What is the correct definition of a settlements' 'Situation'?
(1 Point)

- The actual location of a settlement on the Earth

- An area of very poor housing, often self built by residents.

- The location of a place relative to its surroundings and other places.

- The central area of a city

The observer who measured the difference of 8 min 40 s in the arrival times of P and S waves is like 4,800 km away.

We can determine the distance to the earthquake epicenter by   using the time difference between the arrival of the P and S waves to estimate the distance from the earthquake to the station.

Hence, the observer who measured the difference of 8 min 40 s in the arrival times of P and S waves is like 4,800 km away.

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Answer:

This is all true.

Explanation:

The reason why is you try your best.

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Answer:

all true

Explanation:

mark me brainlies

Answer:

The answer is CCD. The CCD, or the charge-coupled device was used in the Hubble Space telescope and was later adapted for commercial use. CCD is a light-sensitive circuit used for storing and displaying data such as images. This is also used in digital cameras today.

Answer:1. One important cultural site that should be visited while in Senegal is the Gorée Island. This island is a UNESCO World Heritage Site and was the largest slave-trading center on the African coast in the 18th and 19th centuries. Visitors can tour the Maison des Esclaves, a former slave house that has been preserved as a museum, and learn about the history of the transatlantic slave trade. The island also has a vibrant arts scene and is home to many artists and galleries.

2. When taking a flight from Mauritania to Senegal, the flight will cross over the Senegal River and the Cap Vert peninsula.

3. One point of interest between Mauritania and Senegal is the Banc d'Arguin National Park. This park is located on the coast of Mauritania and is an important breeding ground for migratory birds, as well as a nesting site for sea turtles. The park also has a diverse marine ecosystem, including coral reefs and seagrass beds, and is home to many species of fish and marine mammals.

Explanation:

1.Visit the Great Mosque of Touba in Senegal for its religious significance as the spiritual center of the Mouride Brotherhood.

2.Senegal River and Cap-Vert Peninsula are major landforms and waterways crossed when flying from Mauritania to Senegal.

3.Banc d'Arguin National Park in Mauritania is interesting for its diverse ecosystems, including sand dunes, wetlands, and important bird habitats.

1.An important religious, historical, or cultural site that should be visited while in Senegal is the Island of Gorée. This UNESCO World Heritage site holds immense historical significance as it was a major center of the Atlantic slave trade. Visiting Gorée allows individuals to learn about the painful history of the transatlantic slave trade and gain a deeper understanding of its impact on Senegal and the world.

2.When taking a flight from Mauritania to Senegal, the major landform that will be crossed is the Senegal River. This river serves as a natural border between Mauritania and Senegal, and the flight path will likely follow its course. Additionally, as the flight approaches Senegal, it may cross over the Cap-Vert Peninsula, a prominent landform extending into the Atlantic Ocean.

3.One point of interest between Mauritania and Senegal is the Banc d'Arguin National Park. This national park is located along the coast and is known for its diverse ecosystems, including extensive sand dunes, coastal wetlands, and important bird habitats. The park is a significant breeding ground for migratory birds and supports a rich marine ecosystem. It is recognized as a UNESCO World Heritage site and offers unique opportunities for nature lovers and birdwatchers to explore and appreciate the region's biodiversity.

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Answer:Mellah é um antigo bairro judeu que pode visitar em Marraquexe. Tem uma praça e uma das mais antigas sinagogas da cidade marroquina, datada do século XVI. O Mellah tinha uma porta fortificada e era rodeado por uma muralha. Era uma zona de protecção. . Ao caminhar pelas ruas do bairro é possível conhecer bem de perto o modo de vida e a cultura judaica

Mellah é o nome usado em Marrocos para designar um bairro de judeus amuralhado de uma cidade. É um conceito similar ao das judiarias ibéricas e aos guetos da generalidade da Europa. Nas zonas rurais, onde é comum uma certa dispersão nos povoados, que frequentemente eram tradicionalmente um conjunto de ksars, cada um de seu clã ou tribo, os mellahs eram autênticas aldeias separadas habitadas exclusivamente por judeus.

Explanation:

Answer:

The east are closer to the equator.

Answer:

convection is involved in deepwater current

Answer:

When oceanic lithosphere collides with continental lithosphere at a convergent boundary, a subduction zone is formed. A subduction zone is a tectonic boundary where one lithospheric plate is forced beneath another plate and descends into the Earth's mantle.

Here's how the process occurs:

Oceanic lithosphere: The oceanic lithosphere, which is denser than the continental lithosphere, starts to converge with the continental lithosphere.

Subduction: As the oceanic plate moves towards the continental plate, it starts to subduct (dive) beneath the continental plate. This subduction occurs because the oceanic lithosphere is denser and more negatively buoyant than the continental lithosphere.

Trench formation: The point where the oceanic lithosphere begins to subduct beneath the continental lithosphere forms a deep oceanic trench. The trench marks the surface expression of the subduction zone.

Volcanic activity: As the oceanic lithosphere descends into the mantle, it undergoes intense heat and pressure. The subducting plate releases water-rich minerals and undergoes partial melting. This process generates magma, which rises through the overriding continental plate.

Volcanic arc formation: The magma generated from the subducting plate forms a chain of volcanoes known as a volcanic arc on the overriding continental plate. Examples of such volcanic arcs include the Andes in South America and the Cascades in North America.

Earthquakes and mountain building: As the subducting plate continues to descend into the mantle, it can cause intense pressure and deformation in the overriding plate. This leads to earthquakes and may result in the uplift and deformation of the continental crust, contributing to mountain building. Examples of mountains formed through the collision of oceanic and continental lithosphere include the Andes and the Himalayas.

Explanation:

In summary, when oceanic lithosphere collides with continental lithosphere at a convergent boundary, a subduction zone is formed. This results in the formation of a deep oceanic trench, volcanic activity and the creation of a volcanic arc on the overriding plate, earthquakes, and mountain building. The collision and subduction of oceanic lithosphere play a crucial role in shaping the Earth's surface and in the formation of significant geological features.

Answer: Panama and Costa Rica

Evidence:

Those countries are located in Central America.

Answer:

srry

Explanation:

Answer:

During an Earthquake, building start to shake. All of the plate movement leads to stress, stress leads to faults, and faults lead to disaster. The P Waves arrive, compressing and expanding the ground. Along come the S Waves that shake structures violently. Lastly, the surface waves arrive. They cause DRAMATIC ground movement.

Explanation:

Hope this helps! Best of luck!

An earthquake occurs when the stress on the edge exceeds the friction, releasing energy in waves that flow through the earth's crust and produce the shaking we experience.

When two chunks of the ground abruptly slide past one another, an earthquake results. The fault or fault plane is the area where they slide. The epicenter is the point on the earth's surface that is directly above the hypocenter, which is where the earthquake begins under the surface.

Foreshocks can occur during an earthquake. These are smaller earthquakes that take place in the same location as the one that follows the larger one. Before a larger earthquake occurs, scientists are unable to determine whether an earthquake is a foreshock.

The mainshock is the term used to describe the greatest earthquake. Aftershocks that follow mainshocks are a given. These subsequent, weaker earthquakes take place in the same location as the primary shock.

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Answer:

fgdfgdfh

Explanation:

Answer:

I think it's 30N i may be wrong if anyone else can correct me please do so!

The acceleration of 5 kg and 2.5 kg bowling ball at the same force is 0.5 m/s² and 1 m/s² respectively

F = m × a

where,

If

F = 2.5 N

m = 5 kg

F = m × a

2.5 = 5 × a

2.5 = 5a

a = 2.5 / 5

a = 0.5 m/s²

2.

F = m × a

2.5 = 2.5 × a

2.5 = 2.5a

a = 2.5/2.5

a = 1 m/s²

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Answer:

Carbon dating

Explanation:

Carbon dating determines the exact age of a fossil by measuring the amount of Carbon-14, a radioactive isotope of carbon, present in the fossil. Carbon-14 has a half-life of 5,730 years, meaning that after its half-life has passed, there will be half of the original amount of Carbon-14 in the fossil, and this decay continues until there is no Carbon-14 left.

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Answer:

Ummm I guess my first thought was that it evaporated...

Explanation:

The sun's heat turns the water into a gas called vapor... :)

Answer:

Stones and obsidian

Explanation:

Georgia’s natives primarily used stones and obsidian to make arrow heads.

Answer:

It is all important

Explanation:

Mostly: Scientists can analyze changes in chemical concentration of atmospheric gases because this is how we live breath and are present with the moment

Answer: 9

Explanation: Afganistan, Bangladesh, Bhutan, India, Iran, Maldives, Nepal, Pakistan & Sri Lanka.

Answer:

Glaciers can be thought of as rivers of ice, slowly flowing outward from their source to their terminus. Rates of ice flow range widely, but it is thought that the glaciers that affected Indiana probably moved relatively rapidly because they had abundant water at their bases to help "lubricate" their sliding motion over their beds. This sliding motion allows a vast amount of older rock and sediment to be eroded from the bed of the glacier, where it becomes frozen into the lower part of the ice. Thus, glaciers could be viewed in one sense as "conveyor belts", constantly transporting sediment from back up under the ice to the glacier margin. The edge of a glacier is where the ice is always melting. When melting rates are slow (for example, during winter or other especially cold times) and accumulation of new ice is rapid, the ice margin moves outward, or advances, whereas when melting rates are high, the opposite is true. In any event, the constant melting that goes on at the margin of a glacier releases vast amounts of entrained sediment, some of which may have traveled as frozen debris in the glacier for hundreds or even thousands of miles from its source. At the scale of the continental ice sheets, the quantity of sediment transported must have been astonishing. In Indiana alone, countless tens of feet of soil and bedrock were stripped off the landscape and redeposited down-glacier, along with even larger quantities derived from areas farther north. Hence, it is not surprising that the deposits of Ice Age glaciers are the dominant material in the Indiana landscape today, ranging up to several hundred feet thick in some places in the north.

But a landscape need not be directly affected by ice to be dramatically changed. As noted above, conditions just outside of a continental ice sheet are severe. Precipitation of potentially monsoonal proportions, coupled with a far greater frequency and intensity of freezing and thawing can set entire landscapes in motion. Recently thawed, super-saturated sediments on even a gentle slope will move easily under their own weight, creating widespread mud flows and extreme instability of the landscape. This process, called "solifluction", was probably very widespread within a zone of tens to perhaps a hundred miles wide fringing every ice sheet that invaded Indiana. The most extreme example of this landscape is permafrost, where a thick layer of permanently frozen ground exists at a shallow depth beneath a thin upper layer that experiences annual freeze and thaw action. The boundary between the frozen substrate and the soupy surface material is exceptionally unstable and results in constant rearranging of the landscape. There is good evidence that localized permafrost existed in a few places in northern Indiana during the waning stages of the Wisconsin ice sheet, and it seems quite possible that permafrost may have been more widespread during parts of the Illinoian glaciation, when the coldest global temperatures of the Ice Age were recorded in sea floor sediments and the ice sheets in Indiana extended to the Ohio River

Explanation:

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