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INTEGRATED SCIENCE
Posted by Chester Morton / Wednesday, 12 June 2019 / No comments
The effects of the agents of weathering on rocks
ROCKS
Definition
These are
naturally occurring solid aggregate of one or more minerals. There are three
types of rocks.
Igneous
Rocks
These are rocks formed from molten lava(eruptions from volcanoes) when
it cools down and solidifies. They contain primary minerals like quartz,
feldspar, etc. Examples of igneous rocks are granite, quartz, gabbro, and
diorite.
Sedimentary
rocks
These are rocks formed from settling or sticking together of broken down
particles of other rocks. Examples of sedimentary rocks include shale,
sandstone, dolomite, and limestone.
Metamorphic
rocks
These are rocks formed by subjecting any type of rock either igneous
rocks or sedimentary rocks to different temperature and pressure conditions
than those in which the original rocks were formed. Examples of this include
marble, sandstone, schist, etc.
WEATHERING
OF ROCKS
This
refers to the gradual process that disintegrates, decomposes or crumbles rock
into smaller rock particles by agents such as water, changes in temperature,
pressure, chemicals, atmospheric oxygen, wind and roots of plants.
EFFECTS
OF AGENTS OF WEATHERING
PHYSICAL
AGENTS
This refers to the mechanical breakdown of rocks into smaller
particles. In physical weathering, there is no change in the chemical
composition of the rock. Examples of physicals include; effects of temperature,
wind, water, moving ice and pressure.
Temperature
This
refers to the degree of hotness or coldness of a place.
In hotter
regions when the temperatures are high, rocks expand when heated and contract
when cooled. The uneven expansion and contraction of rock minerals cause
cracking and disintegration of rocks into smaller
particles
In colder
regions when the temperature falls below freezing point, water in the crevices
of rocks solidifies and expands in the process, causing the rocks to crack
under stress.
CHEMICAL
AGENTS
This
refers to the breakdown of rocks into smaller particles as a result of various
chemical processes. Some of the agents include:
Carbonation
This refers to the reaction of carbonic acid with rocks to break it down
Hydrolysis
This refers to the chemical reaction between a substance and water which leads
to the breakdown of the bond between hydrogen and oxygen in water.
Hydration
This refers to the process by which water becomes attached to the surface of a
substance
Reduction
This simply refers to the addition of hydrogen or removal of oxygen from a
substance.
Oxidation
This means the addition of oxygen or removal of hydrogen
BIOLOGICAL
AGENTS
This
refers to the breakdown of rocks into smaller particles by activities of living
things. Agents involved in biological weathering of rocks include the following:
a. The
pressure influenced by animals such as elephant
b. The
passage of the roots of plants through cracks in rocks
c. The
boring activities of organisms such as earthworms.
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INTEGRATED SCIENCE
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