welded tuff and muscovite biotite granite rocks which have commercially nonviable tin, tungsten and copper. The Tosham Hill range, west of Bhiwani in Haryana, is the northernmost end of the Aravalli range. A northeastern extension of the Aravalli extends to the national capital of India also. Locally known as a ridge it diagonally traverses to the South Delhi (hills of Asola Bhatti Wildlife Sanctuary), where at the hills of Bandhwari, it meets the Haryana Aravalli range consisting of various isolated hills and rocky ridges passing along the southern border of Haryana.Bhuiyan, C., Singh, R. P., & Kogan, F. N. (2006). Monitoring drought dynamics in the Aravalli region (India) using different indices based on ground and remote sensing data. International Journal of Applied Earth Observation and Geoinformation, 8(4), 289–302 Madhogarh hill Satnali hill Nuh-Ferozepur Jhirka hill range, runs along Haryana-Rajasthan border from Nuh to the south of Ferozepur Jhirka.
      • Rajasthan Alwar range, in the east
    • Ajabgarh Group - Kumbhalgarh Group with carbonate, mafic volcanic and argillaceous rocks
    • Raialo Group with mafic volcanic and calcareous rocks

Human history

The Aravalli Range has been site of three broad stages of human history, early stone age saw the use of flint stones; mid-stone age starting from 20,000 BP saw the domestication of cattle for agriculture; and post stone age starting from 10,000 BP saw the development of the Kalibangan civilization, 4,000 years old Aahar civilization and 2,800 years old Gneshwar civilization, Aarayan civilization and Vedic era civilizations.

Ganeshwar sunari Cultural Complex

Ganeshwar sunari Cultural Complex (GSCC) is a collection of third millennium BC settlements in the area of the Aravalli Hill Range. Among them, there are similarities in material culture, and in the production of copper tools. They are located near the copper mines."The GSCC is east of the Harappan culture, to the north-east of Ahar-Banas Complex, north/north west to the Kayatha Culture and at a later date, west of the OCP-Copper Hoard sites (Ochre Coloured Pottery culture-Copper Hoard Culture). Located within the regions of the Aravalli Hill Range, primarily along the Kantli, Sabi, Sota, Dohan and Bondi rivers, the GJCC is the largest copper producing community in third millennium BC South Asia, with 385 sites documented. Archaeological indicators of the GSCC were documented primarily in Jaipur, Jhunjhunu, and Sikar districts of Rajasthan, India ..."Uzma Z. Rizvi (2010) Indices of Interaction: Comparisons between the Ahar-Banas and Ganeshwar Jodhpura Cultural Complex {{webarchive |url= |date=May 9, 2016 }}, in EASAA 2007: Special Session on Gilund Excavations, edited by T. Raczek and V. Shinde, pp. 51–61. British Archaeological Reports: ArchaeoPressAmong their pottery, we find the incised ware, and reserved slipware.There are two main type sites, Ganeshwar, and Sunari, in Tehsil Kot Putli, Jaipur District (Geo coordinates: N 27° 35' 51", 76° 06' 85" E).


(File:Water body within the Sariska Reserve, Rajasthan.jpg|thumb|240px|A lake nested within Aravali Hills.)


The Northern Aravalli range in Delhi and Haryana has humid subtropical climate and hot semi-arid climate continental climate with very hot summers and relatively cool winters.WEB,weblink Climate of Hisar, PPU, 27 May 2012, yes,weblink" title="">weblink 5 May 2012, dmy-all, The main characteristics of climate in Hisar are dryness, extremes of temperature, and scanty rainfall.WEB,weblink Climate of Hisar, District Administration, Hisar, 27 May 2012,weblink" title="">weblink 27 March 2012, yes, The maximum daytime temperature during the summer varies between {{Convert|40|and|46|C|F}}. During winter, its ranges between 1.5 and 4 Â°C.NEWS,weblink More snowfall in Himachal, The Hindu, 24 March 2016, The Central Aravalli range in Rajasthan has an arid and dry climate.The Southern Aravalli range in Gujarat has a tropical wet and dry climate


Three major rivers and their tributaries flow from the Aravalli, namely Chambal and Sahibi rivers which are tributaries of Yamuna, as well as Loni river which flows into the Rann of Kutch. Berach River, a southern-side tributary of Banas River, originates in the hills of Udaipur District.* Ahar River, a right-side (or eastern side) tributary of the Berach river, originates in the hills of Udaipur District, flows through Udaipur city forming the famous Lake Pichola.* Wagli River, a right-side tributary of the Berach River.* Wagon River, a right-side tributary of the Berach River.* Gambhiri River, a right-side tributary of the Berach river. * Orai River, a right-side tributary of the Berach River.


Wildlife corridors

Northern Aravalli leopard and wildlife corridor

(File:Charging Leopard-001.JPG|thumb|upright|Charging Indian Leopard.){{anchor | Northern Aravalli wildlife corridor | Sariska-Delhi wildlife corridor | Northern Aravalli leopard wildlife corridor | Sariska-Delhi leopard wildlife corridor }}The Sariska-Delhi leopard wildlife corridor or the Northern Aravalli leopard wildlife corridor is a 200 km long important biodiversity and wildlife corridor which runs from the Sariska Tiger Reserve in Rajasthan to Delhi Ridge.Haryana Government moots buffer zone to save Asola sanctuary, Times of India, 30 Jan 2019.This corridor is an important habitat for the Indian leopards and jackals of Aravalli. In January 2019, the Wildlife Institute of India announced that they will undertake the survey of leopard and wildlife, using pugmarks and trap cameras, subsequently, leopards and jackals will be tracked via the radio collars. Urban development, especially the highways and railways bisecting the Aravalli range and wildlife corridor in several places pose a great risk. Large parts of Aravalli are legally and physically unprotected, with no wildlife passages and little or no wildlife conservation work resulting in deaths of over 10 leopards in 4 years between January 2015 to January 2019.Death, proof of leopard life in Asola sanctuary, Hindustan Times, 31 Jan 2019.10-month-old leopard found dead on Gurugram-Faridabad Expressway, India Today, 31 Jan 2019.Leopard killed in accident on Gurugram-Faridabad road, Times of India, 30 Jan 2019.The Haryana side of the Gurugram-Faridabad Aravalli hill forests lack availability of water due to which wild animals are seldom seen there. The Government of Haryana used drones for aerial survey and dug 22 ephemeral pits in 2018 to store the rainwater which become dry during the summer months. In January 2019, the government announced the plan to make the pit perennial by connecting those with pipelines from the nearby villages.Leopards keep away from Haryana side of Asola due to scarcity, Times of India, 1 Feb 2019.Human activity, such as unplanned urbanization and polluting plants, also pose a great threat. There is often reluctance and denial on part of the government officials of the presence of wildlife such as leopard so that the forest land can be exploited and opened up for the intrusive human development.Only 30 villagers turn up for impact study, Times of India, 2018.NGT asks CPCB to test groundwater sample near Bandhwari plant, India Today, 1 Aug 2017.

Southern Aravalli leopard wildlife corridor

This corridor runs from Sariska and Ranthmbor to Gujarat.

Nature reserves

File:Asokan Pillar.JPG|thumb|upright|Ashoka pillar at Delhi Ridge, brought to Delhi from Topra Kalan by Firuz Shah TughlaqFiruz Shah TughlaqThe following national parks, wildlife reserves, and forests lie in the Aravlli range.


The Aravalli Range has several forests with a diversity of environment.Aravalis in Gurugram, Faridabad core area for leopards, finds survey, The Times of India], 17 June 2017]


(File:Ranthambore National Park.JPG|thumb|240px|Ranthambore National Park, in Rajasthan.)The Aravalli Range is rich in wildlife. The first ever 2017 wildlife survey of a 200 square kilometer area crossing five districts (Gurgaon, Faridabad, Mewat, Rewari and Mahendergarh) of Haryana by the Wildlife Institute of India (WII) found 14 species, including leopards, striped hyena (7 sightings), golden jackal (9 sightings, with 92% occupancy across the survey area), nilgai (55 sightings), palm civet (7 sightings), wild pig (14 sightings), rhesus macaque (55 sightings), peafowl (57 sightings) and Indian crested porcupine (12 sightings). Encouraged by the first survey, the wildlife department has prepared a plan for a comprehensive study and census of wildlife across the whole Aravalli Range, including radio collar tracking of the wild animals. Well known leopard and hyena habitat is along the Ferozpure Jhirka-Nuh aravali range as well as Delhi South Ridge (Faridabad-Gurugram) to Farrukhnagar area on the Delhi-Haryana border, with reports of sightings in Saidpur, Lokri and Jhund Sarai Viran villages near the KMP expressway; Bhukarka 7 km from Pataudi; Pathkori, Bhond, Mandawar in Ferozepur Jirka region.Traps set up in four villages of Farrukhnagar after leopard’s presence confirmed by pug marks, Hindustan Times, 18 Jan 2019.


In May 1992, some parts of the Aravalli hills in Rajasthan and Haryana were protected from mining through the Ecologically Sensitive Areas clauses of Indian laws. In 2003, the central government of India prohibited mining operations in these areas. In 2004, India's Supreme Court banned mining in the notified areas of Aravalli Range. In May 2009, the Supreme Court extended the ban on mining in an area of 448 km2 across the Faridabad, Gurgaon and Mewat districts in Haryana, covering the Aravalli Range.SC bans all mining activity in Aravali hills area of Haryana, 9 May 2009.Mission Green: SC bans mining in Aravali hills {{Webarchive|url= |date=8 June 2009 }} Hindustan Times, 9 May 2009.A 2013 report used high-resolution Cartosat-1 & LISS-IV satellite imaging to determine the existence and condition of mines in the Aravalli Range. In the Guru Gram district, the Aravalli hills occupy an area of 11,256 hectares, of which 491 (4.36%) hectares had mines, of which 16 hectares (0.14%) were abandoned flooded mines. In the Faridabad and Mewat districts, about 3610 hectares were part of mining industry, out of a total of 49,300 hectares. These mines were primarily granite and marble quarries for India's residential and real estate construction applications.Rai and Kumar, MAPPING OF MINING AREAS IN ARAVALLI HILLS IN GURGAON, FARIDABAD & MEWAT DISTRICTS OF HARYANA USING GEO-INFORMATICS TECHNOLOGY, International Journal of Remote Sensing & Geoscience, Volume 2, Issue 1, Jan. 2013 In the Central Rajasthan region, Sharma states that the presence of some mining has had both positive and negative effects on neighboring agriculture and the ecosystem. The rain-induced erosion brings nutrients as well as potential contaminants.Sharma, K. C. (2003). Perplexities and Ecoremediation of Central Aravallis of Rajasthan. Environmental Scenario for 21st Century, {{ISBN|978-8176484183}}, Chapter 20


The Aravali Range is the source area of many rivers, resulting in development of human settlements with sustainable economy since pre-historic times. The Delhi Mumbai Industrial Corridor Project, Western Dedicated Freight Corridor, Mumbai–Ahmedabad high-speed rail corridor, North Western Railway network, Jaipur-Kishangarh Expressway and Delhi-Jaipur Expressway, all run parallel to the length of the Aravalli Range providing an economic boost.Jha, Bagis, TNN. 195-km super expressway to link Delhi, Jaipur, The Economic Times, 21 March 2017, Accessed on 20 June 2017.


Aravali range is the home of several forests, wildlife, and protected areas, UNESCO heritage listed forts, hundreds of rivers and ancient history to sustain a large tourism industry.


Damage to the environment and ecology from the unorganised urbanisation, overexploitation of the natural resources including water and minerals, mining, untreated human waste and disposal, pollution, loss of forest cover and wildlife habitat, unprotected status of most of the Aravalli and the lack of an integrated Aravalli management agency are the major causes of concern. Bad implementation of ban on mining in Aravali hills.


File:Aravali range inside Ranthambhore, Rajasthan.jpg|The Aravali Range inside Ranthambhore National Park, in Rajasthan.File:Aravali hills Udaipur Rajasthan India 2014.jpg|Aravalli range near Udaipur RajasthanFile:Mt. Abu.jpg|alt=Mount Abu is the tallest mountain in this range with GURU SHIKHAR as its peak.|Sunset from the sunset point of Mount Abu

See also

{{div col|colwidth=35em}}
  • {{annotated link|Asola Bhatti Wildlife Sanctuary}}, Delhi
  • {{annotated link|Aravali Biodiversity Park, Gurgaon|Aravali Biodiversity Park}}
  • {{annotated link|Arid Forest Research Institute}}
  • {{annotated link|Hill Forts of Rajasthan}}
  • {{annotated link|Pinangwan}}
{{col div end}}

Further reading

External links

{{Commons category|Aravalli Range}}{{Wikivoyage|Western India}}


  • Watershed Management in Aravali Foothills, by Gurmel Singh, S. S. Grewal, R. C. Kaushal. Published by Central Soil & Water Conservation Research & Training Institute, 1990.


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