1.
At high wind velocities silt- and clay-sized particles are carried as bed load.
Correct Answer
B. False
Explanation
At high wind velocities, silt- and clay-sized particles are not carried as bed load. Instead, they are carried as suspended load. Bed load refers to larger particles that are transported by rolling, sliding, or bouncing along the bottom of a river or stream. Silt and clay particles, being smaller and lighter, can be easily lifted and transported in the air as suspended load by strong winds. Therefore, the statement is false.
2.
Grain roundness is therefore a characteristic that can easily be seen in hand specimen using a hand lens, or will be evident under the microscope if a thin-section is cut of an aeolian sandstone
Correct Answer
A. True
Explanation
The statement explains that grain roundness is a characteristic that can be observed easily in hand specimens using a hand lens or under a microscope when a thin-section is cut from an aeolian sandstone. This suggests that the statement is true.
3.
Calcium carbonate (CaCO3) is the principal compound in limestones.
Correct Answer
A. True
Explanation
Calcium carbonate (CaCO3) is indeed the principal compound found in limestones. Limestone is a sedimentary rock primarily composed of calcium carbonate, which is formed from the accumulation of shells, coral, and other marine organisms over millions of years. This compound gives limestone its characteristic hardness and is also responsible for its use in various industries, such as construction and agriculture. Therefore, the statement "Calcium carbonate (CaCO3) is the principal compound in limestones" is true.
4.
Cherts are fine-grained siliceous sedimentary rocks made up of silt-sized interlocking quartz crystals (microquartz) and chalcedony, a form of silica which is made up of radiating fibres a few tens to hundreds of microns long.
Correct Answer
A. True
Explanation
Cherts are indeed fine-grained siliceous sedimentary rocks composed of silt-sized interlocking quartz crystals and chalcedony. Chalcedony is a type of silica that consists of radiating fibers. Therefore, the statement is true.
5.
Sediments and sedimentary rocks with a high proportion of organic matter are termed carbonates because they are rich in carbon.
Correct Answer
B. False
Explanation
The statement is false because sediments and sedimentary rocks with a high proportion of organic matter are actually termed as carbonaceous rocks, not carbonates. Carbonates are sedimentary rocks that are primarily composed of carbonate minerals such as calcite or dolomite.
6.
If all the clasts are of the same material (all of granite, for example), the conglomerate is considered to be polymict
Correct Answer
B. False
Explanation
If all the clasts in a conglomerate are of the same material, it is considered to be monomict, not polymict. Polymict conglomerates contain clasts of different materials. Therefore, the correct answer is false.
7.
Silt is a textural term to define the finest grade of clastic sedimentary particles, those less than 4 microns in diameter.
Correct Answer
B. False
Explanation
Silt is not defined as the finest grade of clastic sedimentary particles less than 4 microns in diameter. Silt is actually defined as particles ranging from 0.002 to 0.06 mm in diameter. Therefore, the statement is false.
8.
When clay- and silt-sized particles are mixed in unknown proportions as the main constituents in unconsolidated sediment we would call this material shale.
Correct Answer
B. False
Explanation
The statement is false because when clay- and silt-sized particles are mixed in unknown proportions as the main constituents in unconsolidated sediment, the material formed is not shale. Shale is a type of sedimentary rock that is formed from the compaction and cementation of fine-grained clay and silt particles over time. In this case, the material is still in its unconsolidated state and has not undergone the processes necessary to become shale.
9.
Feldspar is the most common mineral seen in silt deposits
Correct Answer
B. False
Explanation
The statement that feldspar is the most common mineral seen in silt deposits is false. While feldspar is a common mineral, it is not the most common one found in silt deposits. Silt deposits typically contain a mixture of minerals, including quartz, clay minerals, and various other minerals. Therefore, the correct answer is false.
10.
Montmorillonite minerals can not absorb water within their structure.
Correct Answer
B. False
Explanation
Montmorillonite minerals can absorb water within their structure. This is because they have a layered structure with a high surface area and a negative charge that attracts water molecules. This property allows them to swell and retain water, making them useful in various applications such as in drilling fluids, soil amendments, and as a component in cosmetics and pharmaceuticals.
11.
A well sorted deposit contains a wide range of clast sizes.
Correct Answer
B. False
Explanation
A well sorted deposit contains clasts that are similar in size, rather than a wide range of sizes.
12.
Fabric- If a rock has a tendency to break in a certain direction, or shows a strong alignment of elongate clasts, this is described as the fabric of the rock.
Correct Answer
A. True
Explanation
The explanation for the given correct answer is that fabric in a rock refers to the arrangement and alignment of its constituent particles or minerals. If a rock has a tendency to break in a specific direction or shows a strong alignment of elongate clasts (fragments), it indicates a distinct fabric. Therefore, the statement that describes this characteristic of rocks as fabric is true.
13.
Cement - Fine-grained material occurring between the sand grains
Correct Answer
B. False
Explanation
The statement "Cement - Fine-grained material occurring between the sand grains" is incorrect. Cement is actually a binder material used in construction that hardens and binds other materials together. It is not a fine-grained material occurring between sand grains.
14.
Shale refers to a rock formed from:
Correct Answer
C. Clay minerals
Explanation
Shale is a type of rock that is formed from the accumulation and compaction of clay minerals. Clay minerals are fine-grained particles that are derived from the weathering and erosion of other rocks. Over time, these clay particles settle and become compacted, forming shale. This process usually takes place in areas with calm water, such as lakes or deep ocean basins, where the clay particles can settle and accumulate. Therefore, the correct answer is clay minerals.
15.
A clastic rock is:
Correct Answer
C. A rock formed from the cementation of transported grains
Explanation
The correct answer is "A rock formed from the cementation of transported grains." Clastic rocks are formed from the accumulation and cementation of rock fragments, mineral grains, or organic material that have been transported and deposited by wind, water, or ice. These transported grains are then compacted and cemented together to form clastic rocks.
16.
Which one of the following features is NOT associated with sedimentary rocks?
Correct Answer
D. All may be associated with sedimentary rocks
Explanation
Sedimentary rocks are formed from the accumulation and solidification of sediment, which can contain various features. Bedding is a characteristic feature of sedimentary rocks, as it refers to the distinct layers that form as sediments settle over time. Fossils are also commonly found in sedimentary rocks, as they are the preserved remains or traces of ancient organisms. However, foliation is not associated with sedimentary rocks. Foliation is a feature commonly found in metamorphic rocks, where minerals are aligned in parallel layers or bands due to intense pressure and heat.
17.
Which of the following types of sediments are most abundant?
Correct Answer
B. Fine clastics
Explanation
Fine clastics are the most abundant type of sediments. This is because they are composed of smaller particles, such as silt and clay, which are easily transported by wind or water and can be deposited over large areas. In contrast, coarse clastics, which include larger particles like sand and gravel, are less abundant because they require higher energy environments to be transported and deposited. Chemical and biochemical sediments, which are formed through precipitation or the accumulation of organic remains, respectively, are also less abundant compared to fine clastics.
18.
The tendency for variations in current velocity to segregate sediments on the basis of particle size is called _____.
Correct Answer
B. Sorting
Explanation
Sorting refers to the process by which sediments are separated and arranged based on their particle size. As currents vary in velocity, they have the ability to transport and deposit sediments of different sizes. This leads to the segregation of sediments, with larger particles being deposited closer to the source and smaller particles being carried further away. Therefore, the correct answer is sorting.
19.
Which of the following types of currents can transport sand grains?
Correct Answer
D. All above
Explanation
All three types of currents mentioned in the options - rivers, ocean waves, and wind - have the ability to transport sand grains. Rivers carry sediment, including sand, downstream, and deposit them in other areas. Ocean waves can pick up sand grains from the shore and move them along the coast. Wind can also transport sand grains, causing erosion and deposition in different locations. Therefore, all of the above currents can transport sand grains.
20.
Which of the following processes is not an important cause of subsidence during the development of a sedimentary basin?
Correct Answer
D. Erosion of sediments
Explanation
Erosion of sediments is not an important cause of subsidence during the development of a sedimentary basin. Subsidence occurs when the Earth's crust sinks or settles, and it is primarily caused by processes such as deposition of sediments, cooling and contraction of the crust, and tectonic down faulting. These processes can lead to the accumulation of sediments, the shrinking of the crust due to cooling, and the movement of rocks along fault lines, which result in subsidence. However, erosion of sediments involves the removal or wearing away of sedimentary material, which does not contribute to the sinking or settling of the crust.
21.
Mudrocks that contain a high proportion of organic material that can be driven off as a liquid or gas by heating are called oil shales.
Correct Answer
A. True
Explanation
Mudrocks that contain a high proportion of organic material can indeed be driven off as a liquid or gas by heating, and these rocks are commonly known as oil shales. This process, known as pyrolysis, involves heating the organic material to high temperatures, causing it to break down and release hydrocarbons. Oil shales are an important source of unconventional oil and gas resources and can be found in various parts of the world. Therefore, the statement "Mudrocks that contain a high proportion of organic material that can be driven off as a liquid or gas by heating are called oil shales" is true.
22.
The presence of the oil in the pores of the sediment prevents the formation of any cement, so tar sands remain lithified, held together only by the bitumen that gives them a black or very dark brown colour.
Correct Answer
B. False
Explanation
The explanation for the answer being False is that the presence of oil in the pores of the sediment does not prevent the formation of cement. In fact, the oil can act as a cementing agent itself, helping to hold the sediment together. Therefore, tar sands can be lithified not just by bitumen, but also by the cementation of the sediment.
23.
If over one-thirds of a rock is solid organic matter it may be called a coal
Correct Answer
B. False
Explanation
The statement suggests that if over one-thirds of a rock is solid organic matter, it may be called coal. However, this is not true. Coal is a specific type of rock that is formed from the remains of plants that have been compacted and heated over millions of years. While coal does contain organic matter, it is not simply any rock with organic matter. Therefore, the correct answer is false.
24.
Evaporite - These are minerals formed by precipitation out of solution as ions become more concentrated when water evaporates.
Correct Answer
A. True
Explanation
Evaporite minerals are indeed formed through a process called precipitation, which occurs when water evaporates and the dissolved ions in the water become more concentrated. As the water evaporates, the ions come together and form solid mineral deposits. Therefore, the statement that evaporite minerals are formed by precipitation out of solution as ions become more concentrated when water evaporates is true.
25.
Authigenic minerals - Minerals that grow as crystals in a depositional environment are called authigenic minerals.
Correct Answer
A. True
Explanation
Authigenic minerals are indeed minerals that form and grow as crystals in a depositional environment. These minerals are not transported from elsewhere but are instead formed in situ. This process occurs when certain conditions in the environment, such as changes in temperature, pressure, or chemical composition, promote the precipitation and growth of minerals. Therefore, the statement that authigenic minerals are minerals that grow as crystals in a depositional environment is correct.
26.
The term arenite, which is a sandstone with more than 15% matrix.
Correct Answer
B. False
Explanation
The statement is false because arenite refers to a sandstone with less than 15% matrix, not more than.
27.
Clast spherericity - A progressive rounding of the edges occurs with prolonged agitation of the sediment and hence the roundness is a function of the transport history of the material.
Correct Answer
B. False
Explanation
The statement suggests that clast sphericity increases with prolonged agitation of the sediment, which is false. In reality, clast sphericity is a function of the transport history of the material, not prolonged agitation. The roundness of the clasts is determined by the processes they have undergone during transportation, not how long they have been agitated.
28.
In sedimentary rocks, the fabric developed depends on the depositional environment and can provide information on current directions at the time of deposition
Correct Answer
A. True
Explanation
The statement is true because sedimentary rocks are formed from the accumulation of sediments that are deposited in various environments such as rivers, lakes, oceans, and deserts. The fabric or texture of these rocks is influenced by the specific conditions of the depositional environment, including factors like water currents, waves, and wind. By examining the fabric of sedimentary rocks, geologists can gather valuable information about the direction of currents at the time of deposition, which can help in understanding past environmental conditions and processes.
29.
The subsoil is the region of most intense biological activity: insects, worms, and other animals burrow through it and plants stretch their roots down into it.
Correct Answer
B. False
Explanation
The given statement is false. The subsoil is not the region of most intense biological activity. It is the topsoil that supports the majority of biological activity, including insects, worms, and plant roots. The subsoil, located beneath the topsoil, is generally less fertile and contains fewer organic materials, limiting its ability to support extensive biological activity.
30.
Chemical weathering is most likely to take place in environments that are:
Correct Answer
B. Wet
Explanation
Chemical weathering is most likely to take place in wet environments because water is a key component in many chemical reactions that break down rocks and minerals. Water can dissolve minerals, react with certain rock types, and facilitate the growth of organisms that contribute to weathering processes. In wet environments, there is a higher availability of water, which increases the likelihood of chemical weathering occurring. Cold and dry environments may still experience some form of weathering, but the presence of water is crucial for the chemical reactions involved in the process.