Rock Cycle Notes
Rock Cycle
Weathering and Erosion
Weathering and erosion break down rocks into smaller particles.
Different particle sizes include gravel, sand, silt, and clay.
Transportation and sedimentation are important processes.
Fast flow transports sand.
Medium flow transports silt.
Slow flow transports clay.
Sediments and Sedimentation
Sediments are particles of rock fragments.
Sedimentation is the process where sediments are deposited.
Over time, sediments compact into layers through lithification, which transforms them into sedimentary rocks.
Examples of sedimentary rocks: limestone, sandstone, and claystone.
Weathering and Erosion Examples
The brown color of water from the Ethiopian Plateau is due to weathering and erosion.
Agricultural soil in Egypt was formed over millions of years by the same processes.
Rainfall on the Ethiopian Plateau causes weathering and erosion; rock fragments are transported away.
Properties of Sedimentary Rocks
Sedimentary rocks are porous due to spaces between sediment particles.
Contain fossils.
Importance and Harms of Erosion
Erosion is important for the formation of river deltas.
Erosion can harm coastlines (coastal erosion) due to sea waves.
Metamorphic Rocks
Formation occurs under heat and pressure beneath the Earth's surface.
Particles come closer together.
Spaces between particles decrease.
Hardness increases.
Examples of Metamorphism
Limestone transforms into marble.
Sandstone transforms into quartzite.
Igneous Rocks
Formed from magma.
Formation of Igneous Rocks
Magma cools, forming plutonic igneous rocks.
Lava cools, forming surface igneous rocks.
Types of Igneous Rocks
Plutonic rocks:
Formed from magma.
Cool slowly, resulting in large crystals.
Surface volcanic rocks:
Formed from lava.
Cool quickly, resulting in small crystals.
Examples: Gabbro, Granite, Pumice, Basalt.
Examples of Rock Uses
Marble used in the Taj Mahal in India.
Limestone used in the Pyramids of Giza in Egypt.
Rock Cycle
Magma: Melting.
Igneous rocks: Cooling, and weathering and erosion.
Sediments: Compaction and lithification, and weathering and erosion.
Sedimentary rocks: Heat and pressure, and weathering and erosion.
Metamorphic rocks: Heat and pressure.
Formation of Fossil Fuels
Formed millions of years ago from physical and chemical changes of organic substances in the Earth's interior.
Plants (especially large ones) are the organic origin of coal.
Marine microorganisms are the organic origin of petroleum oil and natural gas.
Methane gas is the major component of natural gas (forms more than 90%).