Minerals - it is a naturally occurring inorganic element of compound having an orderly internal structure and characteristic chemical composition. Building blocks of rocks
Mineralogy - Is the study of minerals
Characteristics of Minerals:
Naturally-Occurring
Inorganic
Homogeneous Solid
Has definite chemical Composition
Crystalline Shape
Properties of Minerals:
Color
Streak
Hardness
Cleavage
Luster
Specific Gravity
Color - is caused by the absorption, or lack thereof, of visible light by their crystalline structure.
Luster - Refers to the quality of light on the surface of a rock, crystal, or mineral
Hardness - ability to resist scratching or abrasion
Cleavage - is the tendency of a mineral to split or cleave along the plane of weakness
Specific Gravity - is to measure of relative density of a mineral
Streak - is the color of powdered mineral produced hen it is dragged across an unweather surface.
Rocks - a natural-occurring aggregate or combination of minerals and mineraloid, such as fossils and glass. The natural building block of the earth's lithosphere
Petrology - is the scientific study of rocks
Igneous rocks - formed from hardening and crystallization of magma or molten material that originated deep within the earth
Two types of igneous rock:
Extrusive / Volcanic rock
Intrusive / Plutonic
Extrusive - forms when magma makes it way to earth's surface as lave and then cools.
Intrusive - it cools slowly beneath the earths surface and are created by magma.
Sedimentary Rocks - rocks that are accumulated on earth's surface in a process called deposition
3 types of sedimentary rocks:
Clastic
Chemical
Organic
Clastic - formed from the accumulation of clasts: little pieces of broken rocks and shells
Chimical - formed when dissolved minerals precipitate from a solution.
Organic - rocks formed from the accumulation of animal debris
Metamorphic rocks - forms from pre-existing rocks: methamorphic, igneous, sedimentary or other metamorphic rocks that have been altered by agents of metamorphism
Metamorphism - transformation of one rock type into another
two types of metamorphism:
Contact
Regional
Contact - the rock minerals and textures are changed mainly by head due to contact with magma
Regional - due to changes in pressure and temperature over large region of the crust. It may happen when rock is buried deep below the surface of the earth
Types of Metamorphic Rocks:
foliated
Non-foliated
Foliated - can be arranged in terms of increasing metamorphism, and it appeared layered or banded with compressed mineral grains.
Non foliated - usually made up of only few mineral
Geomorphic Processes - physical processes create and modify landforms on the surface of the earth
Exogenic process - also called gradational process, the comprise degradation and aggradation. a CONTINUUM of process
Exogenic process - are processes that take place at or near the earth's surface that makes the surface wear away
Types of Exogenic Process:
Weathering
Erosion
Mass Wasting
Weathering - is the general term applied to the combined action of all physical and chemical processes that disintegrate and decompose rocks near the earth's surface through the elements of weathering
Types of Weathering:
Physical
Chemical
Biotic
Physical Weathering - happens whenever rocks are broken up without any change in their chemical composition. Sometimes called as mechanical weathering
Examples of Physical Weathering:
Block disintegration
Exfoliation
Frost Action
Block disintegration - caused by successive heating and cooling that cause the expansion and contraction of rocks
Exfoliation - is the stripping of the outer layers of rocks due to intense heating
Chemical Weathering - is the weakening or disintegration of rocks and the formation of new compounds or new substances caused by chemical reaction