what features are not recognized on the seafloor near monterey, california? multiple choice a broad continental shelf a continental slope faults that cut across the seafloor all these features are recognized on the seafloor. a canyon partly cut into hard granite

Wet igneous rock melts at a lower temperature than the dry version of that same rock because the addition of volatiles in "wet" rocks lowers their melting temperature.

Igneous rocks are created through the crystallization of magma, a liquid. They come in two varieties: The Earth's surface is where magma cools and crystallizes, forming volcanic or extrusive igneous rocks. Igneous intrusive or plutonic rocks are formed when magma crystallizes deep within the Earth.

Magma is a concoction of gas, crystals, and liquid rock. exhibiting a wide variety of chemical compositions, a high temperature, and liquid-like characteristics.

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False. The rotation of the earth on its axis does not affect the length of day and night.

The length of day and night are solely determined by the earth's orbit around the sun. The rotation of the earth on its axis is what causes the sun to rise in the east and set in the west, and also determines the amount of daylight a certain location receives. This, in turn, affects the types of biomes that exist in certain regions.

As the earth rotates, different parts of the earth receive more or less sunlight, which can cause different climates and environments to form. Therefore, the rotation of the earth on its axis does have an effect on biomes, but it does not directly affect the length of day and night.

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The maximum height of a storm surge is influenced by all the following factors except for coastal population. Storm surge is a rise in sea level caused by a storm's winds pushing water toward the shore. The correct answer is option E.

The maximum height of a storm surge is determined by a number of factors, including storm wind direction and strength, air pressure, astronomical tides, and ocean bottom and shore configuration.

However, the coastal population is not a factor that influences the maximum height of a storm surge. Rather, the coastal population is affected by the height of the surge and the extent of flooding it causes.

Storm surge is a rise in sea level caused by a storm's winds pushing water toward the shore. The height of the surge depends on the strength and duration of the storm's winds, the air pressure of the storm, and the shape of the coastline and ocean bottom.

In addition, the presence of astronomical tides can amplify the height of a storm surge.

In conclusion, the maximum height of a storm surge is not influenced by coastal population but rather is determined by storm wind direction and strength, air pressure, astronomical tides, and ocean bottom and shore configuration. The correct answer is option E.

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Answer:

The US annexed Hawaii in 1900.

Explanation:

Answer:

The US annexed Hawaii in 1900.

Explanation:

e2020 A

Answer:

All rocks except obsidian and coal are made of minerals. (Obsidian is a volcanic rock made of glass and coal is made of organic carbon.) Most rocks contain several minerals in a mixture characteristic of the particular rock type. When identifying a rock you must first identify the individual minerals that make up that rock.

Minerals are naturally occurring, inorganic solids with a definite chemical composition and a crystal lattice structure. Although thousands of minerals in the earth have been identified, just ten minerals make up most of the volume of the earth’s crust—plagioclase, quartz, orthoclase, amphibole, pyroxene, olivine, calcite, biotite, garnet, and clay.

Together, the chemical formula (the types and proportions of the chemical elements) and the crystal lattice (the geometry of how the atoms are arranged and bonded together) determine the physical properties of minerals.

The chemical formula and crystal lattice of a mineral can only be determined in a laboratory, but by examining a mineral and determining several of its physical properties, you can identify the mineral. First, you need to become familiar with the physical properties of minerals and how to recognize them.

Minerals can be identified by their physical characteristics. The physical properties of minerals are related to their chemical composition and bonding. Some characteristics, such as a mineral’s hardness, are more useful for mineral identification. Color is readily observable and certainly obvious, but it is usually less reliable than other physical properties.

Answer:

-8

Explanation:

If there is one negative and one positive you know it has to be a negative value! I remember it like this...

2 * 4 = 8 ; no negatives I know it's positive

(-2)(-4) = 8 ; two negatives crossed together makes a + sign

2(-4) = -8 ; one negative means it must be negative

Not stupid, you shouldn't feel bad to ask

I hope this helped!

The product of the integers 2(-4) will be equal to -8. According to multiplication and division of integers, RULE 1: The product of a positive integer and a negative integer is negative.

Two integers can be multiplied together to produce a positive, negative, or zero value. For two integers to be multiplied together:

hence, The product of the integers 2(-4) will be equal to -8. According to multiplication and division of integers, RULE 1: The product of a positive integer and a negative integer is negative.

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Answer:

No the ocean is not considered the dessert.

Explanation:

Answer:

no

Explanation: a desert is something you get at the cheese cake factory

" The convection model relies on differences in density between the top of the convecting cell and the base of the lithospheric plate, and the push/pull model relies on the ridge pushing and pushing the plate outward as the ridge falls in elevation."

The two major models for a mechanism to drive plate tectonics are the ridge-push, slab-pull and the convection models. In this question, we will explain what the convection model relies on and what the push/pull model relies on.

Convection is the transfer of heat from one part of a fluid to another part of the same fluid or to another fluid entirely, where the driving force for the motion is the negative buoyancy that results from differences in fluid density. The convective process also generates new lithosphere at mid-ocean ridges where two plates are diverging. In contrast, the ridge-push/slab-pull model relies on gravity-driven motions of dense lithospheric slabs that sink into the underlying mantle. The weight of the slab and the force of gravity generate a tensional force on the overlying lithosphere, which is manifested as trenchward migration of the subducting slab and landward movement of the upper plate. Along mid-ocean ridges, elevated heat flow and thermal expansion generate a spreading force on the lithosphere that pushes it apart, while the downward pull of gravity on the cool and dense lithosphere beyond the spreading axis generates a sinking force on the plate. These forces together create a force couple that drives the lithospheric plates apart from the spreading axis in a direction perpendicular to the ridge axis.

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The four images of various river channels exhibit unique characteristics and are shaped by dominant forces or processes specific to each scene.

The four images of different river channels showcase distinct characteristics and provide insights into the dominant forces or processes shaping their formations.

Each scene offers a glimpse into the intricate dynamics at play in river systems.

Examining the unique features of each river channel allows us to understand the forces responsible for their formation.

Factors such as the gradient of the channel, the type of sediment transported, and the presence of obstacles or geological structures all contribute to shaping the river channel.

For instance, meandering river channels with sinuous bends suggest the influence of lateral erosion and deposition processes, while straight and narrow channels may indicate a steeper gradient or the presence of resistant bedrock.

The dominant forces or processes at work in each scene can vary widely.

Examples include the erosive power of flowing water, sediment transport and deposition, bank erosion, meander formation, or the impact of human activities on river morphology.

By studying these images and analyzing their unique characteristics, researchers and geologists gain valuable insights into the intricate interplay between forces and processes that shape river channels.

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The exact figures may vary, but there are approximately 2.8 million African immigrants in the United States, with a majority coming from various regions in sub-Saharan Africa, and there are millions of African immigrants living in European countries, with a higher proportion from sub-Saharan Africa compared to North Africa.

1) According to the Migration Policy Institute, as of 2019, there were approximately 2.8 million African immigrants living in the United States.

2) The majority of African immigrants to the United States come from various regions in Africa. However, significant numbers are reported to originate from countries such as Nigeria, Ethiopia, Ghana, Kenya, and South Africa, among others.

3) The number of African immigrants in European countries can vary across different countries. According to available estimates, there are millions of African immigrants residing in European nations, but specific figures may differ by country.

4) The majority of African immigrants to Europe are from sub-Saharan Africa rather than North Africa. This is due to factors such as political instability, conflict, economic opportunities, and migration patterns. However, the exact breakdown between sub-Saharan Africa and North Africa would require more detailed and specific data from individual European countries.

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James Taylor was an a English cricket player. He was a batsman & bowler & played for the Nottinghamshire County Cricket Club. He debuted in 2008 & later on became the youngest Leicestershire one-day centurion and first-class double centurion. In 2009, Taylor also became the youngest player in Leicestershire's history to score 1,000 championship runs in a season.

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RainbowSalt2222

A mixture of air, hot ash, and pumice lapilli that rushes down the side of a volcano in a scalding avalanche is termed a(n) pyroclastic flow.

Pyroclastic flows are all secretions combined with robust materials and gases. The speed of pyroclastic flows on the number of solids and gases. A characteristic of pyroclastic flows is that they can produce a high degree of destruction when they erupt.A pyroclastic flow is a dense, fast-moving flow of solidified lava pieces, volcanic ash, and hot gases. It occurs as part of certain volcanic eruptions. A pyroclastic flow is extremely hot, burning anything in its path.

Exploding gas bubbles shatter the pumice into tiny fragments which we call volcanic ash. Ash clouds are driven high into the atmosphere by the force of these eruptions; the finest particles may spread for hundreds of miles before falling back to Earth.

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The correct order of the processes that occur when oceanic plates spread apart at the mid-ocean ridge, from the first event at the top to the last event at the bottom, is as follows: Cracks appear in the oceanic plates .Lava rises and hardens. The mid-ocean ridge rises up from the ocean floor.

Tectonic plates diverge and move away from each other, leaving a gap in between .The oldest rocks move away from the mid-ocean ridge, while new rocks are formed near the mid-ocean ridge. This occurs at the boundary between the plates on both sides of the mid-ocean ridge.

The mid-ocean ridge is the largest mountain range in the world. It is a chain of submarine mountains that runs across the middle of the ocean, with a crack running down the center. New oceanic crust is formed at the mid-ocean ridge, and old crust is destroyed at subduction zones.

The process by which new oceanic crust is created is called seafloor spreading. As the oceanic plates move apart, magma rises from the mantle and hardens into solid rock, forming new crust on both sides of the ridge.

Cracks appear in the oceanic plates at the mid-ocean ridge, and lava rises from below to fill them.

This lava hardens into solid rock, forming a new layer of oceanic crust. Over time, the oceanic crust moves away from the mid-ocean ridge, and new crust is formed in its place. Over time, the oceanic crust moves away from the mid-ocean ridge, and new crust is formed in its place.

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Maine- Vermont, New Hampshire, Massachusetts, Connecticut, and Rhode Island make up the states that make up the northeastern part of the country known as New England. It is well-known for its Colonial past, Atlantic coastline, changing autumn foliage, and mountainous terrain covered in forests. The core of the region, Boston, Massachusetts, existed before the American Revolution, and the Freedom Trail it leads through traverses key locations in the establishment of the country.

Clam soup, Maine lobsters, Vermont maple syrup, turkey, Boston baked beans, and Boston cream pie are among well-known delicacies from New England. The greatest metropolis in the area, Boston, Massachusetts, existed before the American Revolution, and the Freedom Trail travels through several key locations for the establishment of the country.

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The region in Uranus that current computer models suggest is composed primarily of liquid water is the lowest pressure regions.

According to current computer models, the lowest pressure regions in Uranus are hypothesized to be composed primarily of liquid water. These regions are deep within the planet's atmosphere, where the pressure is higher, and temperatures are more conducive to the formation of liquid water. However, it's important to note that our understanding of Uranus is limited, and these models are based on simulations and theoretical predictions rather than direct observations.

Further exploration and scientific research are necessary to confirm the presence of liquid water in Uranus's atmosphere. Therefore, the answer is that the lowest pressure regions in Uranus are likely composed primarily of liquid water.

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Caves or caverns. In a region where limestone is located close to the surface, numerous collapses can result in sinkholes, which leave a pitted or cratered appearance at the surface referred to as a landscape.

An area of the Earth's surface that can be seen at once from a single location is referred to as a landscape. It consists of the physical characteristics that identify or characterize a specific location. The word "landscape" is a term used to describe paintings of the countryside in Dutch.

Agrarian, salt marsh, wooded, wooded with lagoons for fishing, and river landscape types were the first five to be classified.

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At any point along the surface of an oblique (nonvertical) fault, the hanging wall lies Above the footwall.

In the context of a fault, the hanging wall refers to the block of rock that is positioned above the fault plane, while the footwall refers to the block of rock that is below the fault plane. An oblique fault is a type of fault where the movement occurs along an inclined or diagonal plane rather than vertically. Regardless of the orientation or angle of the fault, the hanging wall always lies above the footwall. This relationship holds true for all points along the surface of an oblique fault, ensuring consistency in the terminology used to describe fault structures.

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Answer:

These resources are considered non-renewables because once they are used up they cannot be replaced. These resources take millions of years to form and cannot be artificially reproduced.

Answer:

The Aztec religion incorporated deities from multiple cultures into its pantheon. Ritual sacrifice played an essential role in the religious practice of the Aztecs, and they believed it ensured the sun would rise again and crops would grow. Everyone was affected by human sacrifice, and it should be considered in the context of the religious cosmology of the Aztec people. Every level of Aztec society was affected by the belief in the human responsibility to pay homage to the gods, and anyone could serve as a sacrificial offering.

Explanation:

Answer:

false?

Explanation:

mostly divided into 60 minutes...

The uneven heating of the Earth's surface creates a temperature difference between land and water, resulting in the formation of convection currents. These currents produce sea breezes as cooler air from the sea moves towards the warmer land during the day.

Convection currents produced by uneven heating of the Earth's surface contribute to the formation of sea breezes in two ways.

1. Differential Heating: During the day, land and water surfaces absorb solar radiation at different rates. Land tends to heat up more quickly than water, which has a higher specific heat capacity. As a result, the air above the land gets heated and rises, creating a region of low pressure. In contrast, the air above the cooler water remains relatively denser, creating a region of high pressure.

2. Air Movement: The pressure difference between the land and water leads to the movement of air from areas of high pressure (over the water) to areas of low pressure (over the land). This movement of air is known as a convection current. As the cooler air moves from the sea towards the land, it is referred to as a sea breeze.

- During the day, when the land heats up, the warm air rises and creates a low-pressure area over the land. The cooler air from the sea rushes in to replace it, resulting in the sea breeze.

- At night, the land cools down faster than the water. The air above the land becomes cooler and denser, leading to a region of high pressure. The warmer air over the water moves towards the land, causing a land breeze.

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As lithospheric plates move away from midocean ridges they cool and become denser. They eventually become more dense than the underlying hot mantle. After subducted, cool, dense lithosphere sinks into the mantle under its own weight. This helps to pull the rest of the plate down with it. This is how slab pull occur

Answer:

Eurasia and North America

Explanation:

Answer: They get their water from groundwater