The john day rock deposits taken together will be 15,000 feet thick, with 180 species in total.
The John Day rock deposits are composed of multiple layers of sedimentary rock that are estimated to be around 15,000 feet thick in total. These rock formations contain a diverse array of over 180 species of plants, 100 species of fish, and several mammals, reptiles, and amphibians.
This region is a paleontological wonder, with fossils of creatures such as sabre-toothed cats, ground sloths, and camels having been discovered here. The John Day fossil beds are an important scientific resource, providing invaluable insights into the evolution of life on Earth.
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A storage site for high-level radioactive waste would have all of the following features except: isolated from major population centers. geological stability. no contact with groundwater. near volcanic activity where waste can be destroyed by high temperatures. no contact with flowing water or air movement.
A storage site for high-level radioactive waste would have all of the following features except being near volcanic activity where waste can be destroyed by high temperatures. The correct option is option D (near volcanic activity where waste can be destroyed by high temperatures).
A storage site for high-level radioactive waste would have all of the following features except being near volcanic activity where waste can be destroyed by high temperatures. A storage site for high-level radioactive waste would have to have the following features:
• Isolated from major population centers.
• Geological stability.
• No contact with groundwater.
• No contact with flowing water or air movement.
High-level radioactive waste is highly hazardous, and it could cause catastrophic results if it were to be released into the environment. As a result, storage facilities must be built in such a way that they can securely contain high-level radioactive waste. They must be situated away from significant population centers to prevent exposure to large groups of people.
They must also be geologically stable, which means they must be constructed on a site that has not experienced tectonic activity for a long period of time. There should be no contact with groundwater to prevent the release of contaminants into the environment. Finally, there should be no contact with flowing water or air movement. The correct option is option D (near volcanic activity where waste can be destroyed by high temperatures).
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Which of the layers in the atmosphere do temperatures vary the most?
Answer:
The Troposphere
Explanation:
It has most of our weather like rain, snow, and clouds. On this part of the atmosphere, the temp gets cold as the amount of space above the earth increases.
mapping does not: group of answer choices provide a baseline against which to measure the impact of improvement efforts. define the boundaries of a process. provide a detailed view of all elements external to the process. create a common understanding of the content of a process.
Mapping does not provide a detailed view of all elements external to the process. Therefore the correct option is option C.
Mapping is a representation of something on paper that is simplified or reduced to its essential characteristics. Mapping is the process of graphically portraying the entire business process to give a visual perspective of how it functions in practice.
The advantages of Mapping are as follows: Maps can be used to simplify complicated concepts or interactions. Maps can assist in the detection of mistakes or improvement areas. Maps provide a clear picture of who is involved, what they do, and how their work connects to the rest of the organization.
Maps help to create a shared understanding and language. A baseline is a reference point or a standard against which something can be assessed or measured. Mapping does not provide a detailed view of all elements external to the process. Therefore the correct option is option C.
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The following question may be like this:
mapping does not: group of answer choices
provide a baseline against which to measure the impact of improvement efforts. define the boundaries of a process. provide a detailed view of all elements external to the process. create a common understanding of the content of a process.relative to the fundamental themes of geography, the grand canyon is best described within which of the five themes?
Relative to the fundamental themes of geography, the Grand Canyon is best described within the theme of "physical geography".
The five fundamental themes of geography are Location, Place, Human-Environment Interaction, Movement, and Regions. These themes are used to describe and understand the physical and human aspects of the world around us.
Let's understand how the Grand Canyon is best described within the fundamental themes of geography:
Location: The location of the Grand Canyon is important to its understanding, but it does not fall within this theme.
Place: The Grand Canyon is a unique place, but it does not fall within this theme as well.
Human-Environment Interaction: The Grand Canyon is formed by the Colorado River and various geological processes. Its formation and how humans have interacted with it over time is best described within this theme.
Movement: The Grand Canyon is not particularly relevant to the movement of people, goods, or ideas, so it does not fall within this theme.
Regions: The Grand Canyon is located within the Southwest region of the United States. It is an important part of this region, but does not fall within this theme.
Therefore, we can conclude that the Grand Canyon is best described within the theme of "physical geography". Physical geography is a branch of geography that studies the natural features of the Earth's surface.
The Grand Canyon is a prominent example of physical geography due to its unique geology and the physical processes that have shaped it over millions of years.
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A stream or river is a body of water flowing in a __________.
A stream or river is a body of water flowing in a channel.
A stream is a small river that can be crossed by wading or hopping from one bank to the other. If the stream is fed by underground water sources or has a large volume of water, it might be deep enough to require a bridge. The water in a stream or river usually flows downhill due to gravity, but it may also flow from high to low pressure or from an area of high elevation to one of lower elevation.
The movement of a river is aided by the slope of the ground, the size and position of rocks and other debris in its bed, and the amount and speed of water in the river. The soil composition and the landscape through which it flows will also influence the river's flow. The banks of a river or stream are often eroded by the water's movement, and the water may transport soil, rocks, and other debris downstream. This process aids in the formation of canyons, gorges, and other geologic formations.
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a characteristically distinct collection of a sediment or feature and its corresponding artifacts is known as what?
An assemblage is a characteristically distinct collection of a sediment or feature and its corresponding artifacts.
An assemblage is a collection of materials from an archaeological site or a series of sites that were excavated. An assemblage, as a term, refers to a collection of artifacts discovered in a single location or region, such as a settlement or archaeological site. The term "assemblage" refers to the materials used by archaeologists to reconstruct human behaviour and culture from the past. An assemblage is frequently used to learn about the life and activities of a particular culture or civilization at a specific moment in time.
For example, an archaeological excavation may have yielded an assemblage of pottery, tools, and human remains. This assemblage could be utilized to learn about the everyday life, traditions, and culture of the people who lived in the area where the excavation was conducted.
An archaeological assemblage, for example, may be a collection of items discovered at a specific site that may be interpreted as having been produced or utilized by the same group of people. An assemblage is frequently used to determine the nature of a cultural site, its occupation duration, and the range of its cultural features. The dating of these features may help to establish a chronological sequence of cultural activity, which may then be used to investigate social and cultural development.
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in the picture above, when dr. alley slices his finger through the sand, he is recreating on a smaller scale what type of geologic process?
Dr. Alley is recreating the process of sedimentation on a smaller scale. Sedimentation is the process by which solid particles settle out of a liquid or a gas. The particles settle due to gravity and settle out of the medium into layers.
These layers are then compressed and cemented together to form sedimentary rocks. In the picture, Dr. Alley is slicing his finger through the sand and the particles settle in layers. This process of sedimentation can occur in a variety of geological settings, including in the ocean and on land. Sedimentation can also be caused by erosion, where material is removed from one location and sediment elsewhere. This is also happening in the picture, as the sand is settling in layers from Dr. Alley’s slicing. Sedimentation is an important process in the rock cycle, as it is how sedimentary rocks are formed.
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a spinel found in metamorphic rock or an aquamarine found within a pegmatite are examples of what type of deposit
A spinel found in metamorphic rock or an aquamarine found within a pegmatite are examples of hydrothermal deposits.
What are hydrothermal deposits?
Hydrothermal deposits are rocks containing mineral deposits that originated from hot water (hydrothermal) fluids circulating in the Earth's crust.
Hot water deposits often contain significant quantities of minerals, which are usually accompanied by the alteration of the surrounding rock. The hot water that makes up these deposits is generated by heat from the Earth's core, which is transferred through the mantle to the Earth's crust.
When the water is heated, it is driven to the Earth's surface, where it flows through cracks and fissures in the rock.
The water then cools, and minerals precipitate out of the solution, forming hydrothermal deposits. There are various types of hydrothermal deposits, including gold, silver, copper, zinc, and lead deposits, among others.
These deposits are commonly found in areas where tectonic plates meet, and the Earth's crust is being pushed and pulled in various directions.
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which of the following is not a low-latitude climate region? mansoon wet equatorial dry tropical tropical savanna humid subtropical
Answer: A low latitude climate is a tropical climate, exemplified by areas in or near the equator.
Assuming the sand dune (illustrated below) was deposited by wind currents 200 million years ago, which way was the wind blowing?Image: similar to the pair&share photo of the Jurassic Navajo Sandstone in Utah from the "Play in the Mud (and Sand)" lectureA) wind was blowing from the left to rightB) wind was blowing from right to leftC) wind was blowing both waysD) can't determine from the information given
The sand dune (illustrated below) was deposited by wind currents 200 million years ago, which way was the wind blowing wind was blowing from right to left. The correct answer is B) the wind was blowing from right to left.
To determine the wind direction, we need to analyze the sand dune's structure. Sand dunes have two distinct sides: the windward side and the leeward side. The windward side is the side facing the wind, and it has a gentle slope. The leeward side is the side sheltered from the wind, and it has a steeper slope.
In this case, we can see that the left side of the dune has a steeper slope, while the right side has a more gentle slope. This indicates that the wind was blowing from the right, carrying sand grains up the gentle slope on the right side of the dune. Once the wind reached the top of the dune, it lost its carrying capacity, causing the sand grains to fall and accumulate on the steeper left side of the dune, forming the leeward side.
So, considering the structure of the sand dune and the slopes, we can conclude that the wind was blowing from right to left 200 million years ago when the sand dune was deposited. The correct answer is B) the wind was blowing from right to left.
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when going from a 5 to a 6 on the richter scale, what is the increase in amplitude of seismic waves?
a. 1 times
b. 2 times
c. 10 times
d. 32 times
When going from a 5 to a 6 on the Richter scale, the increase in amplitude of seismic waves is 10 times.
This means that a magnitude 6 earthquake produces seismic waves with ten times more amplitude than a magnitude 5 earthquake. The Richter scale is a logarithmic scale, which means that each whole number increase represents a tenfold increase in the amplitude of the seismic waves. For example, a magnitude 7 earthquake produces waves with 100 times more amplitude than a magnitude 5 earthquake, while a magnitude 8 earthquake produces waves with 1,000 times more amplitude than a magnitude 5 earthquake, and so on.
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as planet mercury formed, temperatures in this region were around 1400k. thus mercury formed out of...
As the planet Mercury formed, temperatures in this region were around 1400K.
Thus, Mercury formed out of material that had a high melting point. The most abundant elements were metals such as iron (Fe), nickel (Ni), and silicon (Si).
This is because the melting point of these elements is high enough to withstand the high temperature in the region. These elements, particularly iron, dominated the formation of Mercury.
In fact, the planet's density is the second-highest in the solar system, after Earth, which suggests a substantial metallic core.
According to the Giant impact hypothesis, Mercury was formed after a Mars-sized body collided with the early Earth.
The debris from the impact was scattered into space and coalesced into a hot planetesimal which eventually became Mercury.
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when we see venus in its full phase, what phase would earth be in as seen by a hypothetical venetian? group of answer choices first quarter new waning crescent full third quarter
If we see Venus in its full phase, Earth would appear as a new phase to a hypothetical Venetian. The answer is first quarter.
What is the meaning of the term "full phase"?
The term "full phase" refers to the time when the planet is positioned behind the Sun in the Earth-Sun-planet alignment. This alignment causes the planet to appear fully illuminated from Earth’s point of view because it reflects all of the sunlight that is falling on its surface.
The orbital path of Venus is smaller than that of Earth because it is closer to the Sun. When Venus is on the far side of the Sun (as viewed from Earth), we can see its full illuminated face.
At that moment, the Sun-Earth-Venus angle is 180 degrees, and Venus is on the opposite side of the Sun from the Earth.
Hence, when we see Venus in its full phase, Earth would appear as a new phase to a hypothetical Venetian. The answer is first quarter.
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at night, the air above the mountain slopes and drains into the warm valley below, creating a .
At night, a process called radiation cooling causes the air on the mountain slopes to cool more quickly than in the valley below. This creates a temperature inversion, where the air temperature at the top of the mountain is cooler than at the base.
The temperature inversion also has other effects, such as creating a stable layer of air that traps pollutants near the ground and limits visibility. Additionally, the process helps to distribute moisture more evenly throughout the environment.
This is a vital part of many mountain ecosystems, and an important factor to consider when studying climate patterns and air quality in mountainous areas.
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which term describes a soil that remails in place after having formed by weathering of the underlying bedrock? residual relict transformational transported
The term that describes soil that remains in place after having formed by weathering of the underlying bedrock is residual soil.
What is residual soil?
Residual soil, also known as residuum, is soil that forms from the weathering of bedrock that has remained in place. This soil is formed by in situ weathering and usually remains where it is formed. The weathering processes cause the bedrock to disintegrate into small particles, resulting in the formation of residual soil.
Residual soils are usually found on slopes and hilltops, where weathering is highest, and are often composed of coarse particles due to the intense weathering that occurs. They are generally thick and can be of varying depths depending on the bedrock they have formed from. The soil is typically rocky and nutrient-poor, which limits plant growth. Residual soils are classified as 4th-order soils according to the Soil Taxonomy. The Soil Taxonomy ranks soils into 12 orders based on their characteristics.
Residual soil is soil that forms from the weathering of bedrock that has remained in place.
Residual soils are usually found on slopes and hilltops, where weathering is highest. They are typically rocky and nutrient-poor. Residual soils are classified as 4th-order soils according to the Soil Taxonomy.
The word used to describe soil that stays in its original place after being formed by the weathering of the underlying bedrock is "residual soil".
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which element is found in greater amounts in low viscosity magma, than in high viscosity magma? question 12 options: a) si b) fe
Si (Silica) is found in greater amounts in low viscosity magma, than in high viscosity magma. Option A is correct answer.
High silica content magmas will consequently show higher levels of polymerization and have higher viscosities than magmas with low silica concentration. A substance's viscosity is a measurement of its consistency. A substance's viscosity is defined as its capacity to resist flow. Viscosity is, in some ways, the inverse of fluidity. Because cold molasses is less fluid than water, it has a greater viscosity.
The temperature, composition, and gas concentration of a magma all influence its viscosity. The relationship between temperature and viscosity is self-evident. The greater the temperature, like with most liquids, the more fluid the material becomes, reducing its viscosity.
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what does the existence of machu picchu suggest about the power of the inca king?
The existence of Machu Picchu suggests that the Inca king or emperor, Pachacuti Inca Yupanqui, had significant power and resources at his disposal. Machu Picchu is an ancient Inca citadel located in the Andes Mountains of Peru
It is thought to have been constructed in the middle of the 15th century as a royal estate for Pachacuti Inca Yupanqui. It is reasonable to assume that the Inca king had the strength and authority to command the necessary materials and labor force given the amount of labor, resources, and organization required to build such a monumental and elaborate structure in a remote and inaccessible location. Additionally, Machu Picchu's strategic location, with a view of the Urubamba River Valley, may have represented Inca power and control over the neighboring lands symbolically.
However, it's important to note that there are still many unanswered questions about the function and significance of Machu Picchu, and historians continue to disagree about its exact place in Inca politics and society.
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identify the false statement. the rock cycle indicates that: group of answer choices sedimentary rock cannot form from other sedimentary rocks because the pathway is always from one rock type to a different rock type. in order to make a metamorphic rock, burial and/or heating are needed. a granite that was eroded, transported, and then deposited would eventually become a sedimentary rock. input of new melt from the crust enters the rock cycle as an igneous rock.
The false statement is that in order to make a metamorphic rock, burial and/or heating are needed. This is false because metamorphic rock can also form from other metamorphic rocks, and does not necessarily require burial and/or heating.
Metamorphic rocks are formed when existing rocks are exposed to extreme temperature and pressure, which can occur either deep within the earth or near the surface. When existing metamorphic rocks experience these extreme conditions, they can change into different metamorphic rocks, without requiring burial or heating.
This shows that the pathway of the rock cycle is not always from one rock type to another, but can also be from one rock type to the same rock type. For example, a granite that was eroded, transported, and then deposited would eventually become a sedimentary rock.
This sedimentary rock could then undergo metamorphism and be changed into a metamorphic rock, without requiring burial and/or heating. This is an example of how the rock cycle indicates that sedimentary rocks can form from other sedimentary rocks.
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theorize about what landforms are produced as a result of this tectonic boundary. (give examples by referring to the names of these landforms in south america) is there a particular prominent landscape with huge mountains?
The tectonic boundary between the South American Plate and the Nazca Plate is a convergent boundary. At this boundary, the Nazca Plate is subducted beneath the South American Plate, resulting in the formation of a subduction zone.
As a result, various landforms are produced, including volcanoes, mountains, and oceanic trenches .In South America, one of the most prominent landforms produced by this tectonic boundary is the Andes Mountains.
These mountains stretch along the western edge of South America and are the longest mountain range in the world. They are formed by the collision of the South American Plate and the Nazca Plate.
Additionally, the Nazca Plate is being subducted beneath the South American Plate, resulting in the formation of the Peru-Chile Trench, which is the deepest oceanic trench in the world.
This trench is located off the coast of South America and is over 3,700 miles long. Other landforms produced by this tectonic boundary include volcanoes, such as Cotopaxi in Ecuador and Villarrica in Chile.
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describes the tendency for different types of rock to weather at different rates.
The tendency for different types of rock to weather at different rates is known as differential weathering. This phenomenon occurs due to the varying physical and chemical properties of different rocks.
For example, rocks with a greater porosity and permeability are more likely to absorb water, leading to faster weathering.
In contrast, rocks with low porosity and permeability will not absorb water easily and therefore weather more slowly. Other factors that can influence the rate of weathering include the type of minerals that the rock is composed of and the climate in which it is located. Differential weathering affects the landscape, often leading to the formation of distinctive features such as mesas and canyons.
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Match the damage to a house to the correct Fuijita scale classification.1. F32. F13. F54. F0___ roof damage___ wall collapse___ house blown away___ little damage
The match of the damage to a house to the correct Fujita scale classification is given below:
F1 roof damage
F3 wall collapse
F5 house blown away
F0 little damage
The Fujita scale is used to categorize tornadoes based on the intensity of the tornado.
The Fujita scale is a classification system for measuring the intensity of tornadoes based on the damage they cause to buildings and vegetation. The Fujita Scale was designed in 1971 by Ted Fujita, a professor at the University of Chicago, and was first used in the United States in 1973. The scale ranges from F0 (weakest) to F5 (strongest).
The reason for the matching is the level of damage associated with each Fujita scale category. The higher the number, the more severe the damage. Here's the explanation:
F0: Little damage (light damage to trees, signs, and buildings;)
F1: Roof damage (moderate damage to roofs, windows, and vehicles)
F3: Wall collapse (severe damage to walls, roofs, and large trees)
F5: House has blown away (total destruction of houses and buildings)
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basalt is an igneous rock that can be found in which volcanic environment?group of answer choicesmid-ocean ridge volcanismhot spot volcanismsubduction zone volcanism
Basalt is an igneous rock that is most commonly found in volcanoes that form due to subduction zone volcanism.
Subduction zone volcanism is a type of volcanism occurs when one of the Earth's tectonic plates moves beneath another and sinks into the mantle. As the two plates grind against each other, the pressure causes magma to rise up through the lithosphere, forming a volcano.
Basalt is composed of minerals like pyroxene, plagioclase, and olivine, and it forms from the cooling and solidification of lava that is created when the magma rises and erupts. Basalt is one of the most common volcanic rocks and is often used to construct structures such as roads, pathways, and buildings.
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where is light penetration in a river or stream likely to be lowest? a. the source b. the mouth c. the middle portion d. none of the above please select the best answer from the choices provided a b c d
Light penetration in a river or stream is likely to be lowest at the middle portion. The correct option is C.
This is because the middle portion of a river or stream is typically the deepest and has the most sediment, which can block out or reduce the amount of light that penetrates the water.
Additionally, the middle portion is often where the greatest amount of currents and turbulence occur, which can further reduce the amount of light that reaches the bottom of the river or stream.
As light penetration decreases, photosynthesis rates are lowered and the amount of oxygen available to the aquatic life in the river or stream is also reduced. The correct option is C.
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water velocity in a stream varies based on many factors but is usually greater at the mouth than the head. which part of a stream commonly has the highest gradient?
Water velocity in a stream varies based on many factors but is usually greater at the mouth than the head. The part of a stream commonly having the highest gradient is head.
Stream is defined as a body of water, running or moving continuously in a channel or course of considerable width and length. There are a number of different types of streams, each characterized by its size, location, and water velocity.
Some of the important factors that affect water velocity in a stream include the slope of the land, the amount of water in the stream, the shape of the streambed, and the type of sediment in the streambed.
Water velocity is the speed of water in a stream or river. It is the distance the water travels over a particular period of time. Water velocity in a stream is influenced by many factors such as the streambed, the shape of the channel, the amount of water in the stream, and the slope of the land, among others.
Gradient refers to the steepness or slope of a stream channel. The highest gradient in a stream is found at the head. The head is the point where the stream begins or the location where the stream gets its water. As the stream flows downstream, the gradient decreases, and the water velocity decreases.
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LICs receive more income when wealthy people from HICs want to visit their unspoiled natural landscape and culture. What is this called?
LICs receive more income when wealthy people from HICs want to visit their unspoiled natural landscape and culture is called tourism.
What is tourism?Tourism refers to the activity of people traveling to and staying in places outside their usual environment for leisure, business, or other purposes. It involves the visiting of new places, experiencing different cultures and traditions, and engaging in various recreational activities.
When wealthy people from high-income countries (HICs) visit low-income countries (LICs) to experience their unspoiled natural landscape and culture, it can generate significant income for the LICs through the tourism industry. This can include revenue from activities such as lodging, transportation, food and beverages, and various attractions and experiences.
The phenomenon you are referring to is called tourism.
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1 pts as erosion strips off the tops of mountains, the mountains will "bob" upward. this is an example of
This phenomenon is known as isostatic rebound. Isostatic rebound occurs when the pressure exerted by the overlying material is relieved, usually caused by erosion. It is believed that this process occurs due to the removal of material, such as ice or sediment, from the upper layers of the mountain.
As this material is removed, the weight of the mountain decreases, causing the mountain to slowly “bob” upwards. This process is gradual and can take hundreds or even thousands of years to fully complete. Isostatic rebound plays an important role in the overall geology of a region, and can often result in dramatic landscape changes. For example, recently glaciated areas are often characterized by low relief, whereas regions that have experienced isostatic rebound often have steep terrain.
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________ are comprised of members from different geographic areas assembled as needed to collaborate on a certain project.a) work groupsb) virtual teamsc) non-core teamsd) task forcese) command groups
Task Forces are comprised of members from different geographic areas assembled as needed to collaborate on a certain project. The answer is (d) task forces.
Task forces are temporary teams that are created to work on a specific project or problem. They are composed of individuals who have different skill sets and come from different geographic areas within an organization. Task forces can be established for a variety of purposes such as developing a new product, improving a process, or resolving a crisis. Once the task is completed, the team is dissolved.
The members of the task force return to their previous roles within the organization. Task forces are often used in organizations to leverage expertise from various parts of the organization and to ensure that critical issues are addressed in a timely and effective manner. They are a useful way to bring together diverse perspectives and talents to achieve a specific objective.
Therefore, the correct answer is (d) task forces.
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briefly explain why a permanent temperature inversion (temperature increases with height) occurs throughout stratosphere
A permanent temperature inversion, in which temperature increases with height, occurs throughout the stratosphere because of the presence of ozone in the stratosphere.
The absorption of ultraviolet radiation by ozone causes the stratosphere to be heated. Due to the high temperatures of the stratosphere, the temperature increases with increasing altitude.
Additionally, the stratosphere is relatively dry, with little to no water vapor to absorb or emit heat, contributing to the permanent temperature inversion.
A permanent temperature inversion layer in the stratosphere helps to stabilize the atmosphere and prevent vertical mixing between the stratosphere and the troposphere below. This plays an important role in regulating our climate, as it helps to maintain the atmospheric conditions necessary for life on Earth. By preventing mixing, the temperature inversion layer helps to keep the troposphere cooler and drier than the stratosphere, which can have significant impacts on weather patterns and the overall climate system.
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choose the statement that best describes foliation. choose one: a. the texture typical of all metamorphic rocks b. an arrangement of mineral grains such that most are of the same size and shape c. an alignment of mineral grains perpendicular to the direction of compression d. an alignment of mineral grains parallel to the direction of compression
Answer:
d. An alignment of mineral grains parallel to the direction of compression describes foliation.
Explanation:
Foliation is a characteristic feature of many metamorphic rocks, and it refers to the alignment of mineral grains or other constituents in parallel planes or layers. This alignment is typically a result of the application of directed pressure or compression during the metamorphic process, which causes the mineral grains to flatten and orient in the same direction. The resulting texture can give the rock a layered or banded appearance and can also affect its physical properties such as its strength and cleavage.
which type of unconformity is usually easiest to spot, since layers of sedimentary rocks are on top of igneous rocks without layers?
The type of unconformity, which is usually easiest to spot, since layers of sedimentary rocks are on top of igneous rocks without layers is called Disconformity.
What is an unconformity?
An unconformity is a contact between two groups of rock formations. An unconformity is a surface of erosion or non-deposition that separates younger from older rocks. A time gap or hiatus exists at the unconformity between the rock layers, indicating that some time has passed between the formation of the first group of rocks and the second group.
There are three types of unconformities: nonconformity, disconformity, and angular unconformity. An unconformity can be caused by tectonic events, sea-level shifts, or erosion, among other things.
A disconformity is an unconformity in which parallel layers of sedimentary rocks are separated by a break in sediment deposition or a layer of erosional material.
In a disconformity, the bedding planes of the strata above and below the unconformity are parallel, indicating a time gap in the sedimentary record.
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