Doboi glaciers, Gargo, Yunay, Boi Pharai, Hurangi, and Raka Poshi surround the valley from where the rivulets forming the Bagrot River are traced.

The valley is blessed with numerous springs, gushing rivers, lofty peaks, glaciers, and the best part is organic fruits and vegetables.

The Bagrote valley in Gilgit Baltistan, Pakistan, belonging to the Kohistan island arc and southwestern domain of the Karakorum metamorphic complex, respectively, is a location of regional placer gold mining.

The Chalt group consists of a very heterogeneous sequence and is commonly exposed in the surroundings of the upper Gilgit and lower Hunza area.

In Bagrote valley north of Datuche village and near the Gutumi glacier a formation of metamorphic rocks strikes approximately E-W and dips towards the south.

These rocks also attained higher metamorphic grades, such as garnet-staurolite schists and gneisses in certain places of Bagrote valley.

The side of the Rakaposhi mountain towards Bagrot valley is better for camping due to the lush green forests and less crowd.

The villages of Hamaran, Sinaker, Datuchi, Bulchi, Chirah, Farfu, Hopay, Ghosonar, Saat, Gargo and Sililii lie in the valley and are interconnected by an unmetalled road.

Villages on either side of the valley are linked via cable cars (allowing for easy transport of goods and livestock) and wooden bridges, the river passes underneath which comes from glaciers of Karakoram Range.