What causes an earthquake?
A)buildup of magma
B)hard collisions between tectonic plates
C)extreme rock deformation
D)buildup of pressure between tectonic plates

Answer:

The drift of crustal plates due to convection in the asthenosphere.

Answer: D. They strengthened the monarchy.

Explanation:

Hugh Capet established the Capetian dynasty that ruled France for over 300 years. After being elected as King, Capet made Paris his capital and began bringing the rest of France under his control.

In doing so he managed to begin the process of strengthening the monarchy that was continued by his descendants until the end of the dynasty thereby laying the foundation for France as it is today.

Answer:

Sea Floor Spreading

Explanation:

Answer:

its Faults

Explanation:

Answer: b. Different plant types can add or remove nutrients within a soil, thereby changing the type of soil that is formed.

Explanation:

Some plants require more a of particular nutrient than others and so will draw more of these nutrients from the soil whilst giving away some of the ones that they do not want. This is one of the reasons that some plants grow better in a particular area than not.

When these plants give or take away nutrients, they would be changing the type of nutrient composition of the soil and this is what makes crop rotation so effective.

Answer:

A region that is reflective of human feelings and attitudes. Example: Who we are and where we live affects our perception. For instance, we may not all agree on which states belong to the regions that we call the South or the Midwest

Explanation:

comment if u need better explanation ( got this from class notes )

Answer:

C

Explanation:

Some precautions that local residents can take to reduce the impact of Freddy cyclone are:

In the event of an evacuation advisory or mandate from the authorities, it is essential to comply with their directives and promptly relocate to a secure area. Keep up-to-date with the developments of the storm from reliable sources.

To ensure your home's safety, it is recommended to secure all entrances and exits such as windows and doors, and to also avoid leaving any items outside that could potentially become dangerous projectiles during bouts of intense winds.

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Destructive interference happens between the waves when the crest of one wave lines up with the trough of another wave.  

The "positive" and "negative" peaks and troughs of waves can be referred to as the "positive" and "negative," respectively. Therefore, if these two wave components interact with one another, they cancel one another out. When two peaks or two troughs interact, the result is referred to as destructive interference, while the opposite is true when they don't. Energy that travels through water to cause it to move in a circular motion creates waves. As a wave passes, water molecules only move in a very narrow circle. The waves receive energy from the wind. Ocean waves are generated by the wind and released as energy along coasts.

The crest of one wave lines up with the trough of another wave. What happens between the waves?

A. A breaking wave

B. Destructive interference

C. Constructive interference

D. Wave reflection

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Answer: The Himalayan mountain range and Tibetan plateau have formed as a result of the collision between the Indian Plate and Eurasian Plate which began 50 million years ago and continues today.

Explanation:

Answer: Chilliwack, BC is the fastest growing city in Canada because it offers a high quality of life, affordable housing, and attractive amenities.

Explanation: According to the 2021 census data from Statistics Canada, Chilliwack, BC is the second fastest growing census metropolitan area (CMA) in Canada, after Kelowna, BC. It recorded an increase of 12.1 per cent from 2016 to 2021, raising its population to 113,767. Chilliwack is among the four CMAs in B.C. that saw growth of 10% or more in the same period.

Some of the reasons why Chilliwack is attracting more people are:

These factors make Chilliwack a desirable place to live, work, and play for many people who are looking for a change of pace or a more affordable option than other cities.

Hope this helps, and have a great day! =)

A true statement is longshore currents transport sand.

Ocean currents usually occur on the surface and below sea level. For fishermen, ocean currents have an important role because they can determine the direction of shipping.

The definition of ocean currents is the movement of water that causes the horizontal movement of water masses.

Not only horizontally, ocean currents can also cause vertical displacement of water masses. However, this event was minimal. Vertical movement of water masses is also known as upwelling.

Wind is the main factor affecting the movement of ocean surface currents. The faster the wind blows, the greater the friction force that occurs on the sea surface.

Seawater that has a high salt content has a greater density, and vice versa.

Based on the temperature, ocean currents are divided into two types, namely hot currents and cold currents. These two currents occur when there is a difference in seawater temperature with the surrounding area.

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The main characteristics that are used to distinguish the two types of mountain belts are their formation processes and their geologic age.

The first type of mountain belt is referred to as the active or young mountain belt, which is characterized by ongoing tectonic activity and relatively young rocks. These mountain belts are formed by the collision of tectonic plates, resulting in the uplift and deformation of the Earth's crust. The second type of mountain belt is the passive or old mountain belt, which is characterized by the absence of tectonic activity and older rocks. These mountain belts are the remnants of once-active mountain ranges that have been eroded and flattened over millions of years.

In summary, the main answer is that the two types of mountain belts are distinguished by their formation processes and geologic age. Further depth regarding the specific tectonic processes and geologic history that distinguish these two types of mountain belts.

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Answer:

No

Explanation:

it makes the lines longer, but it doesn't change the degrees (size) of the angle

These characteristics are mainly associated with three types of volcanoes such as cinder cone volcano, shield volcano and stratovolcano.

Sorting of characteristics-

Cinder cone volcano - flank eruptions; strombolian eruption

Shield volcano - pillow basalt; fire fountain

Stratovolcano - pyroclastic flow; lahars; felsic lava

A volcano is a crack in a planet's crust, such as the one on Earth, that permits hot lava, volcanism, and gases to emerge from a molten material underneath the surface. Most volcanoes on Earth are located undersea, and they're most predominantly encountered where continental plates are diverging or convergent.

An amazing demonstration of Earth's might is a volcanic eruption. Volcanic eruptions can cause serious destruction of life and property, particularly in areas of the world that are heavily populated, even though that they are spectacular to witness.

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Answer:

False

Explanation:

The probability that both quartz and tourmaline will be found, but not aquamarine is P(A intersection B) = P(A)*P(B) = 0.80 * 0.36 = 0.29.

The Venn diagram for this situation is as follows:

A: Quartz specimens are found  _____

B: Tourmaline specimens are found  ____

C: Aquamarine specimens are found ____

The probability that both quartz and tourmaline will be found, but not aquamarine is P(A intersection B) = P(A)*P(B) = 0.80 * 0.36 = 0.29.

The probability that quartz will be found, but not tourmaline or aquamarine is P(A) – P(A intersection B) – P(A intersection C) = 0.80 - 0.29 - 0.24 = 0.27.

The probability that none of these types of specimens will be found is 1 – P(A) – P(B) – P(C) + P(A intersection B) + P(A intersection C) + P(B intersection C) = 1 - 0.80 - 0.36 - 0.28 + 0.29 + 0.24 + 0.16 = 0.17.

The probability of A intersection (B union C) is P(A)*P(B union C) = P(A)*(P(B) + P(C) – P(B intersection C)) = 0.80 * (0.36 + 0.28 – 0.16) = 0.41.

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Answer:

it's called the lithosphere, it's the crust of the earth; the rocky outer layer of the earth.

Answer:

it's called the lithosphere, it's the crust of the earth; the rocky outer layer of the earth.

Explanation:

Option A - moderate violation of setback requirements is allowed for safety near a high-pressure natural gas pipeline.

Option A, where a moderate violation of setback requirements is allowed to ensure a safe distance from a high-pressure natural gas pipeline, is an example of a zoning variance. A setback requirement typically mandates a minimum distance between buildings and certain features like pipelines. In this case, the local zoning authority may grant a variance to deviate slightly from the setback requirement to ensure safety while still allowing the construction of the office building. Zoning variances are exceptions to the standard zoning regulations, granted under specific circumstances to address unique situations or hardships. Options B, C, and D do not involve zoning variances as they pertain to other aspects such as population density control, deed restrictions on house size, and mandatory swimming pool construction, respectively.

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Answer:

Summer monsoon usually begins in April and lasts till the month of September. ... The winter monsoons are called receding monsoons, and the air above the land surface is denser. The monsoon usually begins in October and lasts till March. The winter monsoons have dry air, and the temperature is cooler.

while faults occur in many locations, most of them are inactive or dormant and unlikely to move again in the future. However, it is still important for geologists and seismologists to continue monitoring these faults and studying their behavior to better understand their potential hazards.

Faults are fractures or breaks in the Earth's crust where rocks on either side of the break have moved relative to each other. These faults occur in many locations and can have different types of movements, including vertical, horizontal, and diagonal. However, most faults had displacement in the distant past and are unlikely to move again in the future. This means that most faults are considered inactive or dormant.
An inactive fault is one that has not moved in a long time, typically thousands or millions of years. These faults have reached a state of equilibrium where the forces acting on them are balanced, and there is no further movement. Over time, inactive faults can be covered by sediments or eroded, making them difficult to identify. However, geologists can still detect them through various methods such as studying the landscape, looking at rock formations, or using remote sensing techniques.
On the other hand, a dormant fault is one that has not moved recently but has the potential to do so in the future. These faults are often associated with earthquakes and can be hazardous to nearby communities. For example, the San Andreas Fault in California is a well-known dormant fault that is capable of producing a large earthquake.

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Answer:

the cause is humans not taking care of the eath by burning fossil fuels like coal gas and oil and the effect is climate change and and global getting hotter and hotter and the meals Antarctica wicth brings floods and cold fronts

Answer:

(hope this helps!)

There are many causes of global warming but the most known causes mainly stem from human activities such as burning fossil fuels, deforestation, and farming.

Fossil fuels produce large amounts of carbon dioxide when burned. Carbon emissions trap heat in the atmosphere which lead to climate change.

The surplus carbon is stored in the plant, helping it to grow. when trees are cut down and burned or allowed to rot, their stored carbon is released into the air as carbon dioxide. Eventually contributing to global warming.  

Farming has the same effect as deforestation because when you nurture and grow the plant the cut it down or uproot it, the carbon it is storing is released back into the air contributing to global warming.

Answer:

Hello. I can help you complete homework and essays instantly on request. Check my profile photo for easy comm uni cation

Explanation:

Answer:

broad and shallow valleys and rounded hills.

Explanation:

The peninsular plateau has broad and shallow valleys and rounded hills. This plateau consists of two broad divisions, namely, the Central Highlands and the Deccan Plateau.

Answer:

3

Explanation:

Answer:

the grassy one

Explanation:

the first one isn't tropical

the second one is a desert where it doesn't rain

the third one is like the desert but rains more for grass to grow

the fourth one is the best because you can tell it rains often

Earthquakes can indeed occur in relatively stable areas away from plate boundaries. These earthquakes are known as induced earthquakes and are typically caused by human activities rather than natural tectonic processes. Some common causes of induced earthquakes include:

1. Fluid Injection: Injecting large volumes of fluids, such as wastewater from oil and gas operations, deep underground can increase pore pressure and change the stress distribution in the rocks. This alteration of stress conditions can trigger seismic activity.

2. Mining Activities: Mining operations, particularly those that involve extracting minerals or extracting and injecting fluids from underground, can cause stress changes and lead to induced seismicity.

3. Reservoir Induced Seismicity: The filling of large reservoirs, such as those created by dams, can induce earthquakes. The weight of the water in the reservoir can exert stress on the underlying rocks, potentially causing faults to slip and generate seismic events.

4. Geothermal Energy Extraction: Geothermal energy extraction involves the extraction of heat from underground reservoirs. The fluid injection and withdrawal processes associated with geothermal operations can induce seismicity.

5. Hydraulic Fracturing (Fracking): Fracking is a technique used in the extraction of oil and gas from shale formations. The high-pressure injection of fluid into the rocks can create fractures, and the release of stored stress in the surrounding rocks can lead to induced seismic activity.

It's important to note that while induced earthquakes can occur in stable areas, they are generally of smaller magnitude compared to earthquakes along major tectonic plate boundaries.

However, in some cases, induced earthquakes can reach significant magnitudes and cause damage to infrastructure and pose risks to local communities.

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The collision of the newly created Laurasia (North America and Baltica) and Gondwana caused the Iapetus Ocean to close which lead to the Taconic orogeny. This is further explained below.

Generally,  The Taconic Orogeny: In the Late Ordovician, the volcanic arc clashed with eastern Laurentia (around 450 m.y. ago). Newfoundland to New York experienced deformation. The previously deposited sedimentary strata underwent metamorphosis and foliation in the center of the newly created mountain belt.

In conclusion, The closing of the Iapetus Ocean was a direct cause of the Taconic orogeny, which was triggered by the collision between the newly formed Laurasia (which included North America and Baltica) and Gondwana.

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The examples of long-term environmental change include mountain building, ice ages, and changes in solar energy reaching Earth.

Mountain building refers to the gradual formation of mountain ranges over millions of years due to tectonic plate movements and processes such as folding, faulting, and volcanic activity. This process results in significant changes to the landscape and alters regional climate patterns.

Ice ages are long-term periods of colder global temperatures characterized by the expansion of ice sheets and glaciers. These ice ages occur over geological timescales and have occurred multiple times throughout Earth's history, leading to the growth and retreat of ice masses and shaping the Earth's surface.

Changes in solar energy reaching Earth are another example of long-term environmental change. Variations in solar radiation, which can be influenced by factors such as changes in Earth's orbit and solar activity, can impact global climate patterns over long periods. These changes in solar energy can lead to shifts in temperature patterns, affect precipitation levels, and influence the overall climate system.

Forest fires, flooding, and small asteroid and comet impacts are examples of short-term or episodic environmental events rather than long-term changes. While they can have significant impacts on localized ecosystems and landscapes, they do not typically result in long-lasting, global-scale environmental transformations.

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