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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 burial and lithification of angular or rounded clasts form these types of rocks.
Glassy igneous rocks
Plutons
Slab-pull force
Conglomerate
2. Sedimentary rock composed of quartz.
Magnetic anomaly
Basaltic lava flows
Siliceous rocks
pahoehoe
3. Type of sedimentary soil/rock; Calcite in a pedocal soil accumulates in the B-horizon and may cement soil together - creating this solid mass.
Oxides
Sedimentary Basins
Ultramafic
Caliche
4. 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.
Why magma rises
Elemental composition of Earth
Sandstone
B-horizon
5. 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.
Organic chemicals
Carbonate rocks
Sulfates
Clastic sedimentary rocks
6. Weathering - erosion - transportation - deposition - and lithification.
Five steps of clastic sedimentary rock formation
Pyroclastic debris
ravertine
Plutons
7. 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.
Bed
collision
Solid-state diffusion
Hydrolysis
8. 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
Agrillaceous rocks
Soil Horizons
Relative plate velocity
Geothermal gradient
9. Sedimentary rocks consisting of carbon-rich relicts of plants.
Calderas
Bedding
Regolith
Organic sedimentary rocks
10. Sublayer of the mantle - depth of 660km.
Upper mantle
Magnetic reversals
Chemical weathering
Chemical sedimentary rocks
11. The layering nature of sedimentary rocks - surface features of layers formed during deposition - and the arrangement of grains within layers.
Upper mantle
Metamorphic foliation
Sill
Sedimentary structure
12. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Halides
Hot-spot track
Lithosphere
Soil Horizons
13. Four settings: in volcanic arcs bordering deep-ocean trenches - isolated hot spots - within continental rifts - and along mid-ocean ridges.
Differential weathering
Area of igneous activity
Basaltic composition
Effusive eruptions
14. 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.
Soil Horizons
Sedimentary structure
Siltstone and mudstone
Fractional crystallization
15. 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
Batholiths
Bedrock
Dipole
Siltstone and mudstone
16. Physical features of the land surface represented by changes in elevation.
Continental rift
Topography
Granite
Mineral
17. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Transported soil
Luster
Melts
Glassy igneous rocks
18. 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
Laccolith
Magnetic inclination
Salt wedging
The effect of viscosity on eruptive style
19. Contributes to formation of soil; occurs when rainwater percolates through the debris and carries dissolved ions and clay flakes downward - This is the region where the downward transport occurs.
Zone of leaching
Rock texture
Arkose
Crystalline
20. 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.
Gabbro
Strata
Bathymetry
Superplumes
21. 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
Sedimentary Basins
Alloy
Outer core
Cement
22. 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
C-horizon
Viscosity
Stratagraphic formation
Metals
23. 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.
Felsic - intermediate - mafic - ultramafic
Crystal structure
Plate tectonics
Facets
24. 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.
Diagenesis
Laterite
Paleopole
Glassy igneous rocks
25. A reference to the sinking of the lithosphere; allows for sediment to accumulate in regions where this occurs.
Magma's speed of flow
Erosion
Conchoidal fractures
Subsidence
26. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Lower mantle
Fracture and cleavage
Hot-spot track
Lava domes
27. Magma type; contains about 45% to 52% silica. Named because it produces rock containing abundant mafic minerals - magnesium and iron combinations.
Mafic
Transition zone
Hydration
Bed
28. Type of soil; forms directly from underlying bedrock.
Spreading rate
Sulfides
Residual soil
Fractional crystallization
29. Equant - meaning that they have the same dimensions in all directions. Or inequant - meaning their dimensions are not the same in all directions.
Grain sizes
12km
Magnetic anomaly
Graded bed
30. A mineral's growth that is uninhibited - has well-formed crystal faces.
Sedimentary rocks
Dark Silicates
Euhedral crystal
Strata
31. Mineral crystal formation type; form from a solution - meaning that atoms - molecules - or ions dissolved in water bond together out of water.
Rhyolitic lava flows
Precipitation
Rock texture
Reason for Earth's internal heat
32. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Hydrolysis
Turbidite
Transported soil
Differential weathering
33. A felsic rock with large grains. Intrusive - phaneritic igneous rock.
Weathering
Symmetry
Mafic
Granite
34. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
Basalt
Luster
Dipole
atmospheres (atm)
35. Sedimentary rocks made up of the shells of organisms.
Biochemical sedimentary rocks
Magnetic reversals
Basaltic magma
Explosive eruptions
36. Refers to the proportions of different chemicals making up the rock - and thus the proportion chemicals affects the proportions of different minerals constituting the rock.
Depositional environment
Rock composition
Granitic magma
Cement
37. 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.
Pangaea
Siltstone and mudstone
Dipole
Glass
38. 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
Glass
Slab-pull force
Melts
Andesitic lava flows
39. 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
Continental rift
Paleopole
Intrusive igneous rock
Decompression
40. 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).
Silicate minerals
Quartz sandstone
Gabbro
Decompression
41. The compiled data from many marine cruises which defined a distinctive - striped and alternating bands of paleomagnetism.
Marine magnetic anomaly
Crystal
Lava domes
Conchoidal fractures
42. In addition to islands that rise above sea level - seamounts have been detected (isolated submarine mountains) - once volcanoes but no longer erupt.
Crystal
Seamount chains
650-1100 degrees C
Compaction
43. 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.
Viscosity
Native metals
Plate tectonics
Transform plate boundary
44. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Coal
The effect of viscosity on eruptive style
Differential weathering
Composite cone (stratovolcano)
45. Type of magma; low in silica - fluid - crystallize at high temperatures.
Continental shelf
Basaltic composition
Siltstone and mudstone
Basaltic magma
46. 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
Sill
Plate tectonics
Hot-spot track
Bed
47. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Inner core
atmospheres (atm)
Frost wedging
The core
48. Low-viscosity (basaltic) lava flows out of a volcano easily - whereas high-viscosity (andesitic and rhyolitic) lava can clog and build pressure within a volcano. Basaltic eruptions are typically effusive and produce shield volcanoes - whereas rhyolit
Assimilation
Clastic
Physical weathering
The effect of viscosity on eruptive style
49. 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
Subsidence
Turbidite
Magma mixing
50. 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
12km
Stratagraphic formation
Spreading rate
Gem