productivity in tropical oceans is: question 5 options: nutrient limited. light limited. light and nutrient limited. oxygen limited.

Mainly a fold and thrust belt bell lets us know that there was net pressure across the plate brokenness and that the stones making up the top plate were of the properties to permit this kind of distortion to happen.

Fold-and-thrust belts are a trademark primary unit saw at the external piece of mountain belts and accretionary crystals framed along concurrent plate limits. The dynamic overlays and pushes normally create at the Piedmonts and inside the foreland bowls of dynamic mountain belts.

It structures due to contractional tectonics. Overlay and push belts regularly structure in the forelands neighboring major orogens as misshapen spreads outwards.

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Yes, this can be seen as an example of collective action. Collective action refers to a situation where a group of individuals come together to achieve a common goal.

In this case, everyone in attendance at the midnight screening of the rocky horror picture show decided to dress in skimpy, revealing clothing despite the theater lobby mandating a dress code of appropriate, everyday attire. This decision was made collectively by the group to adhere to a different set of standards than what was prescribed by the theater. Therefore, this can be seen as an example of collective action. Collective action refers to a coordinated effort by a group of people to achieve a common goal. In this case, the common goal was to express their enthusiasm for the Rocky Horror Picture Show by dressing in skimpy, revealing clothing, despite the theater's dress code. The attendees likely shared a mutual understanding and agreement to ignore the dress code, showcasing their unity and shared interest in the event.

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Answer:

the Indian Ocean basin is the warmest ocean basin on the planet. Temperatures vary according to location and the ocean's currents. As you can imagine, the nearer we are to the Equator, the warmer the water tends to be. In coastal regions near the Equator, the temperature can reach 28°C (82°F).

Explanation:

The semi-major axis of Comet Hyakutake's orbit is approximately 88,000 AU.

We can use Kepler's third law to relate the orbital period of a comet to the semi-major axis of its orbit:

T^2 = (4π²/GM) a³

where T is the orbital period, G is the gravitational constant, M is the mass of the sun, and a is the semi-major axis of the comet's orbit.

We can rearrange this equation to solve for a:

a = [T² (GM) / 4²][tex]^(1/3)[/tex]

Plugging in the values given:

T = 30,000 years

G = 6.6743 × 10⁻¹¹ m³ kg⁻¹ s⁻² (gravitational constant)

M = 1.989 × 10³⁰ kg (mass of the sun)

a = [30,000² (6.6743 × 10⁻¹¹× 1.989 × 10³⁰) / 4π²[tex]]^(1/3)[/tex]

a ≈ 88,000 astronomical units (AU)

Therefore, the semi-major axis of Comet Hyakutake's orbit is approximately 88,000 AU.

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As the depth of geosphere increases the pressure and temperature also increase.

Hence, the answer is Pressure and Temperature increase.

The Earth's temperature increases with depth due to the geothermal gradient. Highly viscous or partially molten rock is found at the margins of tectonic plates, increasing the gradient nearby. The heat content of Earth is estimated to be [tex]10^{31}[/tex] joules.

Much of the heat is created by radioactive decay of elements in the mantle. Heat is also generated by gravitational potential energy release during Earth's accretion. Latent heat is released as the outer core crystallizes. Tidal forces on Earth may also generate heat.

The pressure also increases with depth due to the weight of the rock and other materials above. This is because the Earth's gravity pulls all objects towards the center of the planet, creating pressure on the materials below.

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The given question is incomplete. hence, the complete question should be:

How do pressure and temperature change inside as depth of the geosphere increases?

A. Pressure and temperature decrease.

B. Pressure increases; temperature decreases.

C. Pressure decreases; temperature increases.

D. Pressure and temperature increase.

The gravitational field strength of the unknown planet will be approximately 1.953 times that of Earth.

The gravitational field strength of a planet depends on its mass and radius. The equation to calculate the gravitational field strength at the surface of a planet is:

g = G*M/[tex]R^2[/tex]

where g is the gravitational field strength, G is the gravitational constant, M is the mass of the planet, and R is the radius of the planet.

If the planet has the same density as Earth, but a radius that is 0.8 times that of Earth, then its Bwill be:

M = (4/3)pi(0.8R[tex])^3d[/tex]

where d is the density of the planet.

Substituting the values and simplifying, we get:

M = (4/3)pi(0.8R[tex])^3d[/tex] = (4/3)pi(0.512*[tex]R^3[/tex])d = 1.365M_Earth

where M_Earth is the mass of Earth.

Therefore, the gravitational field strength of the planet will be:

g = GM/[tex]R^2[/tex] = G(1.365M_Earth)/(0.8R)^2 = 1.953*g_Earth

where g_Earth is the gravitational field strength on Earth.

So, the gravitational field strength of the unknown planet will be approximately 1.953 times that of Earth.

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When the lower mantle gets hot from contact with the outer core, the material initially undergoes a process called convection. Convection occurs when the heat causes the material to become less dense and rise, creating a flow of material. As the material rises, it cools and becomes more dense, causing it to sink back down towards the core.

This continual process of rising and sinking material creates a circular motion known as a convection cell. These cells are responsible for moving the Earth's tectonic plates and driving volcanic activity. Additionally, the heat from the outer core can cause the lower mantle to partially melt, forming a region of partially molten material known as the asthenosphere. The asthenosphere is also involved in plate tectonic movement, and is thought to play a role in the formation of magma chambers beneath volcanoes.
Hi! When the lower mantle gets hot from contact with the outer core, the process of mantle convection is initiated. Mantle convection is the slow circulation of solid rock within the mantle, driven by temperature differences. As the lower mantle material heats up due to its proximity to the outer core, it becomes less dense and starts to rise towards the upper mantle. This process is known as upwelling.

As the hot, less dense material ascends, it transfers heat from the lower mantle to the upper mantle. When the rising material reaches the cooler upper mantle, it loses heat and becomes denser. This causes the material to sink back down towards the lower mantle in a process called downwelling. This continuous circulation of material within the mantle helps distribute heat throughout the Earth's interior, contributing to plate tectonics and the movement of Earth's lithosphere.

In summary, when the lower mantle gets hot from contact with the outer core, mantle convection is initiated, leading to upwelling and downwelling of mantle material and the redistribution of heat within the Earth's interior.

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The areas where air converges at Earth's surface are regions of low pressure. The ITCZ (Intertropical Convergence Zone) and the Polar Front are two such regions. The answer is (e) both answer choices (a) and (c).

The ITCZ is a low-pressure zone where the northeast and southeast trade winds converge near the equator, resulting in rising air and the formation of clouds and precipitation. The Polar Front is a zone of low pressure where the cold polar air meets the warm subtropical air, causing the air to rise and leading to the formation of storms. The subtropical high, on the other hand, is an area of high pressure, where air diverges and sinks, resulting in fair weather. Therefore, the answer is (e) both answer choices (a) and (c).

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Explanation:

Scale: Generally, the relationship between the portion of Earth being studied and Earth as a whole, specifically the relationship between the size of an object on a map and the size of the actual feature on Earth's surface.

The continents of Eurasia and North America are currently moving apart at an average rate of approximately 2 inches per year. The movement of continents is due to tectonic plate movement.

The North American plate and the Eurasian plate are moving away from each other, resulting in the separation of the two continents. The rate of this movement is measured in inches or centimetres per year, and currently, the average rate of movement between Eurasia and North America is around 2 inches per year. This slow movement might not be noticeable to humans, but it has a significant impact on the Earth's geology and topography.

The movement of continents is due to the process called plate tectonics, where the Earth's lithosphere is divided into several plates that move over the more fluid asthenosphere. The rate at which the continents move apart can vary, but on average, it is estimated to be around 2 inches per year for Eurasia and North America. This is a relatively slow pace, but it has a significant impact on the Earth's surface over long periods of time.

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Wind or water deposits sediments when they lose energy or velocity. The sediments carried by wind or water are typically sand, silt, and clay particles.

In the case of water, when the velocity of the water flow slows down, it loses its ability to carry the sediment and eventually deposits it on the ground or riverbed. This process is known as sedimentation. Similarly, wind can carry sediments and deposit them when its velocity slows down or is obstructed by obstacles such as rocks or plants. Windblown sedimentation can form dunes or ridges, while water sedimentation can form deltas or floodplains. The deposition of sediments is essential for the formation of various landforms and habitats, including beaches, riverbanks, and wetlands.

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A fold in which rock layers warp up in the shape of an A is called an "anticline".

Anticlines are commonly formed by compressional forces acting on the Earth's crust, causing the layers of rock to buckle and fold. In an anticline, the oldest layers of rock are found at the center, while the younger layers are found towards the edges of the fold. Anticlines can be found in many different types of rock, and are often associated with natural resources such as oil and gas, as these fluids can collect in the crests of the fold.

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Answer:

Explanation:

Seattle, Washington.

The city in the United States that is near an active volcano and would suffer in the event of an eruption is Seattle, Washington.

A major and destructive eruption is a possibility from the active volcano Mount Rainier. Despite the fact that the volcano hasn't erupted recently, its size, position, and history of violent eruptions make it one of the world's most dangerous volcanoes.

A catastrophic eruption of Mount Rainier could result in lahars (volcanic mudflows), which would pose a serious risk to Seattle's population and infrastructure.

A region noted for its volcanic activity, including numerous active and potentially hazardous volcanoes like Mount St. Helens and Mount Baker, is where Seattle is situated.

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The given statement " the evaporator in a refrigeration system must be colder than the refrigerated space in order to absorb heat" is true as evaporator helps in temperature management in refrigerator.

In a refrigeration system the evaporator is where refrigerant evaporates and heat from the refrigerated space is absorbed. In order to absorb heat, the evaporator needs to be colder than the refrigerated space so that heat can move from the latter to the former.

The absorbed heat is then transferred by the refrigerant to the condenser where it is expelled into the outside air. For this reason, the condenser is typically placed outside or in a different location from the evaporator, which is typically housed inside the refrigerator.

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The director of Tidal Wave (2009) chose Busan as the city and Haeundae and Gwangalli Beach as the focus for several reasons. First and foremost, Busan is a coastal city located on the southeastern coast of South Korea. As such, it is an ideal location for a disaster film that centers around a tidal wave or a tsunami.

Furthermore, Haeundae and Gwangalli Beach are two of the most popular and famous beaches in Busan. Haeundae Beach is the largest and most well-known beach in the city, with soft, golden sands, clear waters, and a wide range of beach activities. Gwangalli Beach, on the other hand, is a more laid-back and relaxed beach that is known for its beautiful views of the Gwangan Bridge and the city skyline.By focusing on these two beaches, the director was able to create a more immersive and realistic disaster film that viewers could relate to. For many people, the beach is a place of relaxation and fun, but in Tidal Wave, it becomes a place of danger and chaos.Additionally, the director may have chosen Busan and its beaches because of their cultural significance. Busan is a city that is deeply connected to the sea and the fishing industry, and its beaches are a reflection of this. By showcasing these beaches in the film, the director was able to pay homage to the city's history and traditions.

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Tectonic plates can be made of both continental crust and oceanic crust. The main differences between these two types of crust lie in their composition, density, and thickness.

Continental crust is primarily composed of granitic rocks, which are less dense and lighter than the basaltic rocks found in oceanic crust. Due to this difference in density, continental crust has an average density of about 2.7 grams per cubic centimeter, while oceanic crust has a higher average density of around 3.0 grams per cubic centimeter. In terms of thickness, continental crust is generally thicker than oceanic crust, with an average thickness of 35-40 kilometers, whereas oceanic crust averages at around 7-10 kilometers in thickness. This variation in thickness leads to a difference in the elevation of the Earth's surface, with continental crust forming the higher-standing landmasses and oceanic crust creating the lower-lying ocean basins. Additionally, the age of the crust varies between the two types, as oceanic crust is continuously being formed at mid-ocean ridges and destroyed at subduction zones, resulting in a relatively young age compared to the more stable, older continental crust.

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Rock texture refers to the physical appearance and structure of a rock. It includes characteristics such as grain size, shape, arrangement, and orientation of minerals within the rock. The texture can provide clues to the rock's origin and history.

In activity 4.4, the different rock textures are represented by the various specimens in Fig AA1. For each specimen, we can observe the texture and make an interpretation about whether it is an igneous, sedimentary, or metamorphic rock.

Layered (bedding) texture is typically associated with sedimentary rocks. Sedimentary rocks are formed from layers of sediment that have been deposited and compacted over time. Examples of sedimentary rocks include sandstone and shale.

Layered (foliated) texture is associated with metamorphic rocks. Foliated rocks have been subjected to intense pressure and heat, which has caused the minerals within the rock to reorient and align themselves in a layered pattern. Examples of foliated rocks include slate and gneiss.

Glassy texture is typically associated with igneous rocks. Igneous rocks are formed from the solidification of magma or lava. Glassy texture occurs when the magma or lava cools quickly, preventing mineral crystals from forming. Examples of igneous rocks with glassy texture include obsidian and pumice.

Fine-grained intergrown crystals (crystalline) texture is also associated with igneous rocks. This texture occurs when the magma or lava cools slowly, allowing mineral crystals to grow and interlock with one another. Examples of igneous rocks with crystalline texture include granite and basalt.

Bioclastic texture is typically associated with sedimentary rocks that contain fossils or organic matter. Examples of bioclastic rocks include limestone and coal.

In making these interpretations, we are considering the specific characteristics of each rock texture and how they relate to the formation and history of the rock.
Hi there! Rock texture refers to the size, shape, and arrangement of grains or crystals within a rock. It plays a significant role in classifying rocks into three main categories: igneous, sedimentary, and metamorphic.

1. Igneous rocks are formed from cooling and solidification of magma or lava. They may exhibit textures such as glassy, fine-grained, or intergrown crystals (crystalline).

2. Sedimentary rocks are formed from the accumulation and cementation of mineral and organic particles. They often display layered (bedding) or bioclastic textures.

3. Metamorphic rocks are formed from pre-existing rocks that have undergone changes in their mineral composition and structure due to heat, pressure, or chemical processes. These rocks may have a layered (foliated) texture.

When identifying the type of rock in Fig AA1, look for the specific textures mentioned above and determine whether it is igneous, sedimentary, or metamorphic. Your interpretation will be based on the observed texture and the knowledge of how each rock type forms.

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Ecological succession takes place in an area where a community of organisms undergoes a series of changes over time, eventually leading to the establishment of a stable, mature community.

Ecological succession takes place in an area where there has been a disturbance or change in the environment. This disturbance can be caused by natural events such as fires, floods, landslides, or human activities such as deforestation or construction. As a result of the disturbance, the previous community of organisms may be wiped out or significantly altered, leaving the area open for new species to colonize and establish.

The process of ecological succession can take a long time, often spanning decades or centuries, as the new community gradually replaces the previous one through a series of stages. But it is important to understand the context and factors that contribute to ecological succession. This process occurs in response to disturbances or alterations in the environment, allowing new species to colonize the area and replace the previous community.

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The form of transportation that first opened corridors of development in the United States, provided access to markets for commercial crops, and helped establish towns and cities across the country is the railroad.

Early in the 19th century, the first railroads were constructed in the United States, and they quickly established themselves as a vital means of moving both people and products.

Railroads replaced earlier modes of transportation like horse-drawn carriages or riverboats as a faster, safer, and more dependable way to move people and commodities across great distances.

By facilitating simpler transportation of people and products, the railway system assisted in the establishment of towns and cities across the nation, resulting in increased trade and economic growth.

Railroads made it possible to transport goods from rural areas to urban centres, giving farmers and manufacturers access to new markets.

Additionally, they made it easier for people to move around, which spread population across the nation and helped create new towns and industries.

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The only type of heat transfer possible to transfer energy from the sun to the earth is radiation. Radiation is a form of energy transfer that occurs through space without the need for a medium. This means that the energy from the sun can travel through the vacuum of space and reach the earth without any obstruction.

The sun emits energy in the form of electromagnetic radiation, which includes visible light, ultraviolet light, and infrared radiation. When this radiation reaches the earth, it is absorbed by the atmosphere, land, and oceans, and is ultimately converted into heat energy, which drives the various processes on our planet. Overall, radiation is the primary mechanism through which the sun's energy is transferred to the earth.
The energy transfer from the Sun to the Earth occurs through a process called radiation. Since there is no medium or material connecting the Sun and the Earth, radiation is the only possible method of heat transfer in this scenario. In radiation, energy is transferred as electromagnetic waves, which can travel through a vacuum like the space between the Sun and the Earth.

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The statement that is FALSE about tropical and extratropical cyclones is D. Tropical cyclones cause storm surges, but extratropical cyclones can also cause storm surges.

Tropical cyclones and extratropical cyclones have different characteristics and form under different conditions. Tropical cyclones form over warm ocean waters near the equator, while extratropical cyclones form over land or water in the middle or high latitudes. Tropical cyclones have warm central cores, while extratropical cyclones have cool cores. Both types of cyclones can cause significant amounts of rainfall and high winds, but only tropical cyclones can cause storm surges due to their low-pressure centers and wind patterns. Storm surges can result in significant coastal flooding and damage, which is a major hazard associated with tropical cyclones.

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The statement the upstream end of a stream (headwaters section) usually has the steepest gradient for the stream" is option A) true.

Headwaters are the beginning of a stream, originating from a high elevation, such as a mountain or a spring. At this point, the gradient is steeper due to the stream flowing from a higher to a lower elevation. As the stream flows downstream, the gradient gradually decreases, which leads to a slower flow and the deposition of sediments. This difference in gradient can affect the stream's velocity, erosive power, and sediment transport capabilities. In summary, the upstream end of a stream, or the headwaters section, typically has the steepest gradient compared to the rest of the stream.

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The most likely explanation for the surge in speciation as the supercontinent Pangaea fragmented into smaller land masses is populations being separated from one another and diverging.

Physical obstacles like oceans and mountain ranges restricted gene flow between people as the land masses divided, resulting in isolation. These isolated populations were subjected to various selection pressures as they evolved and adapted to their particular habitats throughout time, which led to the development of distinctive genetic features and, ultimately, the emergence of new species. The development of life on Earth is assumed to have been significantly influenced by this process, known as allopatric speciation, as land masses have moved and drifted over time.

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Full Question;

As the supercontinent Pangaea broke up into smaller land masses, speciation increased: Why might that have occurred? Select one: Species interactions grew more complex: The climate grew warmer everywhere_ There was more gene flow between continents Populations became isolated from one another and diverged:

Answer:

they are classified according to temperature, sorry if this is wrong! this is just based on what I know

Explanation:

Due to the heat energy they emit, planets, nebulae, and stars all produce a continuous spectrum. Cooler gases surround the bodies, which is demonstrated by the dark lines in the spectra that result from some of the energy being absorbed.

A graph describing the amount of light something emits (how bright the object is) at various wavelengths is called a spectrum. We generally do not know the distances to the stars from their spectra, therefore the spectrum of a star tells how bright it appears to be from Earth.

We can determine the "greenness" of our planet and where and how much plant life there is by comparing the near-infrared and red portions of the spectrum. NASA's Landsat satellites and the Moderate Resolution Imaging Spectrometer (MODIS) sensor are frequently used for this method.

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The development of the peppered moths into a separate species may occur through a process called allopatric speciation. This happens when a population of the moths becomes geographically isolated from the main population, resulting in a reproductive barrier.

Over time, genetic mutations and natural selection may lead to differences in the isolated population's gene pool, resulting in the formation of a new species. Additionally, the peppered moths may also undergo sympatric speciation, where genetic differences occur within the same geographic area due to factors such as niche differentiation or mate preference. These mechanisms could eventually result in the development of a distinct and reproductively isolated species of peppered moth.

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Answer:

The Dmanisi hominins, found in Dmanisi, Georgia, exhibit several surprising features that distinguish them from other Homo erectus finds. Some of these distinguishing characteristics include:

1. Morphological variation: The Dmanisi hominins show significant morphological variation within the same population. This variation suggests that early Homo populations had a broader range of physical characteristics than previously thought. Some of the Dmanisi individuals exhibit features similar to Homo habilis, while others more closely resemble typical Homo erectus.

2. Smaller brain size: The brain size of the Dmanisi hominins is notably smaller than that of other Homo erectus specimens found in Africa and Asia. The average cranial capacity of the Dmanisi individuals is around 600-775 cubic centimeters, which is closer to the brain size of Homo habilis than to the larger-brained Homo erectus specimens.

3. Primitive skeletal features: The Dmanisi fossils display a mix of primitive and derived traits. Some features, such as the relatively small brain size and the shape of the skull, are more primitive, whereas other aspects of their anatomy, like the limb proportions, are more similar to later Homo erectus individuals.

4. Early migration: The Dmanisi fossils date back to approximately 1.8 million years ago, making them the earliest known evidence of hominins outside Africa. This early migration challenges the previously held belief that Homo erectus left Africa only after developing more advanced features like a larger brain and more sophisticated tools.

These distinguishing characteristics of the Dmanisi hominins provide valuable insights into the early stages of human evolution and migration and contribute to a deeper understanding of the complexity and diversity within the Homo genus.

Answer:

The Pacific Crest Trail (PCT) is approximately 2,650 miles (4,265 kilometers) long, stretching from the U.S.-Mexico border in California to the U.S.-Canada border in Washington. The time it takes to hike the entire trail varies depending on factors such as hiking speed, daily mileage, and weather conditions.

On average, it takes most thru-hikers about 4 to 6 months to complete the entire Pacific Crest Trail. Some experienced and well-prepared hikers may finish the trail in a shorter time, while others may take longer, especially if they choose to take more rest days or explore nearby attractions along the way.

Long-distance canals carrying water from the colorado river reach as far as (in southern california) and (in southern arizona) is Colorado Aqueduct.

Water from the Colorado River is delivered to Southern California via the Colorado Aqueduct, which was constructed in the 1930s. It is the main source of drinking water for the area and is controlled by the Metropolitan Water District of Southern California (MWD).

Water from the Sacramento-San Joaquin Delta is transported to the San Joaquin Valley and Southern California via the California Aqueduct, an essential component of the State Water Project. The Edmund G. Davis Aqueduct, a $1.75 billion bond that was approved by voters in 1960, was included in the construction of the 444-mile California Aqueduct.

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The complete question is:

Long-distance canals carrying water from the colorado river reach as far as (in southern california) and (in southern arizona) is ____.

The northwestern coast of the United States is near a subduction zone.

Subduction between the Pacific and Juan de Fuca plates and the northwestern American Plate is now taking place in the Cascadia Subduction Zone and Southern Alaska. Parks in the Cascadia Subduction Zone impressively show off the two separate mountain ranges: the volcanic Cascade Range farther inland, where the top of the plate is deeper, and the Coast Range close to where the Juan de Fuca Plate starts to subduct.

The roots of an old volcanic range that developed when the subduction zone reached far further south may be seen at some locations in the Sierra Nevada Mountains. In addition, huge parks in the Southern Alaska Subduction Zone include stunning mountains, layers of rock, and active volcanoes that illustrate the continuous plate convergence along the northwestern Coast.

Therefore, option D is the correct answer.

The complete question is, "The northwestern coast of the united states is:

A. located along a divergent plate boundary.

B. associated with a hot spot.

C. where two tectonic plates move parallel to one another.

D. near a subduction zone.

E. in the middle of a continental plate.

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