The correct answer is B) arrangement of minerals in a rock. Composition is the term used to describe the arrangement of minerals in a rock, specifically the relative abundance of different minerals.
A rock can be composed of a single mineral, or a combination of minerals. The composition of a rock can be determined by looking at the physical properties of the rock, such as its color, grain size, and mineral composition. A rock's composition can also be determined by laboratory testing.
When a rock is composed of several minerals, the minerals can be arranged in several different ways. The arrangement of minerals in a rock can be grouped into three main types: homogeneous, polymict, and monomict.
Homogeneous rocks are composed of a single mineral, while polymict and monomict rocks are composed of several different minerals. Polymict rocks have a random arrangement of minerals, while monomict rocks have a uniform arrangement.
The degree of compaction and cementation of a rock will affect the arrangement of minerals in a rock. Compaction refers to the process by which a rock is compacted by pressure and cementation refers to the process by which the minerals within the rock are bound together. Both of these processes can affect the arrangement of minerals in a rock.
In conclusion, composition is the term used to describe the arrangement of minerals in a rock. A rock can be composed of a single mineral, or a combination of minerals.
The arrangement of minerals in a rock can be grouped into three main types: homogeneous, polymict, and monomict. The degree of compaction and cementation of a rock will affect the arrangement of minerals in a rock.
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Of the following solutions, which has the greatest buffering capacity? Explain. A) They would all have the same buffer capacity. B) 0.821 M HF and 0.217 M NaF C) 0.100 M HF and 0.217 M NaF D) 0.821 M HF and 0.909 M NaF E) 0.121 M HF and 0.667 M NaF
We know the formula β = (d[A-] / dpH) / [HA] by using this formula we can say that option B has the highest buffer.
A) 0.821 M HF and 0.217 M NaF
pH = pKa + log([A-]/[HA])
pH = 3.17 + log(0.217/0.821) = 2.54
β = 0.0025
B) 0.821 M HF and 0.909 M NaF
pH = 3.17 + log(0.909/0.821) = 3.27
β = 0.0036
C) 0.100 M HF and 0.217 M NaF
pH = 3.17 + log(0.217/0.100) = 3.67
β = 0.0022
D) 0.121 M HF and 0.667 M NaF
pH = 3.17 + log(0.667/0.121) = 4.15
β = 0.0022
thus, we can see that option B has the highest buffer capacity coefficient and also would have the highest buffering capacity.
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Consider an air parcel that initially features a northward trajectory from the equator towards the North Pole. How will the Coriolis force act on this air parcel once it starts moving? The parcel's trajectory will veer towards the west The parcel's trajectory will veer towards the east The parcel's trajectory will continue north The parcel's trajectory will reverse and move south
The Coriolis force act on this air parcel once it starts moving the parcel's trajectory will veer towards the east. So the option B is correct.
Once this air parcel begins to move, the Coriolis force will begin to act on it, causing the air parcel's trajectory to veer towards the east. This is because the Coriolis force is a force that acts perpendicular to the direction of motion and the rotation of the Earth. This force causes the parcel to move in a curved path rather than a straight line. The curved path results in the air parcel veering towards the east. So the option B is correct.
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Place the following transportation types in the order in which they became common (oldest on the top, newest on the bottom) Automobiles, Horses, Canals, Steamships, & Railways
"The following transportation types are in the order in which they became common (oldest on the top, newest on the bottom)- Horses, Railways, Steamships, Canals & Automobiles."
The Industrial Revolution substituted human or animal muscle power(mostly horses). The newly invent-ed machines, powered by burn-ing wood or coal, or by the flow-ing water of a stream or river, could accomp-lish the same amount of work that previous-ly required several people or sev-eral animals flexing their muscles.
Not only could the ma-chines do the work of several living be-ings, machines could do it at a mu-ch faster speed. Imagine substi-tuting a horse for the motor of a car; one or two horses co-uld easily pull the wei-ght of a car with its pass-engers, but no horse could run do-wn the high-way at sixty miles an hour, h-our after hour, as a car can.
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In weighing the benefits cities derive from gentrification against the social and human costs, where do you think the balance lies?
Match the image showing different types of continental accommodation of crustal extensionwith the best descriptions of events.
Normal faults divide the crust into wedge-shaped chunks by dipping in opposite directions. On the dropped blocks, fault movement creates basins, and on the upthrown blocks, mountains. Nonrotating fault blocks only experience minor extensions.
A fault is a fracture or a region of fractures that exists between two rock blocks. The blocks are capable of relative movement due to faults. This movement may take the shape of an earthquake if it happens quickly, or it may take the form of creep if it happens slowly. A few millimetres to thousands of kilometres may make up a fault. During geologic time, the majority of faults result in repeated displacements. In the event of an earthquake, the rock on one side of the fault abruptly shifts in relation to the other. The fault surface might be at any angle between vertical and horizontal.
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Dry climates are divided into two types according to moisture. These are A) deserts and tundra. B) deserts and steppe. C) chaparral and tundra. D) steppe and chaparral.
Dry climates are divided into two types according to moisture. These are deserts and steppe
What are dry climates?
Dry climates are defined as areas where the weather is usually dry and there is little precipitation. Dry climates are usually characterized by limited rainfall and high temperatures. According to moisture, dry climates are divided into two types: deserts and steppe.
Here are some characteristics of each:Deserts: The arid desert is the driest of all the climates. They usually get less than ten inches of rain per year. Deserts are classified as having extremely low moisture levels.
There are a few different kinds of deserts, including hot and dry, semiarid, coastal, and cold.Steppe: This climate is known for its grassy, open plains. It receives more rain than the desert but less than the humid areas. There are two kinds of steppe climates: cold and semiarid.
There is enough rainfall in these areas to support grass and scrub, but not enough to support forests. Chaparral and tundra are not dry climates, as they both receive adequate rainfall for their specific vegetation. Hence, the correct option is B) deserts and steppe.
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How is a person's unknown location determined using the location of 3 known points? A. By calculating the ephemeris B. By determining the pseudorange C. By implementing 3D equilateration D. By using the 2D trilateration process
Using the location of 3 known points the unknown location of a person is determined by applying a 3D equilibration. Here option C is the correct answer.
The process of determining a person's unknown location using the location of three known points is known as trilateration. Trilateration is a mathematical process that involves measuring the distance between the unknown point and each of the known points and then using these measurements to calculate the unknown point's location.
Trilateration can be performed in both two-dimensional (2D) and three-dimensional (3D) space. In 2D trilateration, the known points and the unknown point all lie on a flat surface, such as a map, while in 3D trilateration, the points are located in three-dimensional space.
To perform trilateration, the distance between the unknown point and each of the known points must be accurately measured. This can be done using techniques such as GPS (Global Positioning System), where the distance is determined by measuring the pseudo-range between the unknown point and each known point. Once the distances have been determined, the unknown point's location can be calculated using 3D equilibration, which involves solving a system of equations that relates the distances between the points to their respective coordinates.
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in order to be classified as a hurricane, a tropical storm must reach what sustained wind speeds?
As per the Saffir-Simpson Hurricane Wind Scale, a tropical storm must reach sustained wind speeds of at least 74 miles per hour (mph) in order to be classified as a hurricane.
A hurricane is a violent storm that develops in the tropics or subtropics of the Atlantic Ocean, Caribbean Sea, or Gulf of Mexico. They are characterized by strong winds, heavy rainfall, and storm surges that can cause significant damage to coastal regions.
A tropical storm is a type of low-pressure system that develops in the tropics or subtropics and is characterized by thunderstorms and strong winds ranging from 39 to 73 miles per hour. It can cause damage to buildings, power lines, and trees, as well as flooding from heavy rain.Tropical storms are named when they develop sustained wind speeds of at least 39 mph. When they reach sustained wind speeds of 74 mph, they are classified as hurricanes.
Hurricanes are classified into categories based on their sustained wind speeds, with Category 1 being the weakest and Category 5 being the strongest. The Saffir-Simpson Hurricane Wind Scale, which was developed in 1971, is used to categorize hurricanes.
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Subtropical high-pressure system in the Atlantic
The western side of subtropical high pressure cells
a) corresponds with Earth's major desert regions.
b) remains in the same position all year; i.e., they do not migrate with the high Sun.
c) has strong subsidence resulting in dry, semi-arid and arid surface conditions.
d) produces surface winds that pass over warm ocean currents.
e) tends to be cool and moist.
Subtropical high-pressure system in the Atlantic. The western side of subtropical high pressure cells has strong subsidence resulting in dry, semi-arid and arid surface conditions. Option C is the correct answer
Subtropical high-pressure systems are those that are formed in a stable area of the atmosphere around 30 degrees north and south of the equator. The western side of these cells is arid, semi-arid, or arid because of the strong subsidence it undergoes due to the descending air in this zone.
Subtropical high-pressure systems are those that are formed in a stable area of the atmosphere around 30 degrees north and south of the equator. As the atmosphere rises at the equator, it cools and then sinks towards the poles, forming a high-pressure zone in the subtropical regions as the atmosphere warms up.
These zones are usually characterized by stable atmospheric conditions and clear skies, resulting in a lack of moisture in the area. Hence, these zones are associated with arid, semi-arid, or arid conditions.
Subtropical high-pressure systems' western sides are characterized by arid, semi-arid, or arid conditions, according to the above explanation. Therefore, option C is correct.
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The correct option among all the options given in the question is the third option, that is c) has strong subsidence resulting in dry, semi-arid and arid surface conditions.
Subtropical high-pressure system in the Atlantic is a region of high atmospheric pressure situated close to the latitudes of the Tropics. These high-pressure systems occur in a belt that stretches around the world from latitudes of about 20° to 40° north and south of the equator. The western side of subtropical high pressure cells have strong subsidence resulting in dry, semi-arid and arid surface conditions.
In these regions, most of the year is hot and dry. However, in certain locations, there can be enough moisture to support either a desert or a savanna-like environment. For example, the subtropical high-pressure system on the eastern side of the Andes Mountains of South America produces deserts, whereas the one on the western side produces moisture as the trade winds ascend the mountains and create rain clouds.
Apart from the third option, other options are also associated with subtropical high-pressure cells in the Atlantic. The first option states that it corresponds with Earth's major desert regions, which is partly true. The second option that is b) remains in the same position all year; i.e., they do not migrate with the high Sun, is not correct. The position of high-pressure cells shifts with the Sun. The fourth option is d) produces surface winds that pass over warm ocean currents, which is also true. And the last option is e) tends to be cool and moist, which is not correct.
So, the correct option is c) has strong subsidence resulting in dry, semi-arid and arid surface conditions.
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considering how magma composition, temperature, water content, and volatile content affect its viscosity, associate each of the volcanoes described in this activity with the type of eruption it should produce, or indicate whether the described characteristic is not related to eruption style. drag the appropriate items into their respective bins.
To answer this question, first we need to understand the factors that affect a volcano's eruption type. These factors are magma composition, temperature, water content, and volatile content. Based on these factors, we can associate each volcano with the type of eruption it should produce or indicate whether the described characteristic is not related to eruption style.
Volcano Magma Composition Temperature Water Content Volatile Content Eruption Type
A Felsic High Low High Explosive
B Intermediate High Moderate Moderate Explosive
C Mafic Low High Low Effusive
D Felsic High High High Explosive
As seen in the table above, we can associate each volcano with the type of eruption it should produce or indicate whether the described characteristic is not related to eruption style.
Volcano A has felsic magma composition, high temperature, low water content, and high volatile content. This combination of factors indicates that Volcano A should produce an explosive eruption.
Volcano B has intermediate magma composition, high temperature, moderate water content, and moderate volatile content. This combination of factors indicates that Volcano B should also produce an explosive eruption.
Volcano C has mafic magma composition, low temperature, high water content, and low volatile content. This combination of factors indicates that Volcano C should produce an effusive eruption.
Volcano D has felsic magma composition, high temperature, high water content, and high volatile content. This combination of factors indicates that Volcano D should also produce an explosive eruption.
Therefore, we can say that magma composition, temperature, water content, and volatile content are all important factors that determine a volcano's eruption type.
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1 ptWhile it is impossible to predict an earthquake, they typically occur neartectonic plate boundariesfault linesboth a and b
Answer:
Earthquakes typically occur near tectonic plate boundaries, which are regions where two or more tectonic plates meet. As the plates move and interact with each other, they can create stress and strain on the surrounding rocks, which can eventually lead to an earthquake. Therefore, the statement "earthquakes typically occur near tectonic plate boundaries" is correct. The term "fault lines" refers to the fractures or breaks in the earth's crust along which movement can occur during an earthquake. Fault lines often coincide with tectonic plate boundaries, but not all tectonic plate boundaries have visible fault lines. So, statement "a" is also correct, but statement "b" is not always true.
Explanation:
What types of weathering contribute to the lead problem in Picher, Oklahoma? a. Frost wedging b. Biological c. Dissolution d. All of the above.
Option A : Frost wedging.The types of weathering that contribute to the lead problem in Picher, Oklahoma are Frost wedging.
The Picher area of Oklahoma was a mining region for lead, zinc, and other minerals in the early 1900s. The extensive mining operations resulted in a lead-enriched atmosphere that resulted in a soil cover of up to 40 feet in some areas.
Mechanical or physical weathering: Mechanical or physical weathering is the process of breaking rock into smaller pieces without changing the rock's chemical composition. Frost wedging, exfoliation, thermal expansion, and root wedging are all examples of mechanical or physical weathering.
Chemical Weathering: The process of breaking down rock by chemical reactions is known as chemical weathering. The chemical reaction between acid rain and limestone, for example, causes chemical weathering.
Biological weathering: Biological weathering, which is caused by plants and animals, is the process of breaking down rock into smaller pieces. Plant roots, for example, can break through rock as they expand, causing the rock to break down over time.Thus the correct option is A.
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The movement of water and sediments toward the shore is called ______ current and transport, whereas the resulting movement of water and sediments parallel to the shore is called ______ current and transport.
onshore contemporary - movement of water parallel to shore. onshore transport - motion of sediment parallel to shore.
What is the movement of sand parallel to the shore?This is called a longshore present day due to the fact it flows along the shore, parallel to the beach. Sometimes the waves make currents that waft perpendicular to the beach or cross-shore. These are referred to as undertow and rip currents.
Which of the following shoreline administration constructions are parallel to the shoreline?Seawalls and rock revetments run parallel to the beach. Seawalls are vertical structures, built parallel to the ocean shoreline, and are mainly designed to prevent erosion and other injury due to wave action.
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which type of aggregates (igneous, sedimentary, or metamorphic) would you expect to be most suitable as a base-course material?
For a base-course material, the type of aggregate that would be the most suitable is sedimentary aggregate. This is due to its structure, which makes it stable, durable, affordable and easy to compact.
When it comes to aggregate materials, there are three main types: igneous, sedimentary, and metamorphic.
Igneous aggregates are formed from volcanic material that has been solidified. These materials are hard and durable, making them ideal for high-strength concrete and asphalt. They are also useful in railroad ballasts, building materials, and as fill for large voids in construction projects.
Sedimentary aggregates are formed from the erosion of pre-existing rock layers. This type of aggregate is the most commonly used in construction. It's known for its durability, low cost, and easy availability. Sedimentary aggregates include materials like gravel, sand, and limestone.
Metamorphic aggregates are formed by the transformation of pre-existing rocks through heat and pressure. They are the hardest and most durable. Marble, slate, and quartzite are examples of metamorphic aggregates. They are mostly used in high-strength concrete, railroad ballasts, and as fill for large voids in construction projects.
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what affects climate how climate affects living organisms how does weather change in different areas
The climate is influenced by temperature, where climate change will affect changes in the habitat of living things, and changes in the weather depending on the geographical location of an area.
The climate is affected by several factors, some of which are natural and others of which are human-made. Changes in solar radiation, Earth's orbit, and volcanic activity all contribute to the Earth's changing climate. Climate change caused by human activities, such as greenhouse gas emissions from burning fossil fuels, is the most significant driver of current climate change.
Climate change has a significant effect on living organisms. It may cause habitat destruction, changes in food chains, and changes in the timing of biological events like flowering and migration. Climate change is a significant contributor to the decline of biodiversity around the world, as well as the spread of infectious diseases like Lyme disease and West Nile virus.
Weather varies greatly depending on the location. It can be influenced by a variety of factors, including altitude, latitude, and proximity to water bodies. For example, coastal regions tend to have milder climates due to the moderating effect of the ocean, while areas farther inland tend to have more extreme temperature fluctuations. Mountainous regions experience rapid temperature changes as the altitude rises. The amount of precipitation also varies greatly depending on the area's climate.
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places where tectonic plates come together are called
Answer:
it is called convergent boundary.
What is most likely the result of an increase in trade between countries?
A goods and services would become more expensive
B
Highlight
C
D
economic activity would increase
economic activity would decline
both countries would be worse off than before the increase
Answer:
What is most likely the result of an increase in trade between countries?
A goods and services would become more expensive
B
Highlight
C
D
economic activity would increase
economic activity would decline
both countries would be worse off than before the increase
Explanation:
The most likely result of an increase in trade between countries is that economic activity would increase. When countries engage in trade, they can specialize in producing the goods and services that they have a comparative advantage in, and then trade them with other countries for goods and services that they are less efficient in producing. This specialization leads to increased efficiency, productivity, and output, which in turn spurs economic growth and creates more job opportunities. Therefore, increased trade is generally seen as a positive development that can benefit both countries involved by expanding their markets and creating new opportunities for economic activity.
If you can, give me brainliest please!
Please someone explain how to do this
Answer:
i just need pnts
explanation:
im sorry
Match the time period within the Paleozoic Era with examples of the forms of life that existed on Earth.
Early Paleozoic
An explosion of life with hard parts occurred.
Middle Paleozoic
Fish became abundant and diverse in the ocean.
Late Paleozoic
Amphibians and reptiles evolved on land.
The Paleozoic Era was a time of great evolutionary change on Earth. During the Early Paleozoic, there was an explosion of life with hard parts, such as trilobites and brachiopods.
This period also saw the evolution of primitive plants and the colonization of land by arthropods. In the Middle Paleozoic, fish became abundant and diverse in the ocean, with the evolution of sharks and bony fish.
The Late Paleozoic saw the evolution of amphibians and reptiles on land, which led to the development of more complex ecosystems on land. This period also saw the evolution of the first winged insects.
The Paleozoic Era was a period of great change and diversity in the history of life on Earth, and the forms of life that existed during this time have shaped the world we live in today.
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Compared to non-fractured rocks, the rate of weathering in fractured rocks of the same composition is:a) faster
b) slower
c) roughly the same
Compared to non-fractured rocks, the rate of weathering in fractured rocks of the same composition is: a) faster. Fractures can increase the rate of weathering due to increased surface area available for chemical reactions.
For example, when water enters into a fracture, it can react with the minerals in the rock and cause weathering to take place more quickly. Furthermore, fractures can provide pathways for water to reach deeply buried rocks, which can increase the rate of weathering.
On the other hand, fractures can also reduce the rate of weathering if the fracture is filled with sediment or if the fracture is in a place that is not easily exposed to water or other weathering agents. Thus, the rate of weathering in fractured rocks of the same composition depends on the individual characteristics of the fractures and the environment they are in.
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Of the following physical changes that occur to waves as they move into shallow water, which is/are true?a. Wavelength decreases.b. Wave height increases.c. Wave steepness increases.d. The waves touch bottom.
All of the statements are true. As waves move into shallow water, the wavelength decreases because the wave speed decreases due to the increased resistance from the sea floor.
This decrease in wavelength causes the wave height to increase as the wave energy is conserved. The increased wave height results in an increased wave steepness, which is the ratio of wave height to wave length.
Furthermore, when the wave height exceeds the water depth, the waves start to touch the bottom of the sea floor and can cause erosion. All of these physical changes to waves as they move into shallow water are caused by the decrease in water depth, which increases the resistance in the water and decreases the wave speed.
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the distinctive vertical joints seen in this basalt flow most likely formed as a consequence of which of the following?
The distinctive vertical joints seen in this basalt flow most likely formed as a consequence of thermal contraction. Thermal contraction occurs when hot molten rock cools and contracts upon cooling. As the rock cools, fractures form which create the vertical joints seen in the basalt flow.
Thermal contraction is common in basalt flows and can result in a variety of joint types, depending on the rate of cooling. As the molten rock cools, it contracts and fractures, resulting in a network of vertical and horizontal fractures, which can range in size from millimeters to centimeters. As the rock cools further, these fractures can become more pronounced, resulting in distinct vertical columns of rock.
The rate of cooling of the molten rock is a major factor in determining the size and pattern of the vertical joints in the basalt flow. If the molten rock cools quickly, it contracts more rapidly and thus more fractures form, creating a more pronounced pattern of vertical joints.
Conversely, if the molten rock cools slowly, the contraction is slower and less fractures form, resulting in a less pronounced pattern of vertical joints.
The cooling of the molten rock is also affected by the type of environment it is exposed to. Basalt flows in a temperate environment will cool at a slower rate than those exposed to a colder environment, thus producing a different pattern of vertical joints.
In conclusion, the distinctive vertical joints seen in this basalt flow most likely formed as a consequence of thermal contraction. The size and pattern of the joints is affected by the rate of cooling of the molten rock, as well as the type of environment it is exposed to.
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what is carbon dioxide and what causes it to be released into the atmosphere, contributing to global warming?
Answer:
CO2 is a greenhouse gas.
Explanation:
Right now, humans are the main cause of CO2 emissions. CO2 comes from burning fossil fuels primarily such as when we run our cars or in power plants.
four strategies to reduce the impact of human activities on catchment areas
One of the key needs is water designation change. In the Breede WMA, specific catchment management drivers call for a change in how water is allocated.
What strategies for catchment management are there?The yields and environmental impacts of these new water supply schemes are likely to be negligible in comparison to those of the larger regional schemes when viewed separately. However, an increasing number of small water supply schemes are being developed. The Mitchell's Pass Diversion Scheme in the Upper Breede and further augmentation of Steenbras Dam from the Palmiet River in the Western Overberg have been identified as potential water augmentation options for the Berg WMA. Since towns in the upper reaches of catchments discharge treated effluent into the river and towns downstream abstract water from the river, treat it, and supply it as potable water, many water supply projects in the WMA actually fall under the category of unplanned indirect potable re-use.
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what is the approximate frequency of interglacial periods? question 1 options: every 10,000 years every 50,000 years every 100,000 years every 150,000 years
The approximate frequency of interglacial periods is every 100,000 years. Option C
What is An interglacial period?An interglacial period is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age.
This is based on the pattern of glacial cycles that have occurred over the past million years, which show a roughly 100,000-year periodicity between periods of glaciation and interglacial. These cycles are believed to be driven by variations in Earth's orbit and axial tilt, which affect the amount and distribution of solar radiation received by different regions of the planet.
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what is the name of the depression formed after a volcanic eruption?
Answer:
Explanation:
The depression formed after a volcanic eruption is typically called a "caldera." A caldera is a large, basin-shaped depression that forms when a volcano collapses into itself following a massive eruption or series of eruptions. The collapse occurs when the magma chamber beneath the volcano is emptied, causing the overlying rock to lose support and sink downward. Calderas can range in size from just a few kilometres across to many tens of kilometres, and they are often surrounded by steep cliffs or walls that rise several hundred meters above the floor of the depression.
which of the following is a reliable characteristic that can be used to classify a rock? group of answer choices mineral stability texture water content degree of weathering
The most reliable characteristic that can be used to classify a rock is mineral stability. Mineral stability is the amount of chemical and physical resistance that minerals have when exposed to environmental conditions such as temperature, pressure, and chemical interactions.
The characteristic that can be used to classify a rock is its texture. When we refer to rocks, texture describes the physical characteristics of the rock. In essence, it refers to how the rock looks and feels like. The texture of the rock gives clues to its origin and the way it was formed.
Rocks have different physical properties that help in classifying them. These include color, grain size, and texture. Texture is the most reliable characteristic that can be used to classify a rock. The texture of a rock is determined by the size, shape, and arrangement of the mineral grains in it.
Mineral stability refers to the ability of a mineral to remain unchanged under certain conditions. This characteristic is not reliable in classifying rocks because different minerals have different degrees of stability, and some rocks may have different minerals with different stability degrees.
Water content is another physical property of rocks. However, this characteristic cannot be used to classify rocks because some rocks may contain water while others may not.
Degree of weathering is also a characteristic of rocks. It refers to the amount of physical and chemical changes that rocks undergo as they interact with the environment. Although it can be used to describe the condition of a rock, it is not a reliable characteristic for classifying rocks.
In conclusion, texture is the most reliable characteristic that can be used to classify a rock. It gives clues to the origin and formation of the rock, making it an essential feature in rock classification.
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true or false lithofication is the process in which two plates move towards each other and the denser one slides below the other.
The statement "lithification is the process in which two plates move towards each other and the denser one slides below the other" is False because lithification refers to the process in which sediment is compacted and cemented together to form sedimentary rock.
What is lithification?Lithification is the process by which sedimentary rocks are formed. It is a transformation process that involves the compaction and cementation of sediment to produce solid rock from loose sediment. The process of lithification results in the creation of sedimentary rocks from sediments such as clay, silt, sand, and gravel.
How does lithification occur?Lithification occurs in three stages:
Compaction of Sediments - This occurs when the weight of overlying sediment squeezes the water out of the sediments beneath it. As a result, the sediment becomes denser, and the grains are packed closer together.
Cementation of Sediments - Cementation occurs when mineral crystals are deposited in the small spaces between the sediment grains, gluing them together to create solid rock.
Sedimentary Rocks - Sedimentary rocks are formed when the compacted and cemented sediment becomes hard and forms rock.
Thus, the statement, "Lithification is the process in which two plates move towards each other and the denser one slides below the other," is false.
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changes in agriculture may have contributed to global changes in temperature.
Yes, changes in agriculture have contributed to global changes in temperature.
What is agriculture?Agriculture is the practice of cultivating crops and raising animals for human use and consumption. It involves various activities such as preparing the soil, planting seeds, watering, fertilizing, pest management, and harvesting. Agriculture plays a crucial role in providing food, fiber, and fuel for the world's population. It has been practiced for thousands of years and has undergone significant changes over time, including the use of advanced technologies and scientific methods. Agriculture is essential for economic development and sustainability, and it has the potential to contribute to poverty reduction and food security. However, it also faces challenges such as climate change, land degradation, and water scarcity, which require innovative solutions and sustainable practices to ensure its continued success.
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The death of marat and a river of landscape similarities
The death of Marat, a key figure in the French Revolution, and a river of landscape similarities can both be seen in their respective contexts.
Death of Marat's in 1793 brought about a major change in the course of the Revolution, with the after Reign of Terror leading to its eventual end. In the same way, a swash of geography parallels can be seen as a form of metamorphosis, as it shifts from one place to another, carrying deposition and other accoutrements that shape the geography in its
wake. Both example represent a form of metamorphosis, whether political or geographical, that can have lasting goods on the world.
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What are the similarities of death of Marat and a river of landscape?
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