The Earth's rocky outer crust solidified billions of
years ago, soon after the Earth formed. This crust is not a solid
shell; it is broken up into huge, thick plates that drift atop the soft,
underlying mantle.
The plates are made of rock and drift all over the globe; they move both
horizontally (sideways) and vertically (up and down). Over long
periods of time, the plates also change in size as their margins are
added to, crushed together, or pushed back into the Earth's mantle. These plates are from 50 to 250 miles (80 to 400 km) thick.
Answer:
D: The inner core is liquid and moving.
Explanation:
<u>Answer:</u>
Considering the example of Japan, it can be justified that both the primary and the secondary impacts of tectonic hazard cause the most damage.
<u>Explanation:
</u>
- Any tectonic activity of considerable magnitude generates tremors and causes earthquakes and related phenomenons.
- Japan has consistently been subject to the secondary impacts of such tectonic hazards like earthquakes and tsunamis.
- The areas close to the coasts of Japan are tectonically active making Japan vulnerable to its aftermaths.
- Moreover, Japan also has some dormant volcanoes which are a result of tectonic activity.
Answer:
m<E = 105°
Explanation:
The ratio of the corresponding side lengths of ∆STU and ∆DEF are equal. That is:
.
According to similarly theorem, if two ∆s are similar, the ratio of their corresponding lengths would be the same. Therefore, ∆STU is similar to ∆DEF.
Since ∆STU ~ ∆DEF, their corresponding angles are congruent. That is:
<S ≅ <D, this means both are 29° each.
<T ≅ <E, this means they are both equal
<U ≅ <F. this means both are 46° each.
Thus:
m<E = 180 - (m<D + m<F) (sum of ∆)
m<E = 180 - (29 + 46) (substitution)
m<E = 180 - 75
m<E = 105°
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