Describe how urban areas provide opportunities for people.

Use a case study of a city in a lower income country (LIC) or a newly emerging economy (NEE). (6 marks)

One powerful force that influences tides is gravity. Sir Isaac Newton outlined how ocean tides are caused by the sun and moon's gravitational pull on the earth's oceans in 1687. (Sumich, J.L., 1996).

The gravitational attractive force serves as the foundation for tide forces. The distance between two objects is typically more important than their masses when it comes to tidal effects on the Earth. As the cube of the distance from the tidal generating object, tide generating forces change inversely. Only the cube of the distance between the objects has any bearing on the variation of gravitational attractive forces (Thurman, H.V., 1994). The interaction between the sun, moon, and the oceans of the Earth demonstrates how distance affects tidal forces.

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Karekare Beach in New Zealand is located in the southern hemisphere.

Karekare is a tiny coastal community in West Auckland, New Zealand, located between the Waitkere Ranges and a sizable surf beach with black sand. It is situated 35 kilometres (22 miles) west of Auckland's downtown and south of Piha's larger beach.

It is located in the northern part of Whatipu, south of Piha, and west of the Centennial Memorial Park and Water Catchment Area, which together make up the majority of the native bushland Waitkere Ranges. The Company Stream, also known as Waiteahoaho in the past, and the Karekare Stream meet at Karekare Beach. Away from the beach, the Karekare Falls are situated.

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Karekare Beach is found in New Zealand in the southern hemisphere.

West Auckland, New Zealand's Karekare is a small coastal settlement sandwiched between the Waitkere Ranges and a huge surf beach with black sand. It is located south of Piha's main beach and 35 kilometres (22 miles) west of Auckland's city centre.

It can be found in Whatipu's northern region, south of Piha, and west of the Centennial Memorial Park and Water Catchment Area, which together make up the majority of the natural bushland Waitkere Ranges.

At Karekare Beach, the Company Stream—previously known as Waiteahoaho—and the Karekare Stream converge. Karekare Falls are located away from the shore.

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Type C Soils are defined as those that are submerged or have free-flowing water coming from them.

Cohesive soils that have a compressive strength of less than 0.5 tsf (48 kPa) are classified as Type C soils. Other Type C soils include submerged soil, soil from which water is easily seeping, soil that is unstable under water, and granular soils such as gravel, sand, and loamy sand. This category also includes material that is layered and sloping, with layers that drop into an excavation or have a slope of at least 4H:1V (4H:1V) or larger.

Submerged soils are soils that are saturated with water for long enough in a year to produce the oxidation-reduction processes that result in the following characteristic gley horizons:

'A' horizon with some oxidation

A zone that has been shrunk or mottled over time.

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Due to the increased availability of flat ground for cultivation and home construction, there is a significant concentration of people. The soils are quite fertile, making the region very fruitful for farming. Consequently, these plains are extremely densely populated areas of the planet.

A plain, sometimes called flatland, is a flat area of land with a layer of grass that often has little variation in elevation and is largely devoid of trees. Lowlands in valleys or at the foot of mountains, coastal plains, and plateaus or uplands are all examples of plains. Plains are usually abundant in water in the form of rivers or groundwater and thus agriculture is extremely productive there and that causes high population.

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The core of the earth is a hot, compact ball made primarily of iron. There are roughly 1,220 kilometers around it (758 miles).

The Earth's core is our planet's tremendously hot and dense interior. The ball-shaped core lies beneath the cold, brittle crust and the mainly solid mantle. The core is located around 2,900 kilometers (1,802 miles) below the Earth's surface and has a radius of roughly 3,485 kilometers (2,165 miles). The Earth is older than the core. Around 4.5 billion years ago, when Earth was originally forming, it was a uniform ball of hot rock.

The ball heated up even more due to radioactive decay and heat left over after planetary formation (the collision, accretion, and compression of space rocks). After roughly 500 million years, our young planet's temperature reached 1,538° Celsius (2,800° Fahrenheit), the temperature at which iron melts.

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Stanley Park is the largest urban park in Vancouver, BC, Canada

Answer: The distinction between "stock" and "batholith" is based on the area exposed at surface. A batholith has a exposed surface area of at least 100 square km, while a stock has an area of less than 100 square km

Explanation:

Sedimentary rocks are formed through the process of erosion, weathering, and sedimentation.

Erosion is the process by which rock, soil, and other materials are worn away and transported by natural forces such as wind, water, and ice. The materials that are worn away are called sediments.

There are different types of erosion, such as:

For example, sandstone is formed by the sedimentation of sand that has been worn away by erosion and transported by wind or water. Limestone is formed by the sedimentation of shells and other marine debris that has been worn away by erosion. Shale is formed by the sedimentation of mud and clay.

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National Geographic say "Erosion and weathering include the effects of wind and rain, which slowly break down large rocks into smaller ones. Erosion and weathering transform boulders and even mountains into sediments, such as sand or mud. Dissolution is a form of weathering—chemical weathering. With this process, water that is slightly acidic slowly wears away stone. These three processes create the raw materials for new, sedimentary rocks."

Answer:

Explanation:

Erosion and weathering transform boulders and even mountains into sediments, such as sand or mud. Dissolution is a form of weathering—chemical weathering. With this process, water that is slightly acidic slowly wears away stone. These three processes creacreatete the raw materials for new, sedimentary rocks.

Answer:  convergence plate

Explanation:

thats it

Answer:

The sun

Explanation:

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Periods of geological time are identified using index fossils. These fossils are "frequently encountered, widely distributed fossils that are limited in time span," according to the definition. If an index fossil is discovered in a particular layer, one can estimate the layer's age. The geological periods are established using index fossils.

In most cases, it is thought that these periods of time lasted for tens of millions of years. The "geological column," which arranges the periods in chronological order, is made up of the geological eras. Whether the "geological column" actually exists or is just a product of our interpretation of the distribution of fossils is a matter of debate. The geological column is said to be real and represents the order in which different life forms existed in the past since the geological eras always, or almost always, show in the correct sequence in the fossil record, even though some periods may be missing in some places. But this is a circular argument. By employing index fossils to establish the geological periods, it is possible to ensure that the resulting geological periods occur in the correct order.

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Isolated farmsteads in the United States evolved as a result of colonization by individual pioneer families, agricultural private enterprise, government land policy, and physical barriers preventing communal farm practice. The one exception is political stability.

Isolated farmsteads, found mainly in the United States, were originally developed in response to the lack of resources and basic infrastructure in early colonial times. In order to survive and remain self-sufficient, many of these homesteaders had to become adept at farming, hunting, and living off the land. To do this, they had to deforest the land and create fields for planting crops and pastures for raising animals. Over time, these homesteaders developed distinct architectural styles, such as timber framing, which allowed them to build large, durable homes and other structures. They also developed specialized techniques, such as stone wall construction, which allowed them to use the natural resources around them in order to survive and thrive. As technology advanced, farmsteads began to become connected to small towns and large cities, which provided access to resources, markets, and opportunities. However, many farmsteads still remain isolated, providing an excellent example of the hard work and ingenuity of the early American pioneers.

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Answer:

A net torque produces a change in angular momentum that is equal to the torque multiplied by the time interval over which the torque is applied.

Explanation:

Hope it helps:)

Newton's laws of motion can be used to solve motion problems in a variety of situations. Multiple force vectors acting in different directions on an object are present in some problems.

Newton's laws of motion are three fundamental classical mechanics laws that describe the relationship between an object's motion and the forces acting on it.

These laws specify how things move or stay still. Newton's laws govern how cars work, how water flows, how buildings stay standing, and how everything around us moves.

Therefore, Newton’s Laws apply to various situations.

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The magnetic field that surrounds the Earth is produced by the movement of molten iron in the earth's core.

You could argue that Earth's "magnetic" personality is the envy of her interplanetary neighbors among the four rocky planets in our solar system. Earth is encircled by a powerful magnetic field known as the magnetosphere, in contrast to Mercury, Venus, and Mars. Our magnetosphere, which is created by strong, dynamic forces at the core of our planet, protects us from cosmic rays from beyond the solar system, coronal mass ejections (massive clouds of energetic and magnetized solar plasma), and solar wind, which constantly spews charged particles at us and erodes our atmosphere.

The majority of this undesirable energy that is hazardous to life on Earth is trapped in two regions with the shape of doughnuts called the Van Allen Belts by our magnetosphere, which acts as a gatekeeper by resisting it. The magnetic field, which is produced by the movement of molten iron in the Earth's core, shields the globe from cosmic radiation and charged particles from the Sun. It also serves as the foundation for compass navigation.

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Speciation most likely occurs in leopard frogs through reproductive isolation that occurred through behavioral isolation.

The process of evolution is speciation. Populations expand and evolve into new species during this process. Numerous theories exist regarding how speciation took place. The majority of them rely on the beginning of reproductive isolation as well as geographic isolation.

Behavioral isolation is one type of speciation that eventually results in reproductive isolation. This type happens when two populations with the potential to breed with one another choose not to do so (breed) because of the disparity in their courtship customs.

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Ocean trench refers to the deep depression on the ocean floor. Long, narrow depressions on the seafloor are known as ocean trenches.

These chasms are among the deepest natural places on Earth and the deepest portions of the ocean. Every ocean basin on the planet has ocean trenches, but the deepest ones encircle the Pacific Ocean as part of the so-called "Ring of Fire," which is also home to active volcanoes and earthquake-prone regions. Tectonic activity, which refers to the movement of the Earth's lithosphere, is what causes ocean trenches. Ocean trenches in particular are a characteristic of convergent plate borders, which occur where two or more tectonic plates collide. In a process known as subduction, dense lithosphere melts or slides beneath less dense lithosphere along numerous convergent plate borders, forming a trench.

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Answer:

Explanation:

The nations of Nigeria and Niger are named after the river. The people who live along it have a variety of names for it, notably Jeliba in Manding, Isa Ber ("big river" in Songhay), Joliba (a Mandigo word meaning Great River), and Kworra or Quorra.

The Himalayan Mountains are a great example of a continental-continental convergent plate boundary, where two slabs of continental crust impacted, compressing and raising the acretionary wedge material to create the mountains.

A convergent plate barrier between the Indian and Eurasian plates is where the Himalayan Mountains developed. India used to be a sizable island equivalent in size to modern-day Australia. The Indian plate started to move northward toward the Asian section of the Eurasian plate about 225 million years ago. Around 50 million years ago, it slammed into the Eurasian plate, and it still exerts considerable pressure against the larger plate. The Himalayan Mountains were created by collision, but the Indian plate's continuous impact as it advances north continues to shape the mountains today. The mountains grow by about 2.4 inches (6.1 cm) every year on average.

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Scandinavia shares a similar latitude with Europe and North America.

Scandinavia is located in the Northern Hemisphere, specifically in the high-latitude region known as the boreal zone. This region is characterized by long, cold winters and short summers, as well as a relatively low level of solar radiation.

The countries of Norway, Sweden, and Denmark are located at a similar latitude as other northern regions in Europe, such as Finland and Russia, as well as regions in North America, like Alaska and Canada. Because of this similar latitude, these regions experience similar weather patterns and have similar ecosystems.

For example, boreal forests, tundra and glaciers are common in these regions. However, it's important to note that the proximity of the sea, the presence of the Gulf Stream and the local topography can affect the weather and temperature conditions, making some areas milder than others.

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Answer:

Explanation:

Scandinavia shares a similar latitude with Europe and North America.

Scandinavia is located in the Northern Hemisphere, specifically in the high-latitude region known as the boreal zone. This region is characterized by long, cold winters and short summers, as well as a relatively low level of solar radiation.

The countries of Norway, Sweden, and Denmark are located at a similar latitude as other northern regions in Europe, such as Finland and Russia, as well as regions in North America, like Alaska and Canada. Because of this similar latitude, these regions experience similar weather patterns and have similar ecosystems.

For example, boreal forests, tundra and glaciers are common in these regions. However, it's important to note that the proximity of the sea, the presence of the Gulf Stream and the local topography can affect the weather and temperature conditions, making some areas milder than others.

Seasons develop as a result of the tilt of the Earth's axis, which is around 23.4 degrees, and the fact that some areas of the planet receive more solar radiation than others.

Our planet orbits the Sun on a slant due to Earth's axial tilt (obliquity), which causes different parts of Earth to face the Sun in different directions at various times of the year.

The Northern Hemisphere receives more of the Sun's direct rays during the June solstice because the North Pole is inclined toward the Sun. Because of this, the Northern Hemisphere's summer months are June, July, and August.

Winter is created during the months of June, July, and August when the Southern Hemisphere is pointing away from the Sun at the same time. When the South Pole is tilted toward the Sun and the Northern Hemisphere is slanted away, the Southern Hemisphere experiences summer in the months of December, January, and February.

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Gas giants have the feature of rings that terrestrial planets do not. Thus, option B is correct.

Terrestrial planets are Earth-like planets comprised of rocks or metals with a really hard surface. A molten heavy-metal core, a dearth of moons, and topographical features like valleys, volcanoes, and craters are further characteristics of terrestrial planets.

Mercury, Venus, Earth, and Mars are the four terrestrial planets in our solar system that are also the ones that are closest to the sun. There may have been more terrestrial planetoids during the creation of the solar system, but they either combined or were obliterated.

All of the terrestrial planets in the Solar System share the same fundamental structure, which includes a central metallic core made primarily of iron and a surrounding silicate mantle.

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Medieval society was organized according to a "three-class system", divided into three social orders:

The history of the Middle Ages in European history is the history from the 5th century AD to his 15th century. The Middle Ages began with the fall of the Western Roman Empire and continued until Europe plunged into the Age of Renewal and the Age of Discovery.

Western history is traditionally divided into her three periods: ancient, medieval, and modern. In other words, medieval history is a period of transition from antiquity to modern times. Medieval history is divided into his three periods: the Early Middle Ages, the High Middle Ages and the Late Middle Ages.

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The two peace agreements that were signed in October 1648 in the Westphalian cities of Osnabrück and Münster are collectively known as the Peace of Westphalia.

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Answer:

The inner core is solid, the outer core is liquid, and the mantle is solid/plastic