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LANDSLIDE
Submitted by- kushagra, Prince
INTRODUCTION TO TOPIC
Landslides, also known as landslips, are several forms of mass wasting that may include a
wide range of ground movements, such as rock falls, deep-seated slope failures, mudflows,
and debris flows.
A landslide near Cusco, Peru, in 2018
Types of landslides
Landslides are generally classified by type of movement (slides, flows, spreads, topples, or falls) and type
of material (rock, debris, or earth).
CASE STUDY OF MALIN, PUNE
Case study -02
Gangtok, geographically bounded by 27.3325°N latitude to 88.6140°E, longitude is situated
at an altitude of about 1800 m above sea level encompassing the third highest mountain
(Mount Kanchenjunga) in the World. Gangtok city is flanked by two rivers, i.e. Rorochu in the
eastward side and Ranikhola on the west. Both the rivers meet at Ranipool and flow towards
the south before they again join the Teesta at Singtam. The city is located at the south-facing
slope of Eastern Himalaya and has erosional topography bounded and dissected by a large
number of perennial and seasonal springs. The study area experiences a high variation of
rainfall throughout the year.
For the city, 7 June 1997 is often referred as a ‘black day’ since in this particular date, the city had
witnessed a number of landslides due to heavy rainfall (approximately 224 mm) causing more
than 50 fatalities, 60 people injuries, more than 5000 people lost their home and disruption of
National Highway 31A (near Rangpo town).
Location map of the study area.
Annual rainfall in Gangtok for the period of 2006–2017 (Source: Indian meteorological
department)
(a) Geological map of the Gangtok and its surrounding area,
(b) (b) cross-section along A-B line, (c) cross-section along C-D line
Showing landslide scars in study area detected by LISS IV (left side) and google earth pro (right
side)
Landslide inventory map of the study area.
The study area mostly consists of gneissic rocks
and schistose rocks type
due to high rainfall, rocks are highly weathered
and eroded at many places which causes
frequent landslides.
THANKYOU

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LANDSLIDE

  • 2. INTRODUCTION TO TOPIC Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rock falls, deep-seated slope failures, mudflows, and debris flows. A landslide near Cusco, Peru, in 2018
  • 3. Types of landslides Landslides are generally classified by type of movement (slides, flows, spreads, topples, or falls) and type of material (rock, debris, or earth).
  • 4. CASE STUDY OF MALIN, PUNE
  • 5.
  • 6.
  • 7.
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  • 29. Case study -02 Gangtok, geographically bounded by 27.3325°N latitude to 88.6140°E, longitude is situated at an altitude of about 1800 m above sea level encompassing the third highest mountain (Mount Kanchenjunga) in the World. Gangtok city is flanked by two rivers, i.e. Rorochu in the eastward side and Ranikhola on the west. Both the rivers meet at Ranipool and flow towards the south before they again join the Teesta at Singtam. The city is located at the south-facing slope of Eastern Himalaya and has erosional topography bounded and dissected by a large number of perennial and seasonal springs. The study area experiences a high variation of rainfall throughout the year.
  • 30. For the city, 7 June 1997 is often referred as a ‘black day’ since in this particular date, the city had witnessed a number of landslides due to heavy rainfall (approximately 224 mm) causing more than 50 fatalities, 60 people injuries, more than 5000 people lost their home and disruption of National Highway 31A (near Rangpo town).
  • 31. Location map of the study area.
  • 32. Annual rainfall in Gangtok for the period of 2006–2017 (Source: Indian meteorological department)
  • 33. (a) Geological map of the Gangtok and its surrounding area, (b) (b) cross-section along A-B line, (c) cross-section along C-D line
  • 34. Showing landslide scars in study area detected by LISS IV (left side) and google earth pro (right side)
  • 35. Landslide inventory map of the study area. The study area mostly consists of gneissic rocks and schistose rocks type due to high rainfall, rocks are highly weathered and eroded at many places which causes frequent landslides.