The answer is;
The hanging wall rises above the footwall. This type of fault occurs due to compression tectonic movement that squishes the two crusts. This way the faulted section of rock shortens. This is the opposite of normal faults where the hanging wall falls below the footwall. This is due to extension tectonic movements that lengthen the faulted section.
Answer:
measuring the loss of ice in the nunavut region around the arctic circle
Explanation:
it is the closest country greenland with it's many frozen islands in nunavut
Answer:
The water has left the system before if could be measured.
Explanation:
Some of the water has flowed quickly along as surface runoff and through the river channel. Scientists would then missed the chance to measure this rainfall. Some water will have been absorbed by nearby vegetation. The vegetation then releases the water in a vapor state, to the atmosphere. This process is known as transpiration. Heat in the atmosphere causes evaporation and the water never joins the soil of groundwater to be measured as part of the water table.
Answer:
well there's so many factors influencing temperatures like we have clouds in a cloudless place the temperature will be low as the clouds will be absorbing the rays from the sun while in a place where we have no clouds the temperatures will be really high during the day and called in the light then we also have nearness to large water bodies places near large water bodies experience high temperatures while those that are far experience low temperatures we also have altitude places with high altitudes experience low temperatures while places with low altitudes experience high temperatures
True, A 'planar projection map' is helpful for sea navigation.
<u>Explanation:
</u>
A 'planar projection map' that shows the particulars of the globe in a flat surface projection. The pictures projected by the map are shown in rectangular-shaped. If any other map such as Cylindrical map is used then, the edges are not so perfect, they show distortion. With the help of all three coordinates, it shows a 3-D picture of the globe and its objects which can be considered almost as real as the actual object. They are also known as azimuthal projections and are mostly used in projecting polar regions.
