The layers will be denser as you move from the crust to the inner core.
The density are as the following:
crust (2.55 g/cm³)
upper mantle (3.9 g/cm³)
lower mantle (5 g/cm³)
outer core (11.05 g/cm³)
inner core (12.95 g/cm³)
Thus we can also see that the inner core is the densest layer.
Hope it helps!
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.
With the recent technologies and scientific innovations we have now on studying and providing detailed analyses of the polar ice cores, it is roughly estimated that we could profile the ancient climate the Earth had in a time period as early as 800,000 years in order to explain the most recent climate change.
Answer:
The answer is in the picture
Explanation:
Mexico is one of the first Latin American countries to have
a separate ministry of tourism with dedicated funds within its federal
governmental
<span> structure.</span>
