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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. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Special properties of minerals
Soil
3.5km (2 miles)
Lithosphere
2. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Assimilation
Continental drift evidence
Granite
Conglomerate
3. Chemical weathering during Which minerals dissolve into water.
Dissolution
The core
Marine magnetic anomaly
Xenolith
4. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Magma mixing
Chert
Diagenesis
Topography
5. A rock made of solid mass of glass - or of tiny crystals surrounded by glass. Reflect light as glass does and tend to break conchoidally. Examples - obsidian - tachylite - pumice.
Intrusive igneous rock
Explosive eruptions
Glassy igneous rocks
Effusive eruptions
6. A sediment-filled depression; in an area where the lithosphere has subsided.
Loam
Sedimentary Basins
Tephra
Soil Horizons
7. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Effusive eruptions
Siltstone and mudstone
Rock layering
Paleopole
8. Type of soil; forms directly from underlying bedrock.
Conchoidal fractures
Subduction
Residual soil
Magnetic reversals
9. Type of magma; high silica content - viscous - liquid at temperatures as low as 700 degrees C.
Assimilation
Granitic magma
Dipole
12km
10. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Paleopole
Assimilation
Saprolite
Subduction
11. Type of lava flow; mafic - low viscosity - extremely hot - flows very quickly.
Xenolith
Basaltic lava flows
Thermal expansion
Dipole
12. 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
Melts
Viscosity
Chemical weathering
3.5km (2 miles)
13. Lava flowing on dry land cools more slowly that lava erupting underwater.
Glass
Ridge-push force
Paleomagnetism
The effect of the environment on eruptive style
14. Mineral group; feldspars - quartz - muscovite - clay minerals.
Light silicates
Volatiles
Differential weathering
Ripples
15. Mineral class; consist of a metal cation bonded to the anionic group. Many form by precipitation out of water at or near the Earth's surface. Example - gypsum.
Sulfates
Continental drift hypothesis
Reason for Earth's internal heat
Mafic
16. Type of rock; accumulated sand bars - within are mineral grains of quartz and feldspar - this sediment if buried and lithified.
Arkose
Light silicates
Decompression
Peridotite
17. Layering in sedimentary rocks.
Transform plate boundary
Bedding
Basaltic lava flows
Redbeds
18. Cause of melting; the variation in temperature with depth is expressed in the geotherm; because pressure prevents melting - a decrease in pressure can permit melting. Specifically - if the pressure affecting hot mantle rock decreases while the temper
Cinder cone
Cementation
Glassy igneous rocks
Decompression
19. Molten rock that has flowed out onto Earth's surface.
E-horizon
Lava
Transition zone
Convective flow
20. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Specific gravity
Slab-pull force
The effect of viscosity on eruptive style
Jointing
21. Type of volcanic eruption; pyroclastic - produce clouds and avalanches of pyroclastic debris. Gas expands in the rising magma - cannot escape. The pressure becomes so great that it blasts the lava - and volcanic rock - out of the volcano.
Cement
Explosive eruptions
Differential weathering
Volcanic pipes/necks
22. A name for any kind of unconsolidated debris that covers bedrock. Includes both soil and accumulations of sediment that have not evolved into soil.
Fissure eruptions/lava plateaus
Sulfates
Relative plate velocity
Regolith
23. 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.
Factors of magma cooling time
O-horizon
Effusive eruptions
Physical weathering
24. Mineral class; consist of pure masses of a single metal - with metallic bonds. Copper and gold can appear in this way.
Residual soil
Chert
Fragmental igneous rocks
Native metals
25. 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).
Gem
C-horizon
Silicate minerals
Depositional environment
26. 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.
Dunes
Crystal structure
Sedimentary structure
Lithification
27. Sedimentary rocks consisting of carbon-rich relicts of plants.
Organic sedimentary rocks
Rock-forming silicate minerals
Oxidation
Dike
28. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Graded bed
Metals
Xenolith
Frost wedging
29. 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.
Ridge-push force
Assimilation
Transition zone
Seamount chains
30. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Decompression
Coal
Metamorphic rocks
Native metals
31. Active hot-spot volcanoes commonly occur at the end of a chain of dead volcanoes.
Hot-spot track
Coal
Sulfates
Lithification
32. Type of igneous rock composition; composed of light-colored silicates - very rich in felsic (feldspar and silica). Major constituent of continental crust.
650-1100 degrees C
Crystalline igneous rocks
Chemical weathering
Granitic composition
33. Process that occurs after the sediment has been buried - pressure cause by the overburden squeezes out water and air that had been trapped between clasts - and the clasts press together tightly.
Compaction
Pangaea
Soil erosion
Outcrop
34. Distinguishing feature of magma; Because not all minerals melt by the same amount under given conditions - and because chemical reactions take place during melting - the magma that forms as a rock begins to melt does not have the same composition as
Frost wedging
Weathering
Partial melting
triple junction
35. 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
Diagenesis
Ridge-push force
Hydration
Fissure eruptions/lava plateaus
36. 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
Magma mixing
Xenolith
Crystal lattice
Columnar jointing
37. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Oxides
Transgression
Weathering
Fracture zones
38. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Volcanic pipes/necks
Elemental composition of Earth
Crystal habit
atmospheres (atm)
39. 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.
Tuff
Subduction
Metamorphic rocks
atmospheres (atm)
40. A single layer of sediment or sedimentary rock with a recognizable top and bottom.
Rhyolitic lava flows
Bed
atmospheres (atm)
A-horizon
41. Relatively small - elongated ridges that form on a bed surface at right angles to the direction of the current flow of the rock.
Ripples
Transgression
Siliceous rocks
Sandstone
42. A sheet of tuff formed from a pyroclastic flow.
Ignimbrite
Alloy
Partial melting
Explosive eruptions
43. Form from grains that break off preexisting rock and become cemented together - or from minerals that precipitate out of a water solution.
Agrillaceous rocks
Deep-ocean trenches
Fragmental igneous rocks
Sedimentary rocks
44. A vent at Which melt from inside the Earth spews onto the planet's surface. Erupt.
Volcano
Fractional crystallization
Area of igneous activity
Ultramafic
45. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Basalt
Zone of leaching
Apparent polar-wander path
Seamount chains
46. 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.
Continental drift hypothesis
Sedimentary Basins
Laterite
Graded bed
47. In degrees Celsius - the high temperatures at which igneous rocks freeze; the freezing of liquid melt to form solid igneous rock represents the same phenomenon as the freezing of water - except at much higher temperatures.
Cementation
650-1100 degrees C
Large Igneous Provinces (LIPs)
Explosive eruptions
48. Process occurring in arid climates - dissolved salt in groundwater precipitates and grows as crystals in open pore spaces in rocks. This process pushes apart the surrounding grains and so weakens the rock that when exposed to wind or rain - the rock
Weathering
Salt wedging
Lapilli
Deep-ocean trenches
49. 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.
Cinder cone
Factors of magma cooling time
Transform plate boundary
Glassy igneous rocks
50. A fine spray of lava instantly freezes to form fine particles of glass.
Felsic - intermediate - mafic - ultramafic
Dissolution
Fissure eruptions/lava plateaus
Ash