Week 4 - Earth Materials Flashcards
Why are framework silicates stable?
Each silica is sharing its oxygen with another silica atom, making more bonds, the stronger structure is stable.
Made up of one silica (Si4+) and four oxygens (O)
Have a tetrahedral shape, meaning that they can polymerase.
Individual tetrahedra may be polymerized by sharing oxygen atoms between tetrahedra e.g.
rings, chains, sheets, frameworks
What binds minerals in igneous rocks together?
Silicate minerals are bound by tetrahedral structures
What is a felsic rock?
- felsic mineral (light colour, low density) e.g. feldspar, quartz
What is a mafic rock?
- mafic mineral (dark colour, high density) e.g. mica sheets, pyroxenes (single chains), Olivines (isolated tetrahedra)
What is the difference between contact and regional metamorphic processes?
Is the rock cycle a true cycle?
Why is it important ?
Yes
What are the rock forming minerals?
Silica (Si) Oxygen (O) Aluminium (Al) Iron (Fe) Calcium (Ca) Sodium (Na) Potassium (K) Magnesium (Mg)
List the 3 broad classes of rocks
- Igneous rocks - formed by solidification of magma - can be extrusive and intrusive
- Sedimentary rocks - aggregates deposited by transporting medium such as water, wind or ice; deposits of organic origin; chemical properties
- Metamorphic rocks - describe change in mineral assemblage and textures due to elevated temperatures and pressure
What are the implications for these Earth Materials on the landscape?
What are the differences between Minerals and Rocks?
Minerals - naturally occurring inorganic chemical compounds’ having a specific internal structure and regular chemical composition
Rocks - are natural mixture or aggregates of minerals
What is a Mineral?
- Mostly crystaline
- Have specific physical properties which reflect both their composition and atomic structure and affect rate of weathering
- silicates are the most common minerals (make up 95% of Earths crust)
Describe Silicates
Made up of one silica (Si4+) and four oxygens (O)
Have a tetrahedral shape, meaning that they can polymerase.
Individual tetrahedra may be polymerized by sharing oxygen atoms between tetrahedra e.g.
rings, chains, sheets, frameworks
What is an Igneous Rock?
What is it made up of?
- Igneous rocks - formed by solidification of magma, can be..
Extrusive (volcanic) - cool rapidly at Earth’s surface, fine crystal grain size
Intrusive (plutonic) - crystallise deep below the surface and cool slowly, coarse grain size - Mostly made of silicate minerals
- felsic mineral (light colour, low density) e.g. feldspar, quartz
- mafic mineral (dark colour, high density) e.g. mica sheets, pyroxenes (single chains), Olivines (isolated tetrahedra)
Intrusive Rock Structures
Structures when they solidify under the surface:
- Batholiths - largest
- Dykes - vertical structures, magma solidified in fractures
- Sills - horizontal sheets of solidified magma
What is the origin of magma?
Basalt Magma - generated from partial melting of ultramafic rocks in the asthenosphere
Granite Magma - generated from partial melting of rocks in lower crust