why is factfulness useful for geographers to study?

During the Industrial Revolution, which took place in the 18th century, scientific and technological advancements led to the industrialization of rural, agrarian cultures, particularly those in Europe and North America.

The Industrial Revolution began in earnest in Britain in the 1830s and 1840s, but certain improvements were created as early as the 1700s.

It quickly expanded to the rest of the world, including the United States. Modern historians frequently refer to this period as the First Industrial Revolution to distinguish it from the second phase of industrialization that occurred from the late 19th to early 20th century and witnessed tremendous advancements in the steel, electric, and car industries.

Beginning in the middle of the eighteenth century, inventions like the spinning jenny (a wooden frame with numerous spindles), the flying shuttle, the water frame, and the power loom greatly simplified the process of weaving cloth and spinning yarn and thread.

Cloth production became more time and labor-efficient and required much less human labor.

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Answer:

My answer: Both countries are leading agricultural and industrial nations because of their wealth of resources.

Explanation:

My answer: Both countries are leading agricultural and industrial nations because of their wealth of resources. The United States and Canada possess ample water resources, a immense amount of land, fertile soils, large forests. and valuable deposits of iron ore, nickel, copper, gold, silver, and uranium. Both countries also have substantial deposits of coal, natural gas, and oil, and well-developed networks for distributing these energy-producing fossil fuels.

The population of Japan is spread out very differently. Due to the country's hilly terrain, the population has been forced to congregate in the few plains and lowlands, particularly around the Pacific coast.

Thus this is about Japan's population and life in slums.

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Nuclear power generated 16.8% of the electricity produced by Major Power Producers, coal contributed 2.5%, and renewable energy generated 39.9%, matching the amount produced by gas.

Energy that is derived from resources that can be regenerated naturally over time and are therefore considered to be renewable. It includes energy sources like sunlight, wind, water currents, and geothermal heat.

Energy that is produced using renewable resources won't run out. They are organic, self-renewing, and often leave no or very little carbon imprint.

Wind, sunlight, bioenergy (organic matter burned as fuel), and hydroelectricity, including tidal energy, are a few examples of renewable energy sources.

Solar energy, wind, falling water, geothermal heat from the soil, biomass from plants, waves, ocean currents, temperature variations in the oceans, and tide energy are all examples of renewable resources.

Producing energy from fossil fuels with no greenhouse gas emissions while lowering some forms of air pollution increasing energy supply diversity and decreasing reliance on imported fuels. Fostering economic growth and employment in manufacturing, installation, and other fields.

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In cross-sectional view, they show cross beds of sand is the statement about sand dunes which is true .

What is Sand dunes ?

Sand that has been moved by wind or water forms dune landforms. Usually, it resembles a mound, ridge, or hill. A dune system or dune complex is a region having dunes. A huge dune complex is referred to as a dune field, whereas ergs or sand seas are vast, flat areas covered with wind-blown sand or dunes with little to no vegetation. Although dunes come in a variety of sizes and forms, most dunes have a longer stoss (upflow) side where sand is forced up the dune and a shorter slip face on the lee side. A dune slack is a valley or dip between dunes.

The environments with the highest density of dunes are deserts, where a lack of moisture prevents the growth of vegetation that would otherwise obstruct the formation of dunes. Sand deposits, however, are not only found in deserts; dunes can also be found along seashores, by semiarid climate streams, in glacial outwash basins, and in other places where poorly cemented sandstone bedrock crumbles to produce a plentiful supply of loose sand.

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The highlighted features are as follows:-

The majority of the Tarim Basin is made up of the Taklamakan Desert. Due to a variety of circumstances, rivers that cross the desert frequently disappear in the middle of the desert. These include significant river water loss due to excessive evaporation and water infiltration through porous sand particles. Additionally, because the river depends primarily on water from glacier melt, its volume is fairly low and it is easy for it to vanish in the desert.

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Based on the meaning of the two terms, the best explanation that can be given about the relationship between the physical landscape and cultural diffusion is the physical landscape is one of the features that attracts a person to migrate to a place which in turn enables him to spread his culture to his host nation, through cultural diffusion.

This refers to the term that is used to describe and define the movement of culture from its place of origin to other places through forces of migration that allows others to "borrow the culture" and make use of it.

Hence, we can see that in terms of physical landscapes, this is a major factor that can allow people to migrate to a new place, which in turn enables them to share their culture to others.

With this in mind, we can see that the correct answer to the given question has been given above.

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H2o co2 and h2co3 help in the dissolution of limestone.

How does humid climate affect limestone?

Limestone's aesthetic appeal and structural integrity may be harmed by weathering. Rain, snow, temperature, wind, and air pollutants are all factors. Typically, these elements work together or in conjunction with other degradation agents.

Rainwater, especially when combined with air chemicals that frequently produce acid rain, can cause the limestone to dissolve, increasing the amount of salt that moves inside the stone building.

Temperature has an impact on salt migration patterns within the stone as well as rates of disintegration and (in bigger stones) movement of the fragments. Most of the inherent or natural issues that might arise with limestone require some level of moisture, although some issues like wind erosion and vandalism can arise on their own.

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Hard engineering is a coastal management technique used to protect coasts, by absorbing the energy of waves, preventing erosion and flooding. They are highly visible man-made structures used to stop or disrupt natural processes

Soft engineering is where the natural environment is used to help reduce coastal erosion and river flooding. At the coast, soft engineering is where a beach is used to absorb wave energy and reduce erosion. Through hard coastal protection strategies, we try to work against natural interactions in order to protect certain eras. Soft coastal protection strategies are methods to secure and/or restore coastal lines through a body of sand. The other option, soft Engineering, involves using natural defences to protect the coastline.

The movement of the plates is primarily responsible for earthquakes and volcanoes, particularly when plates collide at their edges or borders.

Why do most deep earthquakes occur at subduction zones ?

Deep earthquakes—those that occur at least 300 kilometers below the surface—rarely result in physical harm but are frequently sensed globally. These earthquakes can offer crucial hints for comprehending plate tectonics and the internal structure of the Earth. Deep earthquakes probably result from different physical and chemical processes than earthquakes at the surface because of the extraordinarily high temperatures and pressures below. However, as it is challenging to acquire data on deep earthquakes, scientists do not have a clear theory as to why they occur.

In order to comprehend the dynamics governing plate tectonics, Billen creates numerical simulations of subduction zones, when one plate descends beneath another. Her new research demonstrates that deep earthquakes frequently occur in areas of "high strain" where a sinking tectonic plate bends and folds, helping to explain the distribution of deep earthquakes.

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Oceanic-oceanic convergence is shown in Diagram B. These plates generate a deep marine trench. In the ocean, parallel to the trench, volcanoes can potentially develop.

What are the convergent boundaries?

Different plates on our planet interact with one another, move past one another, and pull apart from one another. There are several diverse plate borders, breathtaking scenery, and perilous perils as a result of these motions between the plates. In general, there are three different types of plate contact. Convergent borders are the first of them, which we shall examine below.

Two or more tectonic plates can move toward one another at convergence borders. The two tectonic plates are squeezed or pushed together during the convergence process by compressional stress. Mountain chains are most frequently recognised to be formed by convergent boundaries. Earth has seen periods of supercontinent creation, during which the continents as we know them now were once combined into one landmass, as a result of tectonic plate collisions. Supercontinents used to exist more than 250 million years ago, and one well-known example is the ancient continent of Pangaea.

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Which diagram shows an oceanic-oceanic convergent boundary? describe what occurs at this type of plate boundary

Part C of the following diagram shows an oceanic- oceanic convergent boundaries.

A convergent boundary is a spot-on Earth where two or more lithospheric plates collide. One plate will always slide under another during subduction. Ocean-ocean, ocean-continent, and continent-continent are the three different forms of convergent boundaries.

Oceanic-continental convergent borders are created when tectonic plates with primarily oceanic lithosphere collide with plates with primarily continental lithosphere.

Compared to the continental lithosphere, the crust is denser because it has more minerals rich in iron and magnesium. The oceanic lithosphere plate will buckle beneath the continental plate and plunge into the warm asthenosphere when these two very distinct plates intersect. Subduction is the term for this action. The melting occurs as the subducting plate is pushed further into the mantle. This generates magma, which rises and erupts. This creates an island arc, a line of volcanoes. Examples of island arcs include Japan, Indonesia, the Philippines, and the Aleutian Islands of Alaska.

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The quote that best supports the answer to Part A is option C. "It is well. I am as a last year's leaf, clinging lightly to the stem.... My eyes no longer show me the way of my feet, and my feet are heavy, and I am tired. It is well." (Paragraph 9).

Jack London demonstrated his naturalistic notion that instincts rule the human mind more so than sentiments or emotional ties in his novel "The Law of Life." Through the events and upbringing of the main character, his outlook on life, and the behaviors of his family members, he made this point clear.

The final five hours of Koskoosh, an elderly and ailing Inuit chief, are depicted in this short narrative. As a result of his tribe's need to move in order to find food and shelter, as well as his advanced age and impaired vision, he is left to perish.

Therefore, the themes of acceptance, mortality, connection, tradition, loneliness, struggle, and selfishness are explored in Jack London's novel The Law of Life.

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The Law of Life

By Jack London1901Jack London (1876-1916) was an American author, journalist, and social activist. He is best known for hisnovelsThe Call of the WildandWhite Fang. In “The Law of Life,” an old man is left behind by his tribe.Asyou read, take notes on how the author uses imagery and symbolism to portray nature.Old Koskoosh listened greedily. Though his sighthad long since faded, his hearing was still acute,1and the slightest sound penetrated to theglimmering intelligence which yet abode behindthe withered forehead, but which no longergazed forth upon the things of the world.

The long trail waitedwhile the short day refused to linger. Life calledher, and the duties of life, not death.  Part A: How does Old Koskoosh feel about being left behind.

Both the surface of the land and the ocean bottom contain per/mafr/ost. It may be found where it s/el/do/m gets above free/zing. As a result, perma/fro/st may be found often in Arctic locations including Green/land, and Ala/ska in the United States, Ru/ssia, Ch/ina, and Eastern Eur/ope.

Generally, On land or in the water, per/mafr/ost is defined as ground that has consistently remained below 0 °C for two or more years. Per/mafr/ost is most prevalent in the Northern Hem/is\ph/ere, covering about 15% of the Northern He/mis/phe\re or 11% of the Ear/th's surface, totaling about 18 million square miles.

An area of the Earth's surface that is permanently frozen is known as per/maf/ ro/st. It is often composed of ice holding soil, gravel, and sand together.

Both on land and below the surface of the ocean, you can find per/maf\ro/st.

It lives in places where the temperature does not typically rise much above freezing.

This indicates that the Arc/tic regions such as Green\land, the state of Ala/ska in the United States, R/ussia, C/hina, and Eastern Europe are likely places to find per/mafr/ost.

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Using the theories of loess, we got that from the Ohio river valley loess deposits in the U.S. mid west are derived.

Loess is classically viewed as the glacially derived sediment, leading to the view that loess deposits denote times of the increased glacial activity and the intercalated paleosols indicate the warmer interglacial or interstadial periods. However, the loess of the North America comes from both glaciogenic and the nonglaciogenic sources. The response of  different loess regions of the North America to glacial and interglacial conditions varies, with the timing of loess deposition depending on  interplay between various factors including the climatic conditions, sediment supply, sediment source, and vegetation cover.

Hence, loess deposits in the U.S. mid west are derived from the Ohio river valley.

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The conquests of Alexander, who was born in Greece, included Anatolia, Syria, Phoenicia, Egypt, Mesopotamia, Persia, Afghanistan, and India. His Macedonian Empire's borders were expanded all the way to Taxila, which is now in modern-day Pakistan.

Two separate empires under the ancient Babylonian rule coexisted in Mesopotamia at the time, with Babylon serving as their capital. These two empires ruled the area from the 19th to the 15th century BC and again from the 7th to the 6th century BC.

Because it was constructed along both banks of the Euphrates river, the city had high embankments to control the river's yearly floods. The ancient city's site is close to Baghdad in the present day.

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Answer:

Inland drainage refers to the drainage system where the streams of the rivers do not meet into an ocean or a sea instead they empty their waters in an Inland ocean or a lake.

Explanation:

The east coast of United States is at high risk because of the presence of barrier islands, low elevation lands and gentle slopes of the coast.

The west Antarctic Ice sheet is collapsing at a faster rate due to the effect of Global Warming. This causes the ice to melt and an increase in the water level of the oceans and other water bodies. The east coast of the United States mainly comprises of the Atlantic Ocean and with the Atlantic Ice sheet melting it is the most vulnerable coast. The sea level if risen to an altitude greater than what is elevated then the people of the east coast will suffer. The presence of islands within the east coast which are called the barren islands provide the seawater a path to travel in the cities. Also, the area of the east coast is at a lower elevation, and this will provide no blockage to the rising seawater from flooding the cities. The slopes towards the coast are also gentle and not steep which will pave way for the seawater. All these reasons make the east coast most vulnerable.

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Answer:

The lakes—Superior, Michigan, Huron, Erie, and Ontario—are located in east-central North America and provide a natural border between Canada and the United States

Answer:

it is NOT answer D, Increased population demands increase groundwater withdrawals every year regardless of precipitation.

Explanation:

just dont want others to get it wrong like I did :c

Answer: C) Fluctuations in groundwater withdrawals are not in response to increases in population growth.

Explanation:

A) couldn't be right because, in the graph, groundwater withdrawal was only increasing up until 1980, and then it started steadying and fluctuating.

B) claims that groundwater withdrawals decreased, which isn't supported by the graph either.

D) isn't true either, because there is clearly a stop in groundwater withdrawals increasing around 1980-1985.

The restricted basin which has the coolest temperatures is Hudson Bay.

Hudson Bay, a constrained basin,  is completely or mostly covered in ice around the summer solstice and for much of the high sun season. The climate in this basin is severely continental.

Nearly the entire bay has average yearly temperatures of 0 °C (32 °F) or lower. Winter weather lows in the extreme northeast can reach 29 °C or 20.2 °F. The average temperature in this basin's region is extremely low throughout the year.

By early November, this basin begins to freeze, and by the end of the month, the northern portion of the basin is usually completely covered in ice.

Therefore, the correct answer is Hudson Bay

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Uniformitarianism is the name of the theory

What is Uniformitarianism?

The theory of uniformitarianism was developed by Charles Lyell in the 19th century and is based on the writings of James Hutton. According to Uniformitarianism, the forces and processes that can be seen at the surface of the earth are the same ones that have sculpted the planet's terrain throughout natural history.

Erosion, deposition, compaction, and uplift are the four processes that are mentioned above as sculpting the ground. These processes happen at incredibly slow rates even though they are constant. Hutton, a farmer, understood that erosion rates were so slow that it would take an impossibly long time to see significant changes in the Earth's landscape.

Furthermore, according to Uniformitarianism, these processes have continued throughout the course of nature. In 1his book Theory of the Earth, James Hutton states, "We find no evidence of a beginning - no hope of an end." The idea that the Earth must be so incredibly old that the mind cannot even begin to estimate its length was first put forth by Hutton.

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An upright open symmetrical fold forms, an inclined asymmetrical fold forms, an overturned fold forms, a recumbent fold forms, a thrust fault forms, a large-offset thrust sheet develops a nappe.

A rock sheet called Nappe is one that has been transported far from its initial location by tectonic pressures. A thrust sheet or similar block of rock that has moved more than 2 km from its original location as a result of tectonic processes is what is referred to as this phenomenon.

Tectonic movements: what are they?

According to the widely recognised scientific hypothesis known as plate tectonics, the Earth's lithosphere is made up of many sizable tectonic plates that have been steadily moving for nearly 3.4 billion years.

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Answer:

Karst features

Explanation:

Karst features are created by solutional erosion below the surface in areas underlain by soluble rock such as limestone and gypsum. These features include sinkholes, dolines, springs, and caves.

Answer:

The two most important factors in the climate of an area are temperature and precipitation. The yearly average temperature of the area is obviously important, but the yearly range in temperature is also important. Some areas have a much larger range between highest and lowest temperature than other areas.

As a result, they decided to lower the water level by 5 meters per year. This is an illustration of mitigation.

Planning and zoning, floodplain protection, land purchase, relocation, and public awareness campaigns are examples of mitigation efforts. Installing catastrophe warning systems, acquiring radio communications equipment, and undertaking emergency response training are examples of preparedness steps.

Hazard-specific control efforts, such as flood levees or bushfire mitigation methods, are examples of mitigation strategies. design infrastructure or service enhancements Decisions on land use planning and design that prevent developments and community infrastructure in hazardous places. Hazard mitigation planning lessens the effect of disasters, hence reducing loss of life and property.

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Answer:

the red river

The deuterium isotopes in cometary water differ from those in water on Earth. This is further supported by the discovery of two 4.5 billion year old meteorites that contained liquid water along with a wide variety of deuterium-poor organic molecules.

The deuterium to hydrogen ratio on Earth today is also consistent with the age of eucrite chondrites, which come from the asteroid Vesta in the outer asteroid belt. Both asteroids and comets are solid celestial entities that were created 4.5 billion years ago during the early solar system. Asteroids are rockier and only found in the Asteroid Belt (between Mars and Jupiter). On the other hand, comets, which originate from the outer solar system, are rich in water ice and other volatiles. The current preferred theory for how the Earth got its water is that it obtained it from elements (planetesimals) rich in water that comprised up a small portion of its building components. These planetesimals with abundant water would have either been comets or asteroids. It has been said that these are "dirty snowballs." They could provide crucial hints about how our solar system formed. The early Earth and other regions of the solar system may have received water and organic compounds from comets.

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In the colonized nation, the sphere of influence would cause the colonists in the area to lose the resources that they have to their colonizers.

In the colonizing economy, they would grow and have more resources from the ones that they take from these nations.

In international politics, sphere of influence refers to a state's assertion of exclusive or predominate control over a foreign region or territory. The word could relate to a formal pact by which another state or states promise themselves to refrain from interfering inside the sphere of influence, or it could refer to a political claim to exclusive control that other nations may or may not acknowledge as a matter of fact.

The fact that the word initially became popular in the 1880s, when the colonial expansion of the European powers in Africa and Asia was about to come to an end, has legal relevance. The effort of the major colonial powers to continue their mutual competition for colonies through established procedures was a defining feature of that expansion's final phase.

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