_______________ form when more resistant rock does not erode and less resistant rock on each side does.

Answers

Answer 1

Rock Formation form when more resistant rock does not erode and less resistant rock on each side does.

What is a Rock Formation?

Rock formations are the result of a geological process that causes rock to break, crack, erode, and form new structures. Rocks are constantly being formed, eroded, and recycled through the rock cycle, but some rocks are more resistant to erosion than others. The more resistant rocks, such as granite, sandstone, or limestone, can resist erosion and weathering, while less resistant rocks, such as shale, clay, or sand, erode more easily. This results in the formation of various landforms, including buttes, mesas, spires, arches, and cliffs.

Rock formations can take millions of years to form and are shaped by a combination of geological processes such as tectonic activity, erosion, weathering, and deposition. They can be found all over the world and provide valuable information about the earth's history and geology.

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Related Questions

what kind of drainage pattern would develop on the slopes of mount rainier, an isolated volcano in washington state? dendritic radial rectangular trellis

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Answer: The kind of drainage pattern that would develop on the slopes of Mount Rainier, an isolated volcano in Washington State, is radial.

Explanation:

What is a drainage pattern?

A drainage pattern refers to the design that is created by the flowing water. When water flows, it creates several channels, and the combination of all these channels forms a drainage pattern.

What is a radial drainage pattern?

A radial drainage pattern refers to a type of drainage pattern that occurs when streams flow in all directions outward from a central peak or dome-like structure. In this kind of drainage pattern, the streams flow in straight lines, and they follow the slopes of the land in a radial manner.

In conclusion, the kind of drainage pattern that would develop on the slopes of Mount Rainier, an isolated volcano in Washington State, is a radial drainage pattern.

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you see an igneous rock next to sandstone, and notice that the sandstone appears discolored and a bit baked along contact. what can you imply about the ages of the 2 rock units

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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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this is a map of paraguay. based on this map, which geographical feature could negatively affect international trade?

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Based on the given map of Paraguay, the geographical feature that could negatively affect international trade is the lack of a seaport.

Paraguay is a landlocked country in South America, and it is bordered by Argentina, Bolivia, and Brazil. It is the only country in South America that does not have a seaport. This lack of access to the sea can make it more difficult and expensive for Paraguay to trade goods internationally.The landlocked status of Paraguay can increase the cost of trading goods internationally. It may require more transportation costs, which may result in more time consumption and additional costs.

Furthermore, the lack of seaport can make it harder for Paraguay to receive goods from other nations. The absence of a seaport can cause additional difficulties for Paraguay in exporting and importing goods. In Paraguay, one of the most essential ways to transport goods is by using the Paraná and Paraguay rivers. However, the waters of the Paraná and Paraguay rivers can be very shallow at times, which means that transportation via water is often only possible during particular seasons.

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what is foliation? group of answer choices parallel bedding in a rock formed by successive depositional events parallel orientation of platy minerals caused by complete melting parallel orientation of platy minerals caused by metamorphism parallel cracking or jointing of a rock due to stress

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Foliation, a result of metamorphism, is the parallel orientation of platy minerals in a rock.

The parallel orientation of flat or platy minerals within a rock is referred to as foliation. The minerals align themselves perpendicular to the direction of the highest stress because to the severe pressure and/or heat that occurs during metamorphism. As a result, the rock develops a characteristic layering or banding pattern. Foliation is distinct from parallel bedding, which is created by several depositional occurrences, and from cracking or jointing, which is brought on by stress but excludes mineral alignment. Metamorphic rocks, such as schist and gneiss, frequently exhibit foliation, which can provide important details about the rock's geological past.

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temperature, pressure, wind and moisture are measured through the depth of the troposphere by what instrument? group of answer choices rawinsonde doppler radar goes satellite

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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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I just need some information I can use please and thank you 50 points
Don’t use the same one with the other just need info

"The Spanish colony of Mexico City, established in the early 1500s, quickly became the most important settlement in Mexican history. Since then, it has grown and developed into the largest city, and capital, of Mexico."

Identify the bias and fallacious argument of the passage above. You may need to conduct quick research to find more information on the topic.

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Answer:

There does not appear to be any clear bias or fallacious argument in the passage above. It simply presents historical facts about the establishment and growth of Mexico City, without any apparent attempt to distort or manipulate the information. However, it is worth noting that the passage only presents a positive view of the city's importance and development, without acknowledging any potential negative aspects such as social inequality or environmental challenges.

what composition of lava will travel further group of answer choices basaltic rhyolitic andesitic dacitic

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Basaltic lava is the most fluid type of lava and can therefore travel further than other types of lava. This is because basaltic lava is composed of lower viscosity magma that is able to flow over greater distances due to its lower density.

This type of lava is also the most common type of lava, which means it is the most likely to be found on Earth’s surface. Rhyolitic lava is more viscous than basaltic lava and therefore does not travel as far.

This is because rhyolitic lava is composed of higher silica and has a higher viscosity than basaltic lava. Andesitic lava is less viscous than rhyolitic lava, but more viscous than basaltic lava.

Andesitic lava is composed of minerals that create a mix of both low and high viscosity magma. Finally, dacitic lava is the least fluid type of lava and therefore has the shortest travel distance. This is because the minerals in dacitic lava create a high viscosity magma that is not able to flow as far as other types of lava.

In summary, basaltic lava is the most fluid type of lava and is therefore able to travel further than other types

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Deserts are formed by a __________ process as large variations in temperature between day and night put strains on the rocks causing them to break into pieces.

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Deserts are formed by a physical weathering process as large variations in temperature between day and night put strains on the rocks causing them to break into pieces.

The physical weathering of rocks is caused by temperature fluctuations in the desert. The rocks heat up during the day and cool down at night, causing them to expand and contract. As a result, the rocks can eventually break apart into small pieces over time. In a desert, there is little vegetation, and the wind can carry the pieces of rock, causing the land to erode and form sand dunes. In areas where there is little rain, the landscape can become arid, which contributes to the formation of a desert. Over time, the desert climate develops, with its distinctive patterns of temperature variation, limited precipitation, and lack of vegetation. Many deserts are found in areas around 30 degrees north or south of the equator, such as the Sahara in Africa and the Mojave in the United States.

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the largest earthen structure in north america, outside of mexico, is found at the site of .

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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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Two agricultural practices related to each biome

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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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what are the most likely changes to atmospheric temperature and precipitation along the west coast of south america during el nino

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During El Nino events, the west coast of South America experiences warmer atmospheric temperatures and reduced precipitation.

El Nino events typically lead to an increase in sea surface temperatures in the central and eastern tropical Pacific Ocean. This warm oceanic anomaly affects the atmospheric circulation and leads to warmer temperatures along the west coast of South America.

El Nino is associated with a shift in rainfall patterns, resulting in decreased precipitation along the west coast of South America. The warm oceanic conditions disrupt the normal atmospheric circulation patterns, leading to a weakening or reversal of the trade winds.

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The oldest abundant fossils of complex multicellular life w/shells and other hard parts date from the: a. Precambrain b. Paleozoic c. Mesozoic d. Cenozoic.

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The oldest abundant fossils of complex multicellular life with shells and other hard parts date from the Paleozoic era. The correct option is B. Paleozoic.

This era, which lasted from about 541 to 252 million years ago, is sometimes referred to as the Age of Invertebrates because of the many different types of invertebrates that thrived during this time. The Cambrian explosion, which occurred about 541 million years ago, marks the beginning of the Paleozoic era.

During this period, there was a sudden and rapid increase in the diversity of life on Earth, including the appearance of the first multicellular organisms with hard parts like shells and skeletons. This included trilobites, brachiopods, mollusks, and other types of invertebrates.

Later in the Paleozoic era, there were several mass extinction events, including the Permian-Triassic extinction event which wiped out 96% of all marine species. However, the survivors of these events went on to diversify and evolve into the complex and diverse array of life we see on Earth today.

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explain how water moves through the water cycle?

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Water in the water cycle moves between the Earth's surface and the atmosphere in a continuous cycle. It begins as water evaporates from the surface of the ocean, rivers, lakes, and wetlands into the atmosphere. The water vapor in the atmosphere rises and is cooled, forming clouds. As the clouds move, they can release water vapor in the form of precipitation, such as rain, snow, and hail. This precipitation then falls back to the surface and collects in bodies of water, such as rivers, lakes, and oceans. The water can also seep into the ground, where it replenishes groundwater sources. As the water in the bodies of water warms, it can evaporate again, and the cycle continues.

precipitation of gypsum due to evaporation of seawater produces which kind of sedimentary rock? group of answer choices biochemical chemical clastic organic

Answers

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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which of the following are types of pyroclastic debris? choose one or more: a. lapilli b. lava c. blocks d. ash e. magma f. gas g. lahar

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

What are Types of Pyroclastic Debris?

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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why might this be? (hint: what processes in both living and dead trees produce co2 ?) tropical rain forests also produce co2 due to living trees' respiration and decomposition of dead trees. due to this fact, relative consumption of co2 is not as great as has been expected.

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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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he san andreas fault is... group of answer choices associated with deep focus earthquakes a world-famous example of a hot spot is an intraplate fault within the juan de fuca plate an oceanic transform fault a continental transform fault

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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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which of the following are foliated intermediate- or high-grade metamorphic rocks that would form in the setting in part 1? choose one or more: a. phyllite b. schist c. marble d. slate e. gneiss f. hornfels

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

Which of the above is a foliated rock of high or intermediate metamorphic grade?

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 primary reason why north america has a high number of, and certainly much more than its global share, severe thunderstorms, is the:

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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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what kind of climate is controlled by elevation more than any other factor? responses temperate continental temperate continental tropical wet tropical wet highland highland polar

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The climate that is controlled by elevation more than any other factor is the highland climate.

What is the highland climate?

A highland climate is a climate that is found in high mountainous areas such as the Andes, the Himalayas, and the Rockies. Due to high altitudes, these regions experience cooler temperatures compared to surrounding lowlands, making it difficult for life to thrive.

The temperature, precipitation, and vegetation of highland areas vary depending on factors such as the altitude and slope orientation. Generally, temperatures decrease with altitude, and rainfall increases.

Highland climates usually experience heavy rainfall and fog, especially in the upper elevations. Due to the cold temperatures, vegetation is limited to alpine tundra and montane forests.

countries with highland climates include China, Mongolia, The United States, Nepal, Kazakhstan, Tajikistan, Kyrgyzstan, Tibet, Uganda, Kenya, Russia, Georgia, Italy, and Switzerland, among others.

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to what extent do we think the geologies of the terrestrial worlds were destined from their births? explain.

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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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kilaunea is not as explosive as the eruption of mt st helens. what is the overall control that dictates this differnecec

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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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what would you look for as evidence that a rock layer formed from materials deposited by ancient turbidity currents?

Answers

Answer:

repeated sequences of graded bedding that begin as coarse material and become finer upward

Explanation:

Evidence that a rock layer was formed from materials deposited by ancient turbidity currents include sedimentary structures such as ripple marks, graded bedding, and load casts. Ripple marks are wave-like undulations formed by currents. Graded bedding occurs when finer-grained material is deposited on top of coarser-grained material. Load casts are hollow molds that form when a current carries material and deposits it.

Other evidence of turbidity current deposits include erosional contact points, angular cross beds, and slump structures. Erosional contact points are found when a turbidity current is so powerful it cuts through underlying strata. Angular cross beds indicate rapid deposition by a fast-moving current.

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which must be true if mars was warmer and wetter in the past? group of answer choices mars was once much closer to the sun. mars once had a much thicker atmopshere mars must somehow have avoided the effects of the heavy bombardment. the sun was much brighter when it was younger.

Answers

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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how do we know that the washington and oregon coasts have experienced numerous large tsunamis in the past?

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There is strong evidence that the Washington and Oregon coasts have been subjected to numerous large tsunamis in the past. When seismic waves are generated by a submarine earthquake, a tsunami is formed.

Seismic activity may cause sea level fluctuations that can lead to surges in water volume and tsunami waves. Tsunamis from earthquakes, landslides, and volcanic activity have affected the Pacific Northwest in the past, as evidenced by the following factors:

The discovery of thousands of old logs on the Washington coast, which have been confirmed to be evidence of past tsunamis. Large deposits of sand in areas that are currently dominated by forest, such as the Willapa Bay area. Layers of sand, gravel, and debris in bogs and other natural landscapes.

A tsunami deposit that has been verified in a test trench in Seaside, Oregon. The evacuation of villages to higher ground on oral and written accounts in Native American and First Nations communities along the coast. Evidence of a tsunami deposit in the area between the most significant historic tsunami in 1964, which struck Alaska and traveled down the west coast, and the previous significant historical tsunami, which struck in 1700.

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__________ are used to prevent the erosion of sand from beaches. They allow the wind and water to blow through, but they help to prevent the movement of sand.

Answers

Answer:

are used to prevent the erosion of sand from beaches. They allow the wind and water to blow through, but they help to prevent the movement of sand.

Explanation:

desert

Sand Dunes are used to prevent the erosion of sand from beaches. They allow the wind and water to blow through, but they help to prevent the movement of sand.

Sand dunes are critical coastal features, providing natural buffers against powerful ocean waves and wind. They absorb the energy of storm surges and act as barriers to protect inland areas. They are also habitats for a range of plants and animals, many of which are threatened by human activities and development. Dunes, often some of the most noticeable and recognizable features of a beach, can be created by a variety of wind patterns and types of sand, and can cover vast land areas with mounds of sand. They also play a vital role in the overall ecosystem of a beach area, both physically and ecologically.

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despite having a lower global warming potential and a shorter residence time in earth's atmosphere, co2 is the most important radiative forcing behind global warming because -

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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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E. Explain ONE challenge a representative might face in connecting with rural constituents as
compared with constituents in urban areas.

Answers

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.

ANSWER ASAP!!!!!
Which of the following East Asian nations lack major deposits of oil or coal? (choose all that apply)
- Japan
- China
- North Korea
- Taiwan

Answers

The East Asian nations that lack major deposits of oil or coal are:

Japan Taiwan North Korea

Which nations lack oil and coal in Asia ?

Japan is the world's third-largest economy, but it has very limited domestic reserves of oil and coal. As a result, Japan is heavily dependent on imports of these resources to meet its energy needs. Japan is one of the world's largest importers of oil and coal.

Taiwan is a small island nation that has very limited domestic reserves of oil and coal. Like Japan, Taiwan is heavily dependent on imports of these resources to meet its energy needs. North Korea has some coal and oil reserves, but they are limited in comparison to other countries in the region.

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can you identify the minerals that comprise igneous rocks? drag the appropriate labels to their respective targets. the specific colors of the referenced mineral crystals within the rocks have been supplied to assist you. labels will only be used once, and not all labels will be used.\

Answers

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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