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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. 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
Dunes
Paleomagnetism
Sandstone
2. Soil section below the A-horizon; a soil level that has undergone substantial leaching but has not yet mixed with organic material. Because it lacks organic materials - this horizon tends to be lighter than the A-horizon. Part of the zone of leaching
Chemical weathering
Five steps of clastic sedimentary rock formation
E-horizon
Basaltic composition
3. 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.
Transported soil
Transform plate boundary
Mantle
Sandstone
4. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Native metals
Large Igneous Provinces (LIPs)
Arkose
Continental drift evidence
5. 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.
Fracture and cleavage
Regression
Sulfides
Siltstone and mudstone
6. Elongate submarine mountain ranges whose peaks lie only about 2-2.5km below sea level. Consist of a ridge axis - are roughly symmetrical - and can include escarpments - axial troughs - and valleys. Examples - Mid-Atlantic Ridge - East Pacific Rise -
Flood basalts
Soil erosion
Mid-ocean ridges
Mineral crystal destruction
7. Pea to plum-sized fragments of pyroclastic debris - consists of pumice or scoria fragments.
a'a'
Lapilli
Subduction
Divergent plate boundary
8. 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
Magma
Sulfates
Silicate minerals
9. Physical property of a mineral; refers to the shape (morphology) of a single crystal with well-formed crystal faces - or to the character of an aggregate of many well-formed crystals that grew together as a group. Depends on the internal arrangement
Crystal habit
Phreatomagmatic eruptions
Conchoidal fractures
Bathymetry
10. Mineral group; olivine group - pyroxene group - amphibole group.
Dark Silicates
Continental drift evidence
Inner core
ravertine
11. A mixture containing more than one type of metal atom. Example - bronze is a mixture of copper and tin.
Upper mantle
Mafic
Alloy
Facets
12. Subsoil - ions and clay leached and transported down from above accumulate here. As a result - new minerals form - and clay fills open spaces. Part of the zone of accumulation.
B-horizon
Limestone
Soil
Strata
13. Fluid basaltic lava extruded from crustal fractures called fissures.
Pyroclastic debris
Divergent plate boundary
Fissure eruptions/lava plateaus
Chemical sedimentary rocks
14. Heat from an intense surface fire bakes and expands the outer layer of the rock. On cooling - the layer contracts - causing the outer part of the rock spall - or break off in sheet-like pieces.
Transition zone
Effusive eruptions
Thermal expansion
Symmetry
15. Inorganic limestone; rock composed of crystalline calcium carbonate formed by chemical precipitation.
ravertine
Soil
Lava domes
Five steps of clastic sedimentary rock formation
16. 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).
Cementation
Carbonates
Sill
Subsidence
17. Sublayer of the mantle - depth of 660km.
Rock composition
Silicate minerals
Continental shelf
Upper mantle
18. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Special properties of minerals
Quartz sandstone
Differential weathering
Caliche
19. Refers to the arrangement of grains in a rock; that is - the way the grains connect each other and whether inequant grains are aligned parallel to one another.
Mafic
Lava tube
Rock texture
Rock composition
20. Lava flowing on dry land cools more slowly that lava erupting underwater.
Lithosphere
Superplumes
The effect of the environment on eruptive style
Outer core
21. The conditions in which sediment was deposited. Examples - beach - glacial - and/or river environments.
Transgression
Chert
Shield volcano
Depositional environment
22. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Asthenosphere
Metals
Elemental composition of Earth
a'a'
23. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Sedimentary rocks
Solid-state diffusion
Oxidation
Marine magnetic anomaly
24. After sand has lost its feldspar composition due to weathering over time - sediment composed entirely of quartz grains gets buried and lithified to form this type of rock.
Quartz sandstone
Melts
Light silicates
Rock composition
25. 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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26. 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
Transported soil
Calderas
Lower mantle
Silicate minerals
27. Chemical precipitates; salt deposits formed as a consequence of evaporation. Examples - rock salt and gypsum.
Lava domes
Crust
Evaporites
Basaltic magma
28. 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.
Hydrolysis
Fragmental igneous rocks
Large Igneous Provinces (LIPs)
Lithification
29. The distance that the world's deepest mine-shaft penetrates into the Earth beneath South Africa.
Rock composition
Pyroclastic debris
3.5km (2 miles)
Glass
30. Sedimentary rocks consisting of carbon-rich relicts of plants.
Organic sedimentary rocks
Limestone
Viscosity
Convergent plate boundary
31. The most common minerals in the Earth. Contain silica (SiO2) mixed in varying proportions with other elements (typically iron - magnesium - aluminum - calcium - potassium - and sodium).
Zone of leaching
Silicate minerals
Turbidite
Chert
32. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Seamount chains
Subduction
Assimilation
Lava
33. 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
Mineral
Hardness
Rhyolitic lava flows
Lithosphere
34. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Andesitic lava flows
Saprolite
Relative plate velocity
650-1100 degrees C
35. 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
Convective flow
The effect of the environment on eruptive style
ravertine
Subduction
36. Form when solid materials become hot and transform into liquid - example - molten rock.
Rock texture
Melts
Luster
Transgression
37. By melting - dissolving - or other chemical reactions.
Streak
Carbonates
Plate tectonics
Mineral crystal destruction
38. A thick accumulation of sediment (10-15km) - the surface of this sediment layer is this broad - shallow region.
Continental shelf
Glass
Xenolith
Mafic
39. 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.
Pangaea
Solid-state diffusion
Magnetic declination
Turbidite
40. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Rock-forming silicate minerals
Bed
Clastic
Transported soil
41. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hydration
Hot-spot track
collision
Grain sizes
42. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Saprolite
Organic chemicals
Sea-floor spreading
The core
43. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Conglomerate
Lava tube
Coal
rifting
44. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Arkose
Jointing
Oxides
Tuff
45. Rocks whose crystals interlock with each other.
Outer core
Crystalline
Weathering
Bedding
46. Distinguishing feature of magma; the process where different magmas formed in different locations from different sources may come in contact within a magma chamber prior to freezing. Thus the originally distinct magmas mix to create a new - different
Paleopole
Hydration
Magma mixing
Lava tube
47. 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.
Ultramafic
Stratagraphic formation
Assimilation
Large Igneous Provinces (LIPs)
48. 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.
Columnar jointing
Decompression
Rocks
Seamount chains
49. An insulated - tunnel-like conduit through which lava moves within a flow.
Magma mixing
Slab-pull force
Lava tube
Columnar jointing
50. A distinctive sequence of strata traced across a fairly large region. For example - a region may contain a succession of alternating sandstone and shale beds deposited by rivers - overlain by beds of marine limestone deposited later.
Dipole
The core
Volcanic blocks/bombs
Stratagraphic formation