Nepal: Geology and Geography

Geological Field Report of Malekhu Area. Sample A Sample B Geological Field Report of   Palpa Area .

After M.Sc Geology/Engineering Geology, one can work as a Geologist/Engineering Geologist in Nepal. There are various opportunities in Governmental and Private Sectors for a Geologist. The major sectors where Geologists/Engineering Geologists engage in Nepal are: 1. Government Sector The Public Service Commission  recruits various positions Geologist, Engineering Geologist, Hydrogeologist, Seismologist. These man powers work in Department of Mines and Geology (DMG), Ground water resource and Irrigation offices, Ministry of Energy and Water Resource, Electricity Development Board. नेपाल इन्जिनियरिङ सेवा जियिलोजि समुह अन्तर्गतका जनरल जियोलोजी, हाइड्रोजियोलोजी र इन्जिनियरिङ  जियोलोजी उप समुहहरुकोको राजपत्राङ्कित तृतिय श्रेणीका पदहरुको खुला प्रतियोगितात्मक परीक्षाको पाठ्यक्रम(Syllabus of Geologist/Engineering Geologist/Hydrogeologist)  ( First Paper    Second Paper) The Public Service Commission also recruits Assistant Geologist/Hydrogeologist with qualification of B.Sc. passed candidates.

  B.Sc. Geology | Tribhuvan University Bachelor of Science in Geology (BSc in Geology) is an undergraduate program offered by Tribhuvan University (TU), under the management of Institute of Science and Technology (IoST). It is a four year annual degree program total that includes theory, laboratory practical, field work and thesis writing. The duration of BSc in Geology program was changed from 3 years to 4 years from the year 2069 BS (2012 A.D) to provide international standard of education to students at a reasonable price in Nepal. Bachelor of Science in Geology program deals with the study of physical and chemical nature, structure and geological process of earth with comprehensive understanding of earth surface processes, earth materials, tectonics, rock forming processes and paleontology including petroleum geology, volcanologist, structural geology, hydrology, sedimentary geology and climate change. This is a rigorous program for students who are excitedly interested and passion

  The Himalaya was formed due to collision of Indian Plate and Eurasian Plate at about 40 million years ago. It extends in 2400km east - west direction. Its width varies from 230 to 320 km and bounded between the Indo-Gangetic Plain in the south and Tibetan Plateau in the north. Nepal Himalaya occupies the central 800km part. Heim & Gansser 1939 , and   Gansser 1964   divided the rocks of the Himalaya into four   tectonostratigraphic   zones that are characterised by distinctive   stratigraphy   and physiography. From south to north, it can be divided into five latitudinal morpho-tectonic zones and these are : 1.  The Gangatic Plain  (Terai) 2.  The Sub Himalayan  (Chure or Siwalik) 3  Lesser Himalayan  (Mahabharat Mountain Range), 4.  Greater Himalayan , and 5.  Tibetan Himalayan zones  (Tethys Himalaya). Each of these zones is clearly identified by their morphological, geological and tectonic features. Main Frontal Thrust (MFT), Main Boundary Thrust (MBT), Main Central Thrust (MC