How the exploration of the world by Europeans changed the spatial conception of the world and how this is reflected in cartographic representations?

Answer:

Unitary

Explanation:

Answer:

d

Explanation:

trust me

Answer:

Because they needed the water. And they needed the fish in the water.

Explanation:

Answer:

The Antarctic Peninsula is probably Antarctica’s most prominent geographical feature and is home to scientific stations operated by the United States, the United Kingdom, France, Australia and other nations. This curved extension of the continent extends nearly 250 miles north of the Antarctic Circle and points toward the southern tip of South America. The Antarctic Peninsula has a number of glaciers and large floating ice shelves that are changing rapidly because this part of Antarctica is warming faster than the rest of the continent.

Running along the length of the peninsula, and extending across the continent is a mountain chain known as the Transantarctic Mountains. In addition to supplying spectacular views, the Transantarctics serve as a sort of dividing line across the continent, separating East and West Antarctica.

A view of the Transantarctic Mountains  during IceBridge's 2013 Antarctic campaign.

A view of the Transantarctic Mountains during IceBridge’s 2013 Antarctic campaign.

Although the Antarctic Ice Sheet is a continuous mass of ice, but it is sometimes helpful to think of it as two separate masses known as the West Antarctic and East Antarctic ice sheets, which are separated by the Transantarctics. Ice on the west side of this line flows west, while the opposite happens east of the divide.

East Antarctica is considerably larger than West Antarctica. The ice sheet covering East Antarctica is thick – nearly three miles (five kilometers) thick in some regions – and its surface is high and home to some of the coldest and driest condition on Earth.

The East Antarctic Ice Sheet is also considered more stable than the West Antarctic. One reason for this is the shape and elevation of bedrock beneath the ice. Heavy masses of ice push down on bedrock, depressing areas in the central part of the ice sheet below mean sea level. If those low-lying areas happen to be near the edge of the ice sheet, which is the case in large parts of West Antarctica, then ocean water can make its way under the ice, speeding up glacier flow.

This is one of the reasons that while both portions of the ice sheet are losing mass, West Antarctica is moving much faster. Recent studies of West Antarctica found that many of the large, fast-moving glaciers there are in an irreversible decline.

sea ice shadow

Shadow of the NASA DC-8 on sea ice in the Weddell Sea. Credit: NASA / Jim Yungel

And while Antarctic land ice is shrinking, sea ice around the continent has been on the rise in recent years. Antarctica is surrounded on all sides by the Southern Ocean. During the winter, ocean water freezes, forming a layer of sea ice of roughly the same area as the Antarctic continent.

The ocean around Antarctica is divided into several seas. Starting to the right of the Antarctic Peninsula on the map above is the Weddell Sea, which extends to Cape Norvegia, a small point of land jutting off of East Antarctica. Moving clockwise we go around the East Antarctic coast all the way to the Ross Sea, south of New Zealand. Next comes the Amundsen Sea, which large West Antarctic glaciers like Pine Island and Thwaites drain into. And continuing on, we complete our trip around Antarctica, coming to the Bellingshausen Sea to the left of the Antarctic Peninsula.

For maps of Antarctica, including some that use imagery from the Landsat satellite, visit:

http://lima.usgs.gov/download.php

To use an interactive Antarctic atlas, visit:

http://lima.usgs.gov/antarctic_research_atlas

Explanation:

What first attracted European explorers to the Pacific Islands

Explanation:

Answer:

A. Choosing a loan with a compound rather than

Answer:

Explanation:

hiii LATIFAA

Here are some characteristics of a volcano and the type of information they provide for assessing potential hazards:

1. Volcano type: The type of volcano (shield, stratovolcano, cinder cone, etc.) can give an idea of the eruption style and frequency, as well as the type of magma being erupted.

2. Volcanic history: Studying the past eruptions of a volcano can help identify patterns and potential future hazards. This includes the frequency and magnitude of eruptions, as well as the types of volcanic activity (e.g. lava flows, ash plumes, lahars).

3. Volcanic gases: Monitoring the gas emissions of a volcano can give insight into the magma composition and potential for explosive eruptions.

4. Seismic activity: Tracking earthquakes and other seismic activity around a volcano can help identify changes in magma movement and potential eruption triggers.

5. Geographical location: The location of a volcano can impact the potential hazards associated with an eruption, such as proximity to populated areas or critical infrastructure.

By studying these characteristics, scientists and authorities can assess the potential hazards of a volcano and develop appropriate mitigation and response plans.

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In the middle of the ocean basin

Explanation:

Fist, the forces acting on the plate are tensional force which act away from each other.

When these forces act away from each other, they cause the place of their origin to stretch hence creating a new feature

 At the boundary where the two plates are pulling apart indicates a place where new plate material is forming. The appropriate response is option C.

When two tectonic plates diverge, a divergent boundary is created. As magma (molten rock) rises from the Earth's mantle to the surface and solidifies to form new oceanic crust, earthquakes frequently occur along these borders.

An area where two plates converge is referred to as a convergent boundary . The borders of one or both colliding plates may bow up into mountain ranges as a result of the impact, or one plate may bend downward into a deep undersea trench.

A transform plate boundary is created by two plates moving past one another. The undersea San Andreas fault zone is one of the most well-known transform plate boundaries.

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Answer:

Age and Genders

Explanation:

It is used by demographers, who study the population study. A population pyramid is a graph that shows the distribution of ages across the population between male and female of population.

A narrow strip of land that connects two larger land masses and separates two water bodies is called an Isthmus.

Since Isthmus lies at the connecting point of two large landmasses, its strategic location makes it ideal for setting up ports, canals, military camps, stations, etc. A natural outcome of such structures would be enhanced communication, exchange of knowledge, culture, and robust trade through this connection.

Some examples include the Isthmus of Panama which links continents of North and South America and separates the Pacific Ocean from the Atlantic Ocean. The Isthmus of Suez links the continents of Asia and Africa and separates the Red Sea from the Mediterranean Sea.

Both the above-mentioned Isthmus are expeditors of large-scale trade across the world. About 14,000 ships cross the Panama Canal between the Atlantic and Pacific Oceans every year.

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Answer:

lack of pollution controls in Eastern Europe before 1989

Answer:

A lack of pollution controls in eastern Europe before 1989

Based on the concept of Experimental procedures and the information given in the question, the correct pairs include: Raya measures the growth rate of plants = Dependable variable.

The experimental procedure is a term that is used to describe the specific techniques utilized in performing a particular experiment.

Generally, the experiment procedures are divided into four major elements which include manipulation, control, random assignment, and random selection.

In this case, the experiment component goes thus accordingly:

Hence, in this case, it is concluded that Raya followed different steps and applied various components to her experiments.

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A saturated, spongy, and impermeable layer or stratum is what the phrase defines as an aquifer.

An aquifer is a rock that contains water and easily transports it to wells and springs. The aquifers can be penetrated by drilling wells and then filled with water. Rainfall replenishes the aquifer's permeable sandstone with water over time.

Stormwater, which is produced by precipitation and snowmelt, seeps into the earth until it reaches layers of rock formation, where it is trapped and stored underground, filling aquifers. The permeable rocks of aquifers are refilled by rainwater that seeps into the soil.

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Answer:

either A or B, leaning towards B

Explanation:

Answer:

Gulf of Mexico

Explanation:

The Gulf Coast of the United States is the coastline along the Southern United States where they meet the Gulf of Mexico. The coastal states that have a shoreline on the Gulf of Mexico are Texas, Louisiana, Mississippi, Alabama, and Florida, and these are known as the Gulf States.

Answer:

No

Explanation:

Answer:

No. i. dont think it their is any hutrricanes

Answer:

The environment is not dependant on humans

Explanation:

Although the environment is needed for us to survive we constantly affect it in an adverse fashion. We tend to pollute the same resources that keep us alive, such as air and water systems. Sadly we are making irreversible changes to our environment and it should stop. However, these decisions need to be made by people with the power to make good in the world.

Answer:

Gymnastics is thought to have began in ancient Greece about 2500 years ago where it was used in training to keep fit for sporting activities. In the Greek city of Athens, gymnastic tournaments were held, including tumbling, rope climbing, and other similar activities. The gymnasium was the hub of cultural activity.

Hope that helps. x

Answer:

=> Gymnastics is thought to have began in ancient Greece about 2500 years ago where it was used in training to keep fit for sporting activities.

=> The gymnasium was the hub of cultural activity.

=> In the Greek city of Athens, gymnastic tournaments were held, including tumbling, rope climbing, and other similar activities.

=> Modern gymnastics began in Germany in the 1800s.

Answer:

all of the above

Explanation:

all 3 countries border the pacific ocean but most countries a connected to an ocean or sea so all over the world is most logical

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 coast of Greenland, and the bottom picture from Bear Meadows Natural Area in central Pennsylvania, are geologically related. As The Greenland picture shows rocks that have been creeping downhill on perma-frost, and Bear Meadows probably was formed when such a creeping mass dammed a stream during the ice age. Option A is the correct answer.

The gradual, downward movement of rock and soil down a low grade slope is known as downhill creep, sometimes referred to as soil creep or simply creep. It can additionally refer to the gradual deformation of these materials brought on by sustained pressure and stress. Option A is the correct answer.

Despite giving the impression of continuous motion to the observer, creep is actually the accumulation of several little, discontinuous motions of slope material brought on by gravity. A very, very slow type of mass waste is soil creep. If you can't see the consequences of the movement, it's merely a steady adjustment of rocks and dirt that is very difficult to observe. Fenceposts that are misaligned are one example of these impacts.

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The complete question is, "The top picture from the coast of Greenland, and the bottom picture from Bear Meadows Natural Area in central Pennsylvania, are geologically related. How?

A) The Greenland picture shows rocks that have been creeping downhill on perma-frost, and Bear Meadows probably was formed when such a creeping mass dammed a stream during the ice age.

B) The Greenland picture shows the tracks of glaciers, and a glacier hollowed out Bear Meadows.

C) The Greenland picture shows where a fast landslide went through, and Bear Meadows was formed when a fast landslide dammed a stream.

D) The Greenland picture shows where a fast landslide went through, and Bear Meadows was formed when a fast landslide ran down a hill, leaving a hollow behind that filled with water to be come Bear Meadows."

B. The size of the fossils is relevant to fossilization because the bigger the organism is in mass and volume, the easier it is to fossilize.

This is because larger organisms are more likely to leave behind hard, durable remains that are resistant to decay and can be preserved over time. However, it's important to note that the size of the organism is not the only factor that determines fossilization and smaller organisms can also be preserved under certain conditions. Ultimately, the process of preservation is complex and depends on a variety of factors including the type of organism, the environment it lived in, and the conditions under which it died and was buried.

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Answer:

Punjab

Explanation:

being the most conducive for cotton production, produces around 70% of country's cotton followed by

Answer:

river

Explanation:

water is represented by blue on the map and it is also a boundary feature used to divide continents.

Explanation:

ok ok ok ok ok ok ok ok. ok 7

Answer:

Urban renewal is a program of land redevelopment often used to address urban decay in cities.

Explanation:

Urban regeneration happens when an urban area is upgraded. The aim is to improve both the economic and social spaces within a city. This usually takes place when areas of dereliction, pollution or brown-field spaces are restored or the area is used for new purposes.

The feedback loop that best describes the example of the melting of sea ice due to increased atmospheric temperatures on earth is positive feedback loop.

A feedback loop is defined as a system process where the output is fed back to the input. Feedback loops are two types: positive feedback loops and negative feedback loops.Positive feedback loopIn a positive feedback loop, the system output is magnified to increase its input signal. This type of feedback loop leads to a snowball effect where a small change in the system output results in an amplified effect.

Positive feedback loops occur when a change in an environmental condition amplifies or increases an initial process or change. The best example of a positive feedback loop is the melting of sea ice due to increased atmospheric temperatures on earth. In this example, human activities, such as the burning of fossil fuels, initially increase atmospheric temperatures on earth.

As a result, arctic ice begins to melt. As the white, reflective ice disappears over time, more of the darker ocean water is exposed, absorbing more and more heat. This further increases, or amplifies, atmospheric temperatures, ultimately causing more arctic ice to melt. The loop will continue to run and amplify the initial change in the system, which is the increase in atmospheric temperature.

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Answer:

The three remaining major languages of Subsaharan Africa are Swahili, Lingala, and Zulu.  

Explanation:

Answer:

none, there is no dominant language

Explanation:

I just had this question and got it right

Answer:

trondheim

Explanation:

it has played such an important role in norway's history

The history of Norway includes an intriguing role for Trondheim. In actuality, Trondheim served as Norway's first capital. Olav Tryggvason, a Viking monarch, built the city in 997, and it remained Norway's capital for 200 years.

Early in the thirteenth century, Bergen progressively replaced Trondheim as the capital of Norway (then known as Nidaros).

After being created as a capstan or trade post by Harald Hardrada in 1048, Oslo was built as a city at the conclusion of the Viking Age in 1040 under the name nalo. In 1070, the city was made a bishopric, and in the early 1300s, Haakon V of Norway made it his capital.

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Based on the information given, it can be deduced that the reliable paleoclimate record was about 800,000 years ago.

Paleoclimatology simply means the study of the climate of the Earth. It's the study of climates where direct measurements were not taken.

It should be noted that the reliable paleoclimate record from the Antarctic and Greenland ice cores provides information back to approximately 800,000 years ago.

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A continent could be struck by oceanic crust. Since the oceanic plate is denser, subduction occurs. This indicates that the oceanic plate is settling beneath the continent. This happens in an ocean trench.

A convergent border occurs when two plates move in the same direction. The oceanic plates will always subduct beneath the continental crust when two oceanic plates meet because the oceanic crust is naturally denser. Greater earthquakes and increased volcanic activity are frequently linked to convergent borders. When a subduction zone forms, the subducted plate eventually becomes partially melted and molten by the earth's interior magma (See Pic). By transferring heat upward and elevating the crust as a result of this melting, a volcano eventually forms.

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