A sedimentary basin which appears when a continent is stretched, causing down-dropped crustal blocks bordered by faults and mountains, is called a rift basin. Therefore the correct option is option A.
A sedimentary basin is a geological basin that has formed from sediment accumulation caused by erosion or sediment deposition. Sedimentary basins occur in the Earth's crust, and they are most commonly formed by tectonic activity.
They also develop as a result of the Earth's thermal evolution, such as in the rift basins that develop on divergent plate boundaries. A rift basin is a type of sedimentary basin that forms when continental crust is stretched and thinning. It is a depressed region of the crust in the form of a valley bounded by fault lines that have uplifted peaks.
Rift basins are formed when the Earth's crust is pulled apart or thinned, resulting in a vertical drop. The depression is filled with sediments that have been eroded from the surrounding mountains, which build up to form thick layers of sediment that cover the basin's floor. Therefore the correct option is option A.
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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
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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According to the US National Snow and Ice Data Center, there have been __________ ice age cycles on Earth during the last 750,000 years.
Answer:
According to the US National Snow and Ice Data Center, there have been eight ice age cycles on Earth during the last 750,000 years.
According to the US National Snow and Ice Data Center, there have been eight ice age cycles on Earth during the last 750,000 years.
The Earth is not the same as it was millions of years ago. In fact, the planet has seen numerous changes and transformations throughout its life. The climate is one of the most significant factors that have impacted the Earth in this process. The climate has gone through many changes over the centuries. The Earth's climate, for example, has gone through a number of ice ages. Ice ages are periods of time when the Earth's temperature falls considerably, resulting in glaciers and ice sheets.
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8. What is the collective role of water vapor, carbon dioxide, ozone, and methane in the atmosphere?
A. They prevent harmful ultraviolet radiation of the sun from reaching earth
B. they are important components of the water cycle, which regulates the earths temperature
C. they regulate earths climate by trapping heat and holding it within earths atmosphere
D. they scatter almost a third of the sunlight that reaches the outer layers of the atmosphere back into space
Answer: C. They regulate Earth's climate by trapping heat and holding it within Earth's atmosphere.
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.
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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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.\
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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he type of turbulence that develops when wind speed changes rapidly with height is: group of answer choices thermal turbulence adiabatic turbulence political turbulence shear-induced turbulence
The type of turbulence that develops when wind speed changes rapidly with height is known as shear-induced turbulence. Therefore the correct option E.
Turbulence is a disruptive event that can cause high-intensity fluctuation flows in different mediums. It is characterized by irregular, chaotic, and random fluctuations in velocity, pressure, and other fluid properties.
Turbulence is commonly observed in many natural and human-made systems, including oceans, rivers, the atmosphere, and industrial applications such as airplane engines and pipelines.
Shear-induced turbulence develops when there is a change in wind speed with height. This phenomenon occurs when the horizontal velocity gradient causes vertical shear and results in turbulent eddies. Therefore the correct option E.
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The following question may be like this:
The type of turbulence that develops when wind speed changes rapidly with height is: a) thermal turbulence b) political turbulence c) adiabatic turbulence d) mechanical turbulence e) shearinduced turbulence
Help me with this please.
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.
What is the evidence about?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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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
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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europe's economy has become strong in the last decade because of what?
a. entrepreneurship
b. better leaders
c. communism
Europe's economy has become strong in the last decade primarily due to A. entrepreneurship.
How has entrepreneurship helped Europe ?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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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.
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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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
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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most sediment on the continental shelf is derived from a. erosion on the continent b. life in the sea c. aliens d. chemical reactions in the water
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.
What is the continental shelf?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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a sandstone bed strikes 140 across a stream. the tresam flows down a narrow gorge with vertical walls. the apparent dip of the bed on the walls of the gorge is 25, 095. what is the true dip of the bed?
Answer : The true dip of that sandstone bed is 25°95'.
The apparent dip of the bed on the walls of the gorge is the angle that the bed strikes across the stream and down the narrow gorge. we calculate the angle of the bed relative to the horizontal plane. The true dip is the angle of inclination of the bed below the horizontal plane.
True dip = 90° - (90° - 25°95') = 25°95'. the true dip of the sandstone bed is 25°95', which is the angle of inclination of the bed below the horizontal plane.
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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
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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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 -
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 primary reason why north america has a high number of, and certainly much more than its global share, severe thunderstorms, is the:
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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a major driving mechanism of the moc is the sinking of water in the north atlantic. this begins with the formation of . as ocean water freezes, ice crystals exclude salt and the salinity of the surrounding water increases.
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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the largest earthen structure in north america, outside of mexico, is found at the site of .
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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which of the followng us states is best represented by a cold continental climate type without a dry season and warm summer?
The best state to represent a cold continental climate type without a dry season and warm summer is Minnesota. Located in the northern United States, Minnesota experiences cold winters and warm summers due to its location near the Great Lakes and distant from the moderating influence of the Atlantic Ocean.
Summers are warm and humid with temperatures from around 70-85 degrees Fahrenheit (20-30 Celsius). Winters are cold and snowy with temperatures ranging from 0-25 degrees Fahrenheit (-18 to -4 Celsius). The state has four distinct seasons and is known for its extreme seasonal climate changes.
In the winter, snowfall can range from a few inches to several feet in just a few days. The state's cold continental climate type without a dry season and warm summer is best represented in the northern part of the state, with average temperatures ranging from 20-30 degrees Fahrenheit (-7 to -1 Celsius). This type of climate is best suited for cold-weather crops such as wheat, barley, peas, and potatoes.
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E. Explain ONE challenge a representative might face in connecting with rural constituents as
compared with constituents in urban areas.
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.
kilaunea is not as explosive as the eruption of mt st helens. what is the overall control that dictates this differnecec
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 was your estimate of earth's albedo during the last glacial maximum? why should it be larger than the earth's current albedo of 0.30?
During the Last Glacial Maximum, it was estimated that Earth had an albedo of 0.32. Due to the greater coverage of ice and snow, it ought to be higher than the Earth's current albedo of 0.30.
During the Last Glacial Maximum, the Earth's albedo was estimated to be 0.32 .The ability to reflect sunlight into space is known as albedo. Sunlight is reflected by deserts, clouds, ice and snow, and aerosols . The more solar energy that is reflected, the higher the albedo; the chillier The albedo is also raised as the ice cover expands as the temperature drops.
The growing conditions for alpine grasslands on the TP, where Climate is the primary constraining factor, are improved by increased vegetation coverage, which results in a lower surface albedo and more energy absorbed.
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to what extent do we think the geologies of the terrestrial worlds were destined from their births? explain.
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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in the absence of friction, the combined effect of the coriolis force and the pressure gradient force produces question 75 options: air flow from low to high pressure centers. surface winds. air flow in a north-south direction. geostrophic winds at altitudes above the ground. air flow perpendicular to the isobars.
winds that are geostrophic at heights above the earth. The creation of high and low-pressure systems is a result of geostrophic winds,
A theoretical wind known as geostrophic wind is produced when the atmosphere's Coriolis force and pressure gradient force are balanced. When there is no friction, the air moves at a constant speed parallel to the isobars. In the upper atmosphere, where the pressure gradient force predominates and the Coriolis force is considerable, this sort of wind is frequently observed. The creation of high and low-pressure systems is a result of geostrophic winds, which are also crucial to the atmosphere's general circulation. But friction and turbulence at the Earth's surface also contribute to the complexity and variability of the wind.
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what is a common distinguishing characteristic of sedimentary rock masses? group of answer choices they are always very colorful. they tend to be layered. all of the choices they are formed by solidification from a melt. they tend to be extremely hard.
A common distinguishing characteristic of sedimentary rock masses is that they tend to be layered.
Sedimentary rocks are created by organic or mineral particles building up or storing at the Planet's surface, then binding those particles together. Sedimentary rocks are often found in strata, which are horizontal layers.
Undisturbed strata have younger layers on top of older levels. The superposition law is in effect here. Sedimentary Strata can be cut by other geologic components like intrusions or faults. An Earth's crustal fracture is known as a fault. Within the Earth's crust, a mass of sedimentary rock known as an incursion was formed. When two features cross, the younger feature is the one that pierces the other.
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would you expect as many impact craters per unit area on the surface of venus as on the surface of mars? why or why not?
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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precipitation of gypsum due to evaporation of seawater produces which kind of sedimentary rock? group of answer choices biochemical chemical clastic organic
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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Rice is the staple food for over half the people in the world. What is meant by this statement?
A basic and crucial part of people's daily existence is a staple meal, item, or activity. For more than half of the world's population, rice is a staple diet.
Is rice the main food consumed by almost half the world's population?The world's major staple meal is rice. Around 80% of the world's population, or more than 50 percent, depends upon rice for food. Almost 95% of the world's rice production is made and eaten in developing nations.
It is one of the most grown crops and is frequently consumed in India. It is suitable for rice farming due to the amount of precipitation, soil fertility, and availability of irrigation. It is a vital source of food and income for the farmers.
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in addition to the mineral above, this rock also contains quartz, plagioclase, muscovite, and kyanite. based on your observations and the mineral assemblage, what kind of rock is this? choose one: a. phyllite b. gneiss c. quartzite d. slate e. schist
Phyllite is a kind of rock that also contains quartz, plagioclase, muscovite, and kyanite. Thus, option a is correct.
Phyllite is generally located black to gray, or light greenish-gray in color inside the earth. It has a wrinkled or wavy formation as its foliation. Phyllite is a stable and very soft rock that is formed naturally by the wind. It is mainly used by cemetery markers in buildings.
Phyllites are most typically found in the Dalradian metasediments of northwest Arran areas. Quartz and feldspar are discovered in large amounts in phyllite. Phyllite has a reasonable preference to break into sheets. Tredorn Phyllite and Woolgarden phyllites are found in North Cornwall along the banks of the rivers.
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in general, what do beaches look like at the end of winter?
Winter – Higher winter waves move sand offshore and narrow the beach. … The summer beach is covered with a layer of sand that is moved south by the longshore currents and onshore by low waves. The winter beach is denuded of sand by high storm waves.
In general, beaches look different at the end of winter compared to the peak of summer. During winter, beaches are often deserted and quiet, with fewer visitors and tourists.
The weather is usually cooler, and the water is colder, making swimming and water sports less popular. Additionally, beaches may be covered in debris, seaweed, and other natural materials that have washed up during storms or high tides. The sand may also be covered in snow, depending on the region.
However, despite the cooler weather and fewer visitors, winter beaches can be a beautiful and peaceful place to visit. Many people enjoy long walks along the shoreline, watching the waves crash against the shore, and taking in the natural beauty of the coast.
In conclusion, beaches look different at the end of winter compared to the peak of summer. They are often quieter, colder, and covered in natural materials. Despite this, they can be a beautiful and peaceful place to visit during the off-season.
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