The country in Europe that has marine west coast climate is Ireland
Explanation:
The marine west coast climate is one of the major climate types according to Koppen's climate classification. This climate type is mostly dictated by the sea. In Europe, the marine west coast climate can be found in a surprisingly high latitude, and the main reason for that are the warm ocean currents. The warm ocean currents of the Atlantic are running along the western coast of Europe, and they manage to have huge influence on the climate of the region.
- This climate type can be found at lower elevations and hills in Western Europe.
- The climate is warmer than it should be considering the latitude where this climate type is found in Europe.
- The summers are mild to warm, the springs and autumns mild to cold, while the winters are cold.
- The temperature extremes in both winter and summer are usually absent, and the climate is much more balanced.
- There is high amounts of precipitation throughout the whole year.
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Answer:
As given below.
Explanation:
1. <u>False</u>, as the number of daylight hours on the globe are mapped by the location f places over the various latitudes and altitudes. And the sun is not with the same both rise and set at both the hemispheres.
2. <u>Yes</u>, there exist changes of 12 hours in sunlight and darkness on earth due to the rotational speed of the earth on its axis as the earth is tilted 23.5 degrees so in both the hemisphere there exists equinoxes and solstices.
3. <u>True</u>, as the known fact the earth rotates in anticlockwise direction hence the eastern side gets to see the sun first and western side later this rule applies everywhere in the earth on both the equinoxes.
4. <u>True</u>, The celestial poles and equator are two points on earth that represent the equinoxes and the point that falls directly over the poles is called the zenith and the plane that touches is called the galactic plane.
Crust:outer silicate solid crust
mantle:highly viscous
core:solid inner core
Answer:
Explanation:
Accretion occurs as mantle is added to the growing edges of a plate, associated with seafloor spreading. This hot added material cools down by conduction and convection of heat. ... Mantle convection causes tectonic plates to move around the Earth's surface.
