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Test your basic knowledge |
Geology
Start Test
Study First
Subject
:
science
Instructions:
Answer 50 questions in 15 minutes.
If you are not ready to take this test, you can
study here
.
Match each statement with the correct term.
Don't refresh. All questions and answers are randomly picked and ordered every time you load a test.
This is a study tool. The 3 wrong answers for each question are randomly chosen from answers to other questions. So, you might find at times the answers obvious, but you will see it re-enforces your understanding as you take the test each time.
1. The nature of Earth's magnetic field - like the familiar magnetic field around a bar magnet - has a North and South pole. The magnetic field is drawn with field lines - the paths along Which magnets would align - or charged particles would flow - if
Columnar jointing
Area of igneous activity
Biomineralization
Dipole
2. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Volatiles
Fissure eruptions/lava plateaus
Outer core
Frost wedging
3. A sediment-filled depression; in an area where the lithosphere has subsided.
Precipitation
Sedimentary Basins
Spreading rate
Explosive eruptions
4. When different rocks in an outcrop undergo weathering at different rates.
Frost wedging
Large Igneous Provinces (LIPs)
Differential weathering
Igneous rocks
5. A fine spray of lava instantly freezes to form fine particles of glass.
Fissure eruptions/lava plateaus
Root wedging
Mafic
Ash
6. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Biochemical sedimentary rocks
Mantle
Regression
Source rock composition
7. Sedimentary rocks made up of the shells of organisms.
Tuff
Sulfates
Biochemical sedimentary rocks
Loam
8. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
pahoehoe
Siltstone and mudstone
Special properties of minerals
Composite cone (stratovolcano)
9. Physical property of a mineral; a measure of a minerals relative ability to resist scratching - and therefore represents the resistance of bonds in the crystal structure being broken. The atoms or ions in crystals of a hard mineral are more strongly
Hardness
triple junction
Earth's atmosphere
Shield volcano
10. Blocks of rock that are solid and durable but composed of rough quartz sand grains cemented together.
Sandstone
Felsic - intermediate - mafic - ultramafic
Transgression
Basaltic composition
11. Core division; between 2900 and 5155km deep. Liquid iron alloy - it exists as a liquid because the temperature here is so high that even the great pressures squeezing the region cannot lock atoms into a solid framework. This liquid iron alloy is able
Redbeds
Regression
Bed
Outer core
12. Physical features of the land surface represented by changes in elevation.
Divergent plate boundary
Topography
Dipole
Granitic composition
13. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Alloy
Topography
Subduction
Convective flow
14. Distinguishing feature of magma; the process where magma sits in a magma chamber before completely solidifying - it may incorporate chemicals derived from the walls rocks of the chamber.
Assimilation
Explosive eruptions
Continental rift
Volatiles
15. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Biomineralization
Redbeds
Calderas
Sulfides
16. Most common mineral on Earth; compose over 95% of the continental crust. Consist of combinations of a fundamental building block called silicon-oxygen tetrahedron - different groups: independent tetrahedra - single chains - double chains - sheet sili
Quartz sandstone
Silicate minerals
Mid-ocean ridges
Subsidence
17. The force that subducting plates apply to oceanic lithosphere at a convergent boundary - arises simply because lithosphere formed 10 million years ago is denser than asthenosphere - so it can sink into the asthenosphere. Thus once an oceanic plate st
Slab-pull force
Carbonates
Sandstone
Soil Horizons
18. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Metamorphic rocks
Fissure eruptions/lava plateaus
Factors classifying clastic sedimentary rocks
Chemical sedimentary rocks
19. A sheet of tuff formed from a pyroclastic flow.
Ignimbrite
Solid-state diffusion
Pangaea
Paleopole
20. Rocks which develop when hot molten rock cools and freezes solid.
Igneous rocks
Lapilli
Sea-floor spreading
Crystalline igneous rocks
21. Develops because mid-ocean ridges lie at a higher elevation than the adjacent abyssal plains of the ocean. The surface of the sea floor overall slopes away from the ridge axis. Gravity causes the elevated lithosphere at the ridge axis to push on the
Arkose
Silicate minerals
Intermediate
Ridge-push force
22. Volcanic landform; pipes are short conduits that connect a magma chamber to the surface.
Five steps of clastic sedimentary rock formation
Volcanic pipes/necks
Volatiles
Extrusive igneous rock
23. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
Granitic composition
Sulfides
Turbidity current
triple junction
24. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
The effect of viscosity on eruptive style
12km
Phreatomagmatic eruptions
C-horizon
25. Some rock bodies appear to contain distinct formations - defined either by bands of different compositions or textures - or by the alignment of inequant grains so that they trend parallel to one another.
Rock layering
Upper mantle
Grain sizes
Hydrolysis
26. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Soil
ravertine
Paleomagnetism
27. Carbon-containing compounds that either occur in living organisms - or have characteristics that resemble the molecules within living organisms. Examples - oil - protein - plastic - fat - and rubber.
Alloy
Organic chemicals
Laccolith
Regolith
28. By melting - dissolving - or other chemical reactions.
Alloy
Mineral crystal destruction
Hydrosphere
Limestone
29. Mineral group; olivine group - pyroxene group - amphibole group.
Turbidite
Dark Silicates
Luster
E-horizon
30. The most important mineral group; comprise the most rock-forming minerals - they are very abundant due to large % of silicon and oxygen in Earth's crust. Examples - oxygen - silica - aluminum.
Superplumes
Paleomagnetism
Specific gravity
Rock-forming silicate minerals
31. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Ash
Marine magnetic anomaly
Area of igneous activity
Oxidation
32. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Polymorphs
Lithification
atmospheres (atm)
Compaction
33. A linear belt in which continental lithosphere pulls apart - the lithosphere stretches horizontally.
Continental rift
Dunes
Glass
Silicate minerals
34. The supercontinent; existence proposed by Wegener - suggested that the supercontinent later fragmented into separate continents that then drifted apart - moving slowly to their present positions.
Plutons
Dark Silicates
Pangaea
Differential weathering
35. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Bathymetry
Pyroclastic flows
Factors classifying clastic sedimentary rocks
Graded bed
36. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Oxides
Assimilation
Hot-spot track
Dunes
37. An insulated - tunnel-like conduit through which lava moves within a flow.
Tephra
Andesitic lava flows
Felsic
Lava tube
38. Aggregates of mineral crystals or grains - and masses of natural glass; a coherent - naturally occurring solid - consisting of an aggregate of minerals or a mass of glass.
Rocks
Biochemical sedimentary rocks
Laccolith
Dike
39. Sea-floor spreading proponents - Hess and others realized that in order for the circumference of the Earth to remain constant through time - ocean floor must eventually sink back into the mantle. This sinking process consumes the ocean floor between
Clastic sedimentary rocks
Symmetry
Coal
Subduction
40. The freely pivoting up and down compass needle's angle of tilt relative to the location upon the Earth's surface. At the equator - the specialized magnetic needle would position horizontally and at a magnetic pole it would point straight down.
Dissolution
triple junction
Magnetic inclination
Carbonates
41. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Regolith
Chemical sedimentary rocks
Sedimentary Basins
Mantle plume
42. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Andesitic lava flows
Continental drift evidence
Dolostone
Bed
43. Type of igneous rock composition; composed of dark silicates and calcium-rich feldspar - referred to as mafic (magnesium and iron). Make up the ocean floor/volcanic islands.
Pangaea
Stratagraphic formation
Relative plate velocity
Basaltic composition
44. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Halides
Metamorphic rocks
Ridge-push force
Xenolith
45. The boundary between two beds is a bedding plane; several beds constitute this structure.
Strata
Transgression
Fissure eruptions/lava plateaus
Lower mantle
46. Created from preexisting rocks which undergo changes - such as the growth of new minerals in response to pressure and heat - and/or as a result of squashing - stretching - or shear.
Lava domes
Zone of accumulation
Metamorphic rocks
Gem
47. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
Weathering
Physical weathering
ravertine
Chemical weathering
48. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Rock texture
Large Igneous Provinces (LIPs)
Gabbro
Relative plate velocity
49. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Residual soil
Sedimentary rocks
pahoehoe
Alloy
50. Sedimentary rock composed of calcite or dolomite.
Carbonate rocks
Assimilation
Crust
Jointing