Due to weathering and erosion, the Sedimentary, MetamorphicIgneous Rocks are turning into sediment.
Due to heat and pressure, the Sedimentary and Igneous Rocks are turning into Metamorphic Rocks.
Due to compaction and cementation, the sediment turns into Sedimentary Rocks.
Due to melting through the atmosphere, the Igneous and Metamorphic Rocks turn into magma.
Due to cooling, the magma forms back into Igneous Rocks.
What is the Weathering process?
> breaking down or dissolving of rocks and minerals on Earth's surface.
What are the factors that can affect the Weathering process?
> temperature and climate
> Moisture or water
> Type ofrocks
MechanicalWeathering - breaking or disintegration of rocks into smaller pieces without changing their composition.
CAUSES:
* Ice wedging
* pressure release
* plant growth
* abrasion
Biological Weathering - It is contributed to or removal of ions and minerals from the weathering environment and physical variations due to movement or development of organisms.
CAUSES: plants, animals, fungi, bacteria.
Soil - surface material that covers most land. It contains mineral particles, organic matter, water, and air.
Composition of Soil:
Water - 25%
Air - 25%
Mineral - 45%
Organic Matter - 5%
WHAT ARE THE SOIL PROPERTIES?
Texture - size of particles; proportion of its composition (sand, silt, clay & loam)
IMPORTANCE:
* aeration
* water drainage/retention
* useful in agriculture.
Structure - arrangement of its composition; influence by the presence of organic matter & other organisms.
IMPORTANCE:
* aeration
* water movement
* useful for plant growth.
Porosity - This is the amount of pore space between soil particles.
Chemistry - chemical composition, properties & reaction of soils.
IMPORTANCE: nutrientsabsorption.
Color - indicates the presence or amount of organic matter and iron.
IMPORTANCE: water drainage.
Profile - shows the different layers/section/horizon.
IMPORTANCE: nutrients content/quality.
HORIZONS IN SOIL PROFILE:
O (Organic) - rich in humus
A (Surface) - known as topsoil
B (subsoil) - rich in minerals
C (Substratum) - partially weathered rocks
R (Bedrock) - mass of rock.
Chemical weathering is a process where rocks and other materials are broken down by chemical reactions, primarily through the interaction with water and dissolved chemicals.