On the coordinate plane below, what is the length of AB

Peru's residents are familiar with Enso as it brings a warm current that reduces populations of Anchovies

A member of the family Engraulidae, an anchovy is a small, common forage fish. The majority of species are found in marine environments, however a few will also live in brackish water, and several are only found in fresh water in South America.

The silver-colored longitudinal stripe that extends from the base of the caudal (tail) fin gives anchovies their tiny, green color and their blue reflections. As adults, they grow to a length of 2 to 40 centimeters (1 to 15+12 inches), and their body forms vary, with more slender fish seen in northern regions.

Anchovies are dispersed across the oceans of the world, however they are more common in temperate regions and rare or nonexistent in extremely cold or extremely warm waters. In general, they are quite tolerant of a wide variety of temperatures and salinities. The shallow, brackish, muddy bottoms of estuaries and bays are good places to look for large schools of fish.

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If a submarine sandwich shop makes sandwiches with one kind of bread, one protein, one choice of cheese, and one vegetable. The number of different sandwiches that  are possible is: 120.

Let's assume there are:

b=  bread

p= protein

c= cheese

v= vegetables

So,

Total number of sandwiches = b *p * c * v

For instance there would be a total of 11 distinct sandwiches if there were 3 bread options, 4 protein options, 2 cheese options, and 5 vegetable alternatives.

Total number of sandwiches = 3 * 4 * 2 * 5

Total number of sandwiches  = 120

With the specified options for bread, protein, cheese, and veggies, there would be 120 distinct sandwiches that might be made in this scenario.

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In the North-east part of China, from Liaoning through Hebei, Tianjin, Beijing, Inner Mongolia, Shanxi, Shaanxi and Ningxia into Gansu

An area in Texas has several months of heavy rain. This season is often following periods of drought. El Nino effect is likely its cause.

An El Niño situation happens when surface water in the equatorial Pacific evolves warmer than moderate and east winds blow weaker than normal. The warm ocean surface warms the atmosphere, which lets moisture-rich air uprise and expands into rainstorms. It varies rainfall imprints for months to seasons.

High-pressure designs lessen evaporation and moisture in the atmosphere. El Niño as the surface temperature of the Pacific Ocean around the central South American coast boosts, storm routines are disrupted. This phenomenon is assumed to build droughts.

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Poor conditions at home are frequently pushing factors. These variables may be economic, political, or societal. People are compelled to emigrate because of these reasons. The correct option is B.

A person who has fled their home country because they fear being persecuted and subjected to severe human rights violations there is known as a refugee. They thought they had no alternative but to leave their nation in search of safety because their own government could not or would not defend them from those dangers because the hazards to their safety and lives were so significant.

War is one of the push forces that "pushes" people from their homes. Better chances are a pull element that entices people to move to a new place. Economic, political, cultural, and environmental factors are the most common drivers of migration.

Thus, the refugee emigrating due to ongoing violence would be considered an example of a Push factor.

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Answer:

The Aksumite Empire at its height extended across most of present-day Eritrea, northern Ethiopia, western Yemen, southern Saudi Arabia, and Sudan. The capital city of the empire was Aksum, now in northern Ethiopia.

Answer:The Tropic of Capricorn lies at 23d 26' 22" (23.4394 degrees) south of the Equator and marks the most southerly latitude at which the sun can appear directly overhead at noon. This event occurs at the December solstice, when the southern hemisphere is tilted towards the sun to its maximum extent.

Explanation:

hope u got the answer that you were looking for <<33

I'm not sure what you're looking for exactly, but the Tropic of Capricorn lies at about 23.5 0 on the imaginary global lines.

The most useful observations for determining the geometry of rock layers deep in the subsurface are typically obtained from geophysical surveys, including seismic reflection and refraction surveys.

Seismic reflection surveys involve sending seismic waves into the subsurface and measuring the reflected waves to determine the location and geometry of subsurface rock layers. This technique is often used in oil and gas exploration and in the study of crustal structure.

Seismic refraction surveys involve measuring the angle and velocity of seismic waves as they pass through different rock layers in the subsurface. This technique can be used to determine the thickness and depth of different rock layers, as well as their physical properties, such as density and seismic velocity.

Other geophysical techniques that can provide information on the geometry of subsurface rock layers include gravity and magnetic surveys, which can be used to detect variations in the density and magnetic properties of different rock units. Electrical resistivity surveys can also be used to map subsurface rock layers, as different rock types have different electrical properties.

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Answer:

345.441051282

Explanation:

2.5 ÷ 78 =0.03205128205

+ 345.409 = 345.44

it is 345.44, the rest is not necessary.

because rounding the answer to a whole number is going to be 345, while to a decimal place it's going to be 345.44.

Answer:

345.441051282

Explanation:

The strategies used to manage the impacts of tourism in glaciated upland areas are ease traffic, enhance public transportation and set up a network of pay-as-you-go auto rentals and bicycles.

Glaciation creates pyramidal summits, and U-shaped valleys. Different land uses exist in glaciated uplands, which can cause conflict. To address issues, strategies need to be used.

To ease traffic, boost public transportation. assemble a network of pay-as-you-go bicycles and cars. Establish safe, continuous paths for those who are in wheelchairs, bicycles, and on foot. Create safe, continuous routes for people who use wheelchairs, bicycles, and other forms of transportation, and offer integrated travel tickets that cover several modes of transportation.

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Answer:

Convergent Plate Boundaries

Explanation:

Co-linear is refers to as the two points are said to be co-linear if they line on the same line.

Co-planar is defined as a two or more points are said to be co-planar if they all lie in the same plane.

In the diagram, AB,BF,EF,AC,CE,DC are all lines while ABEF,ABCD,BDF are planes. thus, A,H,B are co-linear since they all lie on the same line. also, H and J are not co-linear.

The points A,B,E, are co-planar because they all lie in the same plane ABEF while the points A,B,D,F are not co-planar because A,B,F lie on the same plane ABEF while D lies outside the plane.

Therefore, correct option is B.

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no

its in the middle of pacific ocean

closest land is hawaii

chatgpt

bardai

maps are up like chess board or graph paper

you can find things by find where horizontal & vertical lines

its called a

grid system

The order is observation, question, propose a hypothesis, make a prediction, test, results, changing outlets worked, propose a new hypothesis and make a new prediction.

The scientific method can be defined as a series of sequential steps in order to collect empirical evidence and thus test hypotheses that allow making predictions related to their outcomes.

In conclusion, the order is observation, question, propose a hypothesis, make a prediction, test, results, changing outlets worked, propose a new hypothesis and make a new prediction.

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The correct term for the daytime circulatory system along coasts where winds flow from a zone of high pressure over water to a zone of relatively low pressure over land is a sea breeze.

A sea breeze is a type of localized wind that blows from sea to land. During the day, a sea breeze forms when the air over the land is heated more quickly than the air over the ocean. The warm air over land rises and creates a zone of low pressure. The cooler air over the water is then drawn inland, resulting in a sea breeze.

Sea breezes are important because they cool coastal regions, which can become excessively hot during the day. As the sea breeze cools the air, it aids in preventing the formation of thunderstorms and other dangerous weather conditions. Furthermore, sea breezes are critical to marine life, especially during summer months when the heat can become unbearable for creatures that rely on the water for survival.

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Impacting human settlements: Volcanoes can impact human settlements in a variety of ways, including destroying homes and infrastructure, displacing communities, and disrupting economies. For example, the 1991 eruption of Mount Pinatubo in the Philippines caused the evacuation of over 20,000 people, and destroyed homes and farmland in surrounding areas.

Generally, Altering topography: Volcanoes can create new landforms or modify existing ones through the deposition of volcanic materials such as ash, lava, and pyroclastic flows. For example, the eruption of Mount St. Helens in 1980 created a new dome and crater, and buried the surrounding landscape in up to 600 feet of volcanic ash and debris.

Changing hydrology: Volcanic eruptions can cause changes in the water cycle by altering the distribution and availability of water. This can include the formation of new lakes, streams, and wetlands, as well as changes in water quality and quantity. For instance, the eruption of Mount Pinatubo in the Philippines in 1991 caused lahars (mudflows) that blocked rivers and caused flash floods.

Affecting atmospheric conditions: Volcanic eruptions can release large amounts of gas and particulate matter into the atmosphere, affecting air quality and weather patterns. For example, the 1815 eruption of Mount Tambora in Indonesia caused the "Year Without a Summer," a global climate anomaly marked by cooler temperatures and widespread crop failures.

Creating new habitats: Volcanoes can create new habitats for flora and fauna, such as geothermal springs and lava tubes. These habitats can be used by organisms adapted to extreme environments, such as thermophilic bacteria and tube-dwelling insects. The volcanic island of Surtsey, off the coast of Iceland, has been designated a UNESCO World Heritage Site for its unique ecosystem.

Producing fertile soil: Volcanic ash and other materials can enrich soil with nutrients and minerals, making it more fertile for plant growth. This is why many crops are grown in volcanic regions, such as coffee in Central America and grapes in Italy's Mount Etna region.

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Answer:

Moon doest have atmosphere to reflect back heat

Explanation:

need a thanks.......................

water cycle have different water residence times. Residence time is defined as the amount of water in a reservoir divided by either the rate of addition of water to the reservoir or the rate of loss from it. The oceans have a water residence time of 3,000 to 3,230 years.

The amount of time a fluid parcel has spent inside a control volume is known as its residence time (e.g.: a chemical reactor, a lake, a human body). In order to quantify the residence time of a group of parcels, either the frequency distribution of the residence time within the group, known as the residence time distribution (RTD), or the average residence time, known as the mean residence time, must be considered.

In chemistry, particularly in pharmacology and environmental science, residence time is crucial. In supply chain management and queueing theory, where the material that flows is typically discrete instead of continuous, lead time or waiting time, respectively, plays a crucial role.

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Answer:

c

Explanation:

Answer:

uhh ok..

Explanation:

Answer:

The suffix "-ic" means of or pertaining to.

Explanation:

:>

Answer:

A hydrosphere is the total amount of water on a planet. The hydrosphere includes water that is on the surface of the planet, underground, and in the air. A planet's hydrosphere can be liquid, vapor, or ice. On Earth, liquid water exists on the surface in the form of oceans, lakes and rivers.

Explanation:

Answer:berries

Explanation:

The pacific interannual oscillation is currently in a chilly phase in the north Pacific, which will cause the glaciers in the highlands to advance.

A glacier is a sizable, enduring mass of crystallized ice, snow, rock, silt, and frequently liquid water that forms on land and slides down a slope due to gravity and its own weight. One of the fastest-moving ice streams in the world is the Lambert Glacier in Antarctica, the biggest glacier in the world.

Arctic ice, ice caps, & outlet glaciers are the three different forms of glacial ice. An area greater than 50,000 sq miles is covered by an ice sheet (19,305 sq. mil.). Presently, enormous ice sheets cover Greenland and Antarctica.

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Answer:

Inverse relationship.

Explanation:

There is inverse relationship present between energy and distance because when one increases the other decreases. when the distance between objects  increases, the energy decreases while on the other hand, when the distance decreases, the energy between objects increases. Sun is present at one place so if an object go farther from the sun, the intensity of the sun decreases and vice versa.

Answer:

Descriptions elevation variance basically in different types

The utilization of investigative techniques and procedures to evaluate surface and subsurface geologic conditions is called Geophysical exploration. It is a process of studying the physical properties of the earth to determine its geological characteristics.

Geophysical exploration techniques include seismic surveys, magnetic surveys, gravity surveys, electrical surveys, and electromagnetic surveys. These techniques are used to study the physical properties of the earth's interior without drilling. In order to get an accurate interpretation of the subsurface structure and composition of the earth's crust, geophysical methods are often combined with geological, geochemical, and geotechnical data.A relevant example of utilizing investigative techniques and procedures to evaluate surface and subsurface geologic conditions is the use of seismic surveys in the oil and gas industry.

Seismic surveys are used to determine the location, size, and shape of underground oil and gas reservoirs by analyzing the reflection of sound waves off the various layers of rock and sediment. This helps geologists and engineers to make more informed decisions about drilling and production operations.

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The utilization of investigative techniques and procedures to evaluate surface and subsurface geologic conditions is called Geophysical exploration. It is a process of studying the physical properties of the earth to determine its geological characteristics.

Geophysical exploration techniques include seismic surveys, magnetic surveys, gravity surveys, electrical surveys, and electromagnetic surveys. These techniques are used to study the physical properties of the earth's interior without drilling. In order to get an accurate interpretation of the subsurface structure and composition of the earth's crust, geophysical methods are often combined with geological, geochemical, and geotechnical data.A relevant example of utilizing investigative techniques and procedures to evaluate surface and subsurface geologic conditions is the use of seismic surveys in the oil and gas industry.

Seismic surveys are used to determine the location, size, and shape of underground oil and gas reservoirs by analyzing the reflection of sound waves off the various layers of rock and sediment. This helps geologists and engineers to make more informed decisions about drilling and production operations.

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The difference between the volume of water evaporating from and precipitating onto the oceans is known as the oceanic water balance. This balance is influenced by a number of factors, including temperature, humidity, wind patterns, and ocean currents.

Generally, the amount of water evaporating from the oceans is greater than the amount of water precipitating onto them, resulting in a net loss of water from the oceans. This loss is compensated for by the flow of water from rivers and groundwater sources into the oceans, which helps to maintain their overall volume. Overall, understanding the complex dynamics of the oceanic water balance is important for predicting and managing the impacts of climate change on global water resources
To calculate the difference between the volume of water evaporating from and precipitating onto the oceans, follow these steps
Step 1: Obtain the volume of water evaporating from the oceans. This information can be found through research or given data. Let's assume the volume of water evaporating is V1.
Step 2: Obtain the volume of water precipitating onto the oceans. This information can also be found through research or given data. Let's assume the volume of water precipitating is V2.
Step 3: Calculate the difference by subtracting the volume of water precipitating (V2) from the volume of water evaporating (V1).

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The difference between the volume of water evaporating from and precipitating onto the oceans is known as the oceanic water balance. This balance is influenced by a number of factors, including temperature, humidity, wind patterns, and ocean currents.

Generally, the amount of water evaporating from the oceans is greater than the amount of water precipitating onto them, resulting in a net loss of water from the oceans. This loss is compensated for by the flow of water from rivers and groundwater sources into the oceans, which helps to maintain their overall volume. Overall, understanding the complex dynamics of the oceanic water balance is important for predicting and managing the impacts of climate change on global water resources
To calculate the difference between the volume of water evaporating from and precipitating onto the oceans, follow these steps
Step 1: Obtain the volume of water evaporating from the oceans. This information can be found through research or given data. Let's assume the volume of water evaporating is V1.
Step 2: Obtain the volume of water precipitating onto the oceans. This information can also be found through research or given data. Let's assume the volume of water precipitating is V2.
Step 3: Calculate the difference by subtracting the volume of water precipitating (V2) from the volume of water evaporating (V1).

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The main physical effects of a rise in sea level are beach erosion, water body erosion, inundation of deltas, flooding, and the loss of many marshes and wetlands.

In coastal aquifers and estuarine systems, increased salinity will probably become a concern as a result of saltwater intrusion.

Numerous variables can alter sea levels, which are known to have changed significantly throughout geological time spans. The primary driver of the current rise in sea level is human-caused climate change. Mountain glaciers and polar ice caps melt as a result of rising temperatures, adding more water to water bodies. In general, the phrase "above sea level" refers to heights above mean sea level (AMSL).

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Answer:

The vitally actual impacts of an ascent in ocean level are ocean side disintegration, water body disintegration, immersion of deltas, flooding, and the deficiency of numerous bogs and wetlands.

Explanation:

In waterfront springs and estuarine frameworks, expanded saltiness will likely turn into a worry because of saltwater interruption.

Various factors can modify ocean levels, which are known to have changed essentially over the course of land stretches of time. The essential driver of the flow ascend in ocean level is human-caused environmental change  Mountain ice sheets and polar ice covers soften because of climbing temperatures, adding more water to water bodies disintegration,. As a rule, the expression "above ocean level" alludes to levels above mean ocean level (AMSL)

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