A common way in which Philadelphia-size or bigger bodies of rock that were heated and squeezed deep in a mountain range then end up at the surface of the Earth is:

Answers

Answer 1

A common way in which Philadelphia-size or bigger bodies of rock that were heated and squeezed deep in a mountain range then end up at the surface of the Earth is through a "geological process called uplift and erosion."

Uplift occurs when tectonic forces push the crust upward, causing the buried rocks to rise towards the surface. This uplift can be caused by a variety of factors such as plate tectonics, mantle convection, and volcanic activity.

Once the rocks are uplifted, erosion begins to occur. Erosion is the natural process by which rocks and soil are broken down and carried away by wind, water, or ice. The forces of erosion can be incredibly powerful, and over time they can wear down even the largest rock formations.As the rocks are eroded away, they are slowly exposed to the surface of the Earth. This process can take millions of years, but eventually, the once-buried rocks are revealed. Once exposed, these rocks can be studied and analyzed by geologists, providing important insights into the Earth's geological history.In summary, the process by which Philadelphia-size or bigger bodies of rock end up at the surface of the Earth is through a combination of uplift and erosion. This geological process can take millions of years, but ultimately, it is responsible for shaping the Earth's surface and revealing its hidden secrets.

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Related Questions

When winds blow across the sea surface, they transfer their energy to the water by generating ________.

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When winds blow across the sea surface, they transfer their energy to the water by generating waves.

Waves are disturbances that propagate through the water surface due to the transfer of energy from the wind. The wind's energy creates ripples in the water, which merge and grow to form waves.

The size and shape of the waves depend on the wind speed, duration, and fetch, which is the distance over which the wind blows.
Waves are essential to many natural processes and human activities. They redistribute heat and energy in the ocean, which affects climate and weather patterns.

They also play a crucial role in coastal erosion, sediment transport, and nutrient cycling. Waves are also important for recreational activities such as surfing, sailing, and fishing.
In addition to waves, winds also create other oceanic phenomena such as currents and upwelling.

Currents are large-scale movements of water caused by wind, temperature, and salinity differences. Upwelling is the vertical movement of cold, nutrient-rich water to the surface, caused by wind-driven currents.

These phenomena have significant ecological and economic impacts, affecting marine life, fisheries, and climate.
In conclusion, the energy transfer from winds to water generates waves, which are crucial to many natural and human activities in the ocean.

Understanding the dynamics of waves and other oceanic phenomena is essential for sustainable management of marine resources and ecosystems.

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What is the term for the global-scale slow movement of ocean water masses, in which cold, salty surface water sinks to the seafloor and warm equatorial water moves toward the poles

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There is concern that human-induced climate change could disrupt or even shut down the thermohaline circulation, which could have far-reaching consequences for the world's climate and ecosystems.

The term for this global-scale slow movement of ocean water masses is known as thermohaline circulation or the ocean conveyor belt. The term "thermohaline" refers to the combined effects of temperature ("thermo") and salinity ("haline") on seawater density. The circulation is driven by differences in temperature and salinity, which cause changes in seawater density and thus, drive the movement of water masses around the world's oceans.

The process starts with the cooling and sinking of dense, salty water at high latitudes, such as in the North Atlantic. The dense water sinks to the seafloor and flows southward, eventually spreading throughout the deep ocean. This sinking creates a void that is filled by warmer, less dense water from the tropics, which flows towards the poles on the surface of the ocean.

This circulation has a significant impact on Earth's climate by transporting heat from the equator to the poles and influencing global climate patterns. It also plays a critical role in the ocean's carbon cycle by transporting carbon-rich waters to the deep ocean where they can be stored for hundreds of years.

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Before an earthquake, rocks can respond to applied stress to a small degree by bending and warping without breaking. This is termed _________. a. elastic behavior b. brittle deformation c. faulting d. seismic velocity

Answers

D.
Seismic velocity
The correct answer is D

According to Oppenlander, livestock operations on land has caused or created, more than _____________ nitrogen-flooded dead zones around the world in our ocean, and comprise more than ________________ square miles of areas completely devoid of life.

Answers

According to Oppenlander, livestock operations on land have caused or created more than 500 nitrogen-flooded dead zones around the world in our ocean, and comprise more than 95,000 square miles of areas completely devoid of life.

Excess nitrogen fertiliser use in agriculture, particularly in livestock activities, contributes to the establishment of dead zones in the ocean.

Nitrogen from fertilisers moves from land into rivers and eventually into the oceans, where it causes excessive algae growth, depletes oxygen in the water, and leads to the establishment of dead zones where marine life cannot survive.

Livestock activities contribute significantly to this problem since they require a large quantity of land and water to provide feed for the animals, resulting in high fertiliser consumption and nutrient runoff.

This is especially true for large-scale livestock operations, which account for the vast majority of nitrogen contamination in streams.

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After the New Horizons flyby, scientists concluded that Pluto has probably been geologically active within the past 100 million years or less. Why

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One of the key pieces of evidence that led scientists to conclude that Pluto has likely been geologically active within the past 100 million years or less was the presence of relatively young surface features on the dwarf planet.

When NASA's New Horizons spacecraft flew past Pluto in 2015, it took detailed images of the planet's surface, revealing a variety of geological features.

Some of these features appeared to be relatively new, with few impact craters and signs of recent surface activity, such as the presence of mountains, valleys, and other landforms indicating ongoing geological processes.

Furthermore, the detection of gases like nitrogen escaping from Pluto's atmosphere indicated that the planet's surface was being reshaped.

Based on these findings, scientists concluded that Pluto must have seen geological activity within the last 100 million years or less, which is a relatively short time in geological terms.

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The primary difference between lithospheric and asthenospheric mantle that gives rise to numerous different patterns of physical behavior is

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The primary difference between lithospheric and asthenospheric mantle is their physical properties. The lithospheric mantle is a rigid, solid layer of the Earth's mantle that makes up the outermost layer of the Earth's surface, while the asthenospheric mantle is a more ductile, partially molten layer of the mantle that lies beneath the lithosphere.

This difference in physical properties gives rise to numerous different patterns of physical behavior. The rigidity of the lithospheric mantle allows it to be broken into plates that move around the Earth's surface due to plate tectonics, while the ductility of the asthenospheric mantle allows it to flow and convect, which contributes to the motion of the plates.

Furthermore, the lithospheric mantle is colder and more brittle than the asthenospheric mantle, which affects how it responds to stresses and strains. The asthenospheric mantle is more ductile and can flow more easily, which allows it to accommodate stresses and strains more readily. Overall, these differences in physical properties give rise to the complex and varied behavior of the Earth's mantle, including plate tectonics, earthquakes, and volcanic eruptions.

A quantitative perspective on physical geography that helps geographers understand the interconnections in natural processes is

Answers

A quantitative perspective on physical geography is a way to use numbers and data to better understand how different parts of the Earth, like mountains, weather, and plants, are connected and influence each other. This helps geographers understand how natural processes work together.

Foraminifera are microscopic animals commonly preserved as fossils. The change in the assemblage of foraminifera fossils between the limestone rocks above and below a 1 cm thick clay layer indicated to Luis and Walter Alvarez that ______.

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The change in the assemblage of foraminifera fossils between the limestone rocks above and below a 1 cm thick clay layer indicated to Luis and Walter Alvarez that there was a sudden mass extinction event.

This event was later identified as the Cretaceous-Paleogene (K-Pg) extinction event, which occurred approximately 66 million years ago and resulted in the extinction of non-avian dinosaurs, as well as many other species. The detailed answer is that Luis and Walter Alvarez noticed that the limestone rocks above the clay layer contained a diverse assemblage of foraminifera fossils, while the rocks below the clay layer contained significantly fewer and less diverse foraminifera fossils. This indicated a sudden and drastic change in the marine environment, likely caused by a catastrophic event such as an asteroid impact, volcanic eruption, or other natural disaster. The discovery of this evidence helped support the theory that the K-Pg extinction event was caused by an asteroid impact.

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Several lines of evidence suggest that Meteor Crater was formed by an impact event. These include ______.

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Several lines of evidence suggest that the Meteor Crater was formed by an impact event. These include a large circular depression at the site, the presence of shock quartz in the surrounding area, and The area includes the discovery of meteorite fragments. Option D is correct.

Meteor Crater, located in Arizona, USA, is a large circular depression on the surface of the Earth that has long been believed to be the result of an impact event. There are several lines of evidence that support this hypothesis, including the presence of a large circular depression, the occurrence of shocked quartz, and the discovery of meteorite fragments in the area.

The most significant evidence is the large circular depression, which has a diameter of approximately 1.2 kilometers and is over 170 meters deep. The size and shape of the crater are consistent with what would be expected from a large impact event. In addition, the layers of rock and sediment around the crater show signs of being disturbed and shifted by a powerful force, also supporting the impact hypothesis.

The presence of shocked quartz, which is formed when rocks are subjected to high pressures and temperatures, is another strong piece of evidence. The occurrence of this mineral in the area suggests that an extremely powerful event occurred at the site, such as a meteor impact.

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Complete question:

Several lines of evidence suggest that Meteor Crater was formed by an impact event. These include ______.

A) A large circular depression at the site.

B) The presence of shocked quartz in the surrounding area.

C) The discovery of meteorite fragments in the area.

D) All of the above.

A lee-side low forms: Select one: a. over the central Pacific Ocean. b. near the equator. c. on the upwind side of a mountain. d. on the downwind side of a mountain

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A lee-side low forms on D. the downwind side of a mountain.

Lee-side lows, also known as lee cyclones, occur when air flows over a mountain and descends on the downwind (lee) side. As the air moves over the mountain, it cools and loses moisture through precipitation. Upon descending, the air warms due to adiabatic heating, leading to lower pressure on the lee side of the mountain.

This process creates a low-pressure system that can result in localized weather patterns, such as strong winds and varying precipitation. These lows play a significant role in shaping regional climate and weather conditions, especially in areas with prominent mountain ranges. Therefore the correct option is D

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in platoâs cave analogy, the prisoners deep in the cave are chained by

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Plato's cave analogy represents the human condition of being unaware of the true reality.

The prisoners in the cave are chained by their ignorance of the outside world, and the shadows on the cave wall become their only reality. According to Plato, the world outside the cave represents the realm of true knowledge and enlightenment, while the cave represents the world of appearances and illusions. The analogy suggests that humans are often trapped in their own limited perspectives and unable to see the greater reality. Plato's aim was to encourage people to question their own beliefs and perceptions in order to achieve a greater understanding of the world around them. This analogy remains relevant today and serves as a reminder of the importance of critical thinking and open-mindedness.

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A planet is most likely to have tectonic activity if it has Group of answer choices high surface gravity. low internal temperature. a dense atmosphere. high internal temperature. low surface gravity.

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A planet is most likely to have tectonic activity if it has: a high internal temperature. The correct option is D.

Tectonic activity is primarily driven by the planet's internal heat. When a planet has a high internal temperature, it causes the mantle to convect, with hotter material rising and cooler material sinking. This convection leads to the movement of the planet's crust, resulting in tectonic activity such as earthquakes and volcanic eruptions.

High surface gravity (option a) and a dense atmosphere (option c) can influence the planet's surface features and geological processes, but they are not the primary drivers of tectonic activity. Low internal temperature (option b) would result in less convection and therefore less tectonic activity. Lastly, low surface gravity (option e) would have little direct impact on tectonic activity.

In summary, a planet with high internal temperature is most likely to have tectonic activity, as this internal heat drives mantle convection and the movement of the planet's crust.

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Complete question:

A planet is most likely to have tectonic activity if it has:

a. high surface gravity.

b. low internal temperature.

c. a dense atmosphere.

d. high internal temperature.

e. low surface gravity.

Transform boundaries occur MOST commonly perpendicular to __________ boundaries in order to break the __________ into segments so as to accommodate motion on a sphere.

Answers

Transform boundaries, also known as conservative plate boundaries, occur most commonly perpendicular to divergent boundaries in order to break the lithosphere into segments so as to accommodate motion on a sphere.

Divergent boundaries occur where tectonic plates are moving away from each other, while transform boundaries occur where plates are sliding past each other in a horizontal motion.

Transform boundaries are characterized by frequent earthquakes and faulting, as the plates move past each other in opposite directions. These faults can create rift valleys or transform faults, such as the San Andreas Fault in California.

The motion along transform boundaries is not uniform, and the resulting stress can lead to a buildup of potential energy, which is released as earthquakes.

In summary, transform boundaries occur perpendicular to divergent boundaries in order to break the lithosphere into segments and accommodate motion on a sphere. The resulting stress can lead to earthquakes, which are a common feature of transform boundaries.

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As a source rock partially melts into magma, the magma (melt phase) is ____________ than the residual source rock

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As a source rock partially melts into magma, the magma (melt phase) is more silica-rich than the residual source rock. This is because the early-formed melts are more enriched in silica. The correct answer is option E.

Additionally, the magma will generally be less dense than the residual source rock due to the lower density of the liquid phase compared to the solid minerals in the source rock.

The composition of magma is an important factor in determining its behavior, including its ability to flow and erupt explosively. Silica-rich magmas tend to be more viscous and have a greater tendency to trap gas bubbles, which can lead to explosive eruptions.

In contrast, magma with lower silica content is more fluid and less likely to form explosive eruptions. Understanding the composition and behavior of magma is crucial for predicting volcanic activity and mitigating potential hazards.

By studying the relationship between the residual source rock and the resulting magma, scientists can gain valuable insights into the behavior of volcanoes and improve their ability to forecast eruptions. The correct answer is option E.

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Complete Question:

As a source rock partially melts into magma, the magma (melt phase) is ____________ than the residual source rock.

a. lower density

b. higher density

c. more Fe-Mg rich

d. higher melting temperature minerals

e. more silica rich

You're the mayor of Podunk Coast (congrats on your election). Your town has a harbor inside of a bay. The mouth of your bay is filling up with sediment migrating down from a river to the North. What can you build to help you stop the sediment from closing up your bay

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Constructing a sediment trap or regular dredging, coupled with upstream erosion control measures, can help prevent sediment buildup at the mouth of Podunk Coast's bay.

As the mayor of Podunk Coast, I would recommend the construction of a sediment trap to help prevent the buildup of sediment at the mouth of our bay. A sediment trap is a structure designed to slow down the flow of water and allow sediment to settle out, preventing it from being carried further downstream.

To construct the sediment trap, we could install a series of low barriers or berms at strategic locations in the bay, which would slow down the flow of water and allow sediment to settle out. The trapped sediment can then be periodically removed to maintain the effectiveness of the trap.

Another potential solution is to dredge the mouth of the bay on a regular basis to remove the sediment buildup. This approach would require ongoing maintenance and would be more costly than the construction of a sediment trap, but it could be effective in keeping the harbor open.

In addition to these solutions, we should also consider working with upstream communities to reduce the amount of sediment being carried downstream. This could involve implementing erosion control measures or encouraging the adoption of sustainable land use practices to reduce soil erosion.

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Deforestation ________. Group of answer choices is not widespread in North America decreases carbon dioxide in the atmosphere has the greatest impacts in tropical areas and arid regions prevents erosion causes population explosions

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Deforestation has far-reaching impacts on the environment, including contributing to climate change, soil degradation, loss of biodiversity, and population growth. It is important to take measures to prevent deforestation and promote sustainable land use practices to protect our planet's natural resources for future generations.

Deforestation is the process of clearing large areas of forests or woodlands for various reasons, such as agricultural expansion, urbanization, or industrial development. The impacts of deforestation are significant and far-reaching. While it is not widespread in North America, it has the greatest impacts in tropical areas and arid regions.

Deforestation decreases carbon dioxide in the atmosphere by reducing the number of trees that absorb carbon dioxide through photosynthesis. This can lead to an increase in the amount of carbon dioxide in the atmosphere, contributing to global climate change.

Deforestation also prevents erosion by reducing the number of trees that hold soil in place and protect against erosion caused by wind and water. Without trees, the soil can become loose and easily eroded, leading to soil degradation and decreased fertility. This can have serious consequences for agriculture and food security.

Another impact of deforestation is the loss of biodiversity, as many plant and animal species depend on forests for their habitats. Deforestation can also lead to a population explosion, as people migrate to the cleared areas to farm or settle. This can put additional pressure on natural resources and exacerbate environmental problems.

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Explain the formation of the ridges and valleys. what type of drainage pattern is found on this landscape rigde and valley

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The formation of ridges and valleys can be a result of various factors such as tectonic movements, erosion, and weathering. In terms of drainage pattern, the ridge and valley landscape typically exhibits a dendritic drainage pattern.

Tectonic movements such as the collision of plates can push up the land to form ridges, while erosion can carve out valleys between them. Weathering can also contribute to the formation of ridges and valleys by breaking down rock and soil. The drainage pattern is characterized by a network of branching streams and rivers that flow in different directions, similar to the branches of a tree.

The dendritic pattern is a common feature in areas where the underlying geology is flat or gently sloping, which allows water to flow in various directions.

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The ________ is the point in the subsurface where 100% of the pore spaces are filled with water. A. Zone of Accumulation B. Vadose Zone C. Zone of Saturation D. Capillary Fringe

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The Zone of Saturation is the point in the subsurface where 100% of the pore spaces are filled with water. The correct option is C

This zone is also known as the phreatic zone or groundwater table. It is the point in the subsurface where all of the pores and fractures in the rock or soil are filled with water. This zone is below the Vadose Zone, which is the unsaturated zone where the soil or rock contains both air and water.

The Zone of Saturation is important because it is the source of groundwater, which is an important resource for drinking water, irrigation, and industrial uses. The water in this zone is under pressure and can flow through the soil or rock to recharge nearby wells or surface water bodies such as streams, rivers, or lakes.

The Capillary Fringe is the zone above the water table where the soil or rock is partially saturated with water due to capillary action. This zone is important because it can act as a buffer between the Vadose Zone and the Zone of Saturation, slowing down the movement of contaminants from the surface to the groundwater.

The Zone of Accumulation is a term used to describe the area where water is stored in an aquifer, and it can be found both above and below the water table. This zone is important because it can store large volumes of water for future use.

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A characteristic of the stratosphere is A. an overall decrease of temperature with an increase in altitude. B. a relatively even base altitude of approximately 35,000 feet. C. relatively small changes in temperature with an increase in altitude.

Answers

A characteristic of the stratosphere is: relatively small changes in temperature with an increase in altitude. The correct option is C

The stratosphere is the layer of the Earth's atmosphere that extends from about 10 to 50 kilometers (6 to 30 miles) above the Earth's surface. It is characterized by a relatively stable and uniform composition of gases, including a high concentration of ozone that absorbs harmful ultraviolet radiation from the sun.

One of the defining characteristics of the stratosphere is its temperature profile. Unlike the troposphere, which is the layer of the atmosphere closest to the Earth's surface, the stratosphere exhibits a relatively small change in temperature with an increase in altitude.

This is due in part to the fact that the stratosphere is heated from above by the absorption of ultraviolet radiation by ozone, rather than from below by the Earth's surface.

The temperature stability of the stratosphere makes it an important layer of the atmosphere for aviation and weather forecasting. It also plays a crucial role in regulating the Earth's climate, as changes in the concentration of ozone and other stratospheric gases can affect the amount of solar radiation that reaches the Earth's surface.

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Vorticity refers to: Select one: a. the rising and sinking of air along weather fronts. b. the formation of clouds. c. the spin of air parcels. d. the changing of the seasons. e. the development of a wave cyclone.

Answers

Vorticity refers to the rotation or spin of air parcels in the atmosphere. It is an essential concept in the study of weather and atmospheric dynamics. It helps in predicting and understanding weather patterns. The correct answer is option C.

Vorticity can be caused by different factors, including the Earth's rotation, wind shear, and changes in atmospheric pressure.

Positive vorticity is associated with counterclockwise (cyclonic) rotation, while negative vorticity is associated with clockwise (anticyclonic) rotation. Vorticity plays a crucial role in the development of various weather phenomena, including cyclones, anticyclones, and thunderstorms.

For example, regions of high vorticity can be associated with the formation of tornadoes, while regions of low vorticity can be associated with stable atmospheric conditions.

Understanding vorticity is important in predicting and understanding weather patterns, which can have significant impacts on society and the environment. The correct answer is option C.

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Inhabitants of oceanic islands resemble forms of the nearest mainland but show some differences. This is an example of

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Oceanic islanders resemble the nearby mainland in form, although they also exhibit certain distinctions. As an illustration of biogeographical.

In general, islands have fewer species than the nearest mainland due to their isolation and smaller size, but the species present on islands are often closely related to those on the nearest mainland.

The resemblance between island and mainland species can be attributed to a process called colonization, whereby organisms from the mainland migrate to the island and establish a new population. Over time, this population may undergo genetic changes due to isolation, natural selection, and genetic drift, leading to the evolution of distinct island forms. This can result in differences in morphology, behavior, and genetics between island and mainland populations.

The similarities and differences between island and mainland species provide insights into how species evolve and adapt to new environments, and how they respond to changes in their habitats over time.

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The distinction between a valley and a canyon is ________.Group of answer choicesnonexistent; the two terms are synonymousthat valleys are often cut by streams, whereas canyons are eroded by the windthat the sides of a valley are more steep than those of a canyonthat the sides of a canyon are more steep than those of a valley

Answers

The distinction between a valley and a canyon is that valleys are often cut by streams, whereas canyons are eroded by the wind.

A canyon is a small, deep valley with cliff-like sides. The word "canyon" is derived from the Spanish word caon, which is a synonym for "tube" or "pipe." Although "gorge" is frequently used interchangeably with "canyon," a gorge is almost always narrower and steeper.

A valley is a long, low terrain that frequently stretches between hills or mountains. It usually has a river or stream that flows from one end to the other. The majority of valleys are the result of the long-term erosion of the land's surface by rivers or streams. Some valleys are created by glacial ice erosion.


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The urban heat island effect is typically stronger closer to downtown. stronger closer to parks and hiking trails. stronger closer to wooded areas.

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The urban heat island effect is typically: stronger closer to downtown areas. The correct option is C.

This phenomenon occurs when urban areas, such as cities, experience higher temperatures than their surrounding rural areas. This temperature difference is due to several factors, including the concentration of buildings, roads, and other infrastructure that absorb and retain heat, the reduction of vegetation and natural surfaces, and the production of waste heat from human activities.

In downtown areas, there is a higher concentration of concrete, asphalt, and other heat-absorbing materials. These surfaces absorb solar radiation during the day and release it at night, causing temperatures to remain elevated. Additionally, downtown areas usually have less vegetation and natural surfaces, such as parks, wooded areas, or hiking trails, which can help dissipate heat through processes like evapotranspiration.

Conversely, areas closer to parks, hiking trails, and wooded areas tend to have lower temperatures due to the presence of more vegetation and natural surfaces. These green spaces provide shade, reduce the amount of heat absorbed by surfaces, and promote cooling through evapotranspiration. Therefore, the urban heat island effect is less pronounced in these areas compared to downtown locations.

In summary, the urban heat island effect is stronger closer to downtown areas due to the concentration of heat-absorbing materials, lack of vegetation, and waste heat generated by human activities. Green spaces like parks, wooded areas, and hiking trails help mitigate this effect by providing cooling and heat dissipation through natural processes.

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The urban heat island effect is typically:

a. stronger closer to downtown.

b. stronger closer to parks and hiking trails.

c. stronger closer to wooded areas.

Rocks of the continental crust contain different minerals and each mineral has its own melting point. If the minerals with the lowest melting temperatures are the only ones melted, this is referred to as ______ melting. Multiple choice question.

Answers

Rocks of the continental crust contain different minerals and each mineral has its own melting point. If the minerals with the lowest melting temperatures are the only ones melted, this is referred to as partial melting. So the correct option is a.

Partial melting is the process in which only some minerals in a rock melt, typically those with lower melting points. This results in the formation of a melt that is compositionally different from the parent rock. As different minerals have different melting points, partial melting can occur over a range of temperatures as the temperature of the rock increases. This process is important in the formation of magmas that can then cool and crystallize to form igneous rocks.

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Rocks of the continental crust contain different minerals and each mineral has its own melting point. If the minerals with the lowest melting temperatures are the only ones melted, this is referred to as ______ melting. Multiple choice question.

a. partial

b. complete

c. fractional

d. intrusive

A weak trough of low pressure found in the tropics and along which hurricanes occasionally form is called a(n) ____.

Answers

A weak trough of low pressure found in the tropics and along which hurricanes occasionally form is called an easterly wave.

Easterly waves are low-pressure systems that migrate from east to west over the tropics, most notably in the Atlantic Ocean. They are abundant throughout hurricane season (June to November) and, if conditions are favourable, can develop into tropical storms or hurricanes.

Easterly waves are created by the interaction of trade winds and the Earth's rotation, which can induce atmospheric disturbances.

These disturbances can sometimes become more intense, resulting in the formation of tropical cyclones.

However, not all easterly waves develop into tropical cyclones because other factors such as wind shear and sea surface temperatures also play a role in their formation.

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What principle is based on geoscientists observations of natural history where rock layers are deposited in a time sequence, with the oldest on the bottom and the youngest on the top

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The principle that is based on geoscientists' observations of natural history where rock layers are deposited in a time sequence, with the oldest on the bottom and the youngest on top, is known as the principle of superposition.

This principle, which asserts that in an undisturbed sequence of sedimentary rocks, each layer is younger than the one under it and older than the one above it, is a fundamental idea in geology.

This is because sedimentary rocks are generated by the accumulation of particles such as sand, mud, or gravel that settle out of water or air.

As new sediments accumulate on top of older layers, a sequence of rock layers is gradually built up. Through processes such as compaction and cementation, these layers may become buried and lithified, or turned into rock, over time.

Geoscientists can learn about the geological history of a region by researching the different rock strata and their features.

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River ______ are relatively flat benches that are perched above a river or stream and stair-step upward and outward from the active channel.

Answers

River terraces are elevated flat areas found along the sides of a river or stream. They are formed over time as the river cuts into the landscape and erodes its banks.

The terraces are created as the river's flow changes and the water level drops. As the river cuts into the banks, it leaves behind flat, elevated areas that were once the river's floodplain. Over time, the river cuts deeper into the landscape, leaving the terraces higher and farther from the active channel. River terraces can have several different levels, each representing a different time period when the river flowed at a different level. The stair-step appearance is created as the river cuts into the banks and leaves behind different levels of terraces. These terraces can provide important information about the history of the river, including its past flow patterns, changes in water levels, and changes in the landscape around it. River terraces can also be important for human activity, providing flat areas for development and agriculture. However, they can also be vulnerable to erosion and flooding, so it's important to carefully manage any development or activity that takes place on them.

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When a seismic wave hits an interface and some of the energy is sent back toward the surface, that wave is said to have been:

Answers

When seismic waves encounter an interface, some of the energy is reflected back towards the surface, while the rest of the energy can either be transmitted through the boundary or refracted in a different direction. The correct answer is option 3.

Therefore, the wave that reflects back towards the surface is said to have been reflected, while the wave that is bent as it crosses that boundary is said to have been refracted.

Reflection occurs when a wave encounters a boundary separating two different materials with different physical properties, causing some of the energy to bounce back towards the surface.

This phenomenon is used to locate the position of subsurface boundaries and geologic structures. Refraction, on the other hand, occurs when a wave passes through a material with different physical properties, causing the wave to bend.

The amount of bending depends on the angle of incidence and the difference in seismic wave speeds between the two materials.

In summary, seismic waves that hit an interface and are reflected back towards the surface are said to have been reflected, while the waves that are bent as they cross that boundary are said to have been refracted. The correct answer is option 3.

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Complete Question:

When a seismic wave hits an interface and some of the energy is sent back toward the surface, that wave is said to have been ____. whereas when a seismic wave hits an interface and some of the energy is bent as it crosses that boundary, the wave has been ____.

1. defracted; deflected

2. refracted; reflected

3. reflected; refracted

4. deflected; defracted

QUESTION 1 Calculate the relative humidity for the following air parcel. Round your answer to one decimal place (ex. 21.1 or 11.3). You do not need to insert the percent symbol in your answer but do keep in mind to express your answer as a percent (ex. .211 is 21.1%, so your answer would be 21.1) Actual water vapor content 35.5g/kg Maximum water vapor content = 39.1g/kg

Answers

Relative humidity is the ratio of the partial pressure of water vapor in the air to the saturated vapor pressure of water at a specific temperature and pressure. It is expressed as a percentage and indicates how much moisture the air is holding compared to the maximum amount it could hold at that temperature and pressure.

Relative humidity = (Actual water vapor content / Maximum water vapor content) x 100%

Given,

Actual water vapor content = 35.5 g/kg

Maximum water vapor content = 39.1 g/kg

Substituting these values in the above formula, we get

Relative humidity = (35.5 / 39.1) x 100% = 90.8%

Therefore, the relative humidity for the given air parcel is 90.8%.

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When a river is in a steady state in which the balance between the supply of sediment and the amount of sediment that the river can carry is in a near equilibrium, the river is referred to as a(n)

Answers

When a river is in a steady state, in which the balance between the supply of sediment and the amount of sediment that the river can carry is in near equilibrium, the river is referred to as a graded stream.

A graded stream is a river that has achieved a state of balance between the amount of sediment it transports and the amount of sediment it can move, so that its channel maintains a consistent size and shape over time.

In a graded stream, the river's flow and sediment transport are in a state of dynamic equilibrium, with the river eroding sediment in some areas and depositing it in others.

The river's channel is typically well-defined and stable, with a steady flow and predictable behavior. Graded streams are important natural resources and support a variety of ecosystems and human activities.

They can provide habitat for aquatic species, support recreational activities such as fishing and boating, and provide important water resources for human communities.

In summary, a graded stream is a river that has achieved a state of balance between the amount of sediment it transports and the amount of sediment it can move, resulting in a well-defined and stable channel with a steady flow and predictable behavior.

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