Mauna Loa is a example of a shield volcano. Hope this helps you.
Answer:
Kilauea and Mauna Loa are both shield volcanos located in Hawaii . All the volcanoes on the Hawaii islands are shield volcanoes. Examples of shield volcanoes include Kilauea, Mauna Kea, and Mauna Loa in Hawaii, Isabela Island in the Galapagos, and Olympus Mons on Mars.
Explanation:
A shield volcano is a type of volcano that has been formed by lava flow. Shield volcanoes are large and wide with a low profile. The crater at the volcano is not far above sea level in comparison to a composite volcano. Most shield volcanoes are super-volcanoes. A shield volcano is a volcano with shallow-sloping sides. Shield volcanoes are formed from fluid lava that can travel long distances across slight inclines, resulting in their relatively flat, broad profile. In contrast, steeply sloped stratovolcanoes better match the popular stereotype of a volcano.
Answer:
A surface like a mountain.
Explanation:
The mountain cannot absorb the water and when snow melts it wil run down the mountain.
Answer:
The only types of mutations that matter to large-scale evolutionary species are the mutations that can be passed to offspring (Genetic).
Explanation:
If a mutation is passed to offspring, through the generations it will become more and more prevalent...Eventually causing a pretty good dent on a population size. Hope this helps : )!
Answer: plate tectonics
The plate tectonics is the theory in which the solid outer layer of the earth is composed of interconnected plates what move across the earth's surface. It is based on and incorporates the older theory of continental drift.
Answer:
Plate tectonic theory
Explanation:
Plate tectonic theory states that the earth contains numerous small and large lithospheric plates. These plates constantly moving from one place to another in three different ways such as
1) Convergent plate motion- here two plates move towards each other.
2) Divergent plate motion- here two plates move in the opposite direction, away from each other
3) Transform plate motion- here two plates slide passes each other.
This plate motion occurs due to the convection current that generates on the mantle because of the tremendous heat radiated from the core of the earth and this entire process is commonly known as the plate tectonic theory.
In the case of convergent plate motion, the denser plates get subducted beneath the lighter one and form a trench that appears to be a depression within the oceans and there forms a zone known as the subduction zone.
In the case of a divergent plate motion, it then forms a ridge, which later forms an ocean and the zone of separation of these two plates is known as the mid-oceanic ridge.
So a lot of ridges and subduction zones are present on earth.