The Rock Cycle. Arrows point from 1 stage to next. 1. Metamorphic Rock to point K to Magma to point V to Igneous Rock to Melting
back to magma. 2. Metamorphic Rock to point K to Magma to point V to Igneous Rock to Heat and Pressure. 3. Metamorphic Rock to point K to Magma to point V to Igneous Rock to Weathering and Erosion to Sediment to Compacting and Cementing to Sedimentary Rock to Heat and Pressure to Metamorphic Rock. 4. From Sediment to Compacting and Cementing to Sedimentary Rock to Weathering and Erosion back to Sediment. 5. Metamorphic Rock to Weathering and Erosion to Sediment. Which event most likely occurs at point V?
Metamorphic Rock to point K to Magma to point V to Igneous Rock to Heat and Pressure.
Point V would be cooling,
In the rock cycle, one rock can turn into another rock. A metamorphic rock can turn into an igneous rock through 2 process, namely melting and cooling. If a metamorphic will undergo tremendous heat, it could melt into magma. If magma cools down it would turn into an igneous rock.
In summary:
Metamorphic rock→ melting (Point K)→magma→cooling (Point V)→Igneous Rock
Metamorphic Rock to point K to Magma to point V to Igneous Rock to Heat and Pressure.
Point V would be cooling,
In the rock cycle, one rock can turn into another rock. A metamorphic rock can turn into an igneous rock through 2 process, namely melting and cooling. If a metamorphic will undergo tremendous heat, it could melt into magma. If magma cools down it would turn into an igneous rock.
In summary:
Metamorphic rock→ melting (Point K)→magma→cooling (Point V)→Igneous Rock
Majority of the IMF funding comes
from the member countries through their payment of quotas. These quotas are
assigned to each member of the IMF based on its size in the world economy. IMF
can also supplement its resources through bilateral and multilateral borrowing.
They provide a temporary supplement to quota resources.
"If you add 1 to an earthquake's magnitude, you multiply the shaking by 10. An earthquake of magnitude 5 shakes 10 times as violently as an earthquake of magnitude 4; a magnitude-6 quake shakes 10 times as hard as a magnitude-5 quake; and so on."- www.Science.org
The structure of buildings and temples were built many years ago, you see places like Washington DC replicate the same types of structure in their buildings the art of it is beautiful and well liked.
