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Geography

Potential UNESCO Geopark Sites in Rajasthan: Evaluation Against Criteria

UNESCO Geo-parks and Geo-heritage Sites: Potential of Rajasthan

Paper II · Unit 3 Section 6 of 14 0 PYQs 38 min

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Potential UNESCO Geopark Sites in Rajasthan: Evaluation Against Criteria

No Rajasthan site has been formally nominated for UNESCO Global Geopark status as of 2024. However, a structured evaluation of candidate zones against UNESCO's four pillars reveals two sites with strong potential and several with conditional potential.

5.1 Candidate Zone 1: Jaisalmer Geopark

A Jaisalmer Geopark anchored around the Akal Wood Fossil Park, Jaisalmer Basin marine fossil outcrops, and Thar Desert aeolian geomorphology would be the strongest candidate.

UNESCO Criterion Status in Jaisalmer Gap / Action Needed
Geological Heritage Strong — GSI monument, Jurassic fossils, aeolian geomorphology, palaeolake sediments Documentation of additional sites along Ramgarh-Jaisalmer transect needed
Management Structure Weak — GSI monument status only; Desert National Park manages overlapping area Establish dedicated Geopark Authority (state government notification)
Geotourism Development Partial — Sam dunes attract ~4 lakh tourists/year but no geological interpretation Build visitor centres at Akal; develop geological trail maps; train local guides
Education and Outreach Weak — no active school programme; no research partnerships with universities MOU with IIT Jodhpur, JNV University Jodhpur, and GSI Western Region

Source: UNESCO Global Geoparks Operational Guidelines 2022

The overlap between the Desert National Park (a wildlife sanctuary protecting the Great Indian Bustard) and fossil outcrop zones requires inter-departmental coordination between the Forest Department, Mining Department, and Tourism Department — a significant institutional challenge.

5.2 Candidate Zone 2: Bundi-Aravalli Precambrian Geopark

A Bundi-Hadoti Geopark could integrate the Bundi stromatolites, Precambrian fold belt exposures, Chambal geomorphology, and Baroli stone temple architecture (which uses local geological materials) into a multi-heritage geo-cultural trail.

UNESCO Criterion Status in Bundi-Hadoti Gap / Action Needed
Geological Heritage Strong — 1,800 Ma stromatolites, Vindhyan sedimentary sequences, active Chambal geomorphology Formal scientific inventory; AMS radiometric dating publication needed
Management Structure Absent — no designated authority District-level Geopark Committee under Collector's office
Geotourism Development Nascent — Bundi's historical tourism provides base infrastructure Link geological sites to Bundi Heritage Walk; develop geo-interpretation panels
Education and Outreach Minimal Partner with Kota University (geology department) and CSIR-NGRI

Source: UNESCO Global Geoparks Operational Guidelines 2022; GSI Geo-Heritage Sites Manual 2021

5.3 Comparative Summary of Rajasthan's Geopark Candidates

Zone Geological Era Key Assets Geotourism Base UNESCO Readiness
Jaisalmer Basin Jurassic (~180–145 Ma) Akal fossils, marine fauna, aeolian geomorphology High (existing tourism) 5–7 years with investment
Barmer Basin Cretaceous (~100–65 Ma) Dinosaur bones, wood fossils Low 10+ years
Bundi-Aravalli Precambrian (~1,800 Ma) Stromatolites, fold belt Medium (Bundi tourism) 7–10 years
Chambal Ravines Proterozoic–Holocene Badland geomorphology, Vindhyan rocks Low-medium 10+ years
Thar Desert (aeolian) Quaternary (~2 Ma–present) Dune systems, palaeolakes, palaeo-channels High (Sam dunes) 5–8 years (as part of Jaisalmer zone)

Source: Author's assessment based on UNESCO Global Geoparks Operational Guidelines 2022 and GSI documentation