Breakwaters are used to prevent erosion. They are structures built out into the water or parallel to the beach. They cause the wave to hit them first, reducing the carrying power of the waves, which prevents the beach from eroding.
What is erosion?The natural process by which the surface of the earth is worn away by wind, water, or other geological processes is known as erosion. Erosion is a naturally occurring process that affects all landscapes. Human activities, such as farming, deforestation, and construction, can exacerbate erosion issues by eliminating vegetation that would usually hold soil in place and by intensifying the impacts of rain and wind on the land.
How do breakwaters work?Breakwaters work by deflecting wave energy away from shorelines, decreasing the velocity of waves that eventually reach the shore, and increasing the distance over which wave energy dissipates, lowering the erosive force of waves. Breakwaters can be either submerged, which means they're below the water's surface, or above water, which means they're above the water's surface. Breakwaters are often constructed in long lines to reduce wave energy from longshore drift and prevent beach erosion.
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pulque production is increasing in the teotihuacan valley. true or false?
The statement pulque production is increasing in the teotihuacan valley is true as there is an increase in production.
In Mexico, especially in the central region, which includes the Teotihuacan Valley, the production of pulque is a traditional activity. For thousands of years, the maguey (agave) plant's sap has been used to make pulque, a fermented alcoholic beverage.
Due to competition from other alcoholic beverages and the urbanization of rural areas, pulque production has decreased in recent years, but there are still many small-scale producers in the area who continue to make pulque using traditional techniques.
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which of the pre-columbian sites below is located in south america? palenque tikal tiwanaku teotihuacan
Teotihuacan is the pre-columbian archaeological site located in Central Mexico, in the State of Mexico, that was built around 100 BC. It is widely accepted that Teotihuacan was one of the most influential cities of the ancient Americas and one of the largest cities in the world during its prime.
It is the most visited archaeological site in Mexico and is a UNESCO World Heritage Site. Teotihuacan was the largest city in the pre-Columbian Americas, with an estimated population of 200,000 people at its peak. Palenque, Tikal, and Tiwanaku are all pre-Columbian archaeological sites located in Mesoamerica, Central America, and South America, respectively.
Teotihuacan is located in Central Mexico, about 40 miles (64 km) northeast of modern-day Mexico City. Its layout and architecture have been influenced by several different cultures, including the Maya, Zapotec, and Toltec civilizations. The city is laid out in a grid pattern with broad plazas and avenues connecting the various pyramids, palaces, and temples.
Teotihuacan is famous for its monumental architecture, especially the two large pyramids of the Sun and Moon. It is also renowned for its extensive mural and sculptural artwork, and its archaeological record is one of the most important sources of information about ancient Mesoamerican civilizations.
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The _____ ______ of the divide is the Rocky Mountains, and it is called the Continental Divide.
The highest point of the divide is the Rocky Mountains, and it is called the Continental Divide.
The Continental Divide is a long natural boundary that separates the rivers that flow westward from those that flow eastward in North America. The Rocky Mountains of the United States and Canada are its most notable feature. The Continental Divide, also known as the Great Divide, follows a winding route through the Rocky Mountains and across western North America. It extends from Alaska to Mexico, running through the United States and Canada.
The Great Divide runs along the top of the Rocky Mountains. It serves as a geographic boundary separating the continent's western and eastern parts. On the west of the Great Divide, all water drains into the Pacific Ocean. On the east side of the Great Divide, all water runs into the Atlantic Ocean. The height of the divide ranges from just a few inches to more than 14,000 feet above sea level.
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units a through k are sedimentary layers. l and m are intrusive igneous bodies. the surface of erosion below layer h represents a(n) period of time of about 100 years. true false
units a through k are sediment layers. l and m are intrusive igneous bodies. the surface of erosion below layer h represents a(n) period of time of about 100 years. is True
Long-term accumulations of sediment and debris that land on the earth's surface or in bodies of water typically result in the formation of sedimentary strata. Each layer can represent a distinct geological epoch or timeframe, based on the type of rock and the fossils found in it.The amount of time that a layer was exposed to erosion, weathering, or other geological processes is represented by the surface of erosion beneath it. The length of that period, however, will vary depending on a number of variables, including the type of rock, the environment, the area, and the level of erosion.
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the dominant surface winds from the subtropics to high latitudes are the question 63 options: trade winds. westerlies. geostrophic winds. polar easterlies.
The dominant surface winds from the subtropics to high latitudes are the westerlies.
What are westerlies?The winds that blow from west to east in the middle latitudes are known as westerlies. These are observed mainly between 30 and 60 degrees north and south of the equator. As the earth spins on its axis, the Coriolis effect causes the westerlies to appear as westerly winds.
How do westerlies occur?At around 30 degrees north and south of the equator, rising hot air creates an area of low pressure. Air flows away from these low-pressure areas toward areas of high pressure at around 60 degrees north and south of the equator.
Why are westerlies considered significant?The westerlies have a significant impact on the Earth's climate, and they are an essential element of the global circulation system. They play a crucial role in the movement of weather systems across the globe, including storms, hurricanes, and mid-latitude cyclones.
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Assuming the sand dune (illustrated below) was deposited by wind currents 200 million years ago, which way was the wind blowing?Image: similar to the pair&share photo of the Jurassic Navajo Sandstone in Utah from the "Play in the Mud (and Sand)" lectureA) wind was blowing from the left to rightB) wind was blowing from right to leftC) wind was blowing both waysD) can't determine from the information given
The sand dune (illustrated below) was deposited by wind currents 200 million years ago, which way was the wind blowing wind was blowing from right to left. The correct answer is B) the wind was blowing from right to left.
To determine the wind direction, we need to analyze the sand dune's structure. Sand dunes have two distinct sides: the windward side and the leeward side. The windward side is the side facing the wind, and it has a gentle slope. The leeward side is the side sheltered from the wind, and it has a steeper slope.
In this case, we can see that the left side of the dune has a steeper slope, while the right side has a more gentle slope. This indicates that the wind was blowing from the right, carrying sand grains up the gentle slope on the right side of the dune. Once the wind reached the top of the dune, it lost its carrying capacity, causing the sand grains to fall and accumulate on the steeper left side of the dune, forming the leeward side.
So, considering the structure of the sand dune and the slopes, we can conclude that the wind was blowing from right to left 200 million years ago when the sand dune was deposited. The correct answer is B) the wind was blowing from right to left.
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describe the major differences in the abiotic factors observed in the high tide zone versus the lower inter tidal zone.
The abiotic factors observed in the high tide zone versus the lower intertidal zone are different. The major differences in the abiotic factors observed in the high tide zone versus the lower intertidal zone are as follows:
Abiotic factors in the high tide zone: In the high tide zone, the abiotic factors include temperature fluctuations, wave exposure, and variations in salinity. This region is typically less exposed to sunlight and air because the tide comes in and out of this zone quickly.
The high tide zone can experience strong wave action, as well as wind and water fluctuations. These factors all contribute to making it a challenging environment for plants and animals to survive.
Abiotic factors in the lower intertidal zone: In the lower intertidal zone, the abiotic factors include water pressure, light exposure, temperature fluctuations, and salinity. This region is typically more exposed to sunlight and air because the tide takes longer to come in and out.
The lower intertidal zone also experiences less wave action than the high tide zone. These factors make the lower intertidal zone an easier environment for plants and animals to survive.
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how does climate change affectprecipitation patterns which affect the salinity of estuarine habitats.
Climate change has a significant effect on precipitation patterns, which, in turn, affects the salinity of estuarine habitats. Here are the reasons why this occurs: Increased temperatures can cause more evaporation, resulting in less precipitation and a decline in the volume of freshwater entering estuaries.
In contrast, the salinity of estuarine habitats increases with less freshwater because seawater is denser than freshwater, and it sinks below freshwater, causing an increase in salinity. Climate change has also been linked to more frequent and severe weather events, such as droughts, floods, and tropical storms.
These extreme weather events might affect estuaries by altering freshwater inputs and the quantity and quality of nutrients and pollutants that enter them. Therefore, these modifications in precipitation patterns might alter estuarine ecosystems and their communities.
The rise in salinity may have a direct impact on the flora and fauna of estuaries, affecting their ability to adapt and survive. Moreover, high salinity levels could change the rate at which pollutants are eliminated from the ecosystem. As a result, many estuarine habitats will be affected, including those of fish, shellfish, and birds.
The significant effect of climate change on precipitation patterns, which affects the salinity of estuarine habitats, has been mentioned. The rise in temperature can cause increased evaporation, which may result in reduced precipitation and decreased freshwater volume entering estuaries.
In contrast, salinity levels in estuarine habitats increase with less freshwater because seawater is denser than freshwater, and it sinks below freshwater, causing an increase in salinity.
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california has 2 major underground basins one in owens valley what is the geological name for them? v what is the geologic name for them?
Answer:
the basin and range
Explanation:
California has two major underground basins: the Owens Valley Basin and the Salinas Valley Basin. The Owens Valley Basin is a tectonic depression in the Great Basin province of California, named for its location in the Owens Valley region. The Salinas Valley Basin is an underground sedimentary basin located in California's Central Coast region. It is composed of sandstone and shale deposits.
The Great Basin Province is a major physiographic province that covers much of the interior western United States and southwestern Canada. It is composed of four tectonic plates—the Sierra Nevada–Great Valley block, the Pacific block, and consists of numerous valleys and basins, including the Owens Valley and Salinas Valley basins.
The rocks found in the Great Basin Province are sedimentary and range from several million years to over 200 million years old. So two major basins are the Owens Valley Basin and the Salinas Valley Basin.
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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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the majority of the rocks that form at the surface of the earth are group of answer choices intrusive igneous rocks. foliated metamorphic rocks. sedimentary rocks. non-foliated metamorphic rocks.
Intrusive igneous rocks are rocks that form when magma cools and solidifies underground. They form in plutonic (intrusive) environments. The majority of the rocks that form at the surface of the earth are Intrusive igneous rocks. the correct answer choice is first option.
Intrusive rocks are typically more coarse-grained than extrusive igneous rocks because of their slow cooling time. Foliated metamorphic rocks are rocks that have been subjected to intense heat and pressure, causing the minerals within the rock to re-crystallize. These rocks have a foliated (layered) appearance, and are typically formed in tectonic plate boundaries and near active volcanoes. Sedimentary rocks are formed from sediment that is deposited over time, and can include minerals, fragments of rock, and even fossilized plant and animal remains.
Non-foliated metamorphic rocks are rocks that have been subjected to intense heat and pressure, causing the minerals to re-crystallize, but without any foliation or layering. Examples of non-foliated metamorphic rocks include quartzite and marble. All of these rocks are formed at the surface of the Earth and contribute to the overall geology and landscape.
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many macro-level factors have shaped our micro-level choices in dating patterns today. which is not one of these macro-level factors?
Influence of friends on our dating patterns is not a macro-level factor that has shaped our micro-level choices in dating patterns today.
What are macro-level factors?
Macro-level factors refer to broad social and cultural changes that have influenced dating patterns over time. These factors are usually beyond the control of the individual, but they can have a significant impact on the choices people make in their dating lives.
Examples of macro-level factors include demographic changes, economic factors, and technological advancements.
Some of the macro-level factors that have shaped our micro-level choices in dating patterns today include:
1. Demographic changes:
Changes in population size, age, and gender distribution have had a significant impact on the dating patterns of individuals.
2. Technological advancements:
The rise of the internet, social media, and dating apps have revolutionized the way people meet and interact with potential partners.
3. Economic factors:
Changes in the job market and the availability of education and opportunities have affected people's preferences in dating partners.
4. Cultural and social changes:
Changes in attitudes towards gender roles, sexuality, and marriage have influenced people's dating preferences and practices.
5. Influence of friends on our dating patterns:
Influence of friends is not a macro-level factor that has shaped our micro-level choices in dating patterns today. Rather it is a micro-level factor that influences our choices in dating. Friends can help to facilitate or discourage dating relationships, and they can also influence our preferences in potential partners.
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a spinel found in metamorphic rock or an aquamarine found within a pegmatite are examples of what type of deposit
A spinel found in metamorphic rock or an aquamarine found within a pegmatite are examples of hydrothermal deposits.
What are hydrothermal deposits?
Hydrothermal deposits are rocks containing mineral deposits that originated from hot water (hydrothermal) fluids circulating in the Earth's crust.
Hot water deposits often contain significant quantities of minerals, which are usually accompanied by the alteration of the surrounding rock. The hot water that makes up these deposits is generated by heat from the Earth's core, which is transferred through the mantle to the Earth's crust.
When the water is heated, it is driven to the Earth's surface, where it flows through cracks and fissures in the rock.
The water then cools, and minerals precipitate out of the solution, forming hydrothermal deposits. There are various types of hydrothermal deposits, including gold, silver, copper, zinc, and lead deposits, among others.
These deposits are commonly found in areas where tectonic plates meet, and the Earth's crust is being pushed and pulled in various directions.
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geologists measure the orientation of tilted rock layers. dip is the angle of inclination from the horizontal of a tilted rock layer. the compass bearing of a rock layer where it pierces the horizontal plane is called
The dip of a tilted rock layer is the angle of inclination from the horizontal. The compass bearing of a rock layer where it pierces the horizontal plane is called the strike. The dip and strike measurements are important tools used by geologists to understand the structural geology of an area.
Strike is the compass direction of a line formed by the intersection of a tilted rock layer and a horizontal plane. It is measured in degrees, typically with reference to the four cardinal directions (north, south, east, and west). Strike is an important tool for geologists to understand the orientation of a rock layer, which is useful for identifying different kinds of geological structures and interpreting the underlying geology.
The dip is the angle of inclination from the horizontal of a tilted rock layer. It is also measured in degrees and can be described as either up-dip or down-dip. Dip measurements are useful for understanding the attitude of a tilted rock layer relative to the horizontal plane, as well as helping geologists to identify different types of geological structures.
Geologists measure the orientation of tilted rock layers using the dip and strike measurements. The two measurements can be used together to accurately describe the attitude of a rock layer relative to the horizontal plane. These measurements are essential for geologists to understand the underlying geology of an area.
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what element is missing from this diagram of the rock cycle? compacting and cementing sediment sedimentary rock weathering and erosion
The element that is missing from the diagram of the rock cycle is metamorphism.
What is the rock cycle?
The rock cycle is a natural process by which rocks are transformed into other forms. In simpler terms, the rock cycle is the transformation of one type of rock into another type of rock via numerous geological processes.
The rock cycle is composed of three main phases: Igneous rocks that form from molten rocks, Sedimentary rocks that form from weathered and eroded debris and Metamorphic rocks that form from heat and pressure.
What is metamorphism?
Metamorphism is a geological process that involves the transformation of pre-existing rocks into a different kind of rock.
Metamorphism can be caused by an increase in temperature, pressure, or both. In metamorphism, heat and pressure together cause changes in the mineral structure of the rocks, leading to the formation of metamorphic rocks.
In summary, the correct answer is Metamorphism is missing from the diagram of the rock cycle.
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which statement about moist air moving over a mountain is correct?as air falls on the leeward side of a mountain, it expands and becomes warmer.as air rises on the windward side of a mountain, it contracts and becomes cooler.as air falls on the leeward side of a mountain, it contracts and becomes warmer.as air rises on the windward side of a mountain, it expands and becomes warmer.
As air rises on the windward side of a mountain, it cools and can reach its dew point, causing moisture to condense and form clouds is s correct.
In this case option B is correct
This process is known as orographic lifting. As the air moves over the mountain and descends on the leeward side, it compresses and becomes warmer.
Therefore, the correct statement is: as air rises on the windward side of a mountain, it contracts and becomes cooler, while as air falls on the leeward side of a mountain, it expands and becomes warmer.
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which statement about moist air moving over a mountain is correct?
as air falls on the leeward side of a mountain, it expands and becomes warmeras air rises on the windward side of a mountain, it contracts and becomes cooler. as air falls on the leeward side of a mountain, it contracts and becomes warmer. as air rises on the windward side of a mountain, it expands and becomes warmer.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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for a surface low pressure system to intensify, where must the upper-level trough be located relative to the surface low? group of answer choices north of the surface low south of the surface low west of the surface low east of the surface low directly above the surface low
For a surface low pressure system to intensify, the upper-level trough must be located to the west of the surface low. Therefore the correct option is option C.
A low-pressure system is a location on Earth's surface where the air pressure is lower than that of surrounding locations. As air moves away from a low-pressure area, it rises and cools, generating clouds and potentially precipitation.
The cyclonic flow of the air around a low-pressure area, where the air is flowing counterclockwise in the Northern Hemisphere, is another feature of a low-pressure area.
The airflow toward the low-pressure area at the surface is pulled inward and upward, resulting in air rising and the production of clouds, rain, and other weather events. Therefore the correct option is option C.
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The following question may be like this:
For a surface low pressure system to intensify, where must the upper-level trough be located relative to the surface low? group of answer choices
north of the surface low
south of the surface low
west of the surface low
east of the surface low
directly above the surface low
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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how long will it take for a 10km-tall thunderstorm (a thunderstorm whose top is at 10 km in elevation) to form above mt. humphreys if the updraft winds are 350m/min and the cloud base is 500m above the peak?
It will take 28.57 minutes for a 10km-tall thunderstorm to form above Mt. Humphreys if the updraft winds are 350m/min and the cloud base is 500m above the peak.
The amount of time it takes a 10km-tall thunderstorm (a thunderstorm whose top is at 10 km in elevation) to form above Mt. Humphreys provided that the updraft winds are 350m/min and the cloud base is 500m above the peak is calculated as using the formula:
Time required to form the cloud = H/U,
where H is the height and U is the updraft speed
In this case, Height of the thunderstorm = 10 km, Height of the base of cloud = 500 mm and Updraft speed = 350 m/min.
Plugging in values in the formula:
Time taken to form a thunderstorm of height 10 km = 10000/350=28.57 minutes (approx.)
Therefore, it will take approximately 28.57 minutes to form a 10km tall thunderstorm above Mt. Humphreys if the updraft winds are 350m/min and the cloud base is 500m above the peak.
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6.5. what is harmonic tremor? question 5 options: a. a large earthquake that causes landslides b. a seismographic reading that indicates magma is on the move c. ground shaking due to hydrothermal activity d. the manner in which the ground shakes due to a stampede of buffalo
A harmonic tremor is a type of seismic activity characterized by a continuous, low-amplitude ground shaking. The release of large amounts of stored energy in the form of volcanic or geothermal activity generally causes it.
Harmonic tremors can indicate that magma is on the move or that pressure is building up within a volcano's plumbing system. In some cases, they may also be caused by hydrothermal activity or by the motion of glaciers.
In general, harmonic tremors are seen as a warning sign of potential future volcanic activity. They can be used to alert scientists and other officials to take preventive steps to protect nearby populations. It is also possible to monitor harmonic tremors to gain insight into volcanic activity and the behavior of magma within the volcano's plumbing system.
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Suggest materials that can be used to repair damaged weather instruments in a weather station and explain your choices
Some materials that can be used to repair damaged weather instruments in a weather station include:
Epoxy Silicone sealant Lubricant How can we fix instruments at weather stations ?Epoxy is a strong adhesive that can be used to repair cracks or breaks in plastic or metal components of weather instruments. It can also be used to seal leaks in certain instruments.
Silicone sealant is a flexible sealant that can be used to seal joints and gaps in weather instruments. It is particularly useful for instruments that are exposed to moisture or humidity.
For instruments that have moving parts or require periodic maintenance, lubricants such as silicone spray or WD-40 can be used to keep them functioning properly.
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__________ extend into the water to reduce the energy from waves thereby reducing their power. They cause a break in the longshore current.
Breakwaters extend into the water to reduce the energy from waves thereby reducing their power. They cause a break in the longshore current.
A breakwater may be a natural or man-made structure that is intended to act as a barrier against the action of waves. Breakwaters have various forms and designs, but they are typically made of rock, concrete, or other durable materials that can withstand the forces of waves. Breakwaters can help to control the direction of longshore currents by creating a barrier that redirects the flow of water. They cause a break in the longshore current, which can help to reduce erosion along the shoreline. They can also be used to protect harbors and other marine structures from the damaging effects of waves and currents.
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you are hiking in your favorite forest when you encounter a surface that appears to have very fine directional scratches in it. what are these features?
Answer:
The fine directional scratches that appear on a surface could be glacial striations. Glacial striations are scratches or gouges made in bedrock by rock fragments that are embedded in the base of a glacier. As the glacier moves over the bedrock, these rocks act like chisels, carving and scraping the rock beneath them. The scratches or grooves left behind can reveal the direction in which the glacier was moving.
how do present-day rivers compare to what those same rivers would have been like at the end of the glacial ages? multiple choice question.
Rivers today differ significantly from what they would have been like during the glacial ages. The rivers would have been wider, deeper, and more sinuous, with fewer meanders and a greater variety of aquatic species. Additionally, they would have had increased erosion and more sediment in the water. Correct answer is all of the above, option D
Additionally, there would have been more debris and sediment in the water, such as sand, gravel, and boulders, as well as a greater variety of aquatic species. The rivers of today are very different from what they would have been during the last glacial period. Most rivers would have been bigger and deeper at that period because of increased erosion brought on by more glacier runoff. Since that glacial melt water is more strong and swift than current rivers, they would also be more sinuous and have fewer meanders.
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Correct question would be " how do present-day rivers compare to what those same rivers would have been like at the end of the glacial ages? options could include a) wider, deeper, and more sinuous; b) fewer meanders and a greater variety of aquatic species; c) increased erosion and more sediment in the water; or d) all of the above"
this is a map view of a fault. you are looking down on the fault from above. a) what type of fault is it b) what type of forces are involved c) how would you describe the relative lateral motion?
A.) The type of force that causes it is the compressive force that leads to the relative lateral motion towards each other.
B.) A reverse fault is a type of fault where one block of rocks moves vertically above the other in response to compression.
C.) The rocks move vertically along the fault plane, with the block on one side moving up and the block on the other side moving down.
Reverse faults are characterized by a steep angle of the fault plane and are commonly found in regions of continental crust subjected to compression, such as regions of plate convergence.
The given image shows a reverse fault because the block on the right has been pushed up by the block on the left.
Types of forces involved in a reverse fault: When the compression force pushes two blocks of rock towards each other, it creates a reverse fault.
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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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the earth's lowest barometric pressures are associated with hurricanes (typhoons). frontal systems (cold and warm fronts). sea level. cold and dry climates. very cold temperatures.
The Earth's lowest barometric pressures are associated with hurricanes (typhoons).
What are hurricanes (typhoons)?
Hurricanes or typhoons are severe tropical storms characterized by low atmospheric pressure, heavy rain, and strong winds. In the West, hurricanes are called typhoons in the East. Such storms develop in the Atlantic Ocean, Gulf of Mexico, and the Caribbean Sea in the United States.
Typhoons are formed in the Pacific Ocean, especially in Japan and the Philippines.
What is barometric pressure?
Barometric pressure is a measure of air pressure that varies from location to location. The pressure exerted by the weight of the atmosphere on the Earth's surface is known as barometric pressure.
The barometric pressure is measured in units of mercury millimeters (mmHg) or inches of mercury (inHg) in the United States, as well as in millibars (mb) or kilopascals (kPa) in other countries. The Earth's lowest barometric pressures are associated with hurricanes (typhoons).
Hurricanes (typhoons) are storms characterized by low atmospheric pressure, heavy rain, and strong winds. When such a storm passes through an area, it causes the barometric pressure to decrease, resulting in the lowest barometric pressures.
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describe the trend in shallow groundwater and subsurface soil temperatures that you observe moving from north to south along the line you drew
Generally, it is important to note that the trends have significant impacts on ecosystems, agricultural productivity, and human societies, and monitoring and managing these resources is crucial for sustainable development.
What trend do we have in shallow groundwater and subsurface soil temperatures?in general, the trends in shallow groundwater and subsurface soil temperatures can vary depending on the location and time of year. In some areas, there may be a trend towards declining water levels and increasing soil temperatures due to factors such as drought, overuse of groundwater, and climate change.
In some other areas, there may be a trend towards rising water levels and decreasing soil temperatures due to factors such as increased precipitation, improved water management practices, and natural fluctuations in the hydrologic cycle.
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pure loam is considered to be the best kind of soil for a farm or garden and is often defined as a soil with roughly equal proportions of sand, silt, and clay. is that what the diagram shows?
Yes, pure loam is considered to be the best kind of soil for a farm or garden and is often defined as a soil with roughly equal proportions of sand, silt, and clay.
Loam soil is soil that is made up of an even mix of sand, silt, and clay. Loam is a form of soil that is often regarded as the perfect garden soil. It has a granular structure, which makes it easy to work with, and it is very fertile because it contains equal amounts of sand, silt, and clay.
Loam soil contains a lot of organic matter and is well-aerated, so it is ideal for cultivating a variety of crops. The diagram given below shows that pure loam is considered to be the best kind of soil for a farm or garden and is often defined as a soil with roughly equal proportions of sand, silt, and clay.
As a result, it can be concluded that the diagram shows that pure loam is regarded as the ideal soil type for a farm or garden.
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