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Geology of Nepal; significance of HFT, MBT, MCT

Short answer

Nepal's geology consists of five zones separated by thrusts: Terai, Siwalik, Lesser Himalaya, Higher Himalaya, and Tethys. MFT/HFT is active, causing earthquakes and surface rupture. MBT is a crushed zone causing landslides. MCT is a thick shear zone with rockfalls and landslides, all avoided for structures.

Describe the geology of Nepal with a neat sketch and mention the engineering significance of the HFT, MBT and MCT.

From south to north, Nepal is divided into five tectonic zones, separated by major thrusts and faults (discontinuities):

  S                                              N
  Terai | Sub-Him | Lesser Him | Higher Him | Tethys
        |(Siwalik)|            |            |
       MFT/HFT   MBT          MCT          STDS
  1. Terai (Gangetic plain): Quaternary alluvium.
  2. Sub-Himalaya (Siwalik zone): Miocene to Pleistocene molasse sediments.
  3. Lesser Himalaya: Precambrian to Palaeozoic low-grade metamorphic rocks and sediments.
  4. Higher Himalaya (Great Himalaya): high-grade metamorphic rocks and granites.
  5. Tibetan-Tethys Himalaya: Palaeozoic to Cretaceous fossiliferous marine sediments.

Boundaries (major discontinuities)

  • Main Frontal Thrust (MFT) / Himalayan Frontal Thrust (HFT): between the Terai and Siwalik.
  • Main Boundary Thrust (MBT): between the Siwalik and Lesser Himalaya.
  • Main Central Thrust (MCT): between the Lesser and Higher Himalaya.
  • South Tibetan Detachment System (STDS): between the Higher Himalaya and the Tethys zone.

Geological sketch (simplified north-south section)

 Terai |Siwalik| Lesser Him.  | Higher Him. | Tethys
 alluv.|sandst.| phyllite,     | gneiss,     | limest.,
 gravel|mudst. | quartzite,    | schist,     | shale
       |       | limestone     | granite     |
     MFT     MBT            MCT           STDS

Engineering significance of HFT (MFT), MBT and MCT

  • HFT (MFT): the youngest thrust and still active; it can cause earthquakes and surface rupture. It controls the Terai margin, flooding and changes in groundwater, and gives poor ground for structures.
  • MBT: a wide zone of crushed and sheared rock between the Siwalik and the Lesser Himalaya; a major cause of landslides, and difficult ground for tunnels and roads.
  • MCT: a thick shear zone of highly deformed schist and gneiss, with hot springs; it is partly active, has frequent rockfalls and landslides, and is a risk for hydropower projects.

Hence these zones are avoided for dams, tunnels and bridges unless special design is done.

✓ Answer checked by Claude Opus 5.5 (high effort)

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