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Shale Rock



Definition
0

Definition
Shale is a fine-grained sedimentary rock which is formed by the compaction of silt and clay-size mineral particles 0

History
0

Origin
Unknown 0

Discoverer
Unknown 0

Etymology
From German Schalstein laminated limestone, and Schalgebirge layer of stone in stratified rock. From Old English scealu in its base sense of- thing that divides or separate, 0

Class
Sedimentary Rocks 0

Sub-Class
Durable Rock, Medium Hardness Rock 0

Family
0

Group
Not Applicable 0

Other Categories
Fine Grained Rock, Opaque Rock 0

Texture
0

Texture
Clastic, Splintery 0

Color
Black, Brown, Buff, Green, Grey, Red, Yellow 0

Maintenance
More 0

Durability
Durable 0

Water Resistant
No 0

Scratch Resistant
No 0

Stain Resistant
No 0

Wind Resistant
No 0

Acid Resistant
No 0

Appearance
Muddy 0

Uses
0

Architecture
0

Interior Uses
Decorative Aggregates, Homes, Interior Decoration 0

Exterior Uses
As Building Stone, As Facing Stone, Office Buildings 0

Other Architectural Uses
Curbing 0

Industry
0

Construction Industry
Cement Manufacture, Construction Aggregate, for Road Aggregate, Making natural cement, Raw material for the manufacture of mortar 0

Medical Industry
Not Yet Used 0

Antiquity Uses
Artifacts, Sculpture 0

Other Uses
0

Commercial Uses
Creating Artwork, Pottery 0

Types
0

Types
Red Shale, Black Shale, Green Shale, Grey Shale and Yellow Shale 0

Features
Easily splits into thin plates, Generally rough to touch, Very fine grained rock 0

Archaeological Significance
0

Monuments
Used 0

Famous Monuments
Jantar Mantar in India 0

Sculpture
Used 0

Famous Sculptures
Data Not Available 0

Pictographs
Used 0

Petroglyphs
Used 0

Figurines
Used 0

Fossils
Present 0

Formation
0

Formation
Shale forms when very fine-grained clay particles are deposited in water which settle at the bottom of water bodies. They are later compacted hence forming shale. 0

Composition
0

Mineral Content
Albite, Biotite, Calcite, Chert, Chlorite, Dolomite, Hematite, Micas, Muscovite or Illite, Pyrite, Quartz, Silica, Sulfides 0

Compound Content
Ca, Fe, Mg, Silicon Dioxide, Sodium 0

Transformation
0

Metamorphism
No 0

Types of Metamorphism
Not Applicable 0

Weathering
Yes 0

Types of Weathering
Biological Weathering, Chemical Weathering, Mechanical Weathering 0

Erosion
Yes 0

Types of Erosion
Chemical Erosion, Coastal Erosion, Glacier Erosion 0

Properties
0

Physical Properties
0

Hardness
3 0

Grain Size
Very fine-grained 0

Fracture
Not Available 0

Streak
White 0

Porosity
Highly Porous 0

Luster
Dull 0

Compressive Strength
95.00 N/mm2 20

Cleavage
Slaty 0

Toughness
2.6 0

Specific Gravity
2.2-2.8 0

Transparency
Opaque 0

Density
2.4-2.8 g/cm3 0

Thermal Properties
0

Specific Heat Capacity
0.39 kJ/Kg K 23

Resistance
Heat Resistant, Impact Resistant 0

Reserves
0

Deposits in Eastern Continents
0

Asia
Bangladesh, China, India, Russia 0

Africa
Ethiopia, Kenya, Morocco, South Africa, Tanzania 0

Europe
Austria, France, Germany, Greece, Italy, Romania, Scotland, Spain, Switzerland 0

Others
Not Yet Found 0

Deposits in Western Continents
0

North America
USA 0

South America
Bolivia, Chile, Colombia, Ecuador, Peru, Venezuela 0

Deposits in Oceania Continent
0

Australia
New South Wales, New Zealand, Queensland, Victoria, Western Australia 0

Definition >>
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Fossil Rocks

Information about Shale

Rocks are naturally occurring solids which are composed of minerals & have been used by humans since ages. From Stone Age, rocks are used for various purposes. Also, the metals and minerals found in rock play an important role in our life. Get to know all the Shale Uses. We have provided you with all information about Shale rock here. Shale is a fine-grained sedimentary rock which is formed by the compaction of silt and clay-size mineral particles. Shale is available in black, brown, buff, green, grey, red, yellow colors. The streak of a rock is the color of powder produced when it is dragged across an unweathered surface. The streak of Shale is white. Get to know more about Shale rock and characteristics of Shale rock in the next sections.

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