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  2. Main Boundary Thrust - Wikipedia

    en.wikipedia.org/wiki/Main_Boundary_Thrust

    The MBT was formed as a result of the collision of the Indian continent with Asia.It developed to relieve stresses from the compression of the continental collision.When the MBT initially formed around 10-25 million years ago, [1] it was a system of thrust faults which accommodated stresses from the compression of the continental collision which led to Himalayan uplift.

  3. Main Central Thrust - Wikipedia

    en.wikipedia.org/wiki/Main_Central_Thrust

    By lithologic criteria, the Main Central Thrust is defined as the boundary between quartzite and phyllite, from the Lesser Himalayan Sequence; and the orthogneiss biotite-rich schist, which belongs to the Greater Himalayan Crystalline complex. [2] [3] By metamorphic isograd, the Main Central Thrust follows the kyanite isograd. Under this ...

  4. Geology of the Himalayas - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Himalayas

    From south to north, the zones and the major faults separating them are the Main Frontal Thrust (MFT), Subhimalaya Zone (also called Sivalik), Main Boundary Thrust (MBT), Lesser Himalaya (further subdivided into the "Lesser Himalayan Sedimentary Zone (LHSZ) and the Lesser Himalayan Crystalline Nappes (LHCN)), Main Central thrust (MCT), Higher ...

  5. Main Frontal Thrust - Wikipedia

    en.wikipedia.org/wiki/Main_Frontal_Thrust

    The Main Frontal Thrust (MFT), also known as the Himalayan Frontal Thrust (HFT), is a geological fault in the Himalayas that defines the boundary between the Himalayan foothills and Indo-Gangetic Plain. [1] The fault is well expressed on the surface thus could be seen via satellite imagery.

  6. Lower Himalayan Range - Wikipedia

    en.wikipedia.org/wiki/Lower_Himalayan_Range

    Southern slopes of the Himachal Range are steep and nearly uninhabited due to a major fault system called the 'Main Boundary Thrust". The crest and northern slopes slope gently enough to support upland pastures and terraced fields.

  7. 1999 Chamoli earthquake - Wikipedia

    en.wikipedia.org/wiki/1999_Chamoli_earthquake

    The Himalaya Range has been undergoing crustal shortening along the 2,400 km long northern edge of the Indian plate which resulted in the formation of several thrust faults including the Main Central Thrust (MCT), the Main Boundary Thrust (MBT) and the Main Frontal Thrust (MFT). The MCT consists of three sub-thrusts: MCT I, MCT II and MCT III.

  8. Killing of UnitedHealthcare CEO prompts flurry of stories on ...

    www.aol.com/finance/killing-unitedhealthcare-ceo...

    The early morning killing of a top health insurance executive in midtown Manhattan Wednesday has unleashed a flurry of rage and frustration from social media users over denials of their medical ...

  9. Fold mountains - Wikipedia

    en.wikipedia.org/wiki/Fold_mountains

    Fold mountains form in areas of thrust tectonics, such as where two tectonic plates move towards each other at convergent plate boundary.When plates and the continents riding on them collide or undergo subduction (that is – ride one over another), the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak ...