DOCSLIB.ORG

Gomukh Tapovan,Pindari Glacier,Doditaal & Darwa Top,Rupin

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Gomukh Tapovan,Pindari Glacier,Doditaal & Darwa Top,Rupin Gomukh Tapovan Region: Uttarakhand |Grade: Moderate +| Duration: 08 days (Dehradun to Dehradun) | Max Altitude: 14,222 ft ITINERARY Day 1: Dehradun to Gangnani/Gangotri drive – 7/8 h drive Day 2: Gangotri (3,048 m) to Chirbasa (3,600 m) – 6 h trek Day 3: Chirbasa to Bhojbasa (3,800 m) – 3 h trek Day 4: Bhojbasa to Gaumukh (3,900 m) to Tapovan (4,335 m)- 7 h Day 5: Rest day Tapovan (4,463 m) Day 6: Tapovan to Bhojbasa- 5-6 h Day 7: Bhojbasa to Gangotri- 5-6 h Day 8: Gangotri to Dehradun drive- 9 h Best Season: May-June, Sept-Oct Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Pindari Glacier Region: Kumaon, Uttarakhand | Grade: Moderate | Duration: 06 days (Kathgodam to Kathgodam) ITINERARY Day 01: Kathgodam to daw (240 kms) by jeep then 5 kms trek Day 02: Daw to jwarpani 14 kms trek Day 03: Jwarpani to pindari glacier with pack lunch.10 kms trek Day 04: Pindariglacieri- to malyadhor (18 kms trek) . Day 05: Malyadhor to dhakuri 13 kms trek kms trek Day 06: Dhakurito kathgodam. Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Doditaal & Darwa Top Region: Garhwal, Uttarakhand | Duration: 06 days (Dehradun to Dehradun) | Grade: Moderate | Max Altitude: 13,600 ft ITINERARY Day 01: Dehradun to Uttarkashi( 6 – 8 Hrs) Day 02: Uttarkashi to Sangamchatti transport and trek to Manzi Day 03: Manzi to Doditaal (10,170 ft) Day 04: Doditaal to Darwa top (13600 ft) and back to Doditaal (5 kms) Day 05: Doditaal to Agoda 16 kms Day 06: Agoda to Sangamchatti (04 kmstrek ) and drive to Dehradun ( 6 – 8 Hrs) Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Rupin - Supin Valley Region: Garhwal, Uttarakhand | Grade: Moderate | Max. Altitude: 11,548 ft) | Duration: 06 days (Dehradun to Dehradun) One of the most beautiful and less traveled valley in the northwest of Uttarakhand Himalayas. The trail goes along the river Rupin which is adjacent to the GovindPashu National Park on the border of Himachal Pradesh. During this trek, one can have spectacular view of mighty Himalayan snowcapped peaks of Kinnaur Kailash Range. ITINERARY Day 01: Pickup from Dehradun at 7 am Road travel to Himri 195 kms – 8/9 Hrs(stay) Day 02: Himri to Bheetri (2,500 m) to Kurla Thach (2,600 m) – 1 h drive + 5-6 h trek (Stay) Day 03: Kurla (2,600 m) to RikatikOdi (3,520 m) – 6-7 h (stay) Day 04: RikatikOdi to Phitadi village- 4-5 h Day 05: Phitadi to Jakhol to Sankri- 5-6 h trek + 1 h drive Day 06: Sankri to Dehradun drive – 7-8 h drive Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Kuari Pass Region: Garhwal, Uttarakhand |Grade: Moderate | Max. Altitude: 12,600 Ft approx | Duration: 06 Days (Haridwar to Haridwar) ITINERARY Day 01: Dehradun to Karnaprayag (By road) Day 02: Karnrayag to Auli (by road) Trek Starts to Padiyar (stay) Day 03: Padiyar to Tali (14 kms) (stay) Day 04: Tali to Kuari Pass to Khulara(Stay) Day 05: Khulara to Dhak(Trek Ends)Transport to Karnprayag(Stay) Day 06: Karnprayag to Dehradun around 6 pm (by Road) Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Kedarkantha Region: Garhwal, Uttarakhand | Grade: Moderate | Altitude: 12,500 Ft | Duration: 05 days (Dehradoon to Dehradoon) This is one of the most favorite winter treks in Garhwal Himalaya. The trek passes through the pine forests and alpine meadows which are cover in snow during the winter period i.e. December to April. Right from the Kedarkantha Base one can witness jaw-dropping view of famous Snow-covered mountains. The Gangotri and Yamunotri ranges are visible from the summit. ITINERARY Day 01: Departure from Dehradoon to Mori river campsite by road (approx 220 kms) 7 to 8 Hrs Day 02: Mori river campsite to Sankri (by road 25 kms) trek to Kedarkantha Meadows (10500 ft) Day 03:KedarkanthaMedows to Kedarkantha peak 12500 ft and back to the camps site Day 04:Kedarkanthamedow to sankri Trek Ends and back to Mori (by road) Day 05: Mori river campsite to Dedhradoon (220 kms) 8 to 9 Hrs. Best Season: all season trek Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Har Ki Dun Region: Uttarakhand | Grade: Moderate | Max. Altitude: 11,420 ft | Duration: 08 days (Dehradun to Dehradun) Har ki Dun, which means Valley of Gods, is situated deep inside GovindPashu National park. Rich in flora and fauna, the trails are quite often covered in different shades of orchids and other wildflowers. The area was made popular by the Doon school master Jack Gibson after his Banderpunch expeditions. The path winds up alongside the Tons river from Netwar village. The trek is along the Supin river through the scenic Garhwali villages of Taluka, Gangad and Osla. Har ki dun has numerous camping places and one Forest Guest House. An extra rest day is ideal to explore several trails that continue from the Har ki Dun camp. From Har ki Dun one can see the entire North Face of Swargarohini I (6,252 m) peak. This face drops to about 2,000 m in less than 2 km distance and is yet to be climbed. The legends associated with it say that Swargarohini is the path to heaven that was followed by Pandavas of the epic Mahabharata. Though, the same story is also associated with the Swargarohini steps seen from Satopanth Lake, which lies ahead of Badrinath. ITINERARY Day 01: Pick up from Dehradun and Departure for Sankri Day 02: Trek Starts: Sankri to PawniGharat Camp 2700 mts (5/6 Hrs trek) Day 03: Pawni Gharat Camp 2700 mts to Kalkatidhar 3100mts (4/5 Hrs trek) Day 04: Kalkatidhar 3100mts to Harkidun (4/5 Hrs trek) Day 05: Explore Har Ki Dun Day 06: Har Ki Dun to Osla (3/4 Hrs trek) Day 07: Osla to Sankri (4/5 Hrs trek + 1 hr drive) Trek Ends Day 08: Sankri to Dehradun by road (8/10 Hrs Drive) Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Kuari Pass & Pangarchulla Peak Region: Garhwal, Uttarakhand |Grade: Moderate | Max Altitude: 14700 ft | Duration: 07 days (Dehradun to Dehradun) | Age grp: above 13 yrs only KUARI PASS & PANGARCHULLA PEAK Kuari Pass is a very popular and Easy to Moderate level trek. It is also known as Curzon’s trail since the British viceroy, Georg Curzon attempted crossing it and loved exploring this area. Though the pass is not very high it offers excellent views of Nanda Devi, Dunagiri and other Himalayan peaks. The Nanda Devi national park and the Rishi Ganga gorge are visible from the first day itself. While you camp on the lush green, infinitely unfolding meadow of the Gorsons, which can turn white anytime of the year, and as you move your head around, your eyes are gifted with grand views of 4 peaks of Chaukhamba, Neelkanth, Mana, Kamet, Hathi, Ghodi, Trishul, Nandaghunti, Nanda Devi, Dunagiri etc. Itinerary Day 01: Departure for Auli early morning (275 kms 8/10 hrs) stay Day 02: Trek starts Auli to Padiyar Day 03:Padiyar to Tali 11000 ft Day 04:Tali to – Kuari pass – Pangarchula Base (stay) Day 05: Base to Pangarchula Peak (14700 ft) – Back to Base Day 06: Base to Auli 15/16 kms (6 Hrs trek) Trek Ends and Drive to Rudraprayag(150 kms) stay Day 07: Arrival at Dehradun in the evening (program ends) Show Your Interest in this trek by filling below form, our team will get in touch with you. Your Name * Your Email * Mobile Number * Send Valley of Flowers Region: Garhwal, Uttarakhand | Grade: Moderate + | Duration: (06 Days) Dehradoon to Dehradoon | Age grp: Open to all (above 12 yrs) It’s a photographer’s paradise…. Valley of flowers is a vibrant and splendid national park reposing in west Himalayas. Nestled in Uttarakhand, this alluring place is famous for its charming meadows of alpine flowers. Endowed with a diverse range of endemic flora, it is picturesque in its beauty. This lush region is also home to some rare and endangered animal species. You may spot animals like Asiatic black deer, snow leopard, musk deer, red fox, brown bear and blue ship. ITINERARY Day 01: Arrival at Dehradoon and drive to Govindghat / Joshimath 9-10 hrs travel (stay) Day 02: (Trek Starts)Govindghat to Ghangria (14 kms) (stay) Early in the morning after breakfast from GovindGhat, it is a gradual ascent along a well-maintained trail to Ghangria. Spend the rest of the day exploring the surroundings. Day 03: Ghangria – Valley of Flowers – Ghangria (12 kms) (Stay) Valley of Flowers is a beautiful carpet of multi-colored flowers. We spend the entire day in the valley & return to Ghangria in the evening. Day 04: Ghangria – Hemkund – Ghangria (12 kms) (Stay) Hemkund is a beautiful holy lake situated at a height of 15,000 feet. We have to climb continuously for 6 kms.
Load more

Recommended publications
  • Climate-Glacier Relationship in the Monsoon-Arid Transition Zone: a Case Study in Himachal Pradesh, India
    Climate-Glacier relationship in the monsoon-arid transition zone : A Case study in Himachal Pradesh, India Farooq Azam Mohd To cite this version: Farooq Azam Mohd. Climate-Glacier relationship in the monsoon-arid transition zone : A Case study in Himachal Pradesh, India. Earth Sciences. Université de Grenoble, 2014. English. NNT : 2014GRENU032. tel-01230980 HAL Id: tel-01230980 https://tel.archives-ouvertes.fr/tel-01230980 Submitted on 19 Nov 2015 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. THESIS Submitted to obtain the degree of DOCTOR OF THE UNIVERSITY OF GRENOBLE Speciality : Earth Sciences, Universe and Environment Arrêté ministériel : 1 November 2011 Presented by Mohd Farooq AZAM Thesis directed by Patrick Wagnon and co-directed by Christian Vincent & Ramanathan Alagappan Prepared in the Laboratoire de Glaciologie et de Géophysique de l’Environnement/Laboratoire d'Etudes des Transferts en Hydrologie et Environnement, UJF/CNRS in Doctoral school Earth Sciences, Universe and Environment Climate-Glacier relationship in the monsoon-arid transition zone: A Case study in Himachal Pradesh, India. Defended publicly : 17 December 2014, Before the jury : Mr. Gerhard KRINNER Research Director, CNRS, LGGE (France), President Mr. Martin HOELZLE Professor, University of Fribourg (Switzerland), Reporter Mr.
    [Show full text]
  • The Bagpipe Treks
    1 THE BAGPIPE TREKS Small Treks in Lower hills of Kumaun and Himachal Many times I had to visit Delhi for a short visit from Mumbai. Dealing with babus and the bureaucracy in the capital city could be quite exhausting. So to relax, I would meet my friend, philosopher and guide, the famous writer, Bill Aitken . As we had lunch, watching cricket and talking mountains, he would suggest several ideas enough to fill in a year of trekking. Bill specialises and believes in ‘A Lateral Approach to the Himalaya’1 and would firmly suggest ‘more of the lesser’. I would tuck the information away in my mind and when an opportunity arose, I would go on these small treks from Delhi. Some were 10 days and some were only 4 days (return). We called them ‘The Bagpipe Treks’. Chiltha Ridge One such trip was along the well-trodden path to the Pindari glacier. We travelled from Delhi by an overnight train to Kathgodam, drove to Almora and reached Loharkhet, the starting point of this popular route. Our friends Harsingh and others from the nearby Harkot village were waiting for us with all arrangements. We crossed Dhakuri pass the next day enjoying wonderful views. Staying in rest houses, we enjoyed the forest via Khati and Dwali. The Pindari trail may be overcrowded or too popular but it is still beautiful. We retraced our steps back to Khati and climbed up a ridge to the east of village and were soon on the Chiltha Devi dhar (ridge). We spent the first night at Brijaling dhar and were rewarded with exquisite views of Pindari glacier and Nanda Kot peak.
    [Show full text]
  • Pindari & Kafni Glacier
    Pindari & Kafni Glacier Trek Location Kumaon Himalaya, Uttarakhand Area Bageshwar Grade of trek Moderate Co-ordinates 30°14'57"N 80°4'21"E Max. Altitude 3900 m Season mid May - September Duration 10 days The most easily accessible glacier in the Kumaon region, the Pindari Glacier has a beauty of its own. Situated between the snow-capped Nanda Devi and Nanda Kot Mountains, Pindari is a big and steep glacier measuring 3km in length and 0.25km in breadth. River Pindar originates from this Glacier and flows down to confluence into the river Alaknanda. The trekking route to the glacier traverses along the southern wilderness of the Nanda Devi Sanctuary offering some beautiful views of peaks like Panwali Dwar (6683m) and Maiktoli (6803m). A trek to the Pindari Glacier is a "soft adventure" experience and well within the capacity of any trekker who is amply rewarded by the magnificence and grandeur of the towering Himalayas. Trek Itinerary Day 00: Overnight train from Delhi to Kathgodam Day 01 : KATHGODAM - travel to SONG-LOHARKHET (1750 m),6-7 hrs. Our jeep is ready to take us further deep into mountains. Overnight at Rest house. Day 2: LOHARKHET - DHAKURI (2680 M) 11kms It is an 11 km trek today that takes you down into the depths of the valley and then a fair climb to Dhakuri. Overnight is tents. Day 3: DHAKURI - KHATI (2210 M ) 8 kms Trek to Khati, the largest village on this route and is on the banks of the Pindar Ganga. Overnight in Tents / Village huts. Day 4: KHATI - DWALI (2575 M) 11kms (5-6hrs) The trek with the roar of the Pindar Ganga not too far off.
    [Show full text]
  • Nanda Devi : the 'Bliss Giving' Goddess of Kumaun
    1 NANDA DEVI : THE ‘BLISS GIVING’ GODDESS OF KUMAUN Mountains, like men, have their history. They too are born, grow, decay and die. One cannot claim that, like men, they love, but it is true - and how true – that they are loved. Felice Benuzzi, No Picnic on Mount Kenya The twin peaks of Nanda Devi (7,816 m) and Nanda Devi East (7,434 m) of Kumaun stand majestically in the centre of a ring of mountains, distinct and beautiful, particularly as the first and the last rays of the sun caress their summits. Hugh Ruttledge, a British explorer, after his attempt to find a route to these peaks in 1932, described the Nanda Devi Sanctuary in a letter to The Times, London: “A seventy- mile barrier ring on which stand twelve measured peaks of over 21,000 ft, which has no depression lower than 17,000 ft except in the west where the Rishi Ganga rising at the foot of Nanda Devi draining the area of some 250 square miles (800 square kilometres) of snow and ice has earned for itself what must be one of the most terrific gorges in the world.” Without the Sanctuary and its wall of high peaks to absorb the main thrust of the icy Tibetan winds, the Gangetic plains, the granary of India, would have been stripped barren. History In 1883, in one of the first attempts to reach the inner sanctuary, W W Graham, a British traveller, tried to forge a way through the Rishi Ganga gorge, failing to make much headway.
    [Show full text]
  • Page 1 PERSPECTIVE PLAN of LOCATION MAP
    PERSPECTIVE PLAN OF BAGESHWAR DISTRICT - 2021 U T T A R A K H A N D HIMACHAL PRADESH CHINA HARYANA NEPAL UTTAR PRADESH LOCATION MAP Drg. No. Scale 2.1 Not to Scale ERP DIVISION U T T A R A K H A N D S T A T E Town & Country Planning Organisation Govt. of India, M/o. Urban Development, New Delhi PERSPECTIVE PLAN OF BAGESHWAR DISTRICT - 2021 U T T A R A K H A N D LEGEND STRATIGRAPHY NAGTHAT- BEARING FORMATION MANDHALI FORMATION DEOBAN FORMATION RAUTGARA FORMATION DEBGURU PORPHYROID AUGEN GNEISS GRANITE-GRANODIORITE SARYU-GUMALIKHET & MUNSIARI FORMATION CHAMOLI JOSHIMATH FORMATION LITHOLOGY PITHORAGARH AUGEN GNEISS GNEISS .SCHIST.AUGEN GNEISS LIMESTONE.PHYLITE.SANDSTO NE KAPKOT LIMESTONE.SLATE PHYLITE.MARBLE MASSIVE QUARTZITE PHYLITE.SLATE GARUD QRTZ PORPHYRY.PORPHYRITICGRANITE BAIJNATH SLATES.SHALES BAGESHWAR SOURCE: DISASTER CELL, DISTRICT MAGISTRATE OFFICE, BAGESHWAR ALMORA GEOLOGICAL STRUCTURE Drg. No. 2.2 ERP DIVISION Town & Country Planning Organisation Govt. of India, M/o. Urban Development, New Delhi PERSPECTIVE PLAN OF BAGESHWAR DISTRICT-2021 U T T A R A K H A N D PINDARI GLACIER POPULATION DENSITY (PERSONS PER SQ.KM) BELOW 150 151 TO 350 ABOVE 351 KAPKOT CHAMOLI PITHORAGARH GARUD BAIJNATH SOURCE: CENSUS OF INDIA - 2001 BAGESHWAR POPULATION DENSITY ALMORA Drg. No. 3.1 ERP DIVISION Town & Country Planning Organisation Govt. of India, M/o. Urban Development, New Delhi PERSPECTIVE PLAN OF BAGESHWAR DISTRICT-2021 U T T A R A K H A N D PINDARI GLACIER LEGEND DISTRICT BOUNDARY BLOCK BOUNDARY NATIONAL HIGHWAY MAJOR DISTRICT ROADS PROPOSED ROAD RIVER District Headquarters Block Headquarters BASIC VILLAGE CHAMOLI PITHORAGARH TO GWALDAM TO TO MUNSAYARI R I V E R KAPKOT GARUD S A R A Y U G O M A T I R I V E R SOURCE: DISASTER CELL, DISTRICT MAGISTRATE OFFICE, BAGESHWAR Jogiyarimrao BAGESHWAR TO CHAUKODI THAL EXISTING SETTLEMENT GOMATI RIVER PATTERN ALMORA Drg.
    [Show full text]
  • Colonised by Brethren:People and Natural Resource Management In
    Colonised by Brethren: People and Natural Resource Management in Uttaranchal Neema Pathak1 and Seema Bhatt2 The beautiful shrine of Tungnath (3680m) in the Garhwal region of Uttaranchal, attracts many visitors. Few visitors realize that the lush forests and the alpine pastures surrounding this shrine, are under the management and control of a village level institution in the valley called the Makku Van Panchayat (VP). Established in 1958, the Makku VP manages an area of over 2000 ha. The villagers follow strict rules and regulations for extraction of forest resources. In addition to the VP, women through their Mahila Mangal Dal (MMD) are also protecting and using civil forests (outside of the VP) based on consensus decision-making. Not very far from the famous Pindari Glacier and en route to the Namik Glacier, among the high rocky mountains, surrounded by several hundred hectares of temperate forests and high altitude pastures or bhugials lies the village Shama in Bageshwar district. In an area of nearly 1500 ha, the village manages a complex system of bhugials, forests, and water sources. The management of these forests is largely the responsibility of the Van Panchayat established in 1954. However, the entire village actively participates in formulation and implementation of rules and regulations. “If you could walk with us we would show you how women have de-silted the fresh water lakes on top of the mountain and how we have protected our forests” says a very proud 30-year old Nandi Korunga, who returned to the village after completing her post-graduation from Bageshwar and is currently the Gram Pradhan (head of village panchayat).
    [Show full text]
  • Glacier Changes in the Garhwal Himalaya, India, from 1968 to 2006 Based on Remote Sensing
    Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2011 Glacier changes in the Garhwal Himalaya, India, from 1968 to 2006 based on remote sensing Bhambri, R ; Bolch, T ; Chaujar, R K ; Kulshreshtha, S C Abstract: Glacier outlines are mapped for the upper Bhagirathi and Saraswati/Alaknanda basins of the Garhwal Himalaya using Corona and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) satellite images acquired in 1968 and 2006, respectively. A subset of glaciers was also mapped using Landsat TM images acquired in 1990. Glacier area decreased from 599.9 ± 15.6 km2 (1968) to 572.5 ± 18.0 km2 (2006), a loss of 4.6 ± 2.8%. Glaciers in the Saraswati/Alaknanda basin and upper Bhagirathi basin lost 18.4 ± 9.0km2 (5.7±2.7%) and 9.0 ± 7.7km2 (3.3±2.8%), respectively, from 1968 to 2006. Garhwal Himalayan glacier retreat rates are lower than previously reported. More recently (1990–2006), recession rates have increased. The number of glaciers in the study region increased from 82 in 1968 to 88 in 2006 due to fragmentation of glaciers. Smaller glaciers (<1 km2) lost 19.4 ± 2.5% (0.51 ± 0.07% a–1) of their ice, significantly more than for larger glaciers (>50 km2) which lost2.8± 2.7% (0.074 ± 0.071% a–1). From 1968 to 2006, the debris-covered glacier area increased by 17.8 ± 3.1% (0.46 ± 0.08% a–1) in the Saraswati/Alaknanda basin and 11.8 ± 3.0% (0.31 ± 0.08% a–1) in the upper Bhagirathi basin.
    [Show full text]
  • Case of Pindari Glacier Valley
    Topographical influences on high altitude forest line in the Indian Central Himalaya: Case of Pindari Glacier Valley Bhawana Soragi, Arti Joshi, and Subrat Sharma* G. B. Pant National Institute of Himalayan Environment and Sustainable Development Kosi-Katarmal, Almora, 263 643 Uttarakhand *[email protected] Keyword: Himalaya, Watersheds, Treeline, Satellite Image Abstract High altitudes of the Himalaya have been realized to more prone towards temperature increase due to global temperature rise while decrease in temperature limits the plant growth there. Altitudes in high mountains do not support tree growth beyond an elevation and termination of continuum of forests is often termed as forest line/timberline. This is a dynamic state which is influenced by local topography and geography on which a very little knowledge exists for the Himalayan region. This study focuses on the mapping of timberline, using high resolution satellite images, in a glaciated valley (Pindari Valley covering an area of 397.35 km2) having three glaciers (three valleys) in the Indian Central Himalaya. Three valleys exhibit a variation of ~1 km in highest elevation (3050-3970m amsl) of timberline which shows a buffering range for temperature escape for the tree species of timberline. Impact of robust topography will limit this expansion and limit of forest growth as apparent by the fact that about 62% of the area does not have vegetation (snow, glacier, rivers, rock, etc.) in an elevational zone of 4 km (2000-6600m amsl). Presently, vegetation (alpine, forest, and shrubs) are limited to 38% of the area. Timberline also varies considerably (570-700m) in three sub-watersheds of Pindar valley.
    [Show full text]
  • Record of Neotectonic Activity in the Pindari Glacier Valley: Study Based on Glacio-Geomorphic and AMS Fabric Evidences
    Open access e-Journal Earth Science India, eISSN: 0974 – 8350 Vol. 4(I), January, 2011, pp.1-14 http://www.earthscienceindia.info/ Record of Neotectonic Activity in the Pindari Glacier valley: Study based on Glacio-geomorphic and AMS Fabric evidences Rameshwar Bali 1 * , K.K. Agarwal 1, S. K. Patil 2, S. Nawaz Ali 1 Saurabh Kumar Rastogi 1 and Kalyan Krishna 1 1 Department of Geology, Lucknow University, Lucknow-226 007, India 2 Dr. K.S.Krishnan Geomagnetic Research Laboratory, Jhunsi, Allahabad-221 505, India Email: * [email protected] Abstract Systematic geomorphological studies aided by anisotropy of magnetic susceptibility (AMS) along the Pindari glacier valley suggest continued neotectonic activity in the area. The distribution and orientation of a number of glaciogeomorphic features viz. inclined bedding planes within the lacustrine deposits, asymmetrical terraces, deep entrenched gorges, skewed fans, sharp contact between the U-shaped and the V-shaped valleys and higher bifurcation ratio, The shape parameters T and q determined during the systematic AMS study of a glacio-lacustrine pit profile suggests that during its depositional history, there have been at least two phases, where the primary sedimentary fabric has been overprinted by secondary tectonic fabric. The constricted valley indicates a major phase of rejuvenation prior to 25 ka that inhibited the downstream advancement of Pindari trunk glacier. This was followed by another event of rejuvenation post 3 ka. Key words: Neotectonics, Pindari glacier, Anisotropy of magnetic susceptibility, Geomorphology, Kumaun Himalaya. Introduction The Pindari glacier lying between the latitude 30º 06' 30" N to 30º 19' 00" N and longitude 79º 55' 30" E to 80º 05' 30" E, is relatively a smaller glacier of Alaknanda basin falling in the Bageshwar district, Uttarakhand (Fig.1).
    [Show full text]
  • IND:Uttarakhand Emergency Assistance Project (UEAP)
    Initial Environment Examination Project Number: 47229-001 July 2017 Part A: Main Report (Pages 1 - 118) and Annexures (Pages 119 – 131) IND: Uttarakhand Emergency Assistance Project (UEAP) Package: Supply, Installation & Commissioning of Sewage Treatment Plants (STPs) and Installation of Solar Street Lights at various TRHs in Disaster Affected Districts of Pithoragarh & Bageshwar of Kumaon Region, Uttarakhand Submitted by Project implementation Unit –UEAP, Tourism (Kumaon), Nainital This initial environment examination report has been submitted to ADB by Project implementation Unit – UEAP, Tourism (Kumaon), Nainital and is made publicly available in accordance with ADB’s Public Communications Policy (2011). It does not necessarily reflect the views of ADB. This initial environment examination report is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. ADB Project Number: 3055-IND June: 2017 IND: Uttarakhand Emergency Assistance Project Submitted by Project Implementation Unit, Tourism (Kumaon), UEAP This report has been submitted to ADB by the Project implementation Unit, UEAP, Kumaon Mandal Vikas Nigam, Dehradun and
    [Show full text]
  • Agricultural Development in Uttarakhand
    AGRICULTURAL DEVELOPMENT IN UTTARAKHAND ABSTRACT THESIS SUBMITTED FOR THE AWARD OF THE DEGREE OF Boctor of $I)tlas(opt)p IN GEOGRAPHY BY MUMTAJ AHMAD Under the Supervision of Dr. Shamsul Haque Siddiqui ( Reader) DEPARTMENT OF GEOGRAPHY ALIGARH MUSLIM UNIVERSITY ALIGARH (INDIA) 2002 ABSTRACT The study region of the present research work, Uttarakhand comprising eight districts namely, Nainital, Almora, Pithoragarh of Kumaun, Chamoli, Uttarkashi, Tehri-Garhwal, Pauri-Garhwal and Dehradun of Garhwal division. It extends from 28°43'24" and 31°27'30" N latitude and 77°34'27" and 80°7'22" E longitudes. It encompasses an area of 51,125 square kilometres and account total population of 5.926 million (according to Census of India 1991). The eocnomy of this region depends on agriculture, where more than 80 per cent of its population dependent upon this source. Being a hilly area, there is scarcity of agricultural land and the share of per capita cultivated land is very low. The present study is carried out for the period from 1979-80 to 1994-95. It is based on secondary soruces of data. There are the following techniques have bene used by the author for the analysis of the present study as follows. i) The physical setting of Uttarakhand has been described in detail. ii) To examine the trends of agricultural development, trend lines have been plotted with the help of regression equation Y = a + bX, regression lines make it possible to show the exact change in area and production of different crops. iii) To assess the development of agriculture by the diffusion of technological and institutional factors per thousand hectares of cultivated land has been opted for the analysis of agricultural mechanization i.e.
    [Show full text]
  • Pindari and Roopkund Areas of Nanda Devi Biosphere Reserve of Uttarakhand
    Amity Research Journal of Tourism, Aviation and Hospitality Vol. 03, issue 01, Jan-June 2018 Strategic Management for Eco-Tourism Destinations: Pindari and Roopkund areas of Nanda Devi Biosphere Reserve of Uttarakhand Deepak Kholiya Associate Professor, Graphic Era Hill University, Dehradun Akash Rawat Assistant Professor, Graphic Era (Deemed To Be University) Dehradun (U.K.) Ravish Kukreti Assistant Professor, Graphic Era (Deemed To Be University) Dehradun (U.K.) Email: [email protected] Preeti Joshi Ex-Women Scientist Department of Science & Technology Introduction NANDA DEVI BIOSPHERE RESERVE (NDBR) The interest for mountains, amazing common resplendency, princely social assorted variety, financial conventions, history and way of life polarize mountain dwellers, trekkers, naturalists, religious zealots, pilgrims and social voyagers from everywhere throughout the world to Nanda Devi Biosphere Reserve (NDBR) in the Uttarakhand Himalayas. NDBR is among 19 beginning locales in 13 nations that have been incorporated to UNESCO's reality system of biosphere holds. The hold incorporates the Nanda Devi National Park, a World Heritage site, and the Valley of the Flowers National Park in its center zones. Through advancement and aegis of the biosphere hold, nearby networks in the Lata-Tolma-Malari and Pindari territories are profiting by the improvement of elective wellsprings of salary, for example, eco-the travel industry, and from the change of a rich assortment of rural exercises. It includes parts of three Districts, viz. Chamoli, Pithoragarh and Almora of Uttarakhand state. The main portion of the Biosphere falls in Chamoli District of Garhwal Himalayas. It includes, on its eastern side, some portion of Pithoragarh District, and, on its southern side, some portion of Almora District.
    [Show full text]