Bagrote valley

 BAGROTE VALLEY

Bagrote Valley (Urdu: وادی بگروٹ‎) is a valley in the Karakoram Mountain range in the Gilgit–Baltistan locale of northern Pakistan. River Bagrote courses through the valley from north towards  southwest of the valley, supplies water to Jalalabad and Oshikhandass and converges with the Gilgit River.

Geology:

The Bagrot valley stretches out somewhere in the range of 2,500 and 4500 meters above ocean level. The rule region of the valley is Farfu (in the past called Furpui), likewise known for its scene and high mountains, for example, Rakaposhi 7788 m, Diran 7266 m,[3] Bilchar Dobani 6138 m and the culmination of Fafuraj, Miar Peak, Godeli and numerous different pinnacles that outperform 6,000 meters above ocean level. Doboi icy masses, Gargo, Yunay, Boi Pharai, Hurangi and Raka Poshi encompass the valley from where the streams framing the Bagrot River are traced.[4] The River Bagrot passes by every one of the towns of the valley, including Jalalabad and Oshikhandass and converges with the Gilgit River.

The Bagrot valley reaches out somewhere in the range of 2,500 and 4500 meters above ocean level. The guideline area of the valley is Farfu (earlier called Furpui), additionally known for its scene and high mountains, for example, Rakaposhi 7788 m, Diran 7266 m[4], Dubani 6138 m and the culmination of Fafuraj, Miar Peak, Godeli and numerous different pinnacles that outperform 6,000 meters above ocean level. Doboi ice sheets, Gargo, Yunay, Boi Pharai, Hurangi and Raka Poshi encompass the valley from where the creeks shaping the Bagrot River are followed. Bagrote Valley is in the Karakoram Mountain range in the Gilgit–Baltistan district. Waterway Bagrote moves through the valley from north towards southwest of the valley, supplies water to Jalalabad and Oshikhandass and converges with the Gilgit River. This is valley 38 km away from Gilgit and voyaging time is two hours in addition to work Gasunar valley. Topographically it has Rakaposhi ( Raki poshi) and its glacial mass from where individuals from Gilgit bring Ice for business purposes. This valley was stowed away from even neighborhood populace because of clear reasons: that was street condition. Presently 2/third of the street is metalled and the rest is in a condition that even a little vehicle can go on it. The valley favored with numinous springs, spouting waterways, grandiose pinnacles, icy masses and best part is natural foods grown from the ground. The last town is known as Sath Gasunar (otherwise called Gasunar valley, should visit point). It has bouncing point for travelers to cross Haramosh Valley. From Gasunar valley Rakaposhi mountain is noticeable. 

According to narrators, the genuine pixie knolls lies around here. In nearby language "Daiayal" , a male/female chose by pixies, subsequent to sniffing smoke of junipers tree leaves begins conversing with the pixies. Pixies tell "Daiayal" future and furthermore offer answers for the issues of individuals.

BAGROTE VALLEY AREA:

The Bagrote valley in Gilgit Baltistan Pakistan, having a place with the Kohistan island circular segment and southwestern area of the Karakorum transformative complex, separately, are an area of territorial placer gold mining. 

The geography of Bagrote valley is mostly made out of the stones of the Chalt Group. In the examination region, the chalt metvolcanics of this gathering are primarily covering the investigation region along the eastern a western piece of the Bagrote waterway. In any case, a little openness of ultramafic rocks is additionally uncovered in the south-eastern bit of the examination area.The porches of glacio fluvial and fluvial dregs by and large bay the chalt volcanic in the are. The Chalt bunch comprises of an extremely heterogeneous succession and is usually uncovered in the environmental factors of upper Gilgit and lower Hunza region. It comprises of rotating meta-residue and volcanics. The relationship of meta-residue with tuffs and basaltic to andesitic magmas is very much seen in the Bagrote valley. The huge number of diorites and rocks, which have a place with more youthful molten stage, are barged in into the Chalt bunch. In the upper scopes of the Bulchi and Chirah towns the Chalt bunch comprises of meager had relations with records and yellowish pyrite-bearing schists chlorite-epidote hornblende schist with intercalation of this beds of dim to yellowish carbonates and marbles. Towards north there is a progression of phyllites, quartzite-phyllites, and sericite schist, which show a ceaseless change from basaltic magmas tuff to the chlorite and sericites schist. In Bagrote valley north of Datuche town and close to the Gutumi ice sheet an arrangement of transformative rocks strikes around E-W and plunges towards the south. It comprises of phyllites, sericite-chlorite schists with quartz stringers and focal points conveying sulfides. These stones likewise accomplished higher transformative grade,such as garnet-staurolite schists and gneisses in specific spots of Bagrote valley.

BAGROTE VALLEY TOURISM:

Travelers visit this valley generally in summer. The valley is about 30 minutes drive from Gilgit city. This is the closest vacationer location to Gilgit. The side of the Rakaposhi mountain towards Bagrot valley is better for outdoors because of the rich green timberlands and less group. This valley is known for its leafy foods, likewise for the icy masses and high pinnacles. Vegetables, natural products, and other occasional harvests and Ice from the Glaciers during summers is shipped from the valley to the capital Gilgit, fantasies recommend this ice has mending powers. So far no ice plant is working around there. Ice brought from the Glacier of Bagrot is even moved to Ghizer District. 

The towns of Hamaran, Sinaker, Datuchi, Bulchi, Chirah, Farfu, Hopay, Ghosonar, Sat, Gargo and Sililii lie here and are interconnected by an unmettalled street. Towns on one or the other side of the valley are connected through streetcars (taking into account simple vehicle of products and animals) and wooden extensions, the waterway passes under which comes from icy masses of Karakoram Range.The methods for economy is agribusiness. In any case, with the new development of the Karakorum Highway, the region has been presented to western human advancement, with little films, retail source for mountain hardware and attire, and little inns opening to work with guests.