Sedimentary Petrology
Go to: Final Exam
The following quiz assumes that you have the background knowledge from GLGY 491. For additional questions specific to organisms, please check Geology 491 materials. Most concepts related to 491 class has been omitted from this quiz.
Attention: Application questions
Please be aware that you may come across difficult questions. They are usually not directly from one particular lecture but rather application of principles form several different lectures and labs. In this particular class, you are expected to solve this type of questions for the lecture/lab midterms and the finals. It is not my intention to make this quiz questions hard like a jackass.
Geology (GLGY 461-UCAL) Midterm
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Question 1 |
A | Platform slopes |
B | Open-water mud mounds |
C | Shallow internal platform biostromes |
D | Open-water supertidal flats |
E | Outer platform margin biostromes |
Question 2 |
A | Phosphorites |
B | Siliciclastic mudstones |
C | Halites |
D | Siliciclastic sandstones |
E | Limestones |
F | Dolostones |
Question 3 |
A | A. colonial B. solitary |
B | A. aragonitic B. calcitic |
C | A. siliceous B. calcitic |
D | A. calcitic B. siliceous |
E | A. calcitic B. aragonitic |
Question 4 |
A | False, they were found in mounded laminae forms. |
B | False, they were found in laminae, pillars and astrorhizae forms. |
C | True |
Question 5 |
A | No, it is only the chemical formula for a mineral. |
B | Yes it is a mineral. |
C | No, it is neither a mineral nor a valid chemical formula. |
D | No, it is a synthetic material. |
Question 6 |
A | The process in which constituents were broken down during the burial to form new minerals in the sediment. |
B | The process in which constituents were combined to form metamorphic rocks. |
C | The process in which rocks were cooled down after a burial process to from new rocks. |
D | The process in which constituents were transported from the initial deposition location to a basin for burial. |
Question 7 |
A | Echinoderms |
B | Molluscs |
C | Brachiopods |
D | Foraminifera |
Question 8 |
A | Floatstones |
B | Bindstones |
C | Bafflestones |
D | Framestones |
E | Rudstones |
Question 9 |
A | Cross-lamellar |
B | Multiple chemical elements within growth lines |
C | Double-crystal system |
D | Foliation |
Question 10 |
A | Overlap of 1-st and 2-nd Order lamellae. |
B | Foliation grade differences during each growth cycle. |
C | Changes in chemical composition during each growth cycle. |
D | Longitudinal deformation due to stresses during sedimentation. |
E | Due to their orientation to the cut surface of the thin section. |
Question 11 |
A | Fascicular fibrous structures |
B | Single crystal structures |
C | Composite prismatic structures |
D | Foliated structures |
Question 12 |
A | False |
B | True |
Question 13 |
A | Pore/void space: the 2-st Order structures have less void space. |
B | Pattern of the cross; the 2-st Order structures V-shaped. |
C | Pore/void space: the 1-st Order structures have less void space. |
D | Pattern of the cross; the 1-st Order structures V-shaped. |
E | Shape and size; the 2-st Order structures are larger. |
F | Shape and size; the 1-st Order structures are larger. |
Question 14 |
A | Several layers of complex and composite prismatic structures. Hint: Nope; this is for molluscus ONLY. |
B | At least two layers of non-deformed single crystal structures. Hint: Nope; this is mostly for echinoderms. |
C | At lest two layers with 1-st and 2-nd Order aragonitic crossed-lamellar layers. Hint: Nope; this is for molluscus. |
D | Homogeneous prismatic structures with no deformation. Hint: Nope; this is mostly for forminifera and molluscs. |
E | Several layers of foliated or normal prismatic structures. |
Question 15 |
A | Change in the rate at which the burial of sediments occurs. |
B | Change in abundance of organisms in a macro-region. |
C | Change in abundance of chemicals. |
D | Change in abundance of organisms in a micro-region. |
E | Change in temperature and pressure. |
F | Change in temperature only. |
Question 16 |
A | Outer platform margin bioherms |
B | Platform slopes |
C | Supertidal flats |
D | Shallow internal platform biostromes |
E | Open-water mud mounds |
Question 17 |
A | It is often used for pleobilogical stratigraphic analysis. |
B | It is an ideal model of platform environment that will work for most areas of Earth. |
C | It dose not consider effects of sea level changes or climate controls. |
D | It was first published in 1975 by Wilson. |
Question 18 |
A | Depositional setting, sediment type, biota and common lithofacies. |
B | Common lithofacies and biological characteristics. |
C | Common lithofacies. |
D | Nature of the tidal flat, lagoonal faces, shallow ramp and deep shelf ramp. |
E | Variations in the global biological and lithological diversity. |
Question 19 |
A | I. Ahermatypic II. Hermatypic |
B | I. Hermatypic II. Ahermatypic |
C | I. Brain II. Hexacorallia Hint: Both are reef builders. |
D | I. Rugose II. Brain |
E | I. Hexacorallia II. Brain Hint: Both are reef builders. |
Question 20 |
A | Around 300 m |
B | Below 100 m |
C | Between 150 m and 200 m |
D | Between 200 m and 300 m |
E | Around 200 m |
Question 21 |
A | False; they are solitary organisms. |
B | True |
C | False; they are an extinct class of organisms. |
Question 22 |
A | Deep Tidal Flat Facies |
B | Deep Shelf Facies |
C | Lagoonal Facies |
D | Deep Basin Facies |
E | Shallow Ramp Facies |
Question 23 |
A | high energy deep tidal environments. |
B | low energy shallow tidal environments. |
C | low energy reef/ramp environments. |
D | high energy slope environments. |
Question 24 |
A | Biotic |
B | In-situ formation |
C | Reworked lithofied clasts |
D | Alteration of grains |
Question 25 |
A | Large pour spaces caused by entrapment of gaseous substance. |
B | Large volume of spherical/sub-spherical shaped peloids. |
C | Large volume of elongated peloids. |
D | Presence of destructive micritization. |
E | Presence of bio-chemicals and organic matter. |
Question 26 |
A | Presence of biotic peloids as opposed to other types. |
B | very high energy environment. |
C | high global biological activities due to abundance in nutrients. Hint: Think again; usually "abundance of peloidal rocks" found in specific areas in specific geologic time. |
D | high local biological activities due to abundance in nutrients. |
E | very low energy environment. |
Question 27 |
A | True |
B | False; because it is an indication of altered grains forming micritized peloids. |
C | False; because it is an indication of reworked lithofied clasts of carbonates origin. |
D | False; because it is an indication of in-situ formations. |
Question 28 |
A | cyanobacterial destruction. |
B | microborings. |
C | destructive micritization. |
D | constructive micritization. |
Question 29 |
A | Thin cortex very thin cortex and 2-4 counted layers. |
B | Ooids with very thick cortex. |
C | Thin cortex very thick cortex and innumerable layers. |
D | Thin cortex very thin cortex and 1-3 counted layers. |
E | Ooids with very thin cortex. |
Question 30 |
A | Bottom agitation, presence of nuclei and grain degradation. |
B | Presence of nuclei and supersaturated water with respect to calcite. |
C | Presence of nuclei and undersaturated water with respect to calcite. |
D | Usually have a nuclei. |
Question 31 |
A | at the trough of the dunes. |
B | at the peak of the crest (peak) of the dunes. |
C | at the asymmetric surfaces. |
D | at the points of flow convergence. |
E | along the troughs of parabolic bars. |
Question 32 |
A | Blue algae are adapted to deeper water environments and they absorbs blue light. |
B | Red algae are adapted to deeper water environments and they absorbs blue light. |
C | Green algae are adapted to shallow water environments and they absorbs yellow light. |
D | Green algae are adapted to deeper water environments and they absorbs red light. |
E | Red algae are adapted to deeper water environments and they absorbs red light. |
F | Green algae are adapted to deeper water environments and they absorbs blue light. |
G | Blue algae are adapted to deeper water environments and they absorbs red light. |
Question 33 |
A | ....exclusive to marine water environments. |
B | ...most abundant in shallow, protected environments. |
C | ...adapted to deep water environments. |
D | ...exclusive to fresh water environments. |
E | ...were exclusive to fresh water environments during Carboniferous and modern day they are exclusive to marine water environments. |
Question 34 |
A | All types (Green, Blue and Red) |
B | Green |
C | Blue |
D | Red |
Question 35 |
A | They can be in several depositional settings such as marine, fresh-brackish water ponds, tidal flats and shallow sandy bottoms. |
B | Some of them are capable of secreting or depositing carbonate around their body. |
C | They are important sediment produces and reef builders. |
D | This group includes both benthic and planktonic organisms that have the ability to photosynthesize. |
E | They are very important for economic resources such as diamond and gold ores. |
Question 36 |
A | Cynaophyta |
B | Chrysophyta |
C | Chlorophyta |
D | Rhodophyta |
Question 37 |
A | Blue algae |
B | Red algae |
C | Green algae |
D | Yellow algae |
Question 38 |
A | Open marines |
B | Open marine bay shelf lagoons |
C | Restricted marine bays and lagoons |
D | Reef fronts |
E | Tidal flats |
Question 39 |
A | I. spinal core II. external core |
B | I. cortex II. medulla |
C | I. central core II. outer core |
D | I. medulla II. cortex |
Question 40 |
A | Carboniferous |
B | Paleozoic |
C | Ediacaran |
D | Cretaceous |
E | Cenozoic |
Question 41 |
A | Sunlight and high energy water currents |
B | High energy water currents |
C | Sunlight and moisture |
D | Sunlight and availability of calcareous fluids |
E | Sunlight |
Question 42 |
A | CCD or carbon compensation depth is the depth in which the calcite start to become unstable. Hint: Nope; that would be Lysoclines |
B | The partial pressure of CO2 is very high at shallow depths; leads to good cementation. |
C | The best cementation processes occurs at shallow waters such as at the shelf or slopes. |
D | Large portion of the mixing zone is in the marine diagenetic area. |
E | Sediments could undergo marine diagenesis as long as water is present. |
Question 43 |
A | I. Yellow II. green |
B | I. Blue II. green |
C | I. Red II. green |
D | I. Green
II. red |
Question 44 |
A | zoecias. |
B | layering. |
C | pillars. |
D | lamination. |
E | alternating sediment-organic matter layers. |
Question 45 |
A | True |
B | False |
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Credits: Based on the excellent class notes provided by, Dr. Rudi Meyer during Winter 2014.
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