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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. Because different soil-forming processes operate at different depths - soils typically develop into these distinct zones. These zones can be arranged vertically into a soil profile.
Caliche
Tephra
Soil Horizons
Dunes
2. Mineral crystal formation type; form by type of diffusion - the movement of atoms or ions through a solid to arrange into a new crystal structure; process takes place very slowly.
Solid-state diffusion
Paleopole
Caliche
Regression
3. The distance of the deepest well ever drilled - hole in northern Russia. Penetrates only about 0.03% of the Earth.
12km
Depositional environment
Relative plate velocity
Crystalline igneous rocks
4. 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.
Source rock composition
Granitic magma
Siliceous rocks
Crystal
5. 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.
12km
Zone of leaching
Mineral
Rock-forming silicate minerals
6. Molten rock that has flowed out onto Earth's surface.
O-horizon
Ripples
Lava
3.5km (2 miles)
7. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Cement
Earth's atmosphere
Silicate minerals
Caliche
8. Sedimentary rocks consisting of carbon-rich relicts of plants.
Bed
Organic sedimentary rocks
Crystal structure
Flood basalts
9. Chemical weathering during Which minerals dissolve into water.
Silicate minerals
Lower mantle
Deposition
Dissolution
10. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Partial melting
Asthenosphere
Bedding
Weathering
11. Refers to the chemical reactions that alter or destroy minerals when rock comes in contact with water solutions or air.
Regression
ravertine
Chemical weathering
Subduction
12. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
Lapilli
Facets
Lithosphere
Marine magnetic anomaly
13. Molten rock beneath Earth's surface.
Magma
Redbeds
Felsic
Cementation
14. A submarine suspension of sediment.
Evaporites
Cross beds
Stoping
Turbidity current
15. 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.
Outcrop
Rock layering
Organic sedimentary rocks
Special properties of minerals
16. Rock formations still attached to the Earth's crust.
Paleopole
Bedrock
Hardness
Metamorphic rocks
17. Type of lava flow; surface layer of the lava freezes and then breaks up due to the continued movement of lava underneath - becomes a jumble of sharp - angular fragments - yielding a rubbly flow.
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18. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Graded bed
Continental shelf
Cross beds
atmospheres (atm)
19. The Earth radiated heat into space and slowly cooled. Eventually - the early formed sea of lava solidified and formed igneous rock. The cumulative effect of radioactivity has been sufficient to slow the cooling of the planet and subsequently allow fo
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20. The absorption of water into the crystal structure of minerals - causes some minerals to expand.
Soil Horizons
Depositional environment
Hydration
Upper mantle
21. The intrusion of numerous plutons in a region - produces a vast composite body that may be several hundred kilometers long and over 100km wide; an immense body of igneous rock.
Metamorphic foliation
Stoping
Batholiths
Granitic composition
22. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Igneous rocks
Marine magnetic anomaly
Zone of accumulation
Rock-forming silicate minerals
23. The broad - relatively flat regions of the ocean that lie at a depth of about 4-5km below sea level.
Color
Tephra
Volatiles
Abyssal plains
24. Physical property of a mineral; different minerals fracture in different ways - depending on the internal arrangement of atoms. If a mineral breaks to form distinct planar surfaces that have a specific orientation in relation to the crystal structure
Fracture and cleavage
Mantle
Thermal expansion
Xenolith
25. Rocks that forms by the freezing of lava above ground - after it spills out (extrudes) onto the surface of the Earth and comes into contact with the atmosphere or ocean.
Laterite
Extrusive igneous rock
Marine magnetic anomaly
Transported soil
26. Magma type; contains only about 38% to 45% silica. Extreme form of mafic magma.
Ultramafic
Felsic - intermediate - mafic - ultramafic
Volatiles
Hardness
27. Similar to ripples - but are much larger. Small ripples often form on the surface of these structures.
Dunes
Granitic composition
Factors of magma cooling time
Basaltic lava flows
28. A plate boundary at which two plates move toward one another so that one plate sinks beneath the other. Subduction zones; Engage the sinking process known as subduction - between plates - consuming old oceanic lithosphere due to high density. Can sim
Chemical sedimentary rocks
Convergent plate boundary
Rhyolitic lava flows
Silicate minerals
29. The way in which the atoms are packed together within a mineral by chemical bonds. Five difference types of bonding can occur - covalent - ionic - metallic - Van der Waal's - and hydrogen.
Crystal structure
collision
Elemental composition of Earth
Divergent plate boundary
30. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Thermal expansion
Luster
Glass
Lava
31. A term used for all the physical - chemical - and biological processes that transform sediment into sedimentary rock and that alter characteristics of sedimentary rock one the rock has formed.
Rock-forming silicate minerals
Lava domes
Diagenesis
Basaltic lava flows
32. 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.
Turbidity current
Plutons
Rocks
Outcrop
33. The process by which sediment settles out of the transporting medium.
Tephra
Physical weathering
Crystal
Deposition
34. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Turbidite
Root wedging
Columnar jointing
Reason for Earth's internal heat
35. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Turbidite
Volatiles
Mineral
Hot-spot track
36. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Limestone
Volatiles
Basalt
Sedimentary structure
37. Breaks intact rocks into unconnected grains or chunks - collectively called debris or detritus. Grain size from largest to smallest: boulders - cobbles - pebbles - sand - silt - mud/clay.
Tuff
Xenolith
Physical weathering
Weathering
38. Times when the Earth's magnetic field flips from normal to reversed polarity - or vice versa. When the Earth has reversed polarity - the south magnetic pole lies near the north geographic pole - and the north magnetic pole lies near the south geograp
Outer core
Compaction
Magnetic reversals
Residual soil
39. A plate boundary at which one plate slips along the side of another plate. No new plate is formed and no old plate is consumed. But the grinding between the plates generates frequent and destructive earthquakes.
E-horizon
Transform plate boundary
Volcano
Sandstone
40. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
3.5km (2 miles)
Dolostone
Lava
Crystal structure
41. 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
Volatiles
Dipole
Metals
Partial melting
42. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Graded bed
Hardness
Native metals
Shield volcano
43. Deeper sublayer of the mantle - depth of 660km to 2900km.
Clastic
Lower mantle
The effect of gas pressure on eruptive style
Crust
44. Sedimentary rocks made up of minerals that precipitate directly from water solutions.
Heat transfer
Differential weathering
Volcanic blocks/bombs
Chemical sedimentary rocks
45. Sedimentary rock composed of clay.
Elemental composition of Earth
Lava tube
Turbidity current
Agrillaceous rocks
46. When silt and clay accumulate in the flat areas bordering a stream - lagoon - or delta - the silt when lithified becomes this type of sediment. And the mud - when lithified - becomes another type of sediment - also known as shale.
Siltstone and mudstone
Melts
Basalt
Volcano
47. The injection of magma within the magma chamber and conduit generates an outward pressure within the volcano. The presence of gas within the magma increases this pressure - as gas expands greatly as it rises toward the Earth's surface. Rhyolitic and
Elemental composition of Earth
Ridge-push force
Ripples
The effect of gas pressure on eruptive style
48. The four classes of igneous silicate rocks based on the proportion of silicon to iron and magnesium. As the proportion of silicon in a rock increases - the density decreases - thus felsic rocks are less dense than mafic. In order - from greatest to l
Felsic - intermediate - mafic - ultramafic
Fumerolic mineralization
Divergent plate boundary
Dike
49. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Bed
Sedimentary structure
Alloy
Phreatomagmatic eruptions
50. By melting - dissolving - or other chemical reactions.
Siliceous rocks
Hot spots
Sedimentary Basins
Mineral crystal destruction