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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. Rocks that consist of mineral crystals that intergrow when the melt solidifies - interlocking structure. Examples - granite and rhyolite.
Lapilli
Crystalline igneous rocks
Sill
Sedimentary Basins
2. 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.
Fracture and cleavage
Basaltic magma
Physical weathering
The effect of the environment on eruptive style
3. 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.
Volcano
Basaltic composition
Crystalline
Spreading rate
4. The bottom portion of the upper mantle - the interval lying between 400km and 660km deep. Here within the Earth - the character of the mantle undergoes a series of abrupt changes.
Transition zone
Plutons
Luster
Crystal structure
5. Sedimentary rocks made up of the shells of organisms.
Chemical sedimentary rocks
Regression
Continental shelf
Biochemical sedimentary rocks
6. 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
Soil
Explosive eruptions
Outer core
Hydrosphere
7. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
Cementation
Sill
Crystal lattice
Zone of accumulation
8. Iron (35%) - oxygen (30%) - silicon (15%) - and magnesium (10%) - and the remaining 10% consists of 88 naturally occurring elements.
Elemental composition of Earth
Plate tectonics
Metamorphic foliation
Magnetic reversals
9. 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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10. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Lava domes
Basalt
Relative plate velocity
650-1100 degrees C
11. A solid in which atoms are not arranged in an orderly pattern. Forms when a liquid freezes so fast that atoms do not have time to organize into an orderly pattern.
Glass
atmospheres (atm)
Fissure eruptions/lava plateaus
Gabbro
12. 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
Batholiths
Convergent plate boundary
Zone of accumulation
Turbidite
13. A sediment-filled depression; in an area where the lithosphere has subsided.
Felsic - intermediate - mafic - ultramafic
Sedimentary Basins
Granite
Basalt
14. 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
A-horizon
Dipole
Differential weathering
Factors classifying clastic sedimentary rocks
15. Rocks which develop when hot molten rock cools and freezes solid.
Granite
Continental shelf
Igneous rocks
Convective flow
16. Layering in sedimentary rocks.
Gabbro
Bedding
Magnetic anomaly
Regression
17. 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.
Crystal structure
Rock composition
Paleopole
ravertine
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
Turbidity current
Salt wedging
Chemical sedimentary rocks
Superplumes
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
Factors classifying clastic sedimentary rocks
Fissure eruptions/lava plateaus
Volatiles
20. Mineral class; the molecule CO23 serves as the anionic group. Elements like calcium or magnesium bond to this group. Examples - calcite and dolomite.
The effect of gas pressure on eruptive style
Carbonates
Heat transfer
Regression
21. A layer of sediment in which grain size varies from coarse at the bottom to fine at the top.
Quartz sandstone
Graded bed
Chemical sedimentary rocks
Agrillaceous rocks
22. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
collision
Tuff
Melts
Columnar jointing
23. A reference to the supposed position of the Earth's magnetic pole at a time in the past.
Depositional environment
Paleopole
Pyroclastic flows
Crystalline igneous rocks
24. 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.
Outcrop
Rocks
Grain sizes
Jointing
25. Along much of the perimeter of the Pacific Ocean - the ocean floor reaches astounding depths of 8-12km. These areas define elongate troughs - and they border volcanic arcs - the curving chains of active volcanoes.
Hydrosphere
Deep-ocean trenches
Basaltic composition
Lava tube
26. The fit of the continents - locations of past glaciations - the distribution of equatorial climatic belts - the distribution of fossils - and matching geologic units.
Glassy igneous rocks
Crust
Caliche
Continental drift evidence
27. 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).
Hydration
Silicate minerals
Color
A-horizon
28. Physical property of a mineral; results from the way a mineral interacts with light. A mineral absorbs certain wavelengths - so the color seen represents the color wavelengths the mineral did not absorb.
Dark Silicates
Calderas
Pyroclastic debris
Color
29. Forms from a chemical reaction between solid calcite and magnesium-bearing groundwater.
Coal
Caliche
Dolostone
Agrillaceous rocks
30. 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.
Magma
Transition zone
Solid-state diffusion
rifting
31. Mineral class; consist of a metal cation bonded to a sulfide anion. Examples - galena and pyrite. Many have a metallic luster. Can also be considered ores with high proportions of metal within the mineral.
Ripples
Facets
Felsic - intermediate - mafic - ultramafic
Sulfides
32. Type of sedimentary rock; rocks whose grains are stuck together by cement.
Calderas
Crystal
Saprolite
Clastic
33. 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 rocks
Slab-pull force
Andesitic lava flows
Grain sizes
34. Type of volcanic eruption; takes place when water gains access to the hot rock around the magma chamber and suddenly transforms into steam - a pyroclastic eruption involving the reaction of water with magma.
The effect of gas pressure on eruptive style
Extrusive igneous rock
Strata
Phreatomagmatic eruptions
35. 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.
Rock layering
Hot-spot track
Frost wedging
Transported soil
36. Successive turbidity currents deposit successive graded beds - creating this sequence of strata.
Laccolith
E-horizon
Turbidite
Heat transfer
37. Physical property of a mineral; refers to the color of a powder produced by pulverizing the mineral. Provides a fairly reliable clue to the mineral's identity - since the color of the mineral powder tends to be less variable than the color of the who
Volatiles
Streak
Pyroclastic debris
Seamount chains
38. The burial and lithification of angular or rounded clasts form these types of rocks.
Conglomerate
Residual soil
Abyssal plains
Volatiles
39. Type of soil; forms from sediment that has been carried in from elsewhere. Include those formed from deposits left by rivers - glaciers - or wind.
Sea-floor spreading
Rocks
Transported soil
Regolith
40. 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.
Glassy igneous rocks
Arkose
Biochemical sedimentary rocks
Crystal structure
41. Rigid outer layer of Earth - 100-150km thick. Consists of the crust plus the uppermost part of the mantle.
Five steps of clastic sedimentary rock formation
Lithosphere
Ridge-push force
Fracture zones
42. Sedimentary rock composed of clay.
Stoping
B-horizon
Continental shelf
Agrillaceous rocks
43. Some minerals have distinctive properties - such as calcite which reacts with dilute hydrochloric acid to produce carbon dioxide. Dolomite also reacts with acid - graphite can make clear markings - magnetite attracts a magnet - halite tastes salty -
The effect of viscosity on eruptive style
Symmetry
Special properties of minerals
Transported soil
44. A process occurring when sea level falls - the coast migrates seaward.
Root wedging
Regression
Agrillaceous rocks
Graded bed
45. 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
Laccolith
Lower mantle
Granitic magma
46. Refers to the processes that break up and corrode solid rock - eventually transforming it into sediment. Physical and chemical variations.
Transition zone
Weathering
Continental rift
Granitic magma
47. 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.
Cross beds
Light silicates
Frost wedging
Crystal structure
48. Chemical weathering occurring in warm - wet climates can produce a layer of rotten rock - over 100km thick.
Factors of magma cooling time
Saprolite
Coal
Phreatomagmatic eruptions
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.
Transform plate boundary
Siltstone and mudstone
Why magma rises
Coal
50. 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
Partial melting
Dipole
Bathymetry
3.5km (2 miles)