Answer:
Demographers study the growth and decline of human populations, and urban planners plan for the futures of cities (e.g. electricity, water, and transportation needs). Demographers and urban planners would benefit from working together to help solve difficult problems in society and to help plan for the future. A demographer would be very helpful to urban planners as they plan for the future of a city. For example, an urban planner would want to have an idea of the population growth in the city, or of the average growth rate in other cities, when planning for the city's future transportation, water, and electricity needs. Demographers and urban planners are important to each other! They help each other plan for the future of society
Explanation:
Answer:
<h2><em><u>Figure</u></em><em><u> </u></em><em><u>D</u></em><em><u>:</u></em> </h2><h2><em><u>Amazon</u></em><em><u> </u></em><em><u>river</u></em></h2>
Explanation:
<em><u>The Amazon is considered the world's largest river</u></em> by volume, but scientists have believed it is slightly shorter than Africa's Nile.
The Brazilian scientists' 14-day expedition extended the Amazon's length by about 176 miles (284 kilometers), making it 65 miles (105 kilometers) longer than the Nile.
<em>Amazon river is located in South America </em>
Obstical mountains or great britian mountain
Answer: Adults in urban counties, long aligned with the Democratic Party, have ... About two-thirds or more in urban and rural areas say people in other types of ... for the data to be more easily linked among government data sources to analyze ... in urban (53%), suburban (58%) and rural (53%) areas
Explanation:
Answer:
B) The snow and ice you found are not a glacier, because glaciers must have deformation in the ice.
Explanation:
An important characteristic of glaciers is that they move. This is why they are sometimes likened to "rivers of ice." This movement is called glacial motion. There are four main types of ways in which glaciers move. The first one is basal sliding, which occurs when the entire glacier slides over its bed. The second one are glacial quakes. These generate fractional movements of large sections of ice. The third one is bed deformation, which is limited to some areas of sliding. Finally, the fourth one is internal deformation, which happens when the weight of the ice causes the deformation of ice crystals.
