Erosional & Depositional Landforms - Karst (Limestone) Topography
Karst is a distinctive topography formed in a region of chemically weathered limestone with poorly developed surface drainage that appear pitted and bumpy; originally named after the Karst Plateau of Yugoslavia.
- Limestone and chalk are sedimentary rocks of organic origin derived from organic origin of accumulation of coral and shells in the sea.
- Limestone is made up of calcium carbonate in its pure stage while it is known as dolomite when magnesium is also present.
Erosional Landforms
Generally, Karst topography is characterized by: Caves, Karren, Dolines, Sink-Holes, Ponores, Uvala, Polje, Aven, Natural Bridge, Springs, Blind-Valleys, etc.
- Natural Bridge: It is an ....
Do You Want to Read More?
Subscribe Now
Take Annual Subscription and get the following Advantage
The annual members of the Civil Services Chronicle can read the monthly content of the magazine as well as the Chronicle magazine archives.
Readers can study all the material before the last six months of the Civil Services Chronicle monthly issue in the form of Chronicle magazine archives.
Related Content
- 1 Coastal and Desert Landforms of India
- 2 Origin and Characteristics of Major River Systems
- 3 Integrated River Basin Governance
- 4 Interlinking of Rivers and their Ecological-Economic Trade-offs
- 5 Groundwater Stress Mapping
- 6 Patterns of Regional Disparities and Spatial Development in India
- 7 India’s Strategic Location in the Global and Regional Contexts
- 8 Geological Evolution of the Indian Subcontinent
- 9 India’s Geological Uniqueness: Some Salient Aspects
- 10 Peninsular Block, Himalayan Region, and Indo-Gangetic Plains: Comparative Features

