Far below the Earth's surface, intrusive or plutonic igneous rocks are created as lava cools and solidifies in these regions. Stocks, laccoliths, sills, and , among other intrusive features, form. Hence option C is correct
Which feature forms when magma cools beneath Earth's surface?Magma chambers are underground reservoirs where magma is kept in reserve. Conduits are the routes it makes and takes to reach the surface. It's common to refer to this network as the volcano's plumbing system. These networks have a wide region of coverage.
Far below the Earth's surface, intrusive or plutonic igneous rocks are created as lava cools and solidifies in these regions. Stocks, laccoliths, sills, and , among other intrusive features, form. After an , if the conduits are empty, they may to produce calderas or they may persist as lava tubes and caves.
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Answer: C. Batholiths
data indicate that we have overshot earth's biocapacity -- its capacity to support us -- by 50%. we are using renewable natural resources 50% faster than they are being replenished. about how many times larger was the global ecological footprint in 2007 than it was in 1962?
We began to exceed Earth's support capacity in 1970. Over time, the ecological footprint across the globe has generally increased, with brief periods of decrease.
Since then, this situation, which is known as "ecological overshoot," has persisted. The Earth would need 1.5 years to regenerate the renewable resources that people used in 2008 and absorb CO2 waste if the overshoot is 50%.
How much of our planet's biocapacity is being exceeded?1.8 times faster than our planet's biocapacity can regenerate, humanity is using nature. That amounts to utilizing 1.8 Earths' worth of resources.
What happens if our biocapacity is exceeded?When human demands on nature exceed the biosphere's supply, or regenerative capacity, global overshoot occurs. Such overshoot prompts a consumption of Earth's life supporting normal capital and a development of waste.
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Mr. Alvarez works in the city of San Francisco. He drives to his home in a community just outside the city. He lives in A. a rural areaB. an urban areaC. a suburban area
Answer: suburban area
Explanation:
In the triangle DEF, DE = 10 inches and EF = 14 inches. What inequality describes the possible side lengths of side DF, in inches?
In a triangle, one side's length must be more than the difference between the other two sides and less than the total of the lengths of the other two sides.
This can be said in the following way:
DF EF + DE |EF - DE|
Inputting the values provided yields:
|14 - 10| < DF < 14 + 10
When we reduce the inequality, we obtain:
4 < DF < 24
As a result, side DF can have side lengths that are both longer than 4 inches and shorter than 24 inches.
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where are most modern divergent plate boundaries found?
The most modern divergent plate boundaries found in mid-ocean oceanic ridges
New oceanic crust is formed along divergent boundaries, which are also known as spreading boundaries, when two tectonic plates move apart from one another and create space between them. The majority of divergent boundaries may be found running parallel to oceanic ridges in the middle of the ocean. The Mid-Ocean Ridge System is a massive mountain range that is found deep within the ocean and is the most extensive geological formation on the planet.
The new crust that forms at the plate boundary is warmer than the crust that surrounds it. As a result, it has a lower density than the crust that surrounds it, which causes it to sit higher on the mantle, thus producing a mountain chain. A rift valley that is between 25 and 50 kilometers broad and one kilometer deep runs down the middle of the mid-ocean ridge. Oceanic spreading ridges may have the appearance of being curved landforms on the surface of the Earth; but, in reality, the ridges are made up of a sequence of straight-line segments that are offset at intervals by faults that are perpendicular to the ridge and are referred to as transform faults.
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listed below are several sets of soil properties and soil descriptions. match the properties with the descriptions. a) fibrous peat with some sand from ann arbor, michigan b) bentonite (montmorillonite) from billings, montana c) glacial outwash from palmer, alaska d) volcanic ash from hilo, hawaii e) glacial till from chicago, illinois
Matching the properties of soil with given description are Sample 1 is bentonite (montmorillonite) from Billings, Montana (Option B), Sample 2 is volcanic ash from Hilo, Hawaii (Option D), Sample 3 is glacial outwash from Palmer, Alaska (Option C), sample 4 is fibrous peat with some sand from Ann Arbor, Michigan (Option A), and Sample 5 is glacial till from Chicago, Illinois (Option E).
Sample 1 is bentonite (montmorillonite) from Billings, Montana as the presence of montmorillonite mineral in bentonite makes it highly plastic. Sample 2 is volcanic ash from Hilo, Hawaii as the soil consists of finer texture with higher proportion of sand and clay than gravel and lower plasticity. Sample 3 is glacial outwash from palmer, Alaska which is made up of deposit of sand and gravel and low moisture content and specific gravity of 2.65. Sample 4 is fibrous peat with some sand from Ann Arbor, Michigan as peat is characterized by high moisture content and low specific gravity. Sample 5 is glacial till from Chicago, Illinois as it only contains sand and silt with high specific gravity.
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an ecologist estimated 800 star-nosed moles, condylura cristata, per square mile in one woodlot and 1,600 per square mile in another woodlot. what was the ecologist comparing?
Condylura cristata, a star-nosed mole species, population densities in two distinct woodlots were being compared by an ecologist. The ecologist predicted 800 moles per square mile in the first woodlot and 1,600 moles per square mile in the second woodlot.
This suggests that the second woodlot's star-nosed mole population density was twice as high as the first woodlot's.
The results of the ecologist's investigation into the variation in star-nosed mole populations between the two woodlots show that there is a larger density of the species in the second woodlot.
This comparison suggests that the second woodlot may be more favourable for the species than the first, and may need to be better protected and maintained in order to ensure the species' survival. As a result, it may be used to influence conservation and management decisions.
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Answer both questions for Brainliest
In which world region would core countries be predominant? (Check your Wallerstein’s World Systems map)
In which world region would primary countries be predominant? (Check your Wallerstein’s World Systems map)
Answer: Core countries are predominant in western areas, i.e. Western Europe, US, Canada, Australia. I am not sure what the question is referring to by "primary" but semi-periphery countries are developing nations like Mexico and China, while periphery countries are poor, more economically insignificant countries like many African and Asian countries.
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with time, a butte will most likely become a: group of answer choices plateau pillar or pinnacle mesa playa
A butte is a flat-topped hill with steep sides, typically found in arid regions.
One possibility is that a butte could become a mesa, which is a larger, flat-topped hill or mountain with steep sides. Mesas are typically larger than buttes and can be hundreds or even thousands of feet high.
Another possibility is that a butte could become a plateau, which is a large, flat-topped area of land at a high elevation. Plateaus are often created by the gradual uplift of land over millions of years, and they can be thousands of feet in elevation.
A butte could also become a pillar or pinnacle if the surrounding rock erodes away more quickly than the butte itself. This could leave behind a tall, narrow column of rock that rises above the surrounding terrain.
Finally, a butte could become a playa, which is a dry lakebed that forms in a basin or depression. This would happen if the butte erodes away completely, leaving behind a flat, sandy area that can collect water during periods of heavy rain.
So, a butte can become any of these geological features with time, depending on the specific conditions and processes of erosion and weathering in the area.
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what mountain range extends from the black sea to the caspian sea
What would you call a granite that has undergone metamorphism and now exhibits foliation? A. basalt B. lava C. gneiss D. limestone E. granite.
option C. gneiss would you call a granite that has undergone metamorphism and now exhibits foliation.
Metamorphism is the process by which preexisting rocks are transformed into new forms due to increases in temperature, pressure, and chemically active fluids. Igneous, sedimentary, and other metamorphic rocks may be affected by metamorphism.
Contact, regional, and dynamic metamorphism are the three types of metamorphism. When magma comes into contact with an already existing body of rock, contact metamorphism occurs. When this occurs, the existing rocks' temperature rises and they become infiltrated with magma fluid.
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how would you put “Romancy” “Elegancy” and “Distancy” ina sentence
Answer:
The candlelit dinner combined the romancy of a love story, the elegancy of classical music, and a comfortable level of distancy to allow for intimate conversations
Explanation:
Explain two benefits to tourists of accommodation grading.
Answer:
It gives a reliable indication of expected services and offerings. It helps consumers to find hotels of a standard they require. It allows for design and target of training activities. It demonstrates commitment to quality.
can you complete this concept map that reviews the basic concepts of energy? part a drag the terms to the appropriate locations on the concept map.
The complete concept map which reviews the basic concepts of energy is attached.
Energy refers to the ability or capacity to perform work. It is quantitative property transferable to a body or a physical system in recognition of performance of work in the form of heat and light. Energy is a conserved quantity as energy can be converted in form, but not created or destroyed.
Energy exists in various forms such as potential, kinetic, thermal, electrical, nuclear, etc. Hence, the form of energy in the concept maps are kinetic (A) and potential (B). Kinetic energy refers to the energy an object due its motion, hence it is the energy of motion (C). Potential energy refers to the energy which is stored or conserved in an object and depends upon the relative position of various parts of a system. Chemical energy (D) is an example of potential energy.
The transfer or transformation of energy leads to increases in degree of randomness or disorder. Entropy (E) refers to the measurement of degree of randomness. It is the increase in the disorganization within a system. When energy transfers or transforms, some of it is converted to heat (F).
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The series of processes which rock forms, changes from one type to another, is destroyed and forms again by geological processes is called?
The series of processes which rock forms, changes from one type to another, is destroyed and forms again by geological processes is called the rock cycle.
The rock cycle describes how rocks and minerals are formed, transformed, and broken down over time due to the interaction of physical, chemical, and biological processes. The rock cycle involves three main types of rock: igneous, sedimentary, and metamorphic.
Igneous rocks are formed when molten rock (magma or lava) cools and solidifies. These rocks can be weathered and eroded over time, breaking down into smaller particles that can become the building blocks of sedimentary rocks.
Sedimentary rocks are formed from the accumulation and lithification (compaction and cementation) of sediments such as sand, mud, and organic debris. These rocks can be buried and subjected to heat and pressure, which can cause them to transform into metamorphic rocks.
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which of the four main classes of sedimentary rock forms by the precipitation of minerals directly from water, without help from living organisms?
The class of sedimentary rock that forms by the precipitation of minerals directly from water, without help from living organisms, is called "Chemical sedimentary rock".
Chemical sedimentary rocks are formed when minerals dissolved in water precipitate out of the solution due to a change in the environment, such as a change in temperature or pressure, or a change in the chemistry of the water. Examples of chemical sedimentary rocks include rock salt, gypsum, and chert.
Chemical sedimentary rocks are formed when minerals dissolved in water precipitate out of the solution due to a change in the environment. The process of precipitation occurs when the concentration of minerals in the water exceeds their solubility, resulting in the formation of solid minerals that settle out of the water and accumulate on the bottom of a basin or in a body of water.
Chemical sedimentary rocks can form in a variety of environments, including lakes, oceans, caves, and hot springs. For example, rock salt (halite) forms in shallow, salty lakes or basins where water evaporates and leaves behind a deposit of salt. Gypsum, another chemical sedimentary rock, forms in evaporite basins, where the concentration of dissolved calcium and sulfate ions in the water becomes high enough to precipitate gypsum.
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Subduction zones occur at what types of plate boundaries?
Answer:
Convergent Plate Boundaries
Explanation:
the oceanic climate region that is characterized by dry, descending air, little precipitation, and high ocean salinity is:
The oceanic climate region that is characterized by dry, descending air, little precipitation, and high ocean salinity is the subtropical high-pressure belt.
This belt is located between 20 and 35 degrees north and south of the equator, and it is known for its arid conditions, which are caused by descending air that suppresses cloud formation and precipitation.
The subtropical high-pressure belt is also associated with high levels of ocean salinity, as the lack of rainfall causes increased evaporation and concentration of salt in the water.
This climate region is important for agriculture, as it can support crops that are adapted to dry conditions, such as olives, citrus fruits, and grapes. However, it can also pose challenges for water resources and ecosystem health, as the lack of rainfall can lead to drought and desertification.
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which of the following rock types represents the highest grade of metamorphism? radio button unchecked gneiss radio button unchecked slate radio button unchecked phyllite radio button unchecked schist submit
Of the four options provided, gneiss represents the highest grade of metamorphism. Gneiss is a metamorphic rock that forms from the recrystallization of pre-existing rocks under high temperatures and pressures.
Metamorphic rocks are formed through the transformation of existing rocks under high pressure and temperature conditions. Gneiss is one of the most common types of metamorphic rocks and represents the highest grade of metamorphism. This rock type forms through the recrystallization of pre-existing rocks, which leads to the formation of bands of different minerals. The high pressure and temperature conditions under which gneiss forms cause the minerals to align in a characteristic banded pattern. The minerals that make up gneiss may include quartz, feldspar, mica, and amphibole.
Compared to other metamorphic rocks, such as slate, phyllite, and schist, gneiss is considered to be a higher grade of metamorphic rock. Slate is a low-grade metamorphic rock that forms from the recrystallization of shale, while phyllite is a higher grade rock that forms from the recrystallization of slate. Schist is also a higher grade rock that forms from the recrystallization of pre-existing rocks.
In conclusion, gneiss is a high-grade metamorphic rock that forms through the recrystallization of pre-existing rocks under high pressure and temperature conditions. Its characteristic banded pattern and mineral composition make it distinct from other metamorphic rocks, and it is widely used in construction and architectural projects.
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What's the difference living in Kenya than Honduras
The main difference between living in Kenya and Honduras is the climate. Kenya has a tropical climate with hot temperatures and high humidity, while Honduras has a subtropical climate with cooler temperatures and lower humidity.
What makes living in Kenya different from Honduras?As of 2020, Kenya had a GDP per capita of $4,200 whereas Honduras had a GDP per capita of $5,100. have an 86.0% lower chance of being unemployed.
The climate is the primary distinction between living in Kenya and Honduras. Honduras has a subtropical climate with cooler temperatures and lesser humidity, in contrast to Kenya's tropical climate, which is hot and humid. With an estimated population of over 50 million people compared to Honduras' population of just over 9 million, Kenya also has a far higher population density than Honduras. In addition, Kenya has a considerably more varied economy than Honduras, with a significant emphasis on manufacturing, agriculture, and tourism.
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how is land owned in a typical village that practices shifting cultivation
Traditionally, villages would own all of the land; the chief would designate plots of land to individual families, who would reap the benefits of the land's yields. Private individuals now own land in places like Latin America.
Shifting cultivation is an agricultural system in which plots of land are temporarily cultivated and then abandoned, allowing post-disturbance fallow vegetation to grow freely while the cultivator moves on to another plot.
The cultivation period is usually ended when the soil shows signs of exhaustion or, more commonly, when the field becomes overrun by weeds. The time spent cultivating a field is usually shorter than the time spent allowing the land to regenerate by lying fallow.
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three of the images show examples of settings where decompression melting is taking place. one image shows an example of a setting where flux melting is taking place. in which geological setting is flux melting taking place?
Flux melting occurs at subduction zones where one tectonic plate is forced beneath another plate into the Earth's mantle.
Flux melting is a type of melting that occurs at subduction zones, where one tectonic plate is forced beneath another plate into the Earth's mantle. In this process, the descending plate releases fluids such as water, carbon dioxide, and other volatiles that are trapped within the rocks. These fluids act as a flux, lowering the melting temperature of the mantle rocks and resulting in partial melting, which generates magma.
The process of flux melting is different from decompression melting, which occurs at mid-ocean ridges, where hot magma rises to the surface due to the reduced pressure at divergent plate boundaries. Decompression melting can also occur at mantle plumes, where rising hot magma generates volcanoes.
Understanding the different types of melting processes is crucial for studying the formation of igneous rocks and the processes that drive plate tectonics. By identifying the different geological settings where these processes occur, scientists can gain a better understanding of the Earth's interior and the forces that shape our planet.
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What are the 3 most populated cities in Mato Grosso Do Sul?
Answer:
1, Campo Grande, 903,710 ; 2, Dourados, 210,510 ; 3, Três Lagoas, 119,330
Explanation:
Why do farmers in Sub-Saharan Africa utilize slash-and-burn agriculture?
a. to improve soil quality
b. to prevent pest infestations
c. to minimize air pollution
d. to reduce labor needs
The farmers in Sub-Saharan Africa utilize slash-and-burn agriculture to reduce labor needs (option d)
Farmers in Sub-Saharan Africa utilize slash-and-burn agriculture because it is a traditional and low-cost method of clearing land for farming. The method involves cutting and burning trees and other vegetation to clear land and fertilize the soil with the ash produced by the burning. This practice helps to increase soil fertility and control pests and weeds, making the land suitable for farming.
In addition, the ash left from the burning is rich in nutrients, providing a source of fertilization for crops. However, this method can also have negative environmental impacts, such as soil degradation and loss of biodiversity, and it can contribute to greenhouse gas emissions and climate change.
Despite these negative impacts, slash-and-burn agriculture remains a common practice in many areas of Sub-Saharan Africa due to its low cost and its effectiveness in preparing land for farming.
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question what do lines on a contour map indicate? responses degrees east and west of the equator degrees east and west of the equator elevation above sea level elevation above sea level degrees north and south of the equator degrees north and south of the equator where geological features converge where geological features converge
What is an angular distance measured north or south of the equator from the center of Earth termed?
The angular distance measured north or south of the equator from the center of Earth is termed "latitude".
Latitude is an angular distance that measures how far north or south of the equator a location is on Earth, measured from the center of the Earth. The equator is defined as 0 degrees latitude, and the North and South poles are defined as 90 degrees north and 90 degrees south latitude, respectively.
Latitude lines run parallel to the equator and are often used to determine a location's climate, as well as for navigation purposes.
By knowing the latitude of a location, one can determine the length of daylight and the position of the sun in the sky, as well as how far north or south of the equator a person is. Latitude is an important tool for geography and is often used to locate places on maps and globes.
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therm is a unit that is generally used to measure the energy contained in natural gas. true or false?
The statement ''a therm is a unit that is generally used to measure the energy contained in natural gas'' is false because therm is a unit of measurement, it is not specific to natural gas.
A therm is actually a unit of heat energy, and it can be used to measure the energy content of any fuel source. One therm is equal to 100,000 BTUs (British Thermal Units), which is a standard unit of energy commonly used in the United States.
Natural gas is commonly measured in therms, but it is not the only fuel source that can be measured this way. Other fuels that can be measured in therms include propane, oil, and even electricity.
It is important to note that the energy content of natural gas can vary depending on its composition and source. However, the therm provides a standardized unit of measurement that can be used to compare the energy content of different fuel sources.
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State infographic that of berg vinds (2) which the two 14hoo os the reference Process berg Coast atmospheric have conditions. evident resulted in the in the Information to the temperature graph, explain OF temperature Change from from 03.15 to winds blow from the Interior to Skies?
rank the following steps describing how a clastic sedimentary rock forms from its pre-existing parent rock. 1) lithification 2) deposition 3) transportation 4) weathering 5) erosion
Weathering, erosion, transportation, deposition, and lithification are the five steps in the formation of a clastic sedimentary rock from its pre-existing parent rock.
Weathering is the first step in the process of clastic sedimentary rock formation. Weathering is the breakdown of the parent rock into smaller pieces due to the action of wind, water, and temperature changes.
Erosion is the second step in the process of clastic sedimentary rock formation. Erosion is the process by which the smaller pieces of the parent rock are removed from the surface and transported to other locations due to the action of wind, water, and ice.
Transportation is the third step in the process of clastic sedimentary rock formation. Transportation involves the movement of the smaller pieces of the parent rock from one location to another.
Deposition is the fourth step in the process of clastic sedimentary rock formation. Deposition is the process of the smaller pieces of the parent rock being deposited in a new location.
Lithification is the fifth and final step in the process of clastic sedimentary rock formation. Lithification is the process of the smaller pieces of the parent rock being compacted and cemented together to form a solid rock.
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Full Question: Rank the following steps describing how a clastic sedimentary rock forms from its pre-existing parent rock. (5 items) (Drag and drop into the appropriate area). weathering, lithification, deposition, transportation, erosion
was the earthquake that occurred at 17 n latitude and 121 e longitude, at a depth of 124 km, shallow, intermediate or deep? did it occur at a divergent, convergent, or transform plate boundary, or was it not near a plate boundary?
An earthquake at 17 N latitude and 121 E longitude, with a depth of 124 km, is considered to be a deep earthquake.
Deep earthquakes, as the name implies, occur at depths greater than 70 km below the Earth's surface. These types of earthquakes are generally associated with subduction zones, where one tectonic plate is forced beneath another plate. This process creates a deep seismic zone, which can produce earthquakes at greater depths.
Subduction zones occur at convergent plate boundaries, where two tectonic plates are moving towards each other. One plate is forced beneath the other, creating a deep trench and a chain of volcanoes on the overriding plate. The deep earthquakes that occur in subduction zones can be caused by a variety of factors, including the release of stress as the subducting plate bends and deforms, or the movement of fluids and the associated changes in pressure and temperature.
In conclusion, the earthquake that occurred at 17 N latitude and 121 E longitude, with a depth of 124 km, is a deep earthquake that is likely associated with subduction at a convergent plate boundary. However, without additional information about the earthquake, it's impossible to determine the exact cause of the earthquake.
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identify the four tectonic settings of igneous activity.
