fill in the blank...

Assuming no frontal passages, advection of warm/cold air, or anything that could affect temperature, the warmest time of day is afternon.

The afternoon, more specifically late afternoon or early evening, is usually when it's warmest. The delay in temperature response to solar heating is the cause of this. Even though the Earth's surface receives the most solar radiation at midday, it takes some time for the heat to be absorbed and released into the atmosphere.

Because of this the peak temperature is frequently recorded a few hours following solar noon. The precise time of the hottest part of the day can vary depending on factors like geographic location, season and local climate conditions. However, it is typically observed to occur in the late afternoon or early evening.

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Answer:

As a young person, you can establish credit in several ways. For starters, you could open a credit card in your name or take out a loan. Or, you can ask a parent to add you to one of their credit cards. But most importantly you must pay your bills on time and Get and Keep a Steady Job.

Answer:

Cause are:

Heavy rainfall

Strom

Tidial waves

Answer:Heavy rainfall

Strom

Tidial waves

Answer:

The Richter Scale is a measurement of the magnitude of an earthquake. The following are characteristics of a Richter Earthquake Magnitude:

It is a logarithmic scale: The Richter Scale is a logarithmic scale, meaning that the energy released by an earthquake increases exponentially with each whole number increase in magnitude. For example, an earthquake with a magnitude of 6.0 is 10 times more powerful than an earthquake with a magnitude of 5.0.

It measures the amplitude of seismic waves: The Richter Scale measures the amplitude of seismic waves, which are the vibrations that travel through the Earth's crust during an earthquake. The amplitude is determined by measuring the maximum height of the waves recorded by a seismograph.

It has no upper limit: The Richter Scale has no upper limit, meaning that theoretically, there is no limit to the magnitude of an earthquake that could be recorded. However, in practice, the largest earthquake ever recorded had a magnitude of 9.5.

It is widely used: The Richter Scale is one of the most widely used measures of earthquake magnitude, and it is often reported by the news media after an earthquake.

It is not the only scale: While the Richter Scale is a widely recognized measure of earthquake magnitude, there are other scales that are also used, such as the moment magnitude scale and the Mercalli intensity scale. These scales measure different aspects of an earthquake, such as the total energy released or the level of damage caused

Explanation:

The Richter scale is a logarithmic scale used to measure the magnitude of an earthquake.

The scale ranges from 0 to 10 and each whole number increase represents a tenfold increase in the earthquake's amplitude. Some characteristics of a Richter earthquake magnitude include the amount of energy released, the size of the fault rupture, and the depth of the earthquake's epicenter.

Earthquakes with a magnitude of 3.0 or lower are generally not felt, while those with a magnitude of 7.0 or higher can cause widespread damage and loss of life. The Richter scale is often used by the media to quickly and easily communicate the severity of an earthquake to the public.

However, it is important to note that the scale does not necessarily indicate the extent of damage caused by an earthquake, as factors such as distance from the epicenter and soil conditions can also play a significant role.

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Most precipitation on the east coast and southeastern part of the United States is derived from hurricanes, easterly waves, tropical storms, and other weather patterns in the Atlantic Ocean.

Precipitation is any form of moisture that falls from the atmosphere and reaches the surface of the earth. Rain, hail, sleet, snow, and other forms of precipitation are examples. The Earth's environment, including the weather and climate, is affected by precipitation.

The amount, frequency, and location of precipitation may have significant impacts on the environment.

The eastern United States receives the majority of its rainfall from the Atlantic Ocean. Air masses over the ocean are often moist, and when they meet the coast, they are pushed inland, causing precipitation to fall. Weather fronts moving across the continent also bring rain and snow to the eastern United States.

The Appalachian Mountains, which run from Maine to Alabama, act as a barrier, forcing the moist ocean air to rise and form precipitation.

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The pressure zone that is associated with abundant precipitation and warm temperatures is called the tropical zone.

This zone is located near the equator and experiences high levels of solar radiation, leading to warm temperatures and abundant moisture in the atmosphere.

As a result, many areas within the tropical zone experience frequent rainfall and lush vegetation. The pressure zone associated with abundant precipitation and warm temperatures is known as the Intertropical Convergence Zone (ITCZ). This region experiences consistent low pressure, leading to the rising of warm, moist air, resulting in frequent rainfall and consistently warm temperatures.

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The rise of the West African kingdoms of Ghana, Mali, and Songhai can be attributed to several factors. these factors were instrumental in the rise of the West African kingdoms, their decline and eventual downfall were influenced by a combination of internal conflicts, external invasions, and the disruption of trade routes by European powers.

Control of Trans-Saharan Trade: These kingdoms were strategically located along major trade routes that connected West Africa with North Africa and the Mediterranean. They gained wealth and power by controlling and taxing the lucrative trade in gold, salt, and other valuable commodities. The ability to regulate and benefit from this trans-Saharan trade contributed to their economic prosperity and political influence.

Rich Natural Resources: The region encompassed by these kingdoms was abundant in valuable natural resources such as gold, which was highly sought after by traders from North Africa and beyond. The control and exploitation of these resources provided a significant economic advantage to the West African kingdoms.

Political Stability and Strong Leadership: The rise of these kingdoms was also facilitated by strong and centralized political systems. Effective governance, stable institutions, and capable leadership contributed to the consolidation of power and the ability to maintain control over vast territories. Leaders such as Sundiata Keita of Mali and Mansa Musa of Mali are notable examples of influential rulers who contributed to the kingdoms' growth and prominence.

Military Strength and Expansion: Military prowess played a crucial role in the expansion and consolidation of these West African kingdoms. They developed formidable armies and advanced military strategies, which enabled them to conquer neighboring territories, expand their influence, and establish control over trade routes. The military strength of these kingdoms acted as a deterrent to potential aggressors and solidified their position of power.

Cultural and Intellectual Advancements: The West African kingdoms of Ghana, Mali, and Songhai were centers of cultural and intellectual advancements. They fostered vibrant centers of learning, such as Timbuktu, which attracted scholars, traders, and artists from different parts of Africa and beyond. This cultural and intellectual flourishing enhanced the prestige of these kingdoms and contributed to their overall growth and influence.

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Answer:36.33

Explanation:

You use the Pythagorean theorem, a^2 +b^2=c^2; the hypotenuse is the C side being the longest side on the triangle.

The given statement "expressing geographical movement includes expressing the movement of ideas" is True.

Expressing geographical movement includes expressing the movement of ideas, as geography is not only concerned with the physical movement of people and goods, but also with the spread of ideas and the cultural exchange that can occur through this movement.

Geography can also be used to describe the effects of movement, such as the way in which the movement of people, goods, and ideas can shape the environment and societies.

Geography can also be used to describe the ways in which population distribution, access to resources, and other factors affect the development and sustainability of communities. In addition, geography can be used to analyze the impact of transportation and communication networks on the environment and society.

By understanding how different elements interact with each other, geography can provide insight into how human activities can be managed or mitigated.

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A biogeochemical cycle refers to the  exchange of chemicals among magmatic and solid-phase systems.

Hence, option C is correct.

A biogeochemical cycle describes how an element or compound, such as water, moves between its various living and nonliving forms and locations in the biosphere. Water, carbon, nitrogen, phosphorus, and sulfur cycles are all important biogeochemical cycles for living organisms.

Many biogeochemical cycles operate as part of ecological systems (ecosystems), such as the water cycle, carbon cycle, nitrogen cycle, and so on. All chemical elements occurring in organisms are part of biogeochemical cycles.

The term biogeochemical is an abbreviation for considering the biological, geological, and chemical aspects of each cycle.

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The correct answer is option C.

The other reason for the planet to support earth-type life is it is necessary for the planet to have active plate tectonics to close its carbon cycle.

There is no evidence of life on any other planet than earth. It is because earth is a terrestrial planet and has an insulating atmosphere that keeps the planet warm and protected from the UV radiations.

The balanced chemical ingredients, moderate temperature, right climate and water and carbon also support all forms of life on earth.

Moreover, the plate tectonics on earth trap carbon in it and is released into atmosphere as a result of volcanic eruption.

To put it simply, for any other planet to support life, it must be larger than Mars, it should have active tectonic plate to trap carbon cycles in its rocky bodies.

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Answer:

Wednesday, 8:00 PM

Hope this helps :)

Pls brainliest...

If it is 11:00 AM Thursday in Seattle, it is 3:00 AM Friday in Seoul, South Korea. This is because Seoul time is 16 hours ahead of Seattle.

To determine the time and day in Seoul, South Korea when it's 11:00 AM Thursday in Seattle, follow these steps:
1. Calculate the time difference: Seoul is 16 hours ahead of Seattle.
2. Add the time difference to the Seattle time: 11:00 AM + 16 hours = 3:00 AM.
3. Adjust the day accordingly: Since the time difference pushes us into the next day, the day will be Friday.
So, when it's 11:00 AM Thursday in Seattle, it is 3:00 AM Friday in Seoul, South Korea.

Seattle is in the Pacific Time Zone of the United States, which is 16 hours behind South Korea Standard Time, so when it's 11:00 AM on Thursday in Seattle, it would be 3:00 AM on Friday in Seoul. It's important to keep in mind time zones when making plans or communicating with people in different locations around the world.

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Answer:

How far is the seismic station to the epicenter?

100 miles.

Explanation:

In other words, if P-waves travel at 4.00 miles per second, S-waves travel at 2.50 miles per second and the lag time is 15 seconds, the distance of the earthquake epicenter will be 100 miles

Answer:

Explanation:The mean Earth-Moon distance at opposition (i.e., when relative to the Earth, the Moon and the Sun are opposite each other) is 378,000 km. The Earth's diameter is 12,742 km, which makes the Earth-Moon distance about 29.7 Earth diameters. For a 16-inch globe

P-waves are reflected when they encounter a boundary between different types of rocks, such as when they encounter a fault. This would prevent the P-waves from arriving at seismic station B.

P-waves, or primary waves, are compressional waves that travel through the Earth's interior, transmitting seismic energy. P-waves are the fastest seismic waves, and are the first waves to be detected in a seismic event. P-waves are longitudinal waves, meaning they propagate in the same direction as the direction of the wave's vibration. As P-waves travel through the Earth's interior, they create alternating zones of compression and expansion. These alternating zones are what make up the seismic wave. P-waves can travel through a variety of materials, including liquids and gases, and their speed of travel is dependent on the medium and the density of the material. P-waves are an important tool in seismology, as they are used to map the Earth's interior and better understand the structure of the planet.

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You would need 5 contour lines to show change in the elevation of 2,000 feet on map with contour interval of 400 feet.

A contour line of a two-variable function is a curve where the function has a constant value, joining points of equal value. A contour line, used in cartography, connects points that are similar in elevation (height) above a specified level, like mean sea level. A contour map is a map that has contour lines drawn on it, such as a topographic map that displays valleys, hills, and the steepness or leniency of slopes. The elevation difference between a contour map's subsequent contour lines is known as the contour interval. Every time, the function's gradient is parallel to the contour lines. The gradient has a significant amplitude and a steep variation when the lines are near together.

No. of contour lines= 2000/400=5

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The Bedford Level experiment was conducted to measure the curvature of the Earth.

The Bedford-level experiment was conducted during the late 19th and early 20th centuries. This was conducted along the 6-mile length of the Old Bedford River in the United Kingdom. The two major researchers at work here were - Samuel Birley Rowbotham and Alfred Russell Wallace.

During the earlier stages of the experimentation, the Earth was found to be flat, later it was realized that the curvature of the Earth pointed towards a spherical Earth. This experimentation was started in 1838 with a boat and a flag on top of it to understand the angle of flow in the river as the boat was sailed. This was done using a telescope held 8 inches above the water level.

The results so obtained could also be observed during atmospheric refraction. This can be observed as the light rays travel horizontally and vertically to reach the Earth's Surface. These results were used to prove the spherical shape of the Earth.

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Answer:

its prob C

Explanation:

Answer:

Wind Power

Explanation:

Wind power is inexhaustible, meaning that there is an infinite supply of wind since it comes from nature.

Wind power can power things like wind turbines, converting the kinetic power that comes from it to the appropriate energy type(electricity) in order for it to operate.

Grains become sharp/angular in shape Before sediment debris is transported, after they have first broken off their supply rock, their shapes tend to be angular and choppy.

Sediment particles that have traveled further from their source have a tendency to be smoother, extra rounded, and finer.

Debris emerges as sorted on the premise of density, because of the energy of the transporting medium. Excessive energy currents can bring large fragments.

Because the strength decreases, heavier debris is deposited and lighter fragments remain transported. This outcome in sorting due to density.

Very poorly sorted suggests that the sediment sizes are blended (massive variance); whereas well sorted suggests that the sediment sizes are comparable (low variance).

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The correct answer is shale. Very fine mud sediments with a size less than 1/256 mm are classified as clay particles. When these clay particles are deposited and buried under pressure and compaction, they can form a sedimentary rock known as shale.

Shale is a fine-grained sedimentary rock composed mainly of clay minerals, such as illite, kaolinite, and smectite. The small particle size of the clay minerals allows for the formation of a dense, impermeable rock that can be found in a variety of depositional environments, including marine, lacustrine, and deltaic environments. The color of shale can vary from gray to black, and it often exhibits a fissile texture, meaning it can easily split into thin layers or sheets due to the alignment of clay minerals during compaction. Shale can also contain fossils, which can provide valuable information about the environment and conditions under which the rock was formed. In summary, very fine mud sediments with a size less than 1/256 mm are likely to form shale, a fine-grained sedimentary rock composed mainly of clay minerals that can be found in various depositional environments and can contain fossils.

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The least likely part of a slope to be steeper than the angle of repose is the section where the slope reaches a state of equilibrium, also known as the angle of repose. This angle represents the maximum angle at which loose granular materials, such as sand or gravel, can rest without collapsing or sliding.

The angle of repose is determinedpose anhe  by the properties of the material making up the slope, including its grain size, shape, and cohesion. It is the angle at which the gravitational forces acting on the material are balanced by the frictional forces between the particles. If the slope angle exceeds the angle of repose, the material will experience a failure and slide or collapse.

Given that the angle of repose represents the equilibrium state for the material, any section of the slope that is already at or close to this angle is less likely to be steeper. As the slope approaches the angle of repose, it becomes increasingly stable, and further steepening would disrupt the balance between gravitational and frictional forces. Therefore, the part of the slope that is closest to the angle of repose is the least likely to be steeper than this critical angle.

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Considering the available picture and the types of diffusion in human geography, the kind of diffusion in picture A is Relocation diffusion, while picture D has a Stimulus diffusion

Relocation diffusion is a term that is used to describe the type of diffusion whereby people relocate from their point of origin to another place which usually includes changing places along the journey as well as the final destination.

On the other hand, Stimulus diffusion is a term that is used to describe diffusion whereby practices adopted by specific people changes as it is adopted by another group of people due to the practices infused with the customs of the new adoptees.

Hence, in this. case, it is concluded that the correct answer is Relocation and Stimulus diffusion respectively.

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The ability to create a triangle from the supplied angles depends on whether the total of those angles equals 180 degrees, which requires further information to be able to solve for x.

We need additional details about the situation and the context in which it arises in being able to fix for x in the provided problem. Without more information, it is impossible to calculate the value of x since the supplied angle measurements and numbers seem to be a component of a broader issue.

The triangle angle measurements are as follows:

The angles 115, 35, and 30 cannot form a triangle because a triangle must have angles that add up to 180 degrees.

A triangle must have angles that add up to 180 degrees, hence the angles 55, 90, and 45 may all be used to construct one.

Because a triangle must have angles that add up to 180 degrees, the angles 100, 30, and 30 do not constitute a triangle.

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Spatial concepts help to explain the distribution of phenomena on Earth.

Spatial concepts provide a language for explaining the configuration of individuals, places, and environments. Arrangements can be represented in terms of proximity, distance, scale, clustering, distribution, etc.

Geographic concepts permit the exploration of relationships and connections between individuals and both natural and cultural environments. They include a spatial component. They furnish a framework that geographers utilize to interpret and symbolize information about the world.

Geography's unique method of understanding the world exists through spatial patterns and associations. A geographer visualizes and analyses spatial associations between objects i.e. they utilize notions such as location, distance, direction, shape, and pattern.

Spatial distribution in statistics exists in the arrangement of a phenomenon across the Earth's surface and a graphical display of such an interpretation exists as an essential tool in geographical and environmental statistics.

Hence, Spatial concepts help to explain the distribution of phenomena on Earth.

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The correct statement for samples collected at locations C and D is:
[A13+1c < [A13+]D

This means that the concentration of A13+1c (an element or compound) is lower at location C (3000 m in the North Atlantic near Bermuda) compared to location D (3000 m in the North Pacific near Hawaii).
The "<" symbol indicates "less than" or "lower than."

Therefore, the statement [A13+1c < [A13+]D means that the concentration of A13+1c at location C is lower than the concentration of A13+ at location D.

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If an isotope has a half-life of 4 billion years, then in 4 billion years, 1/2 (half) of the original amount will still be present.

The half-life of a radionuclide refers to how long it takes for half of its radioactive atoms to decay. If an isotope has a half-life of 4 billion years, so for 4 billion years after its only decay half of it.

Isotopes are constituents of the same element's family but differ in the number of neutrons they contain for every proton they have. The number of protons each element has in its nucleus determines its atomic number on the Periodic Table. For instance, the carbon atom, which has the number 6, has six protons.

A good rule of thumb is that you will have less than 1% of the initial amount of radiation after seven half-lives. The amount of time it takes for one-half of a radioactive isotope to decay is known as the half-life.

Your question is incomplete but most probably your full question was

If an isotope has a half-life of 4 billion years, then in 4 billion years A. all of the original amount will have decayed. B.1/2 of the original amount will still be present. C. all of the original amount will still be present. D. ¼ of the original amount will still remain. E. none of these

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Illegal settlements​ are obstacles to peace, violations of law,

Illegal settlements typically refer to the establishment of civilian communities in territory that is considered by international law to be occupied by a foreign power. These settlements are usually built by the occupying power within the occupied territory, often leading to significant controversy and conflict.

It's important to note that the issue of illegal settlements is complex and politically charged, and different individuals, governments, and organizations hold diverse opinions and stances on the matter. Resolving the issue requires considerations of legal frameworks, geopolitical factors, historical claims, and the aspirations of different communities involved.

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The interaction of huge, frozen glaciers with the land during the latest ice age on Earth resulted in glacial erosion. This process involved plucking and abrasion, which caused the crushing and flattening of solid, rocky features on the land.

During the latest ice age on Earth, huge, frozen glaciers of snow and ice slowly moved across the surface of the planet. These glaciers interacted with the land in various ways, including crushing and flattening many solid, rocky features. This process is an example of glacial erosion.

Glacial erosion occurs when glaciers, massive sheets of ice, advance and retreat over the landscape. As the glaciers move, they exert pressure on the land beneath them. The weight and movement of the ice cause the glaciers to act as powerful bulldozers, pushing and scraping the land below.

One of the main processes involved in glacial erosion is called plucking. As the glacier moves, it freezes onto rocks and sediments, and when it retreats, it pulls these materials away from the land, incorporating them into the ice. This process can lead to the creation of deep, U-shaped valleys and cirques.

Additionally, glacial erosion involves abrasion. As the glacier moves, the rocks and sediments frozen within it act like sandpaper, grinding against the land beneath. This abrasive action helps to crush and flatten solid, rocky features such as mountains, hills, and ridges.

In conclusion, the interaction of huge, frozen glaciers with the land during the latest ice age on Earth resulted in glacial erosion. This process involved plucking and abrasion, which caused the crushing and flattening of solid, rocky features on the land.

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