Notice
If you get a question wrong, you can still click on the other answers. This will open up hints and explanations(if available) with additional information.My personal advice: Since the exams are written, if you score less than 90% on the following MC questions, seriously reconsider your study strategies for this class.
Disclaimer: While every reasonable effort is made to ensure that the information provided is accurate, no guarantees for the currency or accuracy of information are made. It takes several proof readings and rewrites to bring the quiz to an exceptional level. If you find an error, please contact me as soon as possible. Please provide a description of the question because server may randomize the questions and answers.
Go to: Midterm II | Final
Geology (GLGY 381-UCAL) Midterm Exam I
Congratulations - you have completed Geology (GLGY 381-UCAL) Midterm Exam I.
You scored %%SCORE%% out of %%TOTAL%%. With incorrect multiple attempts your score is %%PERCENTAGE%%
Your performance has been rated as %%RATING%%
Question 1 |
A | Sandy shore (littoral zone) |
B | Abyssal zone |
C | Bathyal zone |
D | Above the normal sea level |
E | Shelf (sublittoral zone) |
Question 2 |
A | superposition |
B | Uniformitarianism |
C | lowerposition |
D | parsimony |
E | original horizontality |
Question 3 |
A | A |
B | F |
C | D |
D | C |
E | B |
F | G |
Question 4 |
A | Every object in a state of uniform motion tends to remain in that state of motion unless an external force is applied to it. |
B | For every action there is an equal and opposite reaction. |
C | Gravitational force is proportional to the mass and acceleration due to gravity. |
D | The relationship between an object's mass m, its acceleration a, and the applied force F is F = ma. Acceleration and force are vectors (as indicated by their symbols being displayed in slant bold font); in this law the direction of the force vector is the same as the direction of the acceleration vector. |
Question 5 |
A | Shallow marine environments |
B | None of the answers posted here are correct. |
C | Warm and tropical wet environments |
D | River bed environments |
E | Deep marine environments |
Question 6 |
A | quartz |
B | biotite |
C | olivine |
D | amphibole |
Question 7 |
A | At the bed, there is no slip conditions due to higher velocity. |
B | Velocity decreases as the depth increases. |
C | The lowest velocity is at the bed. |
D | Velocity increases as the depth increases. |
E | The highest velocity is at the bed. |
Question 8 |
A | True |
B | False |
Question 9 |
A | Planar cross-lamination |
B | Turbulent sweeps |
C | Starved ripples |
D | Climbing ripples |
E | Trough cross-lamination |
Question 10 |
A | Hard organic parts from invertebrates |
B | Calcium carbonate produced as a by product of chemical weathering |
C | Transported rock fragments |
D | Precipitation of inorganic compounds out of water due to evaporation |
E | Magmas rich in calcium carbonates |
Question 11 |
A | Matrix is the substance that binds clasts together while cement is a fined grained material that deposits within crystals. |
B | Matrix is deposited at the same time as clasts while cement forms after the deposition of sediment as precipitate. |
C | Matrix is formed when the clasts are deposited under high temperatures while cement is formed when clasts are deposited under low temperatures. |
D | Both terms describes a material that binds clasts but the term "matrix" is used when the rock is mostly composed of clasts while cement is used when majority of the rock is composed of fined grained materials. |
Question 12 |
A | Bioerosion is the reworking of soils and sediments by animals or plants. Bioturbation is caused by mechanically or chemically cutting/removing the grains by organisms. |
B | Bioturbation is caused by plants. Bioerosion is caused by animal activities. |
C | They are the same except Bioturbation is the British English word for Bioerosion(US-English) |
D | Bioturbation is the reworking of soils and sediments by animals or plants. Bioerosion is caused by mechanically or chemically cutting/removing the grains by organisms. |
Question 13 |
-high viscosity
-poorly sorted grains
-often larger clasts are separated by fine grained materials
-low Reynolds number and considered as a laminar flow
-low velocity (40-50 km/h)
A | Grain flow |
B | Liquified flow |
C | Turbidity flow |
D | Debris flow |
Question 14 |
h(D) = 55 m
g = 9.81 m/s2
u = 33 m/s
A | 0.06116 |
B | 2.37 |
C | 1.95 |
D | 0.6116 |
E | 1.42 |
Question 15 |
A | 75% |
B | 5% |
C | 98% |
D | 50% |
E | 90% |
Question 16 |
A | Significant density contrast |
B | High volume sediment loads |
C | Pressure: soft water-bearing sediments escaping through overlying sediments |
D | Gravity: hard sediments sinking into soft underlying sediments |
Question 17 |
A | False |
B | True |
Question 18 |
A | B |
B | G |
C | C |
D | F |
E | A |
F | E |
G | D |
Question 19 |
A | Dunes have interbedded cross laminations and ripples do not. |
B | Dunes form in marine environments and ripples form in non-marine river type environments. |
C | Dunes forms in turbulent waters and ripples forms in calm waters. |
D | Dunes are distinctly larger than ripples. |
Question 20 |
A | False |
B | True |
Question 21 |
A | paleosols |
B | pedogenesis |
C | sedimentation |
D | erosion |
Question 22 |
A | Burrows are created by pushing the grains to walls of the structure and borings are created by mechanically/chemically cutting the grains. |
B | Borings are created by pushing the grains to walls of the structure and boring are created by mechanically/chemically cutting the grains. |
C | Burrows are trace fossils and borings are body fossils. |
D | Burrows and borings are created by two distinct type of creatures that in burrows the sediments are removed mechanically and in borings the sediments are dissolved chemically. |
E | Borings are trace fossils and burrows are body fossils. |
F | I have no freaking clue what the hell you asking about. |
Question 23 |
A | Neither due to incorrect representation of the internal flow direction. |
B | B |
C | A |
D | Neither due to incorrect representation of the initial flow direction. |
Question 24 |
A | limestone |
B | dolostone |
C | mudstone |
D | gypsum |
E | sandstone |
Question 25 |
A | Below massive/rapid deposition |
B | Within the upper flow regime |
C | Below hemipelagic mud |
D | At the base of the sourced region (very bottom) |
E | None of the answers are correct |
Question 26 |
A | N to S |
B | S to N |
C | NW to SE |
D | NE to SE |
E | SE to NW |
Question 27 |
A | Abyssal zone |
B | Shelf (sublittoral zone) |
C | Sandy shore (littoral zone) |
D | Bathyal zone |
E | Above the normal sea level |
Question 28 |
A | A sample with few discrete traces of bioturbation |
B | Bioturbation is over 90% of sediment bioturbated, and bedding
is barely detectable |
C | Bioturbation is between 30% and 60% of the sediment affected and bedding is distinct |
D | Bioturbation affects less than 30% of the sediment sample and the bedding is distinct |
E | Bioturbation is between 60% to 90% of the sediment bioturbated and bedding indistinct |
F | Sediment is totally reworked by bioturbation |
Question 29 |
A | Organic activities such as roots and biodegradation causing decrease in the mineral volume. |
B | Organic activities such as roots and biodegradation causing increase in the mineral volume. |
C | Freeze-thaw cycle result in change in volume. |
D | Increase of stress as a result of pressure increase. |
E | Release of stress as a result of pressure decrease. |
F | Hydration of minerals result in increase in volume. |
Question 30 |
A | saltation |
B | suspension traction |
C | rolling |
D | paleoflow |
E | sliding |
Question 31 |
A | Temperate climate with long cold winters and short warm summers |
B | Deep sea ocean beds with rich organic matter |
C | Dry climates with year-round permafrost |
D | Dry climates with long periods of droughts |
E | Humid climates |
Question 32 |
A | High pressures excreted on sediments from both through uplift and loading processes. |
B | Differential lateral compaction within bed forms resulting high pressures between bed contacts. |
C | Extreme pressure concentrated at the contacts between grains within sediments. |
D | Differential pressure-temperature gradient that increases with depth. |
E | Extreme temperatures and pressures between different sediment successions. |
Question 33 |
A | Glacial breakups |
B | Slumps |
C | Debris flows |
D | Rock falls |
E | Turbidity currents |
Question 34 |
A | 1. is an antidune 2. is an antidune |
B | 1. is a dune 2. is an antidune |
C | 1. is an antidune 2. is a dune |
D | 1. is a dune 2. is a dune |
Question 35 |
A | Muscovite mica |
B | Kaolinite |
C | Calcium Feldspars |
D | Olivine |
E | Pyroxene |
Question 36 |
A | Study of behavior. |
B | Classification of the trace fossils. |
C | Study of the mode of preservation. |
D | Description of the identifiable parts. |
Question 37 |
A | True |
B | False |
Question 38 |
A | Full relief structures are preserved as 2D structures while semi-relief structures are preserved as 3D structures. Both are preserved within a single type of sediment. |
B | Full relief structures are partially preserved within a single type of sediment while semi-relief structures are fully preserved at an interface between two strata. |
C | Full relief structures are preserved within a single type of sediment while semi-relief structures are preserved at an interface between two strata. |
D | Semi- relief structures are preserved within a single type of sediment while full-relief structures are preserved at an interface between two strata. |
Question 39 |
A | False |
B | True |
Question 40 |
A | A. critical B. subcritical C. supercritical |
B | A. critical B. supercritical C. subcritical |
C | A. supercritical B. subcritical C. critical |
D | A. subercritical B. critical C. supcritical |
E | A. supercritical B. critical C. subcritical |
supercritical = Fr > 1 and the velocity of the stream is greater than the velocity of the surface wave.
subcritical = Fr < 1 and the velocity of the stream is lower than the velocity of the surface wave.
Question 41 |
A | Potential energy |
B | Sediment load |
C | Flow velocity |
D | Gravity |
E | Flow separation |
Question 42 |
A | 98% lithics
1 % feldspar
1% quartz |
B | 98% quartz
1 % lithics
1% feldspar |
C | 50% lithics
40 % feldspar
10% quartz |
D | 60% quartz
1 % lithics
90% feldspar |
Question 43 |
A | grain size in um |
B | flow velocity in cm/s |
C | flow velocity in m/s |
D | grain size in mm |
E | depth in m |
Question 44 |
A | Left side has the scour region and right side is the lee side. |
B | Left side has the scour region and right side is the stoss side. |
C | Left side is the stoss side and right side is the lee side. |
D | Left side is the lee side and right side is the stoss side. |
E | All statements are incorrect. |
Question 45 |
A | Position II just above the ripple |
B | Position V between two ripples |
C | Position IV in the lee side of the ripple |
D | Position III where the flow rate is consistent and smooth |
E | Position I in the stoss side of the ripple |
Question 46 |
A | metamorphic |
B | sedimentary |
C | authigenic |
D | native |
E | detrital |
Question 47 |
A | Geostatic pressure |
B | Salt Diapirs |
C | Pore waters |
D | Pressure dissolution |
Question 48 |
A | A. Recycled origin B. Continental block C. Magmatic arc |
B | A. Quartz B. Lilith fragments C. Feldspar |
C | A. Quartz B. Feldspar C. Lilith fragments |
D | A. Continental block B. Magmatic arc C. Recycled origin |
E | A. Magmatic arc B. Continental block C. Recycled origin |
F | A. Continental block B. Recycled origin C. Magmatic arc |
Question 49 |
A | Chemical |
B | Physical |
C | Hydration/dehydration |
D | Simple solution |
Question 50 |
A | decreasing , decreasing |
B | increasing , increasing |
C | decreasing , increasing |
D | None of the answers are correct because it is not the acidity that is important, it is the pH. |
E | increasing , decreasing |
Question 51 |
A | highest velocity point of the velocity profile. |
B | surface of the fluid. |
C | bed surface of the velocity profile. |
D | (around) middle of the velocity profile. |
Question 52 |
A | The stream lines(red lines) converging at the yellow arrow cause the velocity to increase significantly(at that point). |
B | The stream lines(red lines) converging at the yellow arrow cause the velocity to decrease significantly(at that point). |
C | The lift at the yellow arrow is caused by the high pressure at the top caused by converging streamlines. |
D | The pressure from above is much higher causing the grains to push hard against the bed. |
E | The pressure right above the yellow arrow is much lower than the pressure near the black rocks/sediments. |
Question 53 |
A | True |
B | False-it should be other way around. |
Question 54 |
A | G |
B | C |
C | E |
D | D |
E | F |
Question 55 |
A | Turbidity current |
B | Slump |
C | Debris flow |
D | Rock fall |
E | Sheet wash |
Question 56 |
A | None of the answers are correct. |
B | I. zero II. turbulent |
C | I. lower II. laminar |
D | I. lower II. turbulent |
E | I. higher II. laminar |
Question 57 |
A | period of the wave |
B | amplitude of the wave |
C | viscosity of the fluid |
D | type of fluid |
Question 58 |
A | A. inertial forces driven load B. gravity driven load |
B | A. bed load B. suspended load |
C | A. gravity driven load B. inertial forces driven load |
D | A. suspended load B. bed load |
Question 59 |
A | A. iron rich minerals B. oxygen rich minerals |
B | A. felsic minerals B. mafic minerals |
C | A. mafic and felsic minerals B. silica rich minerals |
D | A. mafic minerals B. felsic minerals |
E | A. oceanic crust B. continental crust |
Question 60 |
A | Under low- to medium-density turbidity currents |
B | Within river deltas |
C | Under high-density turbidity currents |
D | Within oxbow lakes |
E | Under current ripples |
Question 61 |
A | chemical weathering |
B | physical weathering |
C | artificial weathering |
D | biological weathering |
Question 62 |
A | Yep |
B | False |
Question 63 |
A | Freezing(swelling) and thawing(shrinking). |
B | Burial(shrinking) and exfoliation(swelling). |
C | Freezing(shrinking) and thawing(swelling). |
D | Hydration(swelling) and dehydration(shrinking) |
E | Hydration(shrinking) and dehydration(swelling) |
Question 64 |
A | shear stress |
B | sub-normal stress |
C | tangential stress |
D | super-normal stress |
E | normal stress |
Question 65 |
A | True |
B | False |
Question 66 |
A | carbonates |
B | clastic sediments |
C | organic deposits |
D | precipitates |
E | evaporates |
Question 67 |
A | turbulent flow |
B | laminar flow |
C | gravity driven flow |
D | low viscous forces in the folow |
Question 68 |
A | A. carbonates B. silicates |
B | A. silicates B. carbonates |
C | A. mafic rocks B. felsic rocks |
D | A. felsic rocks B. mafic rocks |
Question 69 |
A | High energy and low sedimentation environments. |
B | Low energy and high sedimentation environments. |
C | Low energy and low sedimentation environments. |
D | High energy and high sedimentation environments. |
Question 70 |
A | spatial acceleration |
B | inertial acceleration |
C | temporal acceleration |
D | upwards acceleration |
E | gravitational acceleration |
Question 71 |
A | Between dunes |
B | At the mouth of rivers |
C | Lee side of ripples |
D | Within channels |
E | Stoss side of ripples |
Question 72 |
A | C |
B | A |
C | D |
D | E |
E | B |
Question 73 |
A | Liquified flow |
B | Debris flow |
C | Turbidity current |
D | Grain flow |
Question 74 |
A | A type of depositional environment that provides the best suitable conditions for organisms to thrive. |
B | A a body of rock with specified mineralogical characteristics. |
C | An assemblage of trace fossils that provides an indication of the palaeoenvironment. |
D | A type of trace fossils created by echinoids. |
E | A sub set of beds and laminations that is defined by certain depositional structures. |
Question 75 |
A | Long contacts |
B | Point contacts |
C | Subrounded contacts |
D | Concavo-convex contacts |
E | Sutured contacts |
Question 76 |
A | ~ 50 degrees |
B | ~ 30 degrees |
C | ~ 90 degrees |
D | ~ 100 degrees |
E | ~ 10 degrees |
Question 77 |
A | The rock is composed of highly angular clasts. |
B | The rock is dominated by matrix and has very few clasts. |
C | The rock is composed of just one clast type. |
D | The rock is composed of just two or three clast types. |
Question 78 |
A | Deltaic environment with high sediment influx. |
B | Deep subsurface environments under high pressures and temperatures. |
C | High energy environment with a one single direction of water flow. |
D | Glacial environment where clasts are dragged across a flat surface. |
Question 79 |
A | D |
B | F |
C | No such thing on the diagram above. |
D | E |
E | C |
Question 80 |
A | Base |
B | Base solutions in high temperature environment |
C | High pH solutions |
D | Acids |
E | Low pH solutions in high temperature solutions |
Question 81 |
A | Deeper in the fluid higher the velocity. |
B | At the top of a moving current, the velocity is close to zero. |
C | Deeper in the fluid lower the velocity. |
D | Uniformly moving fluids will have an equal instantaneous velocities regardless of depth. |
E | In the middle of the profile, the velocity is close to zero. |
Question 82 |
A | True |
B | False |
Question 83 |
A | turbulent velocity model |
B | laminar velocity model |
C | rough bed velocity model |
D | smooth current velocity model |
Question 84 |
A | chemical deposits |
B | evaporites |
C | carbonates |
D | ore deposits |
E | clastic deposits |
Question 85 |
A | True |
B | False |
Question 86 |
A | A |
B | B |
C | C |
Question 87 |
A | It is difficult to determine the velocity hence we heavily relies on speed of flowing rivers for analysis. |
B | The highest velocity is at the bed. |
C | At the bed, there is no slip conditions due to lower velocity. |
D | Velocity increases as the depth increases. |
Question 88 |
A | physical weathering |
B | denudation |
C | erosion |
D | chemical weathering |
Question 89 |
A | Feeding |
B | Grazing |
C | Resting |
D | Escape |
E | Dewlling |
F | Crawling |
Question 90 |
A | Minerals that primarily formed from organic materials. |
B | Minerals that are formed as a result of erosion due to chemical weathering. |
C | Minerals that formed as a result of magmatic processes that occurs under water. |
D | Minerals with very high densities resulting deposition at the bottom of a flow. |
E | Minerals that replaces (take others' place) other minerals during sedimentation. |
Question 91 |
A | a type of physical weathering caused by biogenic processes which result in breakdown of rocks/sediments. |
B | a type of chemical weathering caused by dissociation of water into H+ and OH- ions as a result of acidifying agent. |
C | a type of erosion caused by temperature and pressure change caused by exhumation of rocks/sediments. |
D | a type of chemical weathering caused by oxidation of chemical compounds within rocks. |
E | a type of physical weathering caused by water or hydrous fluids penetrate rocks/sediments and expand as a result of freezing; leads to cracks and physical breakdown of materials. |
Question 92 |
A | False |
B | True |
Question 93 |
A | A |
B | B |
C | C |
Question 94 |
A | Change in normality |
B | Change in flow regime |
C | Hydraulic jump |
D | Gradient change |
E | Critical flow |
Question 95 |
Description
-high velocity
-larger Reynold's number
-inertial forces dominates over the viscous forces
A | It could be either A or B because the description is is insufficient. |
B | Neither |
C | A |
D | B |
Question 96 |
A | Genology |
B | Ichnology |
C | Paleotracology Hint: LOL What the hell? |
D | Paleogeology |
Question 97 |
A | False |
B | True |
Antidunes can be formed as a result of beds deposition in phase to the surface water wave.
Question 98 |
A | Even though they have the similar names, they are unrelated each other because sediment is a geologic structure and sedimentary rock is a type of geologic material. |
B | Even though they have the similar names, they are unrelated each other because sedimentary rock is a geologic structure and sediment is a type of geologic material. |
C | Sedimentary rocks are unconsolidated materials that forms at the Earth's surface while sediments are formed as a result of burial and lithification of these sediment materials. |
D | Sediments are unconsolidated materials that forms at the Earth's surface while sedimentary rocks are formed as a result of burial and lithification of these sediment materials. |
Question 99 |
A | It transforms sediments into metamorphic rocks |
B | It transforms igneous rocks into sedimentary rocks |
C | It occurs under temperatures above 500 degree Celsius |
D | It transforms sedimentary rocks into metamorphic rocks |
E | It change the chemical and physical characteristics of sediments after the deposition |
Question 100 |
A | True |
B | False |
Question 101 |
A | Low velocity currents. |
B | Medium velocity currents. |
C | High velocity currents. |
D | Fluctuating velocity currents. |
Question 102 |
A | False because pedogenesis is the process of erosion by both physical and chemical weathering. |
B | True |
C | False because pedogenesis is the process of creating soil. |
D | False because pedogenesis is the process of creating rivers. |
Question 103 |
A | False |
B | True |
Question 104 |
A | dwelling |
B | fighting |
C | feeding |
D | crawling |
E | extractions(pooping) |
Question 105 |
A | Settling velocity of particles in a fluid. |
B | How flow rate, density of the fluid and pathway of flow dictates type of flows. |
C | Depositional sequences in very high energy environments. |
D | Flow of a fluid through a tapered tube results in an increase in velocity. |
← |
List |
→ |
1 | 2 | 3 | 4 | 5 |
6 | 7 | 8 | 9 | 10 |
11 | 12 | 13 | 14 | 15 |
16 | 17 | 18 | 19 | 20 |
21 | 22 | 23 | 24 | 25 |
26 | 27 | 28 | 29 | 30 |
31 | 32 | 33 | 34 | 35 |
36 | 37 | 38 | 39 | 40 |
41 | 42 | 43 | 44 | 45 |
46 | 47 | 48 | 49 | 50 |
51 | 52 | 53 | 54 | 55 |
56 | 57 | 58 | 59 | 60 |
61 | 62 | 63 | 64 | 65 |
66 | 67 | 68 | 69 | 70 |
71 | 72 | 73 | 74 | 75 |
76 | 77 | 78 | 79 | 80 |
81 | 82 | 83 | 84 | 85 |
86 | 87 | 88 | 89 | 90 |
91 | 92 | 93 | 94 | 95 |
96 | 97 | 98 | 99 | 100 |
101 | 102 | 103 | 104 | 105 |
End |
Credits: Based on the excellent class notes provided by, Dr. Melissa Giovanni during Fall 2012.
FAQ | Report an Error
Some of the Lab Midterm sample images | Click here
Concepts and Additional Questions for Fall 2012 Midterm I
Important!
↑ Some of these are already in the exam type questions in the quiz(above) ↑
Answers to these will NOT be posted. These are based on lecture notes!
-velocity profile; what is idealized modal’s limitations; where is the viscous sublayer and what is it
-bed formation; shape of the bed, x-beds, directional flows
-bed load vs suspended load
-Stoke’s law and the settling velocity
-flow separation concepts; eddy; stoss/lee with respect to x-beds in dunes and anti-dunes; water surface in or out of phase of bed formation
-unidirectional flow vs ocillating flow; be able to draw and describe the differences between them; wave base “feel my bottom”.
-type of sediment gravity flows; debris flow; grain flow; liquefied flow (remember that debris flow and liquefied flow are similar in operation, but different in terms of size of rocks/grains involved.
Dr. Spila’s stuff
-4 steps involving accurately identifying fossils; preservation, description, behaviour, classification(we don’t have to know how to name them)
-What is ichnology
-difference between biotrubation and bioerrosion; which is the most common type; what is the formula for degree of bioturbation
-what are borings and what are borrows
-6 major common categories of behaviours and their reliefs; crawling(semi), resting(semi), feeding(full), gazing(semi), dewlling(full), escape(full).
-meniscae and few other definitions
-preservation differences between full and semi-relief