<span>those are Fjords
keep in mind, in </span>Scandinavia our j's are pronounced as y's
Because Antarctica was once connected to the rest of the continents. When Pangaea was together, Antarctica was on the bottom and eventually moved down as the rest of the continents were made.
Answer:
A. Canada
Explanation:
Canada and Greenland are both countries that are not the best ones when it comes to farming. If we have to choose between them which one provides better conditions and higher profit, then that would be Canada with no doubt. Even though the climate is a huge limiting factor for the farming in Canada, in its southernmost parts it is still possible for certain types of crops such as the barley, oats, wheat, and flaxseeds. The farms are not widespread though, and they are localized only at certain parts of the southern part of the country. Greenland, on the other hand, is a country where the farming is pretty much impossible for anything. The climate in Greenland is polar, with most of the island being constantly covered with ice. The temperatures are very low throughout all of the year, the soil is either nonexistent or very thin and poor, so the crops simply can not survive there, yet alone to bring in profit.
Answer:
(a) Lower densities and higher thermal gradient
Explanation:
Over pressured zones during penetrating are those zones where development liquid weight (higher than expected) surpasses the mud weight. These are liable for victories.
- The pore liquid substance in shales of the over constrained zone is higher than the ordinary compelled shales. That implies, the porosity of shales in over pressured zone is higher as well thus the thickness of the over forced zones are lower than the ordinary influenced shales.
- Because of the nearness of more liquids in the pores of an over constrained shale, the warmth produced because of penetrating behaviors gradually in over influenced shale than a shale in typical weight zones. Accordingly, warm inclination will be higher in over forced shales.
<u>Answer:</u>
<em>Climate in the temperate zone can vary widely due to mild to warm heating in the summer months.</em>
<u>Explanation:</u>
The deciduous timberland locales are presented to warm and cold air masses, which cause this region to have four seasons. <em>The temperature shifts generally from season to season with cold winters and sweltering, wet summers. </em>
With less directing impact from sea flows and more impact from tropical and polar enormous size mainland land air-masses they include progressively extraordinary temperatures in each particular season, <em>with summers getting as sweltering as those of subtropical or tropical atmospheres and winters as cold as in sub polar atmospheres.</em>
