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Lake Saiful Muluk is a mountainous lake located at the northern end of the Kaghan Valley, near the town of Naran. It is in the north east of Mansehra District in the Khyber-Pakhtunkhwa province, Pakistan and feeds water to Kunhar river. At an elevation of 3,224 m (10,578 feet) above sea level, it is well above the tree line, and is one of the highest lakes in Pakistan.Malika Parbat, the highest peak in the valley is near the lake.Saiful Muluk was formed by glacial moraines that blocked the water of the stream passing through the valley.
Saiful Muluk (Urdu: جھیل سیف الملوک) is a mountainous lake located at the northern end of the Kaghan Valley, near the town of Naran. Malika Parbat, the highest peak in the valley is near the lake.At an elevation of 3,224 m (10,578 feet) above sea level, it is well above the tree line, and is one of the highest lakes in Pakistan.
international mountain day 11 December 2011
International Mountain Day is an opportunity to create awareness about the importance of mountains to life, to highlight the opportunities and constraints in mountain development and to build partnerships that will bring positive change to the world's mountains and highlands.
nanga parbat "8125 mtrs high"the killer moutnain in pakistan
The Indus is a transboundary river of Asia and a trans-Himalayan river of South and Central Asia. The 3,120 km river rises in mountain springs northeast of Mount Kailash in Western Tibet, flows northwest through the disputed region of Kashmir, bends sharply to the left after the Nanga Parbat massif, and flows south-by-southwest through Pakistan, before emptying into the Arabian Sea near the port city of Karachi.
The green-tinged Indus river meets the slightly muddy Zanskar river which has its source in the Zanskar valley near the scenic Nimmu valley, that falls between Leh and Kargil. The rivers are clearly distinguished by their colours.
While there are so many fascinating spots in Ladakh,India that can catch the eye of the wanderlust, the river confluence of Zanskar and Indus is nothing short of a glimpse of heaven.
In honour of Hans life I made this little star and used a galaxy photo as a background.
This is about 5,5 cm.
Background photo: Milky Way Galaxy shimmering over Nanga Parbat, Pakistan by Pervisha Kahn (Knanumsays)
commons.wikimedia.org/wiki/File:Milky_Way_Galaxy_shimmeri...
Happy Macro Monday.
Thank you for your views, faves and or comments, they are greatly appreciated !!!
Don't use this image on websites, blogs or other media without my explicit permission !!!
© all rights reserved Lily aenee
A view of Fairy Meadows, locally known as Joot, at an altitude of 3,300 meters, which is also located near one of the base camps of Nanga Parbat (The Killer Mountain).
Nanga Parbat Mountains known locally as Diamer, is the ninth-highest mountain in the world at 8,126 metres (26,660 ft) above sea level
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
A stunning view of world's 9th highest peak - Nanga Parbat.
I was lucky to capture this view from Karakoram Highway. Morning with beautiful. and sky was clear to have this heart-touching scene. Nanga Parbat is also know us "The killer mountain"
Il gruppo delle Odle (Geislergruppe o Geislerspitzen in tedesco) è una catena montuosa delle Dolomiti che assieme al gruppo del Puez costituisce la maggior parte del territorio del parco naturale Puez-Odle, contornato dalla val Badia, val Gardena e val di Funes, in Alto Adige.
La cima più alta della catena è il Sass Rigais, a pari merito con la cima della Furchetta, entrambe raggiungono infatti la quota di 3.025 metri.
Le Odle si compongono principalmente di due catene, le Odle di Eores e le "Odle di Funes":
Odle di Eores (Aferer Geisler), sono attraversate dal Sentiero attrezzato Günther Messner, dedicata al fratello di Reinhold Messner, sepolto da una valanga, caduta dal monte Nanga Parbat nel giugno 1970. Il sentiero passa sia sulla sponda meridionale che su quella settentrionale della catena;
Odle di Funes (Villnösser Geisler), rappresentano le principali cime della catena e si trovano a sud, rispetto a quelle di Eores.
Alla base delle Odle di Funes, si può percorrere il cosiddetto "sentiero delle Odle" (in tedesco Adolf Munkel-Weg), che passa alla base settentrionale del gruppo delle Odle, dove si trova anche una palestra di roccia.
Il termine Odle si traduce dalla lingua ladina semplicemente in "aghi", con riferimento alla forma appuntita di molte cime di questo gruppo.
PS) Le Dolomiti sono uno spettacolo naturale meraviglioso e anche per questo son state dichiarate " Patrimonio dell'Umanità " dall'UNESCO!!! Le Odle sono le mie preferite in assoluto!!!!
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km. The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Mt Sangthang སང་ ཐང་ 6430 m.
Almost 90 km distance away.
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
"Claro que uno conoce la montaña y sus peligros: ¿cómo sería posible no sentir respeto? En cada nueva ascensión se desafía a la naturaleza, que puede ser una amiga benévola, pero también una enemiga implacable, así se explica la exaltación que nos embarga cuando, tras el combate con la naturaleza hostil, coronamos la cima radiantes, triunfales, aunque exhaustos, la montaña gigante a nuestros pies. Ahora unidos y en amistad con la naturaleza y todo lo bello de este mundo, pero sabiendo bien que no hemos domeñado la grandiosidad de la montaña, sino tan sólo a nosotros mismos. Cuán minúsculo e insignificante resulta el hombre en el conjunto del universo lo sabemos tal vez mejor que nadie los alpinistas…"
Hermann Buhl: "Del Tirol al Nanga Parbat".
Cumbre invernal con vista al este, al fondo los volcanes Domuyo y Tromen en Neuquén, Argentina.
Región de Ñuble, Chile central.
“¿Puede, pues, esto proporcionar alegría? ¿Un empeño en que a veces pende de una hebra la vida? ¿En que el gran adversario, la muerte, constituye perenne acompañamiento? Eso jamás lo entenderá el que no es montañero... Sabemos lo que significa vivir. Lo que significa conquistar a cada paso la vida. Hay que haber hollado el borde del abismo para saber cuán hermosa es la vida y cuán maravilloso, el mundo."
Hermann Buhl: "Del Tirol al Nanga Parbat".
Al fin del mundo, en el "altiplano" al sur del cerro Betinelli, rumbo al lago Windhond.
Región de Magallanes, Patagonia, Chile.
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km.
The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
www.himalaya2000.com/himalayan-facts/climate-of-himalayas...
Before knowing the weather condition of the Himalayan region we should understand its geography. The Himalayan region covers an area of 2,250 km with an average width of 200 km. The forest belt of the Himalayan region consists of Oak, Rhododendron, Birch, Pine, Deodar, and Fir. And the monsoon season in this region lasts for mid June till the end of September. The Himalayas influences the meteorological conditions in the Indian subcontinent to the south and in the Central Asian highlands to the north to a great extent. It acts a climatic divider circulating the air and water system to a great extent. Because of its altitude and location it blocks the passage of the cold winds coming from the north to the Indian sub continent thereby making India's climate much more moderate. It also influences the rainfall pattern in India. The combined effect of rainfall, latitude and altitude largely influences the forests belts in the Himalayan region. The rainfall is mostly recorded during the monsoon time of June to September but it decreases as you travel from east to west. The snow-capped ranges of the Himalayas stretch 2, 250 km from the Namcha Barwa to Nanga Parbat on the Indus. The range extends from east to west up to central-Nepal and then takes a southeast to northwest direction.
<a href="http://www.himalaya2000.com/himalayan-facts/climate-of-himalayas.html"
This is the Bahordes peak. Its height is 5809 meters above from sea level. It is a very beautiful mountain.
It is this beauty and characteristic of this mountain that once attracts the adventurers who have come to this valley.
And people who come to this valley for the purpose of trekking and adventure take lot of photographs of this mountain.
A British woman expedition tried to summit this mountain in 1978, but didnt reach the summit..
K-2 Ghandogoro La Trek
This trek is one of the most popular trekking routes in Pakistan even in the world due to the traverse through amphitheater of eight of the worlds 30 highest peaks at a distance of about 25 kilometers. The area covered by this trek contains the highest concentration of high peaks any were in the world providing perhaps the greatest mountain scenery on earth. We have a special day free at Concordia to explore the hidden beauty of the surroundings.View Detail www.takpaktour.com/public/Trekking/K-2-ghandogoro-la-trek
K-7 Valley Trek
The village of Hushe is the last Village where jeep road ends. At the edge of Hushe Valley is offer to magnificent view of Masherbrum (7821m) , five large glaciers; Ghandogoro, Masherbrum, Chogolisa, Choraksa & Aling. The k-7 Valley is beautiful & a paradise for rock climbers. Where there are many rock peaks out of which K-7 peak, Fati Peak, Farhad peak, Naisar peak are popular. In this trek, you will be able to see the beautiful places of Skardu Valley, Khaplu Valley, and Masherbrum Valley & K 7 Valley which will be remembered in your life. View Detail www.takpaktour.com/public/Trekking/K-7-valley-trek
Rakaposhi Basecamp Trek
Rakaposhi (7788 m)is ranked 27th highest on the Earth and the 12th highest in Pakistan is popular as one of the most beautiful mountains in the world. The peak is the part of Karakorum mountain range is situated in the Nagar Valley near Gilgit. Rakaposhi was first climbed in 1958 by Mike Banks and Tom Patey, members of a British-Pakistani expedition. Rakaposhi is notable for its exceptional rise over local terrain, almost unmatched in the world. The peak rises just beside the Karakorum Highway on the route through China via Hunza.View Detail www.takpaktour.com/public/Trekking/rakaposhi-basecamp-trek
Biafo Hishper Trek
Biafo & Hishper glaciers combine together forms the worlds longest glacier outside the polar region. The Snow Lake & the Hishper pass give an unmatched trekking experience. After seven hours jeep journey from Skardu the trek will begin at Askole for the 115 km ice corridor trek walking on dancing stones, crossing splashing streams, camping on the summer pastures on the lateral moraines, crossing the 5150 M Hishper pass & four major side glaciers, We will end up the trek at Hishper village, the first permanent settlement after leaving Askoli in 12 days. View Detail www.takpaktour.com/public/Trekking/biafo-hishper-trek
Nanga Parbat Basecamp Trek
Trek Fairy Meadows, named by German climbers ( German Marchenwiese, fairy tale meadows) & locally known as Joot, is a grassland near one of the base sites of the Nanga parbat located in Diamir District, Gilgit-Baltistan At an altitude of about 3,300 meters above the sea level, Fairy meadows is approachable by twelve kilometers-long jeep able trek starting from Riakhot Bridge on Karakorum hight way to the village Tato Further from Tato, it takes about three to four hours hiking by a five kilometers trek to Fairy Meadows. The grassland is located in the Raikhot Valley, at one end of the Raikhot glacier which originates from the Nanga parbat & feeds a stream that finally falls in the river Indus. View Detail www.takpaktour.com/public/Trekking/nanga-parbat-basecamp-...