Earth Science Term 1 Exam Flashcards
Structure of the Earth:
Describe the Earth’s internal differentiation into layers
These processes took place during the early stages of earths formation about 4.5 billion years ago
This was formed by melting would have caused denser substance to sink towards the cent while less dense material would have migrated to the crust. Forming earth layers.
This was led to formation of a core, a curst and eventually continents
Evaluate how seismic waves and meteorites provide evidence for this structure
Seismic waves behave as they move through different materials enable us to know about the layers that make up earth.
Their paths are curved as the waves refract due to the gradually changing density of the layers.
Seismic waves tell us that the Earth’s interior consists of a series of concentric shells, with a thin outer crust, a mantle, a liquid outer core, and a solid inner core
Scientist can calculate the composition of rocks of the earth by studding the materials found in meteorite.
Energy and the Earth’s core
Earth has two energy sources:
Solar Energy: Reaching the earth from the sun
Solar energy: Reaches the earth in a form of radiant energy and is made up of 99.87% of energy received by the earth
Internal- Reaching the surface of the earth the earth itself
Earths inner core is the innermost layer of plant earth
Is a solid ball with a radius about 1,220 km
Earth’s core is usually made of Iron
Decay of radioisotopes
Radioactive decay is happening in all rocks.
It’s a part of earths natural system
Is caused by heat inside the earth
Driving forces such as tectonic system which leads to volcanoes, earthquakes and plate tectonics
The Rock Cycle
Igneous rocks are formed from melted rocks deep inside the earth
Example: Obsidian
Sedimentary rocks are formed from layers of sand. Silt, dead plants, and animal skeletons
Examples: Sandstone
Metamorphic rocks are formed from heat and pressure underground formed for other rocks
Example:
Marble
Effect of melting and crystallisation, weathering and erosion, heat and pressure and compaction and cementation
Effect on melting and crystallisation, weathering and erosion, heat and pressure and compaction and cementation are factors that influence the formation of rock types. Theres factors affect and change the rock types using the rock cycle.
Example: Weathering and erosion from Metamorphic rock will turn it into sediments which compaction and cementation turns it into sedimentary rocks.
Intrusive and extrusive igneous rocks
There are two main types of igneous rocks, and they are extrusive and intrusive
Extrusive rocks are formed on the surface of the Earth from Lava, then is when magma that has emerged from underground.
Intrusive Rocks are formed magma that cools and solidifies within the curst of the planet
So basically Extrusive is magma cooling on the surface of earth while Intrusive is inside of earths that cools and solidifies with the crust.
Mafic and felsic rocks and their mineral composition
Mafic: Enriched d in iron, magnesium, and calcium and typically dark in colour
Mafic has less silica giving it darker colour
Felsic: Typically light in colour, enriched in aluminium, sodium, silicon and potassium.
Felsic has a high amount of silica giving whiter colour
Three types of volcanoes
- Cinder Cone Volcanoes.
- Composite Volcanoes
- Shield Volcanoes.
Effect of silica on lava viscosity
Magma that have high silica content will emphasis greater degrees of polymerization and have higher viscosities than those with lows levels of silica content.
Three types of plate boundaries
- Divergent boundaries -where new crust is generated as the plates pull away from each other.
- Convergent boundaries -where crust is destroyed as one plate dives under another.
- Transform boundaries –where crust is neither produced nor destroyed as the plates slide horizontally past each other.
Magnetic anomalies
Earths Magnetic field results from variations in the chemistry or magnetism of the rocks. Mapping over an area is valuable in detecting structures.
A marine magnetic anomaly is a variation in strength of Earth’s magnetic field caused by magnetism in rocks of the ocean floor
Examine how the transformations of kinetic, gravitational and thermal energy create movement of tectonic plates
Heat energy stored and generated in Earths interior creates convection currents on a massive scale that results in the movement of sections of the Plates.
Tremendous heat and pressure within the earth cause the hot magma to flow in convection currents. These currents cause the movement of the tectonic plates that make up the earth’s crust.
Principles of stratigraphy
- Lateral continuity.
- Original horizontality.
- Faunal succession.
- Cross-cutting relations.
- Superposition.
Stratigraphy is the study of rock layers
Their sequence and their relationship with each other
Provides to interpret geologic events
Deduce age relationships
Stratigraphy can find geological age using the study of rock layers and their relationship with each other. The rock layers usually determine their geological age by their layers.