Geological Structures
- Ankit kerketta
- Oct 25, 2020
- 2 min read
Updated: Apr 6, 2021
The beds of undisturbed sedimentary rock formations generally occur in horizontal disposition(प्रकृति). during earth movements,the strata may be tilted out of horizontal.such inclined rock beds are said to have a "Dip".
1} Dip & Strike
•Dip-- Dip is basically an angle of inclination of Rock beds with horizontal plane.
~True dip & Apparent dip--
-Maximum Angle of dip on rock bed is called "True Dip". it is measured in the direction at right angles to the strike.
-A Dip measured in any other direction than true dip is called "Apparent Dip".
•Strike-- It is the direction of line formed by the intersection of a bedding plane & horizontal plane.
Dip angle is measured by Clinometer & Its direction is measured with compass.
Dip varies from 0°to 90°.
Apparent dip is always less than True Dip.
True Dip & Strike are always perpendicular to each other.
2} Fold,Fault & Joints
•Fold-- Wavy undulations (उतार चढ़ाव ) in the rock beds due to Earth movement are called "Fold".
~Elements of Folds-
Anticline & Syncline-
-An Anticline is an up-fold.
-A Syncline is a down-fold.
•Fault--Fault means fracture(दरार) along Which blocks of rock have been displaced relative to each other.
[अर्थात जब Rock bed में Earth movement की वजह से दरार आ जाती है और वे एक-दूसरे से अलग/विस्थापित हो जाते हैं तो उसे Fault कहते हैं।]
~Some types of Fault--
:Normal Fault- Broken ends do not overlap.
:Reverse Fault- Broken ends overlap.
:Trans current Fault- Broken ends move away in the same level.
It is caused by Tensional & Compressional forces.
•Joints-- Joints mean Fracture with no relative displacement between Block of Rock.
[जब Rock bed में Earth movement की वजह से दरार आ जाती है लेकिन वे एक-दूसरे से अलग नहीं होते, उसे Joints कहते हैं।]
it may be vertical, inclined or horizontal .
3} Sill & Dyke
•Sill-- A Sill is a sheet like Igneous body which runs parallel to the bedding planes of pre existing strata.
•Dyke-- A dyke is a wall like Igneous body that cuts across the strata of the pre existing rocks. Dykes are often vertical or steeply inclined.
Sills are commonly made up of Dolerites & Basalt
they burn surrounding coal & make it hard.
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Blogger- Ankit kerketta
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