bonding, minerals and rocks Flashcards
what are crystals?
homogeneous solid formed by 3D pattern of atoms, ions and molecules. form most of solid earth.
what are molecules?
group of 2 or more atoms of the same or different elements held together by chemical bonds. electrically neutral.
what are minerals?
elements or chemical compounds that are normally crystalline and that has been formed as a result of geological processes.
what does atmophile mean
volatile forms gases mainly in the atmosphere
what does lithophile mean
silicates, oxides, rock forming. dominates crust and mantle
what does chalcophile mean?
affinity for a sulfide liquid phase
what does siderophile mean?
affinity for metallic liquid phase
what is a mineral to a geologist?
homogenous naturally occurring solid substance with definable chemical composition and an internal structure of arranged atoms. they have a crystla lattice.
what are polymorphs?
graphite and diamond have the same composition, but different crystal structures. this is a polymorph.
how do we see inside crystals?
optical microscopy. x ray show individual atoms.
how can you distinguish a mineral?
colour, streak, luster, hardness, specific gravity, crystal habit, fracture and cleavage.
what is luster?
refers to the way the mineral surface scatters light
why are silicate rocks important?
dominate crust in the mantle. mode of oxygen and solicon with other atoms. the ratio with these are important. 95% of the continental crust is made of silicate minerals.
where do diamonds come from?
carbon travels to the mantle by subduction. diamonds can only form in the amntle around 150 km down, due to the extreme temperatures, pressure and conditions.caron containing rocks travel to the mantle when convergent plate boundaries collide, the diamond becomes trapped in the lithosphere mantle beneath continents. the magma rises when rifting occurs, bringing the diamonds with it, in something called kimberlite, and crushing kimberlite to get to it.
why has the continental crust composed differently?
due to the size of the ions and the way elements are packed into mineral lattices.