minerals
• Substance
which having the following five criteria is known as mineral.
- Solid
- Naturally occurring
- Inorganic
- Fixed chemical formula
- Specified atomic structure
Occurrence
of materials
• Minerals
occur as crystals i.e. bodies of geometric shapes which are bounded by faces
arranged in a regular manner and related to internal atomic structure.
• Crystal
Faces: smooth planar surfaces of definite geometrical shapes.
CRYSTAL
SYSTEMS
cube crystal |
In total we have six crystal
systems
- Cubic
- Hexagonal OR Trigonal
- Tetragonal
- Orthorhombic
- Monoclinic
6. 6, Triclinic
Crystal
system
Plane of symmetry
• Plane
of symmetry is a plane in which crystal is divided into equal halves and both
are the mirror image of each other.
PHYSICAL PROPERTIES OF MINERALS
• This
includes color, luster, hardness, cleavage, fracture, tenacity, habit, streak,
diaphaneity, magnetic property, specific gravity.
• Except
this some minerals have their own property which is named as special property.
For example, sulphur having property of odor or a pungent smell, magnetite
having special property of magnetism, etc.
• COLOR:
some minerals have distinctive color like sulphur have yellow color.sometimes traces of other minerals changes the appearance color of specific minerals. So it is identify a pure mineral we have to conduct streak test. Streak gives the powder of mineral which is mostly pure and shows the true color of mineral.
some minerals have distinctive color like sulphur have yellow color.sometimes traces of other minerals changes the appearance color of specific minerals. So it is identify a pure mineral we have to conduct streak test. Streak gives the powder of mineral which is mostly pure and shows the true color of mineral.
• Luster:
It is the appearance of mineral surface in reflected light it may be metallic or dull.
It is the appearance of mineral surface in reflected light it may be metallic or dull.
• Hardness:
It is basically strength or resistance against abrasion. For finding out the hardness
It is basically strength or resistance against abrasion. For finding out the hardness
we have two methods one is direct method and other one is indirect
method.
Hardness
scales
• Finger
nail - 2.5
• Copper
coin – 3.5
• Iron
nail- 4.5
• Sharp
glass- 5.5
• Streak
plate – 6.5
•
CLEAVAGE: Some minerals have tendency to split along
some regular planes. These smooth plane surfaces are known as cleavage planes.
•
Fracture: the nature of broken surface of mineral is
known as fracture. The break become irregular and independent of cleavage.
The fracture may be
conchoidal (curved), Even (nearly flat), uneven (rough) and hackly (small sharp
irregularities)
.
• TENACITY: The response of mineral of hammer blow, to cutting with a knife and to bending is
described by its tenacity. The minerals whose shape can change under the above
said actions are known as MALLEABLE, otherwise most minerals are brittle.
HABIT: Natural shape of mineral. It may be
crystalline, cryptocrystalline and amorphous
•
DIAPHANEITY: The ability of passing light or the
transparency of the mineral is technically known as Diaphaneity. MINERAL may be
transparent, translucent or opaque.
SPECIAL PROPERTIES
•
MAGNETISM: attracted to a magnet contains iron,
nickel, cobalt or magnetite.
•
DOUBLE
REFRACTION: Can see
doubling of things but it is so weak in most of the minerals.
E.g Iceland spar variety of calcite
•
FLOURESCENCE: glows under ultraviolet light.
e.g: autunite mineral
•
Phosphorescence: continues to glow after the removal of UV light.
E.g: Celestine
•
Piezoelectric Electricity : generated
from some mechanical stress or pressure.
E.g quartz, topaz etc.
structure geology
The study of deformation of rock within the earth's geosphere is called structure geology. (deals with the study of the forces that bring
about the deformation).
Faults
Faults doesnot always bend sometime its
break. When rocks move and breaks is called faults
Types of faults
•
Reverse
fault
•
Normal
fault
•
Thrust
fault
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