Minerals Ch. 5

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Created by:

rth004  on February 15, 2011

Subjects:

geology 101

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Minerals Ch. 5

How many minerals are known?
4000
1/21
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How many minerals are known? 4000
What are crystals? rare minerals displaying flat external faces. (form best in open cavities)
Crystalline structure are based on what? atomic patterns
The Crystalline Structure is.. repeated arrangement of atoms bonding with one another
What are 5 recognized types of bonds? covalent, ionic, metallic, van der waals, hydrogen
What does the nucleus consist of? protons (+) and neutrons (no charge)
What are electrons? Negatively charged particles that surround the nucleus.
Located in discrete energy levels called shells.
Ionic Bonding - Atoms gain or lose outermost electrons to form ions
- Ionic compounds- orderly arrangement of oppositely charged ions
Covalent Bonding - Atoms share electrons to achieve electrical neutrality
- Generally stronger than ionic bonds
- Both ionic and covalent bonds typically occur in the same compound
What happens in metallic bonding? outermost electrons are free to migrate among atoms
What are polymorphs? Minerals with same composition but different crystalline structures.
Poly=many, morph=form
98.5% of crustal mineral mass is from what 8 elements? Oxygen (46.6%), Silicon (27.7%), Aluminum (8.1%), Iron (5.0%), Calcium (3.6%), Sodium (2.8%), Potassium (2.6%), Magnesium (2.1%)
What is the most important mineral group? Silicates
Facts about Silicates - most rock-forming minerals
- abundant due to large % of silicon and oxygen in earth's crust
- acts as an atom (molecule) in atomic bonding
What do dark silicates consist of? Fe, Mg silicates
What do light silicates consist of? Ca, Na, K, Al silicates
What are some physical properties of minerals? crystal form, luster, color (streak), hardness, cleavage (fracture), specific gravity (density)
what does luster mean? how mineral reflects light
What is generally unreliable for mineral identification? color
what does streak mean? the color of powdered mineral
what is cleavage? the way a mineral "breaks" into smaller bits of characteristic shape.

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