Skip to main content

Geology and Tectonic. Indian Shield


1. Ch (Chattisgarh Basin): Chattisgarh Basin is a geological region in central India known for its sedimentary rock formations. It's important for its mineral resources, including coal and iron ore.

2. CIS (Central Indian Shear Zone): CIS is a tectonic boundary in central India where the Indian Plate interacts with the Eurasian Plate. It's characterized by significant faulting and seismic activity.

3. GR (Godavari Rift): The Godavari Rift is a geological feature associated with the rifting and splitting of the Indian Plate. It's located in the Godavari River basin in southeastern India.

4. M (Madras Block): The Madras Block is a stable continental block in southern India. It's part of the Indian Plate and is not associated with active tectonic processes.

5. Mk (Malanjkhand): Malanjkhand is known for its copper deposits and is one of the largest copper mines in India.

6. MR (Mahanadi Rift): The Mahanadi Rift is a geological feature related to the rifting of the Indian Plate. It's associated with the formation of the Mahanadi River basin in eastern India.

7. N (Nilgiri Block): The Nilgiri Block is a geological region in southern India, known for its ancient rocks and distinct geological history.

8. NS (Narmada-Son Fault Zone): This fault zone extends across central India and marks a significant tectonic boundary where the Indian Plate meets the Eurasian Plate.

9. PC (Palghat-Cauvery Shear Zone): The Palghat-Cauvery Shear Zone is a major geological fault system in southern India, where the Indian Plate interacts with the Eurasian Plate.

10. R (Rengali Province and Kerajang Shear Zone): These are geological regions in eastern India, possibly associated with shear zones and tectonic activity.

11. S (Singhbhum Shear Zone): The Singhbhum Shear Zone is a tectonic feature in eastern India that has played a significant role in the geological history of the region.

12. V (Vindhyan Basin): The Vindhyan Basin is a sedimentary basin in central India known for its extensive rock formations, which hold clues to the Earth's geological past.



1. Shear Zone:
   A shear zone is a geological area where rocks have experienced significant lateral movement in opposite directions. This movement typically occurs along a fault plane, resulting in rocks being displaced horizontally. Shear zones are often associated with intense deformation and can be important for understanding tectonic processes.

2. Block:
   In geology, a block refers to a section of the Earth's crust that is bounded by faults or tectonic boundaries. Blocks can be large or small and are often used to describe distinct regions within a tectonic setting. For example, "crustal blocks" are pieces of the Earth's crust that have different geological characteristics.

3. Fault:
   A fault is a fracture or zone of rock where there has been movement. It's a boundary where rocks on either side have shifted relative to each other. Faults can be caused by tectonic forces, and they are often responsible for earthquakes when they suddenly release accumulated stress.

4. Rift Valley:
   A rift valley is a linear depression or lowland region on the Earth's surface that forms when the Earth's crust is stretched and pulled apart. Rift valleys are often associated with tectonic plate boundaries and are where continents may begin to split apart, eventually forming new ocean basins.

5. Craton:
   A craton is the stable, ancient core of a continent that consists of thick, relatively undeformed layers of the Earth's crust. These regions have been geologically quiet for a long time and are considered the "nuclei" of continents. They are often surrounded by younger geological features.

6. Shield:
   A shield is a large, stable area of exposed Precambrian rock (rock that is more than 600 million years old) on a continent's surface. Shields are typically found within cratons and are characterized by their lack of significant mountain ranges or recent tectonic activity. They often form the central core of continents.

7. Basin:
   A basin is a low-lying, often bowl-shaped, geographical area with defined boundaries that can be either geological or hydrological. Geological basins may contain sedimentary rocks that have accumulated over millions of years and can be associated with depressions in the Earth's crust. Hydrological basins are areas drained by a river system.


Comments

Popular posts from this blog

How to find drugs against the Corona. Covid 19

FOR SCIENTISTS (and others interested): How to find drugs against the coronavirus: First clues on how we can beat COVID-19. This shows the many ways we can interfere with its replication cycle by repurposing existing drugs - summarized in today's Science journal. LINK TO ARTICLE:  https://science.sciencemag.org/content/367/6485/1412 .... Vineesh V Assistant Professor of Geography, Directorate of Education, Government of Kerala. https://g.page/vineeshvc

Geography of Health or Medical Geography

Health Geography (also known as Medical Geography ) is a sub-discipline of Human Geography that studies the relationships between place, environment, society, and health . It examines how spatial location, environmental conditions, and social and economic factors influence human health, disease patterns, and access to healthcare services. Health geography integrates concepts from geography, epidemiology, medicine, public health, environmental science, sociology, and Geographic Information Systems (GIS) to understand and improve population health. Major Components of Health Geography Health geography is generally divided into two major branches : The Geography of Disease and Ill Health The Geography of Health Care 1. The Geography of Disease and Ill Health This branch studies the spatial distribution, determinants, and diffusion of diseases across different geographical scales, from neighborhoods to global regions. It seeks t...

Artificial Groundwater Recharge: Methods and Benefits

Artificial groundwater recharge is the process of replenishing aquifers through human intervention. It is used to address water deficits, improve groundwater quality, and sustain water resources for long-term use. Methods of Artificial Groundwater Recharge Infiltration Basins – Shallow depressions designed to capture stormwater runoff, allowing it to percolate into the aquifer. Percolation Tanks – Reservoirs where excess runoff is stored and gradually seeps through highly permeable soil to recharge groundwater. Recharge Canals – Water is diverted across the land surface to facilitate infiltration into the aquifer. Injection Wells (Recharge Wells) – Treated surface water is pumped into deep aquifers under pressure, ensuring direct groundwater replenishment. Irrigation Furrows and Sprinkler Systems – Water is applied to the land surface, where it gradually infiltrates into the ground, enhancing recharge. Rainwater Harvesting – Collected surface water, including rainwater, is ...

IDW and Kriging

Kriging and Inverse Distance Weighting (IDW) are both interpolation techniques commonly used in GIS to estimate values at unmeasured locations based on a set of known data points. Here's an explanation and a comparison of Kriging and IDW: Kriging: Kriging is a geostatistical interpolation method that takes into account the spatial autocorrelation of the data. It provides the best linear unbiased prediction of the unknown values. Kriging assumes that the data follows a spatial pattern and calculates weights based on the spatial relationship between known points. It considers the distance between points, the variability of the data, and the spatial structure to generate the interpolated surface. Kriging provides estimates of the spatial variability and uncertainty through the calculation of a variogram or covariance model. IDW (Inverse Distance Weighting): IDW is a simpler interpolation method that assigns weights to known points based on their distance from the target location. The ...

Human impacts on Land, water and air.

Human interaction with the natural environment has changed significantly throughout history. Initially, environmental impacts were localized and small-scale , but with technological development, population growth, and industrialization, these impacts have expanded to regional and global scales . In environmental geography and ecology, this transformation is often explained using concepts such as anthropogenic impact , environmental degradation , land-use change , and the Anthropocene (the proposed geological epoch dominated by human influence). 1. Paleolithic Age (≈ 2.5 million years ago – 10,000 BCE) Key Concept: Hunter–Gatherer Environmental Interaction During the Paleolithic period, humans lived as nomadic hunter-gatherers , relying directly on natural ecosystems for food and shelter. Human population density was very low, so environmental impact was limited. Environmental Impacts Fire Ecology: Humans used controlled burning for cooking, warmth, and landscape management. This pr...