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The '''Aravalli Range''' (also spelled ''Aravali'') is a mountain range in [[North India|Northern]]-[[West India|Western India]], running approximately {{convert|670|km|abbr=on}} in a south-west direction, starting near [[Delhi]], passing through southern [[Haryana]],<ref name=ara8>{{cite web|url=http://aravalibiodiversitypark.in/?q=node/1 |title=Aravalli Biodiversity Park, Gurgaon |url-status=dead |archive-url=https://web.archive.org/web/20120528194722/http://aravalibiodiversitypark.in/?q=node%2F1 |archive-date=28 May 2012}}</ref> [[Rajasthan]], and ending in Ahmedabad [[Gujarat]].<ref name=ara3>{{citation|last=Kohli|first=M.S.|title=Mountains of India: Tourism, Adventure, Pilgrimage|url=https://books.google.com/books?id=GIs4zv17HHwC&pg=PA29|year=2004|publisher=Indus Publishing|isbn=978-81-7387-135-1|pages=29–}}</ref><ref name=ara4>{{cite book|chapter-url=https://books.google.com/books?id=Kpd9lLY_0-IC&q=Aravali&pg=PA92 |chapter=Aravali Range |title=Students' Britannica India |author1=Dale Hoiberg |author2=Indu Ramchandani |publisher=Popular Prakashan |year=2000 |isbn=978-0-85229-760-5 |pages=92–93}}</ref> The highest peak is [[Guru Shikhar]] on Mount Abu at {{convert|1722|m|abbr=on}}. The Aravalli Range is arguably the oldest geological feature on [[Earth]],<ref>{{Cite journal|last1=Verma|first1=P. K.|last2=Greiling|first2=R. O.|date=1995-12-01|title=Tectonic evolution of the Aravalli orogen (NW India): an inverted Proterozoic rift basin?|url=https://doi.org/10.1007/BF00240560|journal=Geologische Rundschau|language=en|volume=84|issue=4|pages=683–696|doi=10.1007/BF00240560|bibcode=1995GeoRu..84..683V |s2cid=129382615|issn=1432-1149}}</ref><ref>{{Cite journal|date=1990-01-01|title=Evolution of the Precambrian Crust of the Aravalli Mountain Range|url=https://www.sciencedirect.com/science/article/pii/S0166263508701737|journal=Developments in Precambrian Geology|language=en|volume=8|pages=327–347|doi=10.1016/S0166-2635(08)70173-7|issn=0166-2635|last1=Roy|first1=A.B.|isbn=9780444883100}}</ref><ref>{{Cite web|date=December 11, 2015|title=International Mountain Day: India has the oldest and the youngest mountains in the world|url=https://www.indiatoday.in/education-today/gk-current-affairs/story/international-mountain-day-276734-2015-12-11|access-date=2021-06-28|website=India Today|language=en}}</ref><ref>{{Cite web|title=Aravalli Hills Are the Oldest Fold Mountains of the World|url=https://www.campwilddhauj.in/aravali-valley-651#:~:text=Aravalli%20Hills%20Are%20the%20Oldest%20Fold%20Mountains%20of%20the%20World|access-date=2021-06-28|website=www.campwilddhauj.in}}</ref> having its origin in the [[Proterozoic]] era.
 
The Aravalli Range is rich in [[natural resource]]s and serves as check to the growth of the western desert.
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*** [[Delhi Ridge]], in the north
*** Haryana Aravalli ranges, in the west
**** [[Tosham Hill range]] basement rocks include quartzite with [[chiastolite]], the upper layers of [[quartz porphyry]] [[Ring dike|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]].<ref name=ara7>{{cite journal |lastlast1=Bhuiyan |firstfirst1=C. |last2=Singh |first2=R. P. |last3=Kogan |first3=F. N. |year=2006 |title=Monitoring drought dynamics in the Aravalli region (India) using different indices based on ground and remote sensing data |journal=International Journal of Applied Earth Observation and Geoinformation |volume=8 |issue=4 |pages=289–302 |doi=10.1016/j.jag.2006.03.002 |bibcode=2006IJAEO...8..289B }}</ref>
**** [[Madhogarh Fort, Haryana|Madhogarh hill]]
**** Satnali hill
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=== Tosham hills Indus civilization mines ===
The [[Tosham Hill range#Tosham Hill range Indus Valley civilization mines and smelters|Tosham hills]] have several [[Indus Valley civilization]] sites in and around the hill range as the area falls under copper-bearing zone of Southwest Haryana and Northeast Rajasthan of Aravalli hill range.<ref name=law3>{{cite journal |firstfirst1=N. |lastlast1=Kochhar |first2=R. |last2=Kochhar |first3=D. K. |last3=Chakrabarti |year=1999 |title=A New Source of Primary Tin Ore in the Indus Civilisation |journal=South Asian Studies |volume=15 |issue=1 |pages=115–118 |doi=10.1080/02666030.1999.9628571 }}</ref><ref name=law4>{{cite book |first=D. K. |last=Chakrabarti |year=2014 |chapter=Distribution and Features of the Harappan Settlements |title=History of India II : Protohistoric Foundation |publisher=[[Vivekananda International Foundation]] |location=New Delhi |isbn=978-81-7305-481-5 |pages=97–143 }}</ref>
 
Investigation of IVC network of mineral ore needs for the metallurgical work and trade shows that the most common type of grinding stone at Harappa is of Delhi quartzite type found only in the westernmost outliers of the Aravalli range in southern Haryana near Kaliana and Makanwas villages of Bhiwani district. The quartzite is red-pink to pinkish grey in colour and is crisscrossed with thin [[haematite]] and quartz filled fractures with sugary size grain texture.<ref name=law5>{{cite book |first=Randall |last=Law |year=2006 |chapter=Moving Mountains: The Trade and Transport of Rocks and Minerals within the Greater Indus Valley Region |title=Space and Spatial Analysis in Archaeology |editor-first=E. C. |editor-last=Robertson |editor2-first=R. D. |editor2-last=Seibert |editor3-first=D. C. |editor3-last=Fernandez |editor4-first=M. V. |editor4-last=Zender |display-editors=1 |publisher=University of Calgary Press |location=Alberta, Canada |isbn=0-8263-4022-9 }}</ref><ref name=law6>{{cite thesis |first=Randall |last=Law |year=2008 |type=PhD thesis |title=Inter-regional Interaction and Urbanism in the Ancient Indus Valley: A Geologic Provenance Study of Harappa's Rock and Mineral Assemblage |publisher=[[University of Wisconsin–Madison]] |pages=209–210 |oclc=302421826 }}</ref>