EXAM ONE Flashcards
Mantle
Ultramafic rock composition, Oxygen, Magnesium, and Silicon
Lithosphere
the rigid outer part of the earth, consisting of the crust and upper mantle.
Seismic Waves
When a material breaks due to stress, energy is released in waves that travels through the material
Tranform plate boundary
Plates that slide past each other without creating or destroying crust (Lithosphere)
This leads to earthquakes of connects other types of plate boundaries
Physical properties of minerals
Streak = color of a powdered mineral
Luster = the appearance of light reflected off of the mineral
Hardness = resistance to abrasion
Specific gravity = dimensionless measure of density calculated by ratio of density of mineral to that of water
Cleavage: geometrical shape when cut
Crystal Habit = shape (geometric or otherwise) of a mineral crystal or aggregate of minerals
Cleavage
breaking along a particular geometric plane
7 major groups of non-silicate minerals and the type of anion in each
- Native Elements-gold, copper
- Carbonates- calcite, dolomite:
Building stone, cement production, acid neutralizers - Sulfates- gypsum, Anhydrite:
Used to make plaster and drywall - Sulfides
- Halites
- Oxides
- Phosphates- Apatite:
Found in the skeletons of all vertebrate organisms. Phosphate rock is used to produce all synthetic fertilizers
Felsic material
Lower density
Rocks with the most silica are called…
Felsic
Rocks with a medium amount of silica are called…
Intermediate
Rocks with 45-55% silica are called…
Mafic
Rocks with the least amount of silica are called…
Ultramafic
Mafic material
Higher density
Intrusive Igneous Rocks
Rocks that are created deep in the Earth
Extrusive Igneous Rocks
Small rocks that are created from exploding volcanoes, and cooled very fast
Intrusive Rocks
Bigger in size (slow cooling)
Extrusive Rocks
Smaller in size (fast cooling)
The main layers of the Earth in correct order, from the surface moving down, are:
crust, mantle, outer core, inner core