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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. 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
Ultramafic
Arkose
Deposition
2. A reference to the pattern structure of a mineral. A material in which atoms are fixed in an orderly pattern - a crystalline solid.
atmospheres (atm)
Intrusive igneous rock
Chert
Crystal lattice
3. 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.
Chemical sedimentary rocks
Quartz sandstone
Lava
Convective flow
4. When water is trapped in a joint freezes - it forces the joint open and may cause the joint to grow.
Turbidity current
Hydrosphere
Frost wedging
Convergent plate boundary
5. Materials that easily transform into gas at the relatively low temperatures found at the Earth's surface.
Slab-pull force
Volatiles
Sill
The core
6. Rock made by the freezing of magma underground - after it has pushed its way (intruded) into preexisting rock of the crust.
Asthenosphere
Intrusive igneous rock
Organic sedimentary rocks
Sedimentary rocks
7. A column of very hot rock that flows upward until it reaches the base of the lithosphere. In this model - such deep-mantle plumes form because heat rising from the Earth's core is warming rock at the base of the mantle. A possible explanation to the
Sea-floor spreading
Mantle plume
Sill
Color
8. An organic sedimentary rock; black - combustible rock consisting of over 50% carbon.
Tephra
Coal
Mineral crystal destruction
Magnetic anomaly
9. Occurs within the asthenosphere - actively drags plates along and attributes partially for the mechanism shifting the plates along the Earth's surface.
Crystal structure
Jointing
Convective flow
Composite cone (stratovolcano)
10. The speed of the movements of the plates with respect to the speed of the other plates' movements. Absolute plate velocity is a measure of the movement of any plates relative to a fixed point in the mantle.
Symmetry
Relative plate velocity
Hydrosphere
Cross beds
11. Measure of pressure or push in units of force - per unit area. 1 atm = 1.04 kilograms per square centimeter.
atmospheres (atm)
Hydrolysis
Andesitic lava flows
Regolith
12. Type of lava flow; higher silica content - greater viscosity - forms a large mound above the vent out of a volcano.
Inner core
Diagenesis
Andesitic lava flows
Cinder cone
13. 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
Volcanic pipes/necks
Source rock composition
Crystal habit
Viscosity
14. 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
Why magma rises
Salt wedging
Bed
Metals
15. 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.
Lithification
Coal
E-horizon
Rocks
16. Clast size - clast composition - angularity and sphericity - sorting - and character of cement.
Factors classifying clastic sedimentary rocks
3.5km (2 miles)
Fumerolic mineralization
Effusive eruptions
17. A pluton formation theory; a process during Which magma assimilates wall rock - and blocks of wall rock break off and sink into the magma.
Polymorphs
Thermal expansion
Stoping
Dike
18. Hot basaltic lava that erupts with such low viscosity that it can flow tens to hundreds of kilometers across the landscape.
Silicates
Flood basalts
Arkose
Magma
19. Physical features of the land surface represented by changes in elevation.
Heat transfer
Volcanic pipes/necks
Topography
Glassy igneous rocks
20. Perhaps the cause for the large igneous provinces; formations within the mantle - plumes that bring up vastly more hot asthenosphere than normal plumes.
Paleomagnetism
Turbidite
Superplumes
Magma
21. Mineral class; the anion within these types of minerals is a halogen ion (such as chlorine or fluorine).
Oxidation
Outcrop
Explosive eruptions
Halides
22. A process occurring when sea level falls - the coast migrates seaward.
Plates
Andesitic lava flows
ravertine
Regression
23. Biochemical sedimentary rock; it's made from cryptocrystalline quartz. Examples - flint and jasper.
Chert
Pangaea
Rhyolitic lava flows
Transition zone
24. Type of magma; low in silica - fluid - crystallize at high temperatures.
Transported soil
Hydrosphere
E-horizon
Basaltic magma
25. Mineral crystal formation type; form at interfaces between the physical and biological components of the Earth system by this process.
Turbidity current
Assimilation
Fragmental igneous rocks
Biomineralization
26. Type of lava flow; the most viscous of any lava flow because it is the most silicic and the coolest in nature. Tends to accumulate in a lava dome above the vent or in short and bulbous flows 1 to 2 km long.
Relative plate velocity
Metamorphic foliation
Loam
Rhyolitic lava flows
27. Mineral group; feldspars - quartz - muscovite - clay minerals.
Melts
Light silicates
Laterite
Bed
28. Rocks which develop when hot molten rock cools and freezes solid.
Facets
Igneous rocks
Magma mixing
Plates
29. Type of volcano; broad and slightly domed - primarily made of basaltic lava - large and erupt large volumes of lava. Form from either low viscosity basaltic lava or from large pyroclastic sheets.
Shield volcano
Magma mixing
Carbonates
Crystal habit
30. Forms a 2885-km-thick layer surrounding the core. In terms of volume - it is the largest part of the Earth. It consists entirely of ultramafic rock - peridotite.
Mantle
Elemental composition of Earth
Intrusive igneous rock
Plate tectonics
31. 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
Fragmental igneous rocks
Chert
Siliceous rocks
32. Volcanic landform; bulbous mass of congealed lava - associated with explosive eruptions of gas-rich magma.
Granitic magma
Asthenosphere
Crystalline igneous rocks
Lava domes
33. Layering in metamorphic rocks.
Metamorphic foliation
Peridotite
Elemental composition of Earth
Relative plate velocity
34. Physical property of a mineral; refers to the way a mineral surface scatters light. Metallic versus non-metallic in nature.
Plutons
Luster
Metamorphic foliation
Dipole
35. Forms when clots of lava fly into the air in lava fountains and then freeze to form solid chunks before hitting the ground. Some forms when the explosion of a volcano shatters preexisting rock and ejects the fragments over the countryside.
Frost wedging
Pyroclastic debris
Magma
Continental shelf
36. Built up deposit of volcanic bombs and lapilli - known as volcanic agglomerate.
triple junction
Diagenesis
Polymorphs
Tuff
37. A type of carbonate rock; rocks formed from the calcite or aragonite skeletons of organisms form this biochemical sedimentary rock.
Limestone
Granitic composition
Bedrock
Tuff
38. Rocks whose crystals interlock with each other.
Lapilli
Crystalline
Strata
Magnetic declination
39. Rock formations still attached to the Earth's crust.
Bedrock
Regolith
Tephra
Glass
40. Natural cracks that form in rocks due to removal of overburden or due to cooling.
Composite cone (stratovolcano)
Jointing
Conchoidal fractures
Volcanic blocks/bombs
41. Lava flowing on dry land cools more slowly that lava erupting underwater.
The effect of the environment on eruptive style
Flood basalts
Differential weathering
Upper mantle
42. 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.
Hot spots
Metamorphic foliation
C-horizon
Color
43. The boundary between two beds is a bedding plane; several beds constitute this structure.
Strata
Sedimentary Basins
Sandstone
Chemical weathering
44. 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.
Area of igneous activity
Euhedral crystal
Rock-forming silicate minerals
Crystal habit
45. 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.
Calderas
Root wedging
Rock composition
A-horizon
46. 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
Continental drift evidence
Marine magnetic anomaly
Partial melting
47. 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
Explosive eruptions
Facets
Fracture and cleavage
Large Igneous Provinces (LIPs)
48. 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.
Slab-pull force
Turbidite
Rock texture
Inner core
49. 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
Sulfates
Spreading rate
Regression
Carbonates
50. The angle between the direction that a compass needle points at a given location and the direction of the 'true' (geographic) north. Through this process - the magnetic poles never stray more than 15 degrees of latitude from the geographic pole.
Root wedging
Asthenosphere
Fissure eruptions/lava plateaus
Magnetic declination