Use LEFT and RIGHT arrow keys to navigate between flashcards;
Use UP and DOWN arrow keys to flip the card;
H to show hint;
A reads text to speech;
53 Cards in this Set
- Front
- Back
What is a mineral? (6 characteristics)
|
Naturally occurring
Solid Formed by geologic processes Definable chemical composition Orderly arrangement of atoms Inorganic |
|
What is a polymorph?
|
Two different minerals that have the same composition but different crystal structure.
|
|
5 Ways that Crystals can form
|
Solidification of a melt
precipitation from a solution Solid-state diffusion Biomineralization from a vapor |
|
What is a geode?
|
A mineral-lined cavity in a rock
|
|
Euhedral crystl
|
Well-formed crystal faces
|
|
Anhedral
|
Do not have well-formed crystal faces
|
|
How can you tell one mineral from another?
|
Color, streak, luster, hardness, specific gravity, crystal habit, cleavage, fracture, special properties
|
|
Streak
|
the color of a powder produced by scraping the mineral
|
|
Luster
|
the way a mineral surface scatters light (metallic vs nonmetallic, silky, satiny, resinous, pearly, earthy)
|
|
Hardness
|
the measure of the relative ability of a mineral to resist scratching
|
|
Specific gravity
|
Density of a mineral
|
|
Crystal habit
|
The shape of a single crystal with well-formed crystal faces
|
|
Fracture
|
Some minerals lack planes of weakness
Due to equal molecular bonds in all directions These minerals fracture and hence don't have cleavage |
|
Cleavage
|
Tendency to break along planes of weakness
Cleavage produces flat surfaces Described by number of planes and their angles 1, 2, 3, 4, and 6 cleavage planes possible |
|
Calcite dilutes with...
|
dilute hydrochloric acid
|
|
Conchoidal fracture
|
smoothly curving, clamshell-shaped surfaces. typically form in quartz
|
|
Mineral classes (most important)
|
Silicates
|
|
Silicates
|
Earth's crust is silicone-oxygen tetrahedron
|
|
Silicate minerals compose over...what percent of the continental crust
|
95%
|
|
Theory of Plate Tectonics
|
The outer layer of the earth (the lithosphere) consists of separate pieces or plates, that move with respect to each other.
|
|
Lithosphere
|
consists of crust plus the uppermost (coolest) part of the upper mantle
|
|
Asthenosphere
|
the lithosphere floats on this relatively soft or "plastic" layer which can undergo convection
|
|
Does the continental lithosphere lie at a higher or lower elevation than that of the oceanic lithosphere?
|
Higher.
|
|
Thick crust, low-density
|
Continental lithosphere
|
|
Thin crust, dense rock
|
Oceanic lithosphere
|
|
Pieces of the lithosphere
|
plates
|
|
Breaks in these
|
Plate boundaries
|
|
How many major plates?
|
12
|
|
Active margin
|
Plate boundaries
|
|
rate at which plate movement occurs
|
1 to 15 cm per year
|
|
because of plate tectonics
|
the Earth's surface constantly changes
|
|
divergent boundary
|
a boundary at which two plates move apart from one another
|
|
convergent boundary
|
a boundary at which two plates move toward one another so that one plate sinks beneath the other
|
|
where does sea-floor spreading occur
|
mid-ocean ridge
|
|
what else is a divergent boundary called?
|
mid-ocean ridge or just a ridge
|
|
ocean crust forms layers of what blobs?
|
basalt blobs aka pillow basalt
|
|
true or false, the lithospheric mantle and oceanic lithosphere grow progressively thicker away from the ridge
|
true
|
|
subduction
|
sinking process, convergent boundaries known as subduction zones
|
|
margins also called...?
|
trenches
|
|
amount of oceanic plate consumption world wide equals what?
|
amount of sea-floor spreading worldwide so the surface area of the Earth remains constant throughout time
|
|
at what rate does oceanic lithosphere sink?
|
less than 10 to 15 cm per year
|
|
what happens to the downgoing plate at convergent boundaries?
|
it grinds along the base of the overriding plate which generates large earthquake
|
|
the belt of earthquakes in a downgoing plate is called what?
|
Wadati-Benioff zone
|
|
a chain of volcanoes known as a what develops behind the accretionary prism
|
volcanic arc
|
|
Transform fault
|
the actively slipping segment of a fracture zone between two ridge segments
|
|
what happens at a transform boundary?
|
one plate slides sideways past another but no new plates are formed and no old one is consumed
|
|
what is a triple junction
|
where three plate boundaries intersect at a point
|
|
hot spots
|
volcanoes that exist as isolate points and appear to be independent of movement at a plate boundary
|
|
what is rifting
|
when most new divergent boundaries form when a continent splits and separates into two continents
|
|
What is collision?
|
A convergent boundary ceases to exist when a piece of buoyant lithosphere such as a continent or an island arc moves into the subduction zone.
|
|
Ridge-push force
|
develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean
|
|
Slap-pull force
|
the force that subducting plates (also called downgoing slabs) apply to oceanic lithosphere at a convergent margin arises simply because lithosphere that was formed more than 10 million years ago is denser than the asthenosphere so it can sink into the asthenosphere
|
|
Why does sea-floor spreading occur?
|
in response to the ridge-pull force. subducting lithosphere generates a slap-pull force that tows the rest of the plate along with it.
|