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Shale and Hornblendite


Hornblendite and Shale


Definition

Definition
Shale is a fine-grained sedimentary rock which is formed by the compaction of silt and clay-size mineral particles  
Hornblendite is a type of igneous plutonic rock consisting mainly of amphibole hornblende and is a type of Amphibolite rock  

History
  
  

Origin
-  
-  

Discoverer
Johann Gottlob Lehmann  
Unknown  

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,  
From German, Horn horn + blende  

Class
Sedimentary Rocks  
Igneous Rocks  

Sub-Class
Durable Rock, Medium Hardness Rock  
Durable Rock, Hard Rock  

Family
  
  

Group
-  
Plutonic  

Other Categories
Fine Grained Rock, Opaque Rock  
Coarse Grained Rock, Medium Grained Rock, Opaque Rock  

Texture

Texture
Clastic, Splintery  
Banded, Foliated, Massive  

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

Maintenance
More  
Less  

Durability
Durable  
Durable  

Water Resistant
No  
Yes  

Scratch Resistant
No  
Yes  

Stain Resistant
No  
No  

Wind Resistant
No  
Yes  

Acid Resistant
No  
No  

Appearance
Muddy  
Foliated  

Uses

Architecture
  
  

Interior Uses
Decorative Aggregates, Homes, Interior Decoration  
Countertops, Decorative Aggregates, Entryways, Flooring, Homes, Hotels, Interior Decoration, Kitchens  

Exterior Uses
As Building Stone, As Facing Stone, Office Buildings  
As Building Stone, As Facing Stone, Paving Stone, Garden Decoration, Office Buildings  

Other Architectural Uses
Curbing  
Curbing  

Industry
  
  

Construction Industry
Cement Manufacture, Construction Aggregate, for Road Aggregate, Making natural cement, Raw material for the manufacture of mortar  
As Dimension Stone, Building houses or walls, Cobblestones, Construction Aggregate, for Road Aggregate, Landscaping, Production of Glass and Ceramics, Roadstone  

Medical Industry
-  
-  

Antiquity Uses
Artifacts, Sculpture  
Artifacts, Sculpture, Small Figurines  

Other Uses
  
  

Commercial Uses
Creating Artwork, Pottery  
Cemetery Markers, Commemorative Tablets, Creating Artwork  

Types

Types
Red Shale, Black Shale, Green Shale, Grey Shale and Yellow Shale  
Hornblende Gabbro and Hornblende Peridotite  

Features
Easily splits into thin plates, Generally rough to touch, Very fine grained rock  
Clasts are smooth to touch, Matrix variable, Surfaces are often shiny  

Archaeological Significance
  
  

Monuments
-  
-  

Famous Monuments
Jantar Mantar in India  
-  

Sculpture
-  
-  

Famous Sculptures
-  
-  

Pictographs
-  
-  

Petroglyphs
-  
-  

Figurines
-  
-  

Fossils
Present  
Absent  

Formation

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.  
Hornblendite is a fine-grained, hard rock which is a type of metasomatite, essentially altered basalt. It forms with or without crystallization, either below the surface as intrusive rocks or on the surface as extrusive rocks.  

Composition
  
  

Mineral Content
Albite, Biotite, Calcite, Chert, Chlorite, Dolomite, Hematite, Micas, Muscovite or Illite, Pyrite, Quartz, Silica, Sulfides  
Amphibole, Calcite, Hornblade, Magnetite, Plagioclase, Wollastonite  

Compound Content
Ca, Fe, Mg, Silicon Dioxide, Sodium  
Aluminium Oxide, CaO, Iron(III) Oxide, FeO, Potassium Oxide, MgO, MnO, Sodium Oxide, Phosphorus Pentoxide, Silicon Dioxide, Titanium Dioxide  

Transformation
  
  

Metamorphism
No  
No  

Types of Metamorphism
-  
-  

Weathering
Yes  
Yes  

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

Erosion
Yes  
Yes  

Types of Erosion
Chemical Erosion, Coastal Erosion, Glacier Erosion  
Chemical Erosion, Water Erosion, Wind Erosion  

Properties

Physical Properties
  
  

Hardness
3  
6-7  

Grain Size
Very fine-grained  
Medium to Coarse Grained  

Fracture
-  
Irregular to Conchoidal  

Streak
White  
White to Grey  

Porosity
Highly Porous  
Less Porous  

Luster
Dull  
Vitreous to Dull  

Compressive Strength
95.00 N/mm2  
30
250.00 N/mm2  
5

Cleavage
Slaty  
-  

Toughness
2.6  
2.3  

Specific Gravity
2.2-2.8  
2.5  

Transparency
Opaque  
Opaque  

Density
2.4-2.8 g/cm3  
2.85-3.07 g/cm3  

Thermal Properties
  
  

Specific Heat Capacity
0.39 kJ/Kg K  
30
0.84 kJ/Kg K  
15

Resistance
Heat Resistant, Impact Resistant  
Heat Resistant, Pressure Resistant, Wear Resistant  

Reserves

Deposits in Eastern Continents
  
  

Asia
Bangladesh, China, India, Russia  
Russia, Turkey  

Africa
Ethiopia, Kenya, Morocco, South Africa, Tanzania  
Burundi, Djibouti, Eritrea, Ethiopia, Kenya, Madagascar, Rwanda, Somalia, South Africa, Sudan, Tanzania, Uganda  

Europe
Austria, France, Germany, Greece, Italy, Romania, Scotland, Spain, Switzerland  
Germany, Greece, Iceland, Norway, Poland  

Others
-  
-  

Deposits in Western Continents
  
  

North America
USA  
Canada, USA  

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

Deposits in Oceania Continent
  
  

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

Summary >>
<< Reserves

All about Shale and Hornblendite Properties

Know all about Shale and Hornblendite properties here. All properties of rocks are important as they define the type of rock and its application. Shale belongs to Sedimentary Rocks while Hornblendite belongs to Igneous Rocks.Texture of Shale is Clastic, Splintery whereas that of Hornblendite is Banded, Foliated, Massive. Shale appears Muddy and Hornblendite appears Foliated. The luster of Shale is dull while that of Hornblendite is vitreous to dull. Shale and Hornblendite are available in black, brown, buff, green, grey, red, yellow colors. The commercial uses of Shale are creating artwork, pottery and that of Hornblendite are cemetery markers, commemorative tablets, creating artwork.

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