Global climate change and global warming
I. are both examples of global change
II. are only caused by humans
III. refer only to changes in an area's temperature

a) I
b) III
c) I and II
d) II and III

Answer:

You would expect to find a deep ocean trench at the following types of plate boundaries:

Ocean-ocean convergent boundary

Ocean-continental convergent boundary

Engineers typically define soil as any loose material on the surface of the Earth, which includes unconsolidated rocks, sediments, and organic matter. Earth scientists, on the other hand, prefer a more specific definition of soil that emphasizes its formation through weathering, its composition, and its ability to support plant life.

In contrast, earth scientists have a more specific definition of soil that takes into account its formation and characteristics. They define soil as the upper layer of the earth's surface that is composed of mineral particles, organic matter, and other living organisms. This layer has developed over thousands of years through the weathering of underlying rock and the accumulation of organic matter and nutrients.Earth scientists also consider the properties of soil, such as its texture, structure, and composition, when studying its function and role in the environment. They may analyze soil samples to determine its chemical and physical properties, and use this information to understand its impact on plant growth, erosion, and water retention.

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Answer:

The pollution in streams will flow downstream which will eventually lead its way into the oceans.

Explanation:

If there is pollution in the ocean, this will be harmful to the animals living in the ocean.

Convergent boundaries occur when two tectonic plates move towards each other. Subduction zones are a type of convergent boundary where one plate is forced beneath another plate into the mantle.

This usually happens when an oceanic plate collides with a continental plate, as the denser oceanic plate is forced down into the mantle. Continental collision is also a type of convergent boundary, but instead of one plate subducting beneath the other, both plates collide and buckle, causing the formation of mountains. If an oceanic plate is colliding with a continental plate, it is likely a subduction zone. If two continental plates are colliding, it is likely a continental collision. Another way to distinguish is by looking at the geological features in the area. Subduction zones often result in volcanic activity and the formation of trenches, while continental collision results in the formation of mountain ranges.
Distinguish between convergent boundaries involving subduction zones and continental collisions, you can consider the following points:
1. Types of plates involved:
- Subduction zones: These occur when an oceanic plate converges with either another oceanic plate or a continental plate. The denser oceanic plate subducts, or slides beneath, the less dense plate.
- Continental collisions: These occur when two continental plates converge, as both plates are of similar density and neither can subduct. Instead, they collide and form mountain ranges.
2. Geological features:
- Subduction zones: These boundaries are characterized by deep oceanic trenches, volcanic island arcs (in oceanic-oceanic subduction), or volcanic mountain ranges along the edge of the continent (in oceanic-continental subduction).
- Continental collisions: These boundaries result in the formation of large mountain ranges, such as the Himalayas or the Alps, due to the compression and uplift of the Earth's crust.
3. Seismic and volcanic activity:
- Subduction zones: These areas are prone to frequent earthquakes and volcanic activity due to the friction and pressure caused by the subducting plate. The melting of the subducting plate generates magma, leading to volcanic eruptions.
- Continental collisions: These areas experience frequent earthquakes due to the immense pressure and stress from the colliding plates. However, volcanic activity is generally absent in continental collision zones, as there is no subduction of a plate to generate magma.
By considering these factors, you can distinguish between convergent boundaries involving subduction zones and those involving continental collisions.

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Answer:

The four major reasons why Pakistan has been unable to realise its potential and succeed like other countries having similar resources include:

1. Corruption among the ruling classes leading to underdevelopment of the country.

2. Nepotism among the civil servants. This is where families and friends are given government contracts.

3. Population also has an effect on the development of the country. Lack of family planning and inadequate planning leads to exponential population which affect the limited resources.

4. Lastly, economic and unemployment factors also affect the potential of Pakistan. A situation where, the population of unemployed is far above the resources and jobs available leads to underdevelopment in Pakistan.

Explanation:

Explanation: (2,-8) because thats how i got the answer

Answer:

Causes depletion of resources, possible species extinction, and pollution.

Explanation:

DRILLL BABY DRILL!!! and I mean that I am not sarcastic.

Based on the geological analysis, the Contour line map is created by drawing on a map with equal elevation points, such that the elevation would be steady if the individual followed the contour line physically.

A contour line is a term that is used geographically, to describe the typical line drawn on a topographic map to reveal ground elevation or depression.

Generally, a contour interval is a vertical distance or difference in elevation between contour lines.

A contour line is used to show the elevation and terrain shape, and it is valuable because they show the form of the land surface on the map.

Hence, in this case, it is concluded that the contour line map is created using lines drawn on a map with equal elevation points.

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The earth has many energy sources present on its surface and beneath the surface but they are not unlimited. They are of non renewable nature and have to be used accordingly without wasting.

Therefore the example that best describes a benefit of one type of nonrenewable energy is "Natural gas does not produce greenhouse gases as other energy sources do" and OPTION B is correct.

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Answer:

C: Coal is relatively inexpensive compared to other forms of energy.

Explanation:

First let's use process of elimination

Look at the question again "Which of the following best describes a benefit of one type of nonrenewable energy?"

I underlined the important words in the question

Now we know we are looking for a benefit for nonrenewable energy

Let's look at the first answer choice

Petroleum can be found nearly anywhere and is easily extracted.

Well, this seems like an okay answer, but it really doesn't say anything about creating energy it is just a benieft

Now let's look at the second answer choice "Natural gas does not produce greenhouse gases as other energy sources do."

natural gasses do create so much greenhouse gasses. For example, natural gas like fossil fuel emissions and the burning of coal create so much pollution so this is false it definitely gives off greenhouse gases

Now let's look at the third answer choice "Coal is relatively inexpensive compared to other forms of energy."

This gives a benieft but it also talks about energy therefore this seems like the best answer so far

Now let's look at the final answer "Nuclear power increases water vapor in the atmosphere."

This does not give a benieft it gives it the opposite; water vapor is one of the main things that helps created pollution therefore this could not be the answer

Now it is down to A or C

C is more detailed and talks about a benieft and talks about energy so imma say it that one

Hope I helped have a great day :)

Answer:

b

Explanation:

Answer:it tells that there are many breaks in the earths plates under the earths rhino s layer over the mantle the crust

Explanation:because I know from my previous science class

Answer:

The strong ocean currents are undermining both areas causing earthquakes. ... Both areas are on the boundary of active plates, the motion of the plates causes earthquakes.

Explanation:

The field of telescopes has been advancing rapidly in recent years, with numerous new developments and technologies changing the way we view and understand the universe.

One of the most significant new developments in telescopes is the increasing use of adaptive optics, which allow for the correction of distortions caused by Earth's atmosphere. This technology is being used to build increasingly larger ground-based telescopes, which can produce images comparable to those captured by space-based telescopes.

Another major development is the increasing use of interferometry, which involves combining data from multiple telescopes to produce high-resolution images. This technique is allowing researchers to study objects in unprecedented detail, including black holes and other phenomena that were previously difficult to observe.

In addition, new telescopes are being designed and constructed with advanced optics and detectors, allowing them to capture data across multiple wavelengths, including infrared and X-ray. These telescopes are revolutionizing our understanding of the universe, revealing new insights into the nature of dark matter, the origins of galaxies, and the evolution of the universe itself.

Overall, the new developments in telescopes are allowing us to explore and understand the universe in ways that were previously unimaginable, paving the way for groundbreaking discoveries and advancements in our knowledge of the cosmos.

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Answer:

Hope it helps

Explanation:

نعم - yes

لا. -. no

Answer:

Severe drought and associated food insecurity, flooding, rains, and temperature rises due to El Niño are causing a wide range of health problems, including disease outbreaks, malnutrition, heat stress and respiratory diseases.

Explanation:

South America becomes drier than normal.

(APEX Verified)

Answer:

The statement is false.

Explanation:

The largest percentage of total magma production on Earth occurs at convergent plate boundaries, not divergent plate boundaries. At convergent plate boundaries, where two tectonic plates collide or come together, one plate typically subducts beneath the other, forming a subduction zone. The subducting plate sinks into the mantle, where it undergoes melting, generating magma. This magma can then rise to the surface, leading to volcanic activity and the formation of volcanic arcs.

Divergent plate boundaries, on the other hand, are where two tectonic plates move away from each other, creating a gap or rift zone. While magma is indeed produced at divergent plate boundaries, the overall magma production is lower compared to convergent plate boundaries.

Therefore, the largest percentage of total magma production on Earth occurs at convergent plate boundaries, not divergent plate boundaries.

The statement  is true .The largest percentage of total magma production on earth occurs at divergent plate boundaries

.A divergent plate boundary is a boundary where two plates move away from each other, resulting in a gap that magma can fill to form new crusts. Divergent boundaries are where the majority of the Earth's magma is produced, as magma rises to fill the void that was left when the plates moved apart.

At divergent boundaries, magma production is significant because magma is produced as part of the process of creating new oceanic lithosphere. When magma solidifies into rock, it forms new oceanic lithosphere, which spreads away from the spreading center in both directions. Magma production is minimal at other plate boundaries like transform boundaries and convergent boundaries, where magma is produced by the melting of rocks in the subduction zone, and volcanic eruptions occur along the convergent boundary.

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The supporting material that can be used by Yolanda is a hypothesis. This is because the material used by Yolanda is presumptive or temporary.

The etymological hypothesis comes from the Greek, namely Hypo which means weak and Thesis which means theory. So the meaning of the hypothesis is a statement that is still weak in nature because it still needs to be proven. The hypothesis can also be regarded as a temporary guess in a study.

The hypothesis serves as a temporary answer or conclusion to a problem. Directing researchers in finding and collecting data. Clarify a situation that was still vague. Helps predict things that might happen.

The hypothesis has the following characteristics. It needs to be tested for truth, must state a relationship, must be testable, the shape is simple, and based on facts.

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Answer:

Tectonic plate motions generate volcanoes around the boundary of the plate, which erupt and form the mountains. A volcanic arc structure is a sequence of volcanoes forming near a subduction zone where the surface of a sinking oceanic plate melts and drags water down with the subducting crust.:

Answer:

Volcanoes form in the central rift valley of a divergent boundary when two tectonic plates move away from each other. This is because the plates create a gap in the Earth's crust between them, which allows molten rock from the mantle below to rise up and form a volcano. This molten rock is called magma, and when it rises to the surface it is called lava. As the tectonic plates move away from each other, the gap created by them is constantly widened, allowing more magma to escape and form a volcano.

The total annual precipitation at Poamoho of about 5000 mm (200 in.) indicates a very wet climate, which is typically associated with rainforests. Therefore, it is likely that the surrounding indigenous vegetation is a rainforest or a wet forest.

Rainforests are characterized by tall trees, a dense canopy, and a diverse understory. The high precipitation in this region supports the growth of lush vegetation and provides a suitable environment for epiphytes, such as ferns, mosses, and orchids.

On the other hand, near Waianae, where the annual precipitation is about 560 mm (22 in.), you would expect a very different type of vegetation. With such low precipitation, it is more likely that the surrounding indigenous vegetation would be a desert or a dry grassland.

Deserts are characterized by sparse vegetation, with plants adapted to store water or withstand extreme heat and drought. The dry conditions also promote the growth of succulents, such as cacti, and xerophytic shrubs. Therefore, the contrasting levels of precipitation between Poamoho and Waianae would result in very different types of vegetation.

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Answer:

it is a fun sport but what bout it

Explanation:

Answer:

lacroseeeee

Explanation:

hshshshshshssssssssssss erge4e

skrt skrt skieter

Answer:

The correct answer is D.

The shape of Earth is not a reason for the seasons. The other three options - Earth's axial tilt, the revolution of Earth around the Sun and the timing of Earth's perihelion and aphelion - are all contributing factors to the changing of the seasons.

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Rocky material from the Earth's interior can reach the surface, and be pushed and folded upward during the process of mountain building. One of the processes that work to return this material to the Earth's interior is erosion.

The process of mountain building is known as Orogenesis. The Greek word Orogenesis is derived from Oros means mountain and Genesis mean formation. Due to the tectonic movements sometimes the earth's interior materials are pushed to the earth's surface and get folded and rise upward this is known as mountain building. In this way, fold mountains are formed.

When the newly formed folded structure undergoes some sort of changes due to the erosional activities by the agents of nature like air, water, glacier, etc. known as erosion.  

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The Navier-Stokes equation expresses the balance between forces acting on a fluid and its change in velocity over time.

Like in general fluid mechanic, the Naiver-Stoke equation in dynamic meteorology expreases the motion of a fluid in a given time interval. The equation states that the change in velocity (or momentum) of a fluid over a given time interval is equal to the sum of the forces acting on the fluid (such as pressure gradients, viscous forces, and external forces) divided by the mass of the fluid. The equation is given by:

\($$\frac{\partial \mathbf{v}}{\partial t} + \mathbf{v}\cdot\nabla \mathbf{v} = -\frac{1}{\rho}\nabla p + \nu\nabla^2\mathbf{v} + \mathbf{f}$$\)

Where:

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Answer:

Colonists in the new England colonies endured bitterly cold winters and mild summers. land was flat close to the coastline but became hilly and mountainous farther inland. soil was generally rock, making farming difficult.

Answer: i found this on google oof

Colonists in the new England colonies endured bitterly cold winters and mild summers. land was flat close to the coastline but became hilly and mountainous farther inland. soil was generally rock, making farming difficult

Explanation:

A model for Earth's elevation based only on oceanic crust being denser than continental crust results in a phenomenon called isostasy.

Isostasy is a state of balance or equilibrium between the lithosphere (the rigid outermost layer of Earth's crust) and the underlying asthenosphere (a more ductile and less rigid layer in the upper mantle). According to the theory of isostasy, the lithosphere "floats" on the asthenosphere, and the elevation of the lithosphere is determined by the balance between its own weight and the buoyant force of the asthenosphere.

When the oceanic crust is formed at mid-ocean ridges and moves away from the ridge, it cools and becomes denser. As a result, it sinks lower into the mantle than the continental crust, which is generally less dense. The denser oceanic crust, therefore, exerts a greater weight on the asthenosphere than the less dense continental crust. The asthenosphere responds by flowing upward beneath the continental crust, supporting it, and maintaining its elevation.

Therefore, the model for Earth's elevation based on oceanic crust being denser than continental crust results in a dynamic equilibrium in which the elevation of the lithosphere is determined by the balance between the weight of the lithosphere and the buoyant force of the asthenosphere.

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