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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 rate of increase in temperature - decreases with increasing depth. The dashed lines represent the solidus and liquidus for mantle rock (peridotite). The solidus line defines the conditions of pressure and temperature at Which mantle rock begins t
Geothermal gradient
Rocks
Laccolith
Sill
2. Physical property of a mineral; represents the density of a mineral - as specified by the ratio between the weight of a volume of the mineral and the weight of an equal volume of water a 4 degrees C.
Specific gravity
Rock composition
Organic chemicals
Convective flow
3. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Fracture and cleavage
Dissolution
Gem
Abyssal plains
4. Theory confirmed by 1968 - geologists had developed the complete model of continental drift - sea-floor spreading - and subduction. Within this model - Earth's lithosphere consists of about 20 distinct pieces - or plates - that move relative to each
Evaporites
Salt wedging
Plate tectonics
Native metals
5. Rocks which develop when hot molten rock cools and freezes solid.
Plates
Igneous rocks
Stoping
Continental rift
6. 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.
Gabbro
Sedimentary Basins
Conglomerate
Basaltic composition
7. 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.
Organic chemicals
Soil erosion
Mineral
Conglomerate
8. The shape of the sea floor surface. Investigation of the sea-floor revealed the presence of several important features: mid-ocean ridges - deep-ocean trenches - seamount chains - and fracture zones.
Differential weathering
Bathymetry
Deep-ocean trenches
Oxides
9. 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.
Crystal habit
Intermediate
Sedimentary structure
Rock-forming silicate minerals
10. 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
Sedimentary Basins
Slab-pull force
Felsic - intermediate - mafic - ultramafic
Pyroclastic flows
11. 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
Hydrosphere
Continental rift
Ridge-push force
atmospheres (atm)
12. The display of the pattern of atoms or ions within a mineral. Meaning that the shape of one part of a mineral is a mirror image of the shape of another part.
Factors classifying clastic sedimentary rocks
Sedimentary rocks
Transition zone
Symmetry
13. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Pyroclastic debris
Gabbro
Native metals
Bed
14. Lava flowing on dry land cools more slowly that lava erupting underwater.
Cement
The effect of the environment on eruptive style
The core
Oxides
15. A sediment-filled depression; in an area where the lithosphere has subsided.
Spreading rate
Differential weathering
Redbeds
Sedimentary Basins
16. The resistance to flow of magma. Reflects its distinct silica content - for silica tends to polymerize - meaning it links up to form long - chainlike molecules whose presence slows down the flowing ability of magma. Thus felsic magmas flow less easil
Viscosity
Metals
Symmetry
Rhyolitic lava flows
17. 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.
Subduction
Partial melting
Weathering
Rock layering
18. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Regolith
The effect of viscosity on eruptive style
Convergent plate boundary
Rock layering
19. The removal of soil by running water or by wind.
Basaltic composition
Redbeds
The effect of gas pressure on eruptive style
Soil erosion
20. Rocks with a fragmental texture consist of igneous fragments that are packed together - welded together - or cemented together after having solidified. Examples - pyroclastic rocks such as tuff or breccia.
Saprolite
Fragmental igneous rocks
Pyroclastic flows
Basaltic composition
21. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Regolith
Magnetic declination
Thermal expansion
Residual soil
22. Distinguishing feature of magma; the composition of the melt reflects the composition of the solid from which it was derived. Not all magmas form from the same source rock - therefore not all magmas have the same compositions.
O-horizon
Crystal lattice
Lithification
Source rock composition
23. Fluid basaltic lava extruded from crustal fractures called fissures.
Gabbro
Organic sedimentary rocks
Fissure eruptions/lava plateaus
Crystalline igneous rocks
24. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Dark Silicates
Rhyolitic lava flows
Compaction
Plate tectonics
25. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Carbonates
Calderas
Lapilli
Chert
26. Deeper sublayer of the mantle - depth of 660km to 2900km.
Plates
Transition zone
Lower mantle
Composite cone (stratovolcano)
27. The crust moves away from the Mid-Atlantic Ridge axis at a rate of 1cm per year. This velocity of sea-floor spreading is determined by the relationship between the paleomagnetic anomaly-stripe's width and the reverse polarity duration - the data reve
Spreading rate
Marine magnetic anomaly
Solid-state diffusion
The effect of gas pressure on eruptive style
28. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
ravertine
C-horizon
Tuff
Glass
29. Center of the Earth - consists mainly of iron alloy.
The core
Igneous rocks
Dark Silicates
Specific gravity
30. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Lithosphere
Transition zone
Biochemical sedimentary rocks
Pyroclastic flows
31. A sedimentary bed that has developed a reddish color. The red comes from a film of iron oxide (hematite) that forms on grain surfaces.
Conglomerate
Dunes
Hydrosphere
Redbeds
32. Sedimentary rocks consisting of carbon-rich relicts of plants.
Stoping
Convergent plate boundary
Organic sedimentary rocks
Cement
33. The base of the soil profile; consists of material derived from the substrate that's been chemically weathered and broken apart - but has not yet undergone leaching or accumulation.
Saprolite
Mineral crystal destruction
Paleomagnetism
C-horizon
34. Mineral crystal formation type; from directly from a vapor - occurs around volcanic vents or around geysers. At such locations - volcanic gases or steam enter the atmosphere and cool - so certain elements cannot remain in gaseous form.
Fumerolic mineralization
3.5km (2 miles)
The effect of gas pressure on eruptive style
Soil Horizons
35. Lava flow; associated with felsic magma - consists of ash and pumice fragments - material is propelled from the vent at a high speed.
Gem
Stratagraphic formation
Pyroclastic flows
Polymorphs
36. Molten rock that has flowed out onto Earth's surface.
Lava
Biomineralization
Residual soil
Conchoidal fractures
37. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Hydration
Topography
Effusive eruptions
Intrusive igneous rock
38. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Clastic
Factors classifying clastic sedimentary rocks
Gabbro
Continental rift
39. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Cinder cone
Flood basalts
Factors of magma cooling time
Oxidation
40. 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
Lava domes
E-horizon
Silicate minerals
Cinder cone
41. Magma viscosity depends upon temperature - volatile content - and silica content. Hotter magma - more volatiles - and mafic magma all have less viscosity.
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42. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Volatiles
Stratagraphic formation
Effusive eruptions
Outcrop
43. 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
Apparent polar-wander path
Mid-ocean ridges
Hardness
Evaporites
44. Some rocks develop their magnetization - their ability to produce a magnetic field - at the time that the rocks themselves formed. Such rocks - preserve a record of the Earth's magnetic field at known times in the past.
Conchoidal fractures
Five steps of clastic sedimentary rock formation
rifting
Paleomagnetism
45. Type of soil; forms in tropical regions where abundant rainfall drenches the land during the rainy season - and the soil dries during the dry season.
Crust
Laterite
12km
Transition zone
46. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Hot-spot track
Strata
Rock-forming silicate minerals
Crystalline igneous rocks
47. A plate boundary at which two plates move apart from one another by process of sea-floor spreading. Mid-ocean ridges or simply a ridge. New crust is formed at ridges through the buoyant rising of magma from beneath the surface and solidifies to creat
Divergent plate boundary
Graded bed
Andesitic lava flows
Fragmental igneous rocks
48. Process occurring after sediment has been compacted - can then be bounded together to make coherent sedimentary rock. Binding material consists of minerals (commonly quartz or calcite).
Sandstone
Cementation
Batholiths
Gem
49. Process where a convergent boundary ceases to exist when a piece of buoyant lithosphere - such as a continent or island arc - moves into the subduction zone. Yield some of the most spectacular mountains/mountain ranges on the planet including the Him
Factors classifying clastic sedimentary rocks
collision
Alloy
Area of igneous activity
50. Volcanic landform; steep walled depression at the summit - size exceeds one kilometer in diameter.
Slab-pull force
Ridge-push force
Calderas
Pyroclastic flows