This method involves identifying potential avalanche areas and using explosives to trigger small avalanches before they can become larger and more dangerous.
Expansive water drainage systems and allowing skiers to use only avalanche chutes are not effective methods for managing snow avalanches, as they do not address the root cause of the problem. Increasing the slope's load by planting vegetation on the cornice of mountain slopes is also not a suitable method, as it can actually increase the risk of avalanches by adding weight to the already unstable slope.
Targeted, controlled explosions are used to trigger smaller, controlled avalanches, which can reduce the risk of larger, more dangerous avalanches occurring naturally. This method is commonly used in ski resorts and mountainous regions to protect people and infrastructure.
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Why is it important to protect the Chowanoke Crayfish, a resident of sluggish woodland streams in the Chowan River Basin?
First, as an endemic species, it is unique and irreplaceable. Second, the Chowanoke Crayfish plays an important role in the ecosystem as a predator and prey. Third, protecting the Chowanoke Crayfish and its habitat can have broader ecological benefits.
Only in the Chowan River Basin, notably in the slow-moving wooded streams of the basin, can one find the endemic Chowanoke Crayfish.
The Chowanoke Crayfish should be protected for a number of reasons. It is special and distinct because it is an indigenous species. Once a species is gone, it cannot be brought back, and its loss can have a ripple effect on the ecosystem as a whole.
Second, the Chowanoke Crayfish is a significant predator and prey in the ecology. Crayfish are a crucial component of the aquatic food chain because they provide food for a variety of other species.
Third, safeguarding the habitat of the Chowanoke Crayfish may have wider ecological advantages.
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What is the size in square miles of the Chowan River Basin?
The Chowan River Basin is a vital and complex ecosystem that plays an important role in the health and well-being of the region. Its size and diversity make it a unique and valuable resource, providing habitat for wildlife, recreation opportunities for residents and visitors, and essential water resources for local communities.
The Chowan River Basin is a large and complex system of rivers, streams, wetlands, and other waterways that covers a significant portion of northeastern North Carolina. In terms of size, the basin encompasses a total area of approximately 4,800 square miles. This includes a wide range of habitats and ecosystems, from forested uplands to marshy wetlands, that are home to a diverse array of plant and animal species. The basin is also an important source of water for the surrounding communities, supporting agriculture, industry, and recreation.
One of the key features of the Chowan River Basin is its extensive network of tributaries, which feed into the main stem of the Chowan River and ultimately flow into the Albemarle Sound. This network includes major rivers such as the Meherrin, Nottoway, Blackwater, and Roanoke, as well as numerous smaller streams and creeks. The basin is also home to several large reservoirs, including Lake Gaston and Kerr Lake, which are used for water supply, flood control, and other purposes.
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Which trees are dominant at Merchants Millpond State Park, according to the CRB article?
According to the CRB article, the dominant trees at Merchants Millpond State Park are bald cypress (Taxodium distichum) and tupelo (Nyssa spp.).
These trees thrive in the park's wetland habitat and play an essential role in shaping the natural community. The bald cypress is notable for its adaptations to marshy circumstances, such as its "knees" that protrude from the water and aid in root aeration.
Many birds and mammals rely on the tupelo, also known as the black gum, for food, and its leaves turn a brilliant red in the autumn.
At Merchants Millpond State Park, the combination of bald cypress and tupelo creates a distinct and beautiful landscape.
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What is the precipitation like in the arctic tundra?.
Precipitation in the Arctic tundra is relatively low, with an average annual precipitation ranging from 15 to 25 centimeters (6 to 10 inches).
The typical winter temperature is -34° C (-30° F), whereas the average summer temperature is from 3-12° C (37-54° F), allowing this biome to thrive. Rainfall may differ in different parts of the Arctic. The annual precipitation, including melting snow, ranges between 15 and 25 cm (6 and 10 inches). Soil takes time to create. The tundra receives 150 to 250 mm of precipitation each year, including melting snow. That is less than most of the world's most beautiful deserts! Despite this, the tundra is frequently moist because the low temperatures allow water evaporation to be sluggish.
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According to the Chowan River Basin article, where is Hydrilla beginning to be found?
The Chowan River Basin article mention that Hydrilla is an invasive aquatic plant species that is present in many water bodies in the United States, including the Chowan River Basin.
Although it is native to Asia, the hydrilla plant has been spread throughout the world, including to North America, where it is regarded as one of the most troublesome aquatic weeds. It has the potential to grow quickly and produce thick mats on the water's surface, which can obstruct recreational activities, worsen water quality, and endanger local aquatic life.
Since the 1980s, Hydrilla has been in the Chowan River Basin and has had a substantial impact on the ecosystem. The adoption of integrated pest management and the creation of a long-term management strategy are two strategies mentioned in the article for managing and controlling the spread of Hydrilla in the basin.
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apatosaurus, allosaurus, diplodocus, and stegosaurus have all been excavated from the late jurassic found at dinosaur ridge, colorado.
T/F
True. Dinosaur Ridge is a famous paleontological site located near Morrison, Colorado, in the western United States. It is part of the Morrison Formation, which dates back to the Late Jurassic period, around 150 million years ago.
Numerous dinosaur fossils have been discovered at Dinosaur Ridge, including Apatosaurus, Allosaurus, Diplodocus, and Stegosaurus, as well as other dinosaur genera. These fossils have helped paleontologists to understand more about the diversity and evolution of dinosaurs during the Late Jurassic period, including their behavior, ecology, and morphology.
In addition to dinosaur fossils, Dinosaur Ridge also contains other geological features, such as sedimentary rocks, sandstone cliffs, and petrified wood, that provide valuable insights into the ancient environment and climate of the region.
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what is drawdown, and how does it relate to the cone of depression? view available hint(s)for part a what is drawdown, and how does it relate to the cone of depression? drawdown is when the water table in an entire region is lowered because of water discharge. a cone of depression results when the rock or sediments around the point of discharge undergo subsidence. drawdown is when the water table around a well is lowered because of water discharge. this depression in the water table is conical and is called a cone of depression. drawdown occurs when water is drawn down into the groundwater from a recharge area. a cone of depression occurs if an area has not been recharged in a very long while. a drawdown describes a natural lowering of the water table. cones of depression form around streams where the water table is lowering. drawdown is when the water table around a well is lowered due to water recharge. this depression in the water table is conical and is called a cone of depression.
Drawdown is the lowering of the water table around a well due to water discharge. It is closely related to the cone of depression, which is the conical-shaped depression in the water table that forms around the point of discharge.
When water is pumped out of a well, the water table around the well is lowered. This lowering of the water table is called drawdown. As more water is extracted, the area affected by the drawdown expands, and the shape of the depression in the water table forms a cone-like shape, known as the cone of depression. The cone of depression represents the zone where the groundwater level has been lowered due to the pumping of water from the well.
Drawdown and the cone of depression are interconnected concepts in groundwater management. Drawdown is the process of lowering the water table around a well due to water discharge, while the cone of depression is the resulting conical-shaped depression in the water table that forms around the point of discharge.
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The drainage density on clay soils is likely to have what relationship to the drainage density on gravel soils?.
The drainage density on clay soils is likely to be lower than on gravel soils. This is because clay soils have a higher density than gravel soils, which means that they can hold more water and have less space for water to drain through. As a result, the drainage density on clay soils is lower and water tends to accumulate on the surface for longer periods of time.
This can lead to issues such as waterlogging, which can affect plant growth and soil health. It is important to consider the drainage properties of different soil types when planning land use and management practices, as this can have a significant impact on productivity and environmental sustainability.
Hi! The drainage density on clay soils is likely to be lower compared to the drainage density on gravel soils. This is due to the differences in their properties. Clay soils have higher density and smaller pore spaces, which limit water infiltration and movement through the soil. On the other hand, gravel soils have a lower density and larger pore spaces, allowing water to easily infiltrate and drain through the soil. As a result, clay soils tend to have poorer drainage while gravel soils exhibit better drainage characteristics.
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The drainage density on clay soils is likely to be lower than the drainage density on gravel soils. This is because clay soils have smaller pore spaces and slower infiltration rates compared to gravel soils, which can lead to increased runoff and less efficient drainage.
It's important to note that drainage density is a measure of the number of stream channels in a given area and is influenced by a variety of factors including soil type, topography, and precipitation patterns. Clay soils are known for their low permeability and high water-holding capacity, which means that water moves slowly through the soil and can easily become saturated. This can result in increased runoff and decreased drainage density because there is less water available to flow through stream channels. Gravel soils, on the other hand, have higher permeability and lower water-holding capacity, which allows water to move more freely through the soil and results in higher drainage density. Therefore, it can be concluded that the drainage density of clay soils is likely to have a negative relationship with the drainage density on gravel soils.
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The presumed solution to the paradox is that the greenhouse gas concentration was ______ earlier in Earth's history than it is today.
The presumed solution to the paradox is that the greenhouse gas concentration was lower earlier in Earth's history than it is today.
According to theory, the Sun luminosity was much lower in its early years, which should have caused Earth's climate to be much colder. The Earth did however have a relatively stable and warm climate during this time, as indicated by the geological and paleontological evidence.
This paradox is explained by the higher greenhouse gas concentration in the early Earth's atmosphere, which helped to trap heat and sustain a warmer climate despite the lower solar output. In light of this, the statement implies that the Faint Young Sun Paradox can be resolved thanks to the atmosphere's earlier Earth's higher concentration of greenhouse gases.
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(q020) tillites group of answer choices offer evidence of one ice age on the earth before the pleistocene ice age. contain clasts that have been glacially polished and striated. consist of sandstone and mudstone. are rocks composed of well-sorted sediment.
Tillites offer evidence of one ice age on the earth before the Pleistocene ice age, contain clasts that have been glacially polished and striated and consist of sandstone and mudstone.
Tillite is a sedimentary rock made up of consolidated masses of unweathered blocks, which are massive, angular, disconnected rock bodies, as well as glacial till, which is unsorted and unstratified rock material that glacial ice deposited in a rock flour-matrix or paste of unweathered rock. Tillite is made up of a matrix with relatively fine-grained rock fragments, ranging in size from pebbles to bigger chunks.
The matrix, which makes up a sizable portion of the rock, is often an extremely fine-grained paste made of angular quartz and feldspar grains and rock pieces. Its color ranges from dark gray to greenish black. The only tillites with a decent likelihood of being preserved in the geologic record are those produced from the till deposited by continental ice sheets.
Therefore, option A, B and C are the correct answers.
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Part D
The bar graph shows the cost per megawatt-hour comparison of various renewable and nonrenewable energy sources in the United States. The blue portion of the bars represents the cost of electricity. The red portion represents the additional system costs of harnessing that type of energy. Systems costs may include equipment expenses and costs of connection to a power grid.
Based on the graph, compare and contrast the total cost of renewable and nonrenewable energy sources. Explain what might account for the differences in cost. Do additional research as necessary.
The bar graph illustrates the cost per megawatt-hour comparison of renewable and nonrenewable energy sources in the US, considering blue as the cost of electricity and red as the extra system cost incurred. Wind energy is the cheapest source with a system cost of around $3/MWh, followed by solar and hydroelectric energy. Natural gas and coal have lower electricity costs but high system costs ($28/MWh and $60/MWh, respectively). Nuclear energy has the highest system cost ($105/MWh), making it one of the most expensive energy sources. Overall, the graph highlights the significant difference in system costs among energy sources, making renewable sources a more cost-effective option.
most of the loess deposits seen in the united states and europe are the product of: group of answer choices desert basins tsunami deposits glacial outwash mass transport deposits
Most of the loess deposits seen in the United States and Europe are the product of glacial outwash.
The majority of the loess deposits still present in central USA were laid down during the last glacial epoch, a time of exceptionally high silt production rates from the LIS and other nonglacial sources in the midcontinent. Thus, loess deposition occurred during the last glacial period even in areas where nonglacial sources were significant, such as the Great Plains.
Loess is pale and haphazardly arranged. It is readily crumbled. Loess is robust enough to serve as substantial walls while remaining malleable enough to be carved. Although glaciers can also form loess, wind is the primary cause of its formation. Loess may occur when glaciers pulverize rocks into a fine powder. The powder travels to the glacier's terminus by streams. The sediment turns into loess.
Therefore, option C is the correct answer.
The complete question is, "Most of the loess deposits seen in the united states and Europe are the product of
A. desert basins
B. tsunami deposits
C. glacial outwash
D. mass transport deposits
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Which u. K. Country does not have any national parks?.
Although there have been contentious efforts to establish a national park in the Mourne Mountains, Northern Ireland does not currently have any national parks.
A public park is the biggest created and kept up with by country states for biodiversity protection. A sovereign state likewise lays out or possesses a booking of regular, decently, or made property. More than 22,500 square kilometers make up all of the national parks in the United Kingdom.
The Cairngorms National Park is the largest, while the Broads National Park is the smallest. Over 100 million people visit the UK's national parks each year, especially those in England and Wales. Northern Ireland's landscapes are renowned for their quality and variety.
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Convection occurs in the troposphere but not in the stratosphere because:.
Answer:
The temperature structure of the stratosphere is one of warmer air over colder air. No, convection never occurs in the stratosphere because of this temperature structure.
which of the following pieces of evidence most strongly supports the common origin of all life on earth?fduring periods of rapid environmental change, what may happen to a species that was well-suited to the former environment
The piece of evidence that most strongly supports the common origin of all life on earth is the universal genetic code.
All living organisms on earth use the same genetic code to translate DNA sequences into proteins, indicating a common ancestor.
Regarding the second part of the question, during periods of rapid environmental change, a species that was well-suited to the former environment may struggle to adapt and survive. This can lead to a decline in population, extinction, or evolution into a new species better adapted to the new environment.
Environmental changes can include natural disasters, climate change, or human activities such as deforestation or pollution. Therefore, it is important to understand the impact of environmental changes on different species and take steps to protect the natural world.
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which of the following geologic features provide paleoclimatic information that indicates the latitude of an area while such features formed?
The correct Answer: C) Fossil coral reefs Fossil coral reefs provide paleoclimatic information that can indicate the latitude of an area when they formed.
Coral reefs form in warm, shallow waters, and their distribution in the geological record can be used to infer the latitude of the landmass where they formed. This is because the growth of coral reefs is limited by temperature, so they are found only in regions where the water temperature is warm enough to support coral growth. As a result, the presence of fossil coral reefs in a particular area can provide information about the latitude and paleoclimate of that region during the time when the reefs formed. Glacial till and cross-bedded sandstones are not typically used to infer the latitude of an area during their formation.
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Full Question ;
Which of the following geologic features provide paleoclimatic information that indicates the latitude of an area while such features formed?
A) Glacial till
B) Cross-bedded sandstones
C) Fossil coral reefs
What is the relationship between the development of trade and the development of technology?
A. The developments of trade and technology are not related.
B. A region can only trade if it has modem transportation technology
C. Regions that want to develop trade avoid the development of technology
D. The development of technology can encourage the advancement of trade.
The relationship between the development of trade is: The development of technology can encourage the advancement of trade. Option D
What is the relationship between the development of trade and the development of technology?There is a close relationship between the development of trade and the development of technology. Technology is a major driver of economic development throughout history.
The development of technology has enabled the advancement of trade by making it easier, faster, and more efficient to produce, distribute, and sell goods and services, and to connect with customers and suppliers across the globe.
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Explain why there are three ways to measure the size of an earthquake.
There are three ways to measure the size of an earthquake because each method provides different information about the earthquake.
The first way is the Richter Scale, which measures the amplitude of the seismic waves at a specific distance from the earthquake's epicenter. This scale is logarithmic, meaning that each whole number increase represents a ten-fold increase in wave amplitude and a thirty-fold increase in energy released. The second way is the moment magnitude scale, which measures the total energy released during an earthquake, including both the amount of movement along the fault and the area of the fault that ruptured. This scale is more accurate for larger earthquakes than the Richter Scale. The third way is the intensity scale, which measures the effects of an earthquake on people, buildings, and the environment. This scale is subjective, as it depends on the perception of people in the affected area. By using these different methods, scientists can gain a more complete understanding of the size and impact of an earthquake.
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Estimate the range of time (XX to YY MYA) that the rocks in Death Valley were deposited in a marine environment. Explain your answer in 1-2 sentences.
The rocks in Death Valley were deposited in a marine environment during the Paleozoic era, which occurred between approximately 541 to 252 million years ago (MYA).
Based on geological studies, the rocks in Death Valley are estimated to have been deposited between 570 to 250 MYA, spanning the entire Paleozoic era. This range includes the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian periods, during which marine sedimentary rocks were formed due to the area being submerged under the ocean. The different types of sedimentary rocks found in Death Valley, including limestone, sandstone, and shale, provide evidence of the various marine environments that existed during this time period.
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given enough time, what would happen to the shape of a typical shoreline? question 1 options: a) it would become more jagged b) it would become deeper c) it would become straighter d) it would become more angled
The correct option is D) it would become more jagged. Shorelines are constantly changing due to natural processes such as erosion and deposition caused by waves, tides, and currents.
Over time, the shape of a shoreline would become more jagged as erosion removes material from some areas and deposition adds material to others, creating curves and irregularities. Additionally, geological processes such as faulting and volcanic activity can cause significant changes to shoreline shape over long periods of time.
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Full Question ;
Given enough time, what would happen to the shape of a typical shoreline? a) it would become more angled b) it would become deeper Oc) it would become straighter d) it would become more jagged
landforms are created through destructive forces such as weathering. which of these is an example of physical weathering?
Landforms are created through destructive forces such as weathering, so abrasion is an example of physical weathering that is in Option B as the physical weathering is a type of weathering that involves mechanical breakdown.
What is the significance of weathering in the environment?
Physical weathering is caused by physical forces, such as the expansion and contraction of rock due to changes in temperature and abrasion is a specific type of physical weathering that occurs when rock or soil is rubbed against other rock or soil. In physical weathering, rock fragments or particles are carried by water, wind, or ice, and the repeated collisions and friction caused by abrasion can lead to significant changes in the shape.
Hence, landforms are created through destructive forces such as weathering, so abrasion is an example of physical weathering that is in Option B as the physical weathering is a type of weathering that involves mechanical breakdown.
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Full Question ;
Landforms are created through destructive forces such as weathering. Which of these is an example of physical weathering? A acid rain. B abrasion. C hydrolysis. D oxidation
which rule tells you whether the basalt or layer d is younger? the principle of cross cutting relations the principle of superposition the principle of inclusions the principle of lateral continuity
The principle that tells us whether basalt or layer D is younger is the Principle of Superposition. This principle states that in a sequence of undisturbed sedimentary rock layers, the oldest layer is at the bottom and the youngest layer is at the top.
In this case, if layer D is found on top of the basalt, then layer D is younger than the basalt. If the basalt is found on top of layer D, then the basalt is younger. This is because the basalt, being a volcanic rock, would have been formed after the deposition of the sedimentary layer D.
The Principle of Cross-Cutting Relations, on the other hand, is used to determine the relative ages of features that cut across rock layers, such as faults or intrusions. The Principle of Inclusions is used to determine the age of a rock unit based on the inclusion of fragments of an older rock within it. The Principle of Lateral Continuity states that layers of sedimentary rock were originally continuous and extended in all directions until they thinned out or were deposited against an obstruction.
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in a stream's headwaters, what size of stream channel material would most likely be found? group of answer choices sand, silt, and clay dissolved minerals large, angular boulders well-rounded stones and pebbles
In a stream's headwaters, the size of stream channel material would most likely be well-rounded stones and pebbles. The headwaters of a stream refer to the uppermost part of a stream, where the water originates from springs, snowmelt, or groundwater.
The water in the headwaters is usually fast-moving and turbulent, which causes erosion of the stream channel. The erosion process results in the formation of small, well-rounded rocks and pebbles that are carried along by the water. These materials are transported downstream, where they are further broken down into smaller particles such as sand, silt, and clay. Dissolved minerals can also be found in the water, as they are picked up by the water as it flows through the rocks and soil of the surrounding landscape. Overall, the stream channel material in a headwater stream tends to be larger and more angular than the material found downstream.
Hi! In a stream's headwaters, you would most likely find large, angular boulders as the dominant stream channel material. This is because headwaters are typically located in higher elevations where erosion and weathering processes are more intense. As water flows downstream, it gradually transports and rounds the materials, resulting in smaller and more rounded stones, pebbles, sand, silt, and clay. Dissolved minerals can be found throughout the stream, but they don't contribute to the size of the stream channel material.
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true or false. if the environmental temperature is greater than the parcel temperature, the air parcel is stable.
The given statement, "if the environmental temperature is greater than the parcel temperature, the air parcel is stable." is false because if surrounding temperature is greater than the parcel temperature, it is said to be unstable.
The air parcel has a propensity to descend if its temperature is lower than that of the surrounding air mass because it is dense than the surrounding air. A stable air is defined as air that tends to sink. The parcel of air is less dense and has a tendency to ascend if its temperature is higher than that of the surrounding air mass. Air rising is said to as unstable.
As it rises, air tends to chill and condense, and as it descends, it tends to warm and become dry. A parcel of air is a hypothetical air mass that doesn't interchange characteristics with nearby air masses. Air masses do in fact interchange attributes, however this frequently happens extremely slowly, particularly when the air mass are huge. When there is no heat transfer between a parcel of air and the air around it, the process is said to be adiabatic.
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what are georiga´s famous mountains lakes and rivers.
Georgia, a state positioned in the southeastern United States, is host to famous mountains, lakes, and streams.
Mountains:
Brasstown Bald: The highest elevation in Georgia, situated in the northern part of the state.
Blood Mountain: A popular trekking locale found in the Appalachian Mountains.
Rabun Bald: A mountain summit in the Chattahoochee-Oconee National Forest.
Lakes:
Lake Lanier: A huge reservoir sitting northeast of Atlanta, renowned for its boating and angling.
Lake Allatoona: An acclaimed leisure lake located northwest of Atlanta.
Rivers:
Savannah River: A substantial river making up part of the boundary between Georgia and South Carolina.
Ocmulgee River: A significant river in core Georgia, well-known for its ancient Native American sites and captivating prettiness.
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a wide volcano that produces mainly basaltic lava flows is called a _____
A wide volcano that produces mainly basaltic lava flows is called a shield volcano.
These types of volcanoes have a low profile and broad shape that resemble a warrior's shield. They are formed by repeated eruptions of basaltic lava that flows out in a gentle manner, creating a broad and flat surface. Shield volcanoes are typically found in areas with hotspots, such as the Hawaiian Islands.
Due to the slow-moving nature of basaltic lava, these eruptions are not typically explosive and do not pose as much of a threat to human populations as other types of volcanoes. Shield volcanoes can grow to be extremely large and are some of the largest volcanoes on Earth.
The Hawaiian shield volcano Mauna Loa, for example, stands at over 13,000 feet tall and covers an area of around 2,035 square miles.
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List the order of events, first on top, that would lead to the formation of a tsunami due to an earthquake.1.) megathrust is locked, causing the seafloor to bulge under stress 2.) megathrust ruptures, and bulging plate changes shape 3.) water above the plate lifts up toward the surface, forming a ridge of higher water 4.) a tsunami radiates away from the disturbance; not noticeable in the open ocean 5.) tsunami approaches shore; energy concentrates in shallows to create a higher wave
Answer:
Megathrust
Explanation:
(q001) groundwater group of answer choices completely fills the zone of saturation above the water table. flows mainly in underground river channels. flows faster through shale than sandstone. typically moves slowly within the ground through permeable rock layers like sandstone.
Groundwater completely fills the zone of saturation above the water table.
Groundwater is the water that is stored below the earth's surface in soil and rock formations. This water fills the spaces between soil and rock particles and flows through permeable layers of rock like sandstone, as well as underground river channels. The movement of groundwater can vary depending on the type of rock it flows through, with shale allowing for faster flow than sandstone. Despite these differences, groundwater generally moves slowly within the ground due to the nature of permeable rock layers.
Groundwater is water that is stored in and moves through the pores and cracks in underground rock layers. It fills the zone of saturation and is found above the water table. Permeable rock layers, such as sandstone, allow water to flow more easily compared to less permeable layers like shale. This slow movement of groundwater is an important part of the natural water cycle and contributes to the replenishment of aquifers and surface water bodies.
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which of the following rock / mineral types would make a good tombstone in an arid region but not in a humid region?
Answer:
marble
Explanation:
because its really strong
In a hot-spot volcanic island chain, such as the Hawaiian Islands, which of the following is true?All volcanoes in the chain can be simultaneously active.The ages and distance between volcanoes can be used to calculate plate velocities.The presence of volcanism is related to a plate boundary.The magma source moves to form a hot-spot track.
In a hot-spot volcanic island chain, such as the Hawaiian Islands, the magma sources move to form a hot-spot track. Option d is correct answer.
In a hot-spot volcanic island chain, the volcanoes are formed by magma rising from a hot spot within the mantle, which could be an area of unusually high temperature and a warm stream. As the structural plate moves over the hot spot, a series of volcanoes is shaped, with the most seasoned and most disintegrated volcanoes at one end of the chain and the youngest and most dynamic volcanoes at the other end.
The movement of the tectonic plate over the hot spot causes the magma source to move, making a hot-spot track that's checked by a chain of volcanic islands. As the plate moves away from the hot spot, the magma source is cut off and volcanism ceases. In this way, as it were the volcanoes that are as of now over the hot spot are dynamic, whereas the others are dormant or terminated.
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