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

KSHEC Scholarship 2024-25

KSHEC Scholarship 2024-25 Alert! First-Year UG Students Only, Don't Miss This Golden Opportunity! πŸ’‘βœ¨ Are you a first-year undergraduate student studying in a Government or Aided College in Kerala? Do you need financial assistance to continue your education without stress? The Kerala State Higher Education Council (KSHEC) Scholarship is here to support YOU!  This scholarship is a lifeline for deserving students, helping them focus on their studies without worrying about financial burdens. If you meet the criteria, APPLY NOW and take a step towards a brighter future! 🌟 βœ… Simple Online Application – Quick & easy process!  πŸ“Œ Who Can Apply? βœ”οΈ First-year UG students ONLY βœ”οΈ Must be studying in an Arts & Science Government or Aided college in Kerala βœ”οΈ Professional Course students are not eligible  πŸ”Ή Scholarship Amounts Per Year: πŸ“Œ 1st Year FYUGP – β‚Ή12,000 πŸ“Œ 2nd Year FYUGP – β‚Ή18,000 πŸ“Œ 3rd Year FYUGP – β‚Ή24,000 πŸ“Œ 4th Year FYUGP – β‚Ή40,000 πŸ“Œ 5th Year PG – β‚Ή60,000  Great News...

Disaster Management

1. Disaster Risk Analysis β†’ Disaster Risk Reduction β†’ Disaster Management Cycle Disaster Risk Analysis is the first step in managing disasters. It involves assessing potential hazards, identifying vulnerable populations, and estimating possible impacts. Once risks are identified, Disaster Risk Reduction (DRR) strategies come into play. DRR aims to reduce risk and enhance resilience through planning, infrastructure development, and policy enforcement. The Disaster Management Cycle then ensures a structured approach by dividing actions into pre-disaster, during-disaster, and post-disaster phases . Example Connection: Imagine a coastal city prone to cyclones: Risk Analysis identifies low-lying areas and weak infrastructure. Risk Reduction includes building seawalls, enforcing strict building codes, and training residents for emergency situations. The Disaster Management Cycle ensures ongoing preparedness, immediate response during a cyclone, and long-term recovery afterw...

Pre During and Post Disaster

Disaster management is a structured approach aimed at reducing risks, responding effectively, and ensuring a swift recovery from disasters. It consists of three main phases: Pre-Disaster (Mitigation & Preparedness), During Disaster (Response), and Post-Disaster (Recovery). These phases involve various strategies, policies, and actions to protect lives, property, and the environment. Below is a breakdown of each phase with key concepts, terminologies, and examples. 1. Pre-Disaster Phase (Mitigation and Preparedness) Mitigation: This phase focuses on reducing the severity of a disaster by minimizing risks and vulnerabilities. It involves structural and non-structural measures. Hazard Identification: Recognizing potential natural and human-made hazards (e.g., earthquakes, floods, industrial accidents). Risk Assessment: Evaluating the probability and consequences of disasters using GIS, remote sensing, and historical data. Vulnerability Analysis: Identifying areas and p...

Recovery and Rehabilitation

Disaster management involves several phases, including mitigation, preparedness, response, recovery, and rehabilitation . Recovery and rehabilitation are post-disaster activities that aim to restore normalcy and improve resilience in affected areas. 1. Recovery Recovery is the long-term process of rebuilding communities, infrastructure, economy, and social systems after a disaster. It focuses on restoring normalcy while incorporating resilience measures to withstand future disasters. Short-term Recovery – Immediate efforts within weeks or months to restore essential services (e.g., water, electricity, healthcare, shelter). Long-term Recovery – Efforts that take months to years, including rebuilding infrastructure, economic revitalization, and mental health support. Resilience – The ability of a community to recover quickly and adapt to future disasters. Livelihood Restoration – Providing economic support to affected populations through job creation, skill training, a...

Mapping Process

The mapping process involves several systematic steps to transform real-world spatial information into a readable, accurate, and useful representation. Below is a structured explanation of each step in the mapping process, with key concepts, terminologies, and examples. 1. Defining the Purpose of the Map Before creating a map, it is essential to determine its purpose and audience . Different maps serve different objectives, such as navigation, analysis, or communication. Types of Maps Based on Purpose: Thematic Maps: Focus on specific subjects (e.g., climate maps, population density maps). Topographic Maps: Show natural and human-made features (e.g., contour maps, landform maps). Tourist Maps: Highlight attractions, roads, and landmarks for travelers. Cadastral Maps: Used in land ownership and property boundaries. Navigational Maps: Used in GPS systems for wayfinding. Example: A disaster risk map for floods will highlight flood-prone areas, emergency shelters, and ...