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Girnar
EntityQ1747217· pop 24· linked from 265 articles

Also known as Girnar Hill, Girinagar

Girnar is an ancient hill in Junagadh, Gujarat, India. It is one of the holiest pilgrimages of Jains, a Mahatirth, where the 22nd Tirthaṅkar, Lord Neminath attained omniscience, and later nirvana at its highest peak (Neminath Shikhar), along with other five hundred and thirty three enlightened sages. This is well described in ancient texts such as Kalpa Sūtra written by acharya Bhadrabāhu and Shri Uttaradhyayana Sutra by Arya Sudharmaswami. It is administered by the Junagadh Municipal Corporation.

Key facts

Mountain.name
Girnar Mount
Mountain.photo
Girnar 1.jpg
Mountain.photo_alt
Girnar
Mountain.photo_caption
Mount Girnar
Mountain.map
India#India Gujarat
Mountain.location
Junagadh, Gujarat
Mountain.elevation_m
1145
Mountain.prominence_m
1130
Mountain.listing
List of Indian states and territories by highest point, Ribu
Mountain.other_name
ગિરનાર પર્વત Revatak Parvata
Mountain.type
Igneous

via Wikipedia infobox

Wikidata facts

Elevation
1117
Image
Dattatreya Temple of Girnar.JPG
Width
15
Length
16
Show 1 more fact
Commons category
Girnar
Sources (1)

via Wikidata · CC0

~29 min read

Article

16 sections
Contents
  • Geology
  • History
  • Ashoka edicts
  • Jain sources
  • Jaina Inscriptions
  • Girnar Ropeway
  • Jain Temples
  • Ambika Temple
  • Hindu Temples
  • Girnar's Initial trek
  • Current situation at Neminath Shikhar
  • Festivals
  • Tanks
  • See also
  • References
  • Works cited

Girnar is an ancient hill in Junagadh, Gujarat, India. It is one of the holiest pilgrimages of Jains, a Mahatirth, where the 22nd Tirthaṅkar, Lord Neminath attained omniscience, and later nirvana at its highest peak (Neminath Shikhar), along with other five hundred and thirty three enlightened sages. This is well described in ancient texts such as Kalpa Sūtra written by acharya Bhadrabāhu and Shri Uttaradhyayana Sutra by Arya Sudharmaswami. It is administered by the Junagadh Municipal Corporation.

==Geology== Mount Girnar is a major igneous plutonic complex which intruded into the basalts towards the close of the Deccan Trap period. The rock types identified in this complex are gabbros (tholeiitic and alkalic), diorites, lamprophyres, alkali-syenites and rhyolites. The parent gabbroic magma is shown to have given rise in sequence to diorites, lamprophyres and alkali-syenites. The rhyolite, though previously considered as a product of differentiation, is now believed to be an independent magma without any genetic link with the gabbro and its variants.

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On the map

3 mapped locations

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