What was one positive impact that Europe had on Africa?

Answer:

In a religious standpoint, the parable of the lost sheep, which comes from the Holy Bible, essentially states that Jesus (the shepherd in the story), would go out of his way to find the sinners (the lost sheep), and bring them back to God. It can also be taken in the context that the lost sheep are those who do not believe, and that the shepherd would go and 'save' them, or convert them to Christianity. Essentially, it is God's promise to go out to save those who stray from the path.

Answer:

Brainliest are appreciated ;)

Explanation:

All tourists are travelers because they only roam all the tourist attractions. The tourists purpose is to visit new places. But all travelers are not tourists because some go in search of jobs and to participate in several competitions, tournaments, business purposes etc.

Answer:

Hey mate.....

Explanation:

This is ur answer.....

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Answer:

D.  highly trained or skilled professionals away from their home country

Explanation:

The term human capital flight refers to the emigration/immigration of highly skilled workers from low-income countries to higher-income countries.

Answer:

suitable for crop farming

It started when we were younger you were mine my boo

The annual rainfall for the year 2020 at the average altitude of the river basin (330m) can be calculated based on the rainfall recorded at meteorological station A, located at an altitude of 25m.

To estimate the annual rainfall at the average altitude of the river basin, we can make use of the altitude effect on rainfall. Generally, as altitude increases, the amount of rainfall tends to increase due to the orographic effect. However, if the terrain is mild, the increase in rainfall with altitude may not be as significant.

In this case, the meteorological station A recorded an annual rainfall of 482mm at an altitude of 25m. To calculate the annual rainfall at the average altitude of the river basin (330m), we can use the concept of a lapse rate. The lapse rate is the rate at which temperature or other atmospheric variables change with altitude.

Assuming a mild terrain, we can approximate the average lapse rate for rainfall to be around 7% per 100 meters of elevation. Using this approximation, we can estimate the change in rainfall with respect to the change in altitude.

The difference in altitude between meteorological station A (25m) and the average altitude of the river basin (330m) is 330m - 25m = 305m. Dividing this by 100m and multiplying by the lapse rate of 7%, we get (305/100) * 7% = 21.35%.

To calculate the annual rainfall at the average altitude of the river basin, we can apply this percentage increase to the rainfall recorded at meteorological station A.

Annual rainfall at the average altitude of the river basin = 482mm + (482mm * 21.35%) = 482mm + 102.91mm ≈ 584.91mm.

Therefore, the estimated annual rainfall for the year 2020 at the average altitude of the river basin (330m) is approximately 584.91mm.

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Answer:

dacă și părul tău mut este rece prea flamingo oh oh oh drăguțul tău col

Explanation:

Answer:

Monsoons produce the very wet summers and dry winters that occur on nearly all of 2015, it began to rain in Mumbai, India, and it did not stop until the next day. From June to August, which are summer months in the Northern Hemisphere, of what is typical during the wet season and farmers could not plant their crops.

Answer:

The phases are always the reverse of each other. When we see the moon as nearly full, any moon people would see a slim crescent Earth. When we see a completely full moon, the moon, Earth and sun are in a line – with Earth in the middle.

Explanation:

Answer:

Mantle

Explanation:

Cirques and horns are glacial erosional features associated with alpine glaciers. Option A is the correct answer.

What are cirques and horns?

A cirque is a bowl-shaped hollow that is shaped like an amphitheater. It is carved by alpine glaciers. A cirque is an erosional feature formed as a result of the plucking of rocks by glaciers. Cirques are generally located at the head of a valley glacier, where snow and ice accumulate, and they may be up to several kilometers across. This type of glacial erosion forms steep ridges and sharp peaks that jut up into the sky above a glacier.

Horns are spires of rock that are sharpened by glaciers. They are formed as a result of the cirques. Horns are high, sharp, and jagged peaks that are shaped like pyramids. They are created as several cirques cut into the mountain from different sides until only one peak remains in the middle. Examples of horns are the Matterhorn in the Alps and the Hornli ridge in Switzerland.

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Global climate change has been observed to have several negative effects on biodiversity. Biodiversity refers to the variety of living organisms on earth, including genetic, species, and ecosystem diversity.

Climate change has led to rising temperatures and changes in precipitation patterns, which have altered the natural habitats of various organisms. For instance, species that are unable to adapt to these changes have been forced to migrate or risk extinction.Therefore, Global climate change affects biodiversity through altering natural habitats, changing seasons and precipitation patterns, and causing extreme weather events such as droughts and floods. As a result, the loss of biodiversity also has a significant impact on global climate change.

For example, deforestation and other land-use changes can release large amounts of greenhouse gases into the atmosphere, thereby exacerbating global warming. To overcome both problems, a combination of measures will be necessary.

These include: Developing and implementing climate change mitigation strategies to reduce greenhouse gas emissions and slow the rate of global warming Protecting and restoring natural habitats and ecosystems, which will help to conserve biodiversity as well as capture and store carbon Providing financial incentives to support biodiversity conservation and climate change mitigation Researching and promoting the use of renewable energy sources Reducing meat consumption to reduce greenhouse gas emissions caused by livestock production Encouraging public education on the importance of biodiversity and the effects of climate change.

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The 40° F isotherm follows a slightly northward path from the Pacific Ocean across North America in January. It moves through the West Coast along the coastal region of Oregon, Washington, and British Columbia. The isotherm then takes a slight bend towards the north-east as it crosses into Canada, tracing an eastward path through Alberta and Saskatchewan before continuing its eastern trajectory in Manitoba and Ontario.

The deviation of the 40° F isotherm from a true east-west trend arises from the influence of the Rocky Mountains, which create a southerly flow of moist air from the Pacific Ocean heading towards the Great Plains of the United States. This results in the 40° F isotherm taking an irregular path, which sees it veer northward as it crosses the continent. This phenomenon is known as an orographic effect, which occurs when air masses are forced to rise over a mountain range. As the air rises, it cools and the isotherm follows the gradation in temperature, producing the irregular east-west trend.

In January, the path of the 40°F isotherm (a line connecting points with an average temperature of 40°F) over North America generally exhibits an east-west trend.

However, when it crosses from the Pacific Ocean onto the continent, the isotherm deviates from this true east-west pattern.

The deviation occurs primarily due to the influence of oceanic currents and air masses. Along the Pacific coast, the cold California Current flows southward, carrying colder ocean waters from higher latitudes. This current cools the adjacent coastal areas, resulting in lower temperatures compared to inland regions at the same latitude.

As the isotherm encounters this cooler coastal area, it is forced to shift southward or southeastward, following the path of the colder temperatures influenced by the California Current. This deviation from the true east-west trend reflects the impact of the oceanic currents on the local climate and temperature patterns.

Additionally, other atmospheric factors such as prevailing wind patterns, mountain ranges, and local topography can contribute to further deviations of the isotherm. For example, coastal mountains can act as barriers, causing air masses to rise, cool, and potentially enhance precipitation, leading to cooler temperatures near the coast.

Overall, the deviation of the 40°F isotherm from a true east-west trend where it crosses from the Pacific Ocean onto the continent is primarily influenced by the cooling effect of oceanic currents and other regional atmospheric factors.

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Dark matter refers to mass that does not emit, absorb, or interact with light or other electromagnetic radiation, making it invisible and difficult to detect. It is not related to mass disappearing into a black hole or made of anti-matter whose effects cancel those of gravity.

Dark matter is not mass that disappears into a black hole but still exerts gravitational attraction on nearby objects (option A) or mass made of anti-matter whose effects cancel those of gravity (option B).

Instead, dark matter is believed to be a type of matter that does not interact with light or other forms of electromagnetic radiation, hence the term "dark." Its presence is inferred from its gravitational effects on visible matter, such as stars and galaxies.

Dark matter is a hypothetical form of matter that is believed to make up a significant portion of the total matter in the universe. It does not emit, reflect, or interact with light or any other form of electromagnetic radiation, which is why it is called "dark." Its existence is inferred from its gravitational effects on visible matter and the way it influences the motions of galaxies and galaxy clusters.

Dark matter is thought to be composed of non-baryonic particles that have not yet been directly observed or identified. While its exact nature remains a mystery, scientists continue to study and search for evidence of dark matter through various astrophysical and cosmological observations.

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Answer:

Impacts of Egypt's Aswan Dam

Subtropical xerophytic forest  is a forest that is characterized dry or  rid climate  or environment and  plants that  are found in such forest can adapted in such environment they are characterized with deep tap root with which enable them to store water which their major tool for adaptability and home to different  kind of animals, rodents, birds, and various reptile species.

Examples of Subtropical xerophytic forest are found in dry or  rid climate are The Guanica Forest Biosphere Reserve in Puerto Rico. ,thorn forest in India  Sonoran-Sinaloan Subtropical Dry Forest in Northern Mexico etc.

Example  of Xerophytes plants are different species of cactus such as  jumping cholla cactus, barrel cactus, organ pipe cactus ,palms ,torote prieto (elephant tree ) ,Agave ,Acacia trees ..Oleander Mesquite .Condea emoryi (desert lavender),euphorbias ,cacti,scrub oak.  etc.

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Answer:

Discrimination,  exploitation, and unsafe working conditions.

Answer:

Language could be a difficulty causing communication barriers and making the migrants have trouble expressing their thoughts or perspectives. Discrimination is often faced by migrant workers, as they are not from their host country. Health care can sometimes be a struggle as not having a citizenship of the host country may make it hard to obtain health care.

People build jettys for a variety of reasons. One of the most common is to protect the beach from smaller waves and currents that can erode the beach shoreline.

Jettys are also commonly built as an entryway to a marina, to keep the waterway deep enough for boats to navigate through. Additionally, jettys are sometimes used to create a funnel for currents to carry sediment and sand to a specific place, such as a beach, to replenish lost sand contributing to beach nourishment.

Finally, jettys may also be used to keep birds away from beachgoers - for example, in areas where seagulls may try to steal food from sunbathers. As such, while jettys can have negative effects on beach nourishment, they may have positive impacts in other areas which make them worth the risk.

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Answer:

As average temperatures at the Earth's surface rise, more evaporation occurs, which, in turn, increases overall precipitation. Therefore, a warming climate is expected to increase precipitation in many areas.

Explanation:

(hope this helps)

Answer:

This is the drainage map of africa

The planetary nebula expands at a rate of 28 km/s. To determine the distance it will expand in 4 million years, we can multiply the expansion rate by the given time.

To calculate the distance the planetary nebula will expand in 4 million years, we multiply the expansion rate of 28 km/s by the time of 4 million years.

This can be calculated using the formula: distance = rate × time. Plugging in the values, we have distance = 28 km/s × 4,000,000 years. Performing the multiplication, we find that the nebula will expand approximately 112,000,000 km in 4 million years.

Therefore, in the given time period, the planetary nebula will expand about 112 million kilometers.

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Answer:

Layer A is youngest after tilting because tilting did Layer A small.(But I am not sure I hope it's help!)

Explanation:

When high-speed winds build an upper layer over the Atlantic Ocean, the circumstances that lead to hurricane season in the Atlantic area are favorable. as a result, Option d

The Atlantic hurricane season is when the majority of tropical storms in the northern Atlantic Ocean are likely to form. The season is now defined as the period from June 1 to November 30, however, it was formerly classified as a shorter period.

The Atlantic hurricane season peaks on September 10th, with the majority of activity taking place between mid-August and mid-October.

As a result, option d represents the appropriate hurricane season circumstances.

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Surface temperatures vary from the equator towards the poles in the following ways:The equator region has high temperatures compared to the regions located at the poles.

The poles experience cold temperatures due to the low angle of incidence of solar radiation. The heat from the sun is distributed over a larger area as it travels further towards the poles. Also, the earth's rotation causes the earth's axis to be tilted which causes differences in the angle of incidence of solar radiation.

These cause differences in the temperature of the earth surface towards the poles. Therefore, the likely cause of variation in surface temperatures from the equator toward the poles is the distance from the sun, the angle of incidence of solar radiation, and the earth's tilt.

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Answer:

Florida's

Explanation:

The "river" of high-speed ocean water, known as the Gulf Stream, passes in closest proximity to the Florida coast.

The Gulf Stream is a powerful and swift ocean current that originates in the Gulf of Mexico and flows along the eastern coast of the United States. It carries warm water from the tropics northward along the Florida coast and then veers eastward towards the Atlantic Ocean.

As it flows along the Florida coast, the Gulf Stream is closest to the eastern coast of the state. The warm waters of the Gulf Stream have significant impacts on the region's climate, marine ecosystems, and even navigation. It influences weather patterns, provides habitat for diverse marine species, and can influence ocean currents and ship routes.

The proximity of the Gulf Stream to the Florida coast makes it an important feature of the region, both ecologically and economically.

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The Greek war with Persia was a significant conflict that occurred between the Persian Empire and various Greek city-states in the 5th century BCE. Persia had a rich culture, strong governmental organization, and significant influence in the region.

The Persian Empire, under the Achaemenid dynasty, encompassed a vast territory and had a diverse and influential culture. Persia had a centralized government led by a powerful ruler, known as the Great King, and had established an efficient administrative system. They also exerted influence through their military might and tribute collection from conquered regions.

The Greeks, on the other hand, had several advantages that allowed them to resist the Persian Empire. Firstly, the geography of Greece, with its mountainous terrain and numerous islands, provided natural barriers that made it challenging for the Persians to deploy their forces effectively. Additionally, the Greeks displayed a remarkable sense of unity during the war, coming together despite their political differences to form a united front against the Persian invaders.

The Greeks also had superior naval tactics, demonstrated notably in the Battle of Salamis, where their smaller but more maneuverable ships outmaneuvered the Persian fleet. Furthermore, the Greeks possessed a strong sense of national identity and pride, valuing their independence and freedom. This motivated them to resist the Persian Empire's attempts at conquest and defend their way of life.

In combination, these factors contributed to the Greeks' ability to resist and ultimately repel the Persian Empire. The Greek city-states' strategic advantages, unity, naval tactics, and national identity played crucial roles in their successful defense against the mighty Persian Empire.

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When a stream is in a V-shaped valley running on bedrock, the stream is called an incised stream.

What are incised streams?An incised stream is a term that refers to a stream or river that flows through a channel that is significantly lower than the surrounding landscape. This may result from changes in the elevation of the land through tectonic or volcanic processes, as well as a stream or river eroding into the earth.

A V-shaped valley is typical of incised streams.Incised streams have a high energy level, which means they can erode the landscape quickly. They may be difficult to navigate, and can be dangerous if the water is flowing too quickly or the bedrock is unstable. Because of their ability to carve through the landscape, incised streams are often responsible for shaping canyons, gorges, and other distinctive geological features.

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