in nasa's a short tour of the cryosphere, why is the snow of the rockies important to the midwest united states? group of answer choices

Prairies are the most valuable biome for agriculture in light of the fact that the dirt is by and large profound and fruitful. Very nearly one billion individuals depend on prairies for their occupation or as a food source.

"Arable cultivating" and "Peaceful cultivating" are the two fundamental kinds of agribusiness in light of the accessibility of land. Arable cultivating: This is the development of harvests, for the most part on complement land where the dirt is of more excellent.

Most unmodified prairies are utilized for broad domesticated animal creation, with fire and brushing the essential administration apparatuses.

There are five significant sorts of biomes: amphibian, prairie, timberland, desert, and tundra, however, a portion of these biomes can be additionally partitioned into additional particular classifications, like freshwater, marine, savanna, tropical rainforest, mild rainforest, and taiga. Amphibian biomes incorporate both freshwater and marine biomes.

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Igneous rocks are made up of different minerals depending on the type of rock. The most common minerals found in igneous rocks are quartz, feldspar, mica, hornblende, and pyroxene. Quartz is usually colorless or white, feldspar can be white, pink, or gray, mica can range from green to brown to black, hornblende is usually black or green, and pyroxene is usually black.

Granite is an example of an igneous rock that contains quartz, feldspar, mica, and hornblende. Basalt is an example of an igneous rock that contains feldspar, pyroxene, and sometimes olivine. Peridotite is an example of an igneous rock that contains olivine, pyroxene, and sometimes hornblende.

The minerals in igneous rocks can be identified using a variety of methods including color, hardness, streak, luster, and cleavage. Color can be used to distinguish between different minerals; quartz is usually colorless or white, feldspar is usually pink, gray, or white, mica is usually green, brown, or black, hornblende is usually black or green, and pyroxene is usually black.

Hardness is another way to distinguish between different minerals. Quartz is the hardest mineral and has a hardness of 7 on the Mohs scale. Feldspar is slightly softer with a hardness of 6, mica has a hardness of 2-3, hornblende has a hardness of 5-6, and pyroxene has a hardness of 5-6.

The streak of a mineral is the color it leaves when scratched on a streak plate. The streak of quartz is white, the streak of feldspar is white or gray, the streak of mica is white, the streak of hornblende is black, and the streak of pyroxene is black.

Luster is another way to identify different minerals. Quartz has a vitreous luster, feldspar has a pearly or dull luster, mica has a pearly or silky luster, hornblende has a vitreous or pearly luster, and pyroxene has a vitreous or dull luster.

The cleavage of a mineral is how it breaks when it is struck or compressed. Quartz has no cleavage, feldspar has two directions of cleavage, mica has one direction of cleavage, hornblende has two directions of cleavage, and pyroxene has two directions of cleavage.

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The geologic materials most commonly associated with earth failures are clay minerals. option 2 is correct.

Clay minerals: clay mineral is natural or synthetic, might include non-phyllosilicates, without size criterion, plastic, and hardens on drying or firing. The clay minerals consist of essential elements like silica, magnesia or alumina, or both, and water, but iron substitutes for aluminum and magnesium in varying degrees, and appreciable quantities of potassium,  calcium, and sodium are frequently present as well.

Geological materials are the material extracted as-is from the earth in sediment or rock form, including rocks, sands, clays, limestone, and other industrial minerals. Earth failures are falling, exfoliating, sliding, and toppling.

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The complete question is -

The geological materials most commonly associated with earth failures are?

options

1. quartz

2. clay minerals

3. granite

4. basalt

Clastic sedimentary rock is formed when precipitation of gypsum due to evaporation of seawater occurs.

Clastic sedimentary rock is formed when fragments of pre-existing rocks or minerals are compacted and cemented together.  Clastic sedimentary rocks are formed from the accumulation and consolidation of fragments of pre-existing rocks or minerals, which are transported and deposited by various agents such as water, wind, or ice. Examples of clastic sedimentary rocks include sandstone, shale, and conglomerate.

Gypsum is a mineral that can be precipitated from evaporating seawater, but it does not form clastic sedimentary rock. Gypsum can form chemical sedimentary rocks, such as rock gypsum or alabaster.

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Kilauea is not as explosive as the eruption of Mt. St. Helens due to the difference in magma viscosity and gas content. The overall control that dictates this difference is magma composition and gas content.

The magma composition of Kilauea is primarily basaltic, which has a low viscosity, and gas content is less than that of Mt. St. Helens. Due to these properties, the lava can flow easily and doesn't create any blockages or blockage pressure. Hence, the eruption is effusive and not explosive. The effusive eruption leads to slow-moving lava flows that do not have the potential to be very destructive.

On the other hand, Mt. St. Helens has an andesitic composition, which has a higher viscosity and more gas content. It leads to the creation of blockages within the vent of the volcano, which ultimately leads to an explosive eruption. When the pressure built up inside the vent due to the blockage, it eventually led to an explosive eruption.

The difference in the viscosity of magma, and gas content is an overall control that dictates the difference between the two volcanoes' eruption. Therefore, it is concluded that the difference in magma composition and gas content is responsible for the difference in the explosiveness of Kilauea and Mt. St. Helens' eruption.

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In the environment, foliated intermediate- to high-grade metamorphic rocks called gneiss would form.

Slate, phyllite, schist, & gneiss are the several types or foliated metamorphic rocks, ordered by of the grade or severity of metamorphic rocks and the type of foliation.

Metamorphic rocks of intermediate grade also contain garnet and mica. At 800 degrees Celsius, high grade metamorphic stones develop in regions that are so hot they virtually melt. Sillimanite, a mineral that is commonly found inside the rock gneiss, is one that develops in this extreme heat.

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The types of pyroclastic debris include the following: a) lapilli, d) ash, c) blocks, and g) lahars.

Lapilli are small fragments of volcanic debris with a size range between 2 mm to 64 mm. Ash is fine volcanic debris with a size less than 2 mm. Blocks are large, solid pieces of volcanic material that can be greater than 64 mm.

Lahars are mudflows composed of volcanic material mixed with water. Lava, magma, and gas are not considered pyroclastic debris since they are not ejected explosively during volcanic eruptions but rather flow out of the volcano in a more controlled manner.

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If an igneous rock is in contact with sandstone and the sandstone appears discolored and baked, it can be inferred that the igneous rock is younger than the sandstone.

This is because the heat and pressure generated by the intrusion of the molten igneous rock would have altered the sandstone, creating a zone of contact metamorphism. The high temperatures of the molten rock would have caused the minerals in the sandstone to recrystallize and fuse together, leading to a change in texture and color. This type of contact metamorphism occurs when an intrusion of magma or lava comes into contact with cooler rocks and is a useful tool in determining the relative ages of rocks in an area.

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The main circumstance which most Central African nations experienced since gaining independence is problem of corruption and ethnic conflict. The Option 1 is correct.

Corruption has been a major issue in many African countries, with government officials and business leaders embezzling public funds and engaging in other forms of corrupt practices. This has led to widespread poverty, economic stagnation, and political instability.

Ethnic conflict has also been a recurring problem in many Central African nations, often fueled by political or economic competition between different groups. These conflicts have led to displacement, violence, and loss of life.

Also, poor transportation systems, lack of infrastructure, and other development challenges have also been prevalent issues in the region. While some countries have experienced resource booms from minerals such as diamonds and natural gas, many have struggled to benefit from their natural resources due to corruption and mismanagement.

Full question "Which circumstances have most Central African nations experienced since gaining independence? 1. corruption and ethnic conflict 2. ethnic conflict 3. pollution of the air and destruction of plants and animals 4. iron ore diamonds and natural gas 5. palm oil 6. exploiting the colonies for profit 7. Portugal 8. Central African Republic 9. Men and women eat in separate rooms. 10. poor transportation system"

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Temperature, pressure, wind and moisture are measured through the depth of the troposphere using Rawinsonde instrument.

Rawinsonde is an instrument used to measure various meteorological parameters, including wind, temperature, and humidity. Rawinsonde is a balloon-borne instrument that is released into the air, and it sends back data as it rises. The balloon can rise to an altitude of around 100,000 feet before bursting, and the Rawinsonde instrument falls back to Earth. The data from the instrument are used to create a sounding, which is a profile of the atmosphere's temperature, pressure, and humidity as a function of altitude. The troposphere is the region of the atmosphere that is closest to the surface. It extends from the Earth's surface up to about 7-20 kilometers, depending on the latitude. The Rawinsonde instrument is used to measure the various meteorological parameters in the troposphere.

The Rawinsonde instrument consists of a weather balloon that is filled with helium gas. The balloon is released from the surface, and it rises through the atmosphere. As the balloon rises, the Rawinsonde instrument collects data on various meteorological parameters, including wind, temperature, and humidity. The data collected from the instrument are used to create a sounding, which is a profile of the atmosphere's temperature, pressure, and humidity as a function of altitude.

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Answer:

One challenge a representative might face in connecting with rural constituents as compared with constituents in urban areas is the issue of geographic distance. Rural areas are often more spread out and have lower population densities than urban areas, which can make it more difficult for representatives to physically reach their constituents. This can make it harder for representatives to hold town hall meetings, attend community events, and meet with constituents one-on-one. Additionally, rural areas may have limited access to technology and internet connectivity, which can make it harder for representatives to communicate with their constituents through email, social media, and other digital channels. As a result, representatives may need to be more creative in finding ways to connect with their rural constituents, such as holding virtual town hall meetings or partnering with local organizations to reach out to rural communities.

The geological features of the terrestrial worlds have been influenced factors such as the initial composition of the protoplanetary disk, the planet's distance from the Sun, its size, the presence or absence of a magnetic field, and others.

The geological features of these planets are thus not predetermined from their birth but are influenced by various factors that continue to act on them.

 The geological features of these planets are therefore not predetermined from their birth but are influenced by a variety of factors that continue to act on them.

What is the Terrestrial World?

Terrestrial planets, also known as rocky planets or telluric planets, are planets that are primarily composed of silicate rocks or metals. In contrast to gas giants, which are primarily composed of hydrogen and helium, terrestrial planets have a solid surface layer and a central core that is made up of metal. Mercury, Venus, Earth, and Mars are the four terrestrial planets in our solar system.

The geology of the terrestrial worlds is therefore dependent on a variety of factors, which include factors such as the planet's size, distance from the Sun, and its history of volcanic activity.

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Evidence Card: Prevailing Winds in a Normal Year.

Explanation of Evidence: Prevailing winds near the equator affect ocean temperatures and currents, which in turn can influence weather patterns globally, including in Christchurch.

Best Supported Claim: Christchurch's air temperature during El Niño years is cooler than usual because the prevailing winds near the equator change, leading to altered ocean temperatures and currents that affect global weather patterns.

The evidence from the Prevailing Winds in a Normal Year card suggests that the prevailing winds near the equator can influence ocean temperatures and currents, which in turn can have a global impact on weather patterns. This information is relevant to the question at hand because El Niño is a phenomenon that occurs when the prevailing winds in the equatorial Pacific weaken or reverse, causing warmer than usual ocean temperatures and altering weather patterns globally.

Therefore, the best-supported claim is that Christchurch's air temperature during El Niño years is cooler than usual because the prevailing winds near the equator change, leading to altered ocean temperatures and currents that affect global weather patterns.

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Explanation:

Because of the short length of the carbon-14 half-life, carbon dating is only accurate for items that are thousands to tens of thousands of years old. Most rocks of interest are much older than this. Geologists must therefore use elements with longer half-lives.

Answer: Because of the short length of the carbon-14 half-life, carbon dating is only accurate for items that are thousands of years old. Most rocks that scientists study are much older than thousands.

Hope it helped : D

Chemical reactions in the water and aliens are not significant sources of sediment on the continental shelf. The correct option is d.

Most sediment on the continental shelf is derived from erosion on the continent.

The shallow oceanic area is known as the continental shelf.

It is located next to the shore and extends from the shore to the continental slope.

The water depth in the continental shelf ranges from 100 meters to 200 meters, depending on the location, and the slope of the shelf ranges from 0.1 to 1 degree.

The main source of sediment on the continental shelf is erosion on the continent.

When rocks and soil are exposed to the elements, such as wind, rain, and temperature fluctuations, they begin to erode.

This can result in sediment that is transported by rivers to the ocean and deposited on the continental shelf.

Other sources of sediment on the continental shelf include volcanic eruptions, underwater landslides, and other natural events.

Life in the sea is also a source of sediment, as organisms such as corals and clams produce shells and other materials that eventually break down and contribute to the sediment on the sea floor.

However, the primary source of sediment on the continental shelf is erosion on the continent.

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The primary reason why North America has a high number of severe thunderstorms is the collision of air masses.

North America is located in an area where cold air from Canada meets warm, moist air from the Gulf of Mexico. This creates a boundary called a "front" where the two air masses collide, causing the warm air to rise rapidly and form thunderstorms. This collision of air masses occurs frequently in North America, leading to a high number of severe thunderstorms. Additionally, the geography of North America, with its varied topography and large bodies of water, creates ideal conditions for the formation of thunderstorms.

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Answer:

The thickness of each layer in terms of the troposphere's thickness is 1.75 for the stratosphere, 1.75 for the mesosphere, and 20.6 for the thermosphere.

If Mars was warmer and wetter in the past, the following must be true: Mars once had a much thicker atmosphere. The correct option is "Mars once had a much thicker atmosphere.

Mars is a terrestrial planet that is the fourth from the Sun in the Solar System. Mars is smaller than Earth, but it is still one of the planets that scientists are interested in exploring. It is a cold and desert-like planet now, but it was once warmer and wetter.

The atmosphere of Mars is one of the primary reasons for its present-day state. The Martian atmosphere is very thin and has a lower pressure than Earth's atmosphere.

Mars' magnetic field was destroyed four billion years ago by an intense solar storm, leaving the planet unprotected from the Sun's radiation. Mars has a thinner atmosphere today than it did in the past.

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The San Andreas Fault is a continental transform fault, which is a type of fault that occurs at the boundary between two tectonic plates.

The San Andreas Fault marks the boundary between the Pacific Plate and the North American Plate. The two plates slide past each other horizontally in opposite directions. As the plates move, they cause earthquakes with deep focus, which are powerful earthquakes that occur far beneath the surface.

An example of a world-famous hot spot is the Hawaii Islands, which form due to magma rising up from the Earth's mantle. This is a form of intraplate volcanism, which occurs at locations that are not on tectonic plate boundaries. In contrast, transform faults are located on plate boundaries, and the San Andreas Fault is a prominent example.

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One similarity in life expectancy between developed and developing countries is that people tend to live longer in both types of countries compared to historical periods.

One difference in life expectancy between developed and developing countries is that there is often a significant gap in life expectancy between the two.

Developed countries generally have higher life expectancies than developing countries due to factors such as greater access to healthcare, higher standards of living, and better infrastructure. In some cases, this gap can be quite large, with people in developed countries living many years longer on average than people in developing countries.

However, it is worth noting that the gap in life expectancy between developed and developing countries has been decreasing over time as developing countries continue to make progress in improving healthcare and other factors that contribute to longer lifespans.

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The major driving mechanism of the MOC (Meridional Overturning Circulation) is the sinking of water in the North Atlantic.

This begins with the formation of sea ice. As ocean water freezes, ice crystals form and the salt that is excluded from the crystals increases the salinity of the surrounding water, which causes it to become denser and sink.

Meridional Overturning Circulation (MOC) is a north-south (meridional) overturning circulation in the sea calculated by zonal accumulation (east-west) of the amount of water mass transport in depth or density layers.

This somersault circulation occurs in the North Atlantic, away from the subpolar regions, the MOC (which is in principle an observable quantity) is often identified with the thermohaline (THC) circulation, which is more of a conceptual interpretation.

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Europe's economy has become strong in the last decade primarily due to A. entrepreneurship.

Entrepreneurship has played a crucial role in driving economic growth in Europe, with many startups and innovative businesses contributing to the economy. These businesses have created new jobs, brought new products and services to market, and helped to increase overall productivity.

Communism, on the other hand, is not a major factor in Europe's economic growth. Most European countries have moved away from communism over the past several decades, and instead have adopted market-based economies that prioritize private enterprise and competition.

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The answer to this question is no, we would not expect as many impact craters per unit area on the surface of Venus as on the surface of Mars. The reason for this is because Venus has a much thicker atmosphere than Mars, which acts as a shield that protects the surface of the planet from incoming objects.

Additionally, Venus has a much stronger gravity than Mars, which pulls objects that enter the atmosphere back towards the planet rather than letting them reach the surface. This further reduces the amount of impact craters on the surface of Venus.

In comparison, Mars has a much thinner atmosphere, which does not provide as much protection from incoming objects. The weaker gravity also means that objects that enter the atmosphere have a much better chance of reaching the surface of the planet. This contributes to more impact craters forming on the surface of Mars.

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The largest earthen structure in North America, outside of Mexico, is found at the site of Cahokia.

Cahokia is a UNESCO World Heritage site located in southern Illinois. It is known for its earthen mounds and was once the largest pre-Columbian settlement north of Mexico.

The city was built by the Mississippians, a Native American civilization that flourished in the Mississippi River valley from around 800 to 1500 AD.

The largest mound at Cahokia, known as Monks Mound, is a massive earthen structure that stands 100 feet tall and covers 14 acres of land.

It was likely used for ceremonial purposes and is believed to have been the focal point of the city. Other notable mounds at Cahokia include the Grand Plaza, which was likely used for public gatherings and ceremonies, and the Woodhenge, a circular arrangement of posts that may have been used for astronomical observations.

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CO2 is the most important radiative forcing behind global warming because it is the most abundant of all the greenhouse gases in the atmosphere and its residence time in the atmosphere is very long.

This allows it to accumulate and persist over a long period of time, and so its radiative forcing effect is greater than other greenhouse gases with a lower global warming potential and a shorter residence time.

While other greenhouse gases, such as methane and nitrous oxide, have a greater warming potential, they are present in much smaller quantities in the atmosphere than CO2.

Furthermore, CO2 emissions have been increasing steadily due to human activities such as burning fossil fuels and deforestation, leading to a buildup of CO2 in the atmosphere over time

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The current interglacial period, which began around 11,700 years ago, is part of the Quaternary Ice Age that has been occurring for the past 2.6 million years.

During this period, the Earth has experienced multiple ice ages with cooler and warmer periods known as glacial and interglacial phases. The present interglacial period, known as the Holocene, has been in the peak of its cycle for about 11,000 years.

During this time, global temperatures have been relatively stable, with sea levels rising and falling as the glaciers advance and retreat. This has enabled human civilizations to flourish and expand.

Despite this, the Earth is still in the Ice Age and the current interglacial period could end at any time, leading to a new glacial phase. The duration of this interglacial period is unknown, but it is likely to last several thousand years more before the next glacial period begins.

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In the event that two glaciers collide, their advancing glacial till meets in the middle as a MEDIAL moraine.

A medial moraine refers to a linear ridge that forms when two glaciers merge or conjoin together. The medial moraine, which is also referred to as the median moraine, runs down the middle of the newly created glacier. A medial moraine may consist of debris that originated from either of the merging glaciers or from the glacial bedrock.

When two glaciers combine, the dirt and rocks on both glaciers combine to form a medial moraine. This linear ridge is generally found in the middle of glaciers, and it can often be seen as a dark line or stripe down the center of a glacier. Medial moraines are formed when two glaciers merge or converge. As the glaciers move closer to one another, they begin to push and shove the rocks and debris that have been trapped within them for years. These rocks and debris are then pushed to the center of the glacier, where they begin to pile up and form a linear ridge known as a medial moraine.

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The controversial oil drilling project called the Willow project has been approved by the Biden administration, which will be located in the US state of Alaska. The correct option is Alaska.

The Willow project is a proposed oil drilling project by the US oil company ConocoPhillips. The company plans to develop the project on Alaska's North Slope. The Willow project includes the construction of five drill sites, an airstrip, about 28 miles of ice roads, and 85 miles of pipelines, among other facilities. The Willow project is a controversial project because it could harm the wildlife and habitat of the area.

Moreover, environmentalists argue that the project's carbon footprint will contribute to climate change, a matter of global concern. Therefore, environmentalists and other groups are opposing the Willow project, and some have even sued the US government to halt the project. Nonetheless, the Biden administration has approved the Willow project. Alaska is the US state where the Biden administration approved a controversial oil drilling project called the Willow project.

Alaska is the northernmost state of the United States of America. It is the largest state of the country by area and is the 3rd least populated state. Alaska is famous for its rugged, remote wilderness areas, glaciers, mountains, abundant wildlife, and hunting and fishing opportunities. The correct option is Alaska.

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"The characteristics of hot deserts include high temperatures in summer; greater evaporation than precipitation; considerable variation in the occurrence of precipitation, its intensity and distribution; and low humidity."

Hot deserts are characterized by extreme temperatures in summer, with daytime temperatures often reaching above 40°C. The combination of high temperatures and low humidity can make these environments challenging for human habitation. These arid regions typically receive very little rainfall, and what precipitation does occur is often sporadic and highly variable in intensity and distribution.

As a result, evaporation rates are typically much higher than precipitation rates, leading to a scarcity of water and limited vegetation. Despite these challenges, hot deserts are home to a variety of unique plant and animal species that have adapted to survive in these harsh conditions.

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Tropical rain forests produce CO2 due to both the respiration of living trees and the decomposition of dead trees. This leads to a lower relative consumption of CO2 than is expected.

Both living and dead trees contribute to the production of carbon dioxide (CO2) through respiration and decomposition processes. Living trees release CO2 through cellular respiration, which is the process by which they use oxygen to convert sugars into energy. Dead trees also release CO2 as they decompose, either through the action of microorganisms or through physical processes like wind and erosion.

While it's true that tropical rainforests produce CO2 through respiration and decomposition, they also play an important role in removing CO2 from the atmosphere through photosynthesis. Trees absorb CO2 from the air and use it to build their cells and grow, releasing oxygen as a byproduct. This process helps to offset the CO2 produced by other sources, such as human activities.

However, the extent to which tropical rainforests are able to absorb and sequester CO2 depends on a variety of factors, including the density and diversity of the forest, the health of the trees, and the availability of nutrients and water. Additionally, deforestation and other human activities that destroy or disrupt rainforest ecosystems can greatly reduce their ability to act as carbon sinks.

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