The correct answer is B. Extrusive Igneous
Explanation
The image shows an image of an Obsidian rock and at the top a text fragment that says "The photo below shows a sample of Obsidian forms when lava from a volcanic eruption cools very quickly aboveground"
Igneous rocks are a group of rocks that includes all those that have been formed by the solidification of magma or lava expelled from the earth's lithosphere through a process called crystallization. In general, when the solidification of magma occurs within the lithosphere, the resulting rock is called intrusive. On the other hand, if the cooling occurs (at least in part) at the surface or a shallow depth, the resulting rock is called extrusive.
Taking into account the text that complements the image of the question and the previous information, it is possible to affirm that the correct answer is B. Extrusive Igneous because the rock is the result of the solidification of lava above the ground.
Answer:
Instead of Tokyo im gonna do New Zealand. from an article During normal years energy transfers from the ocean to the air. However, during El Nino years, the current is not as warm, so less energy will transfer from the current to the air, making Christchurch cooler than usual.
Explanation:
<span>-- The latitude at the northern end of the main runway at
Yakutsk Airport is 62.106° N. That point is roughly 460 miles
from the closest point on the seacoast.
-- The latitude at the northern end of the main runway at
Anchorage International Airport is 61.199° N. That point is
roughly 0.32 mile from the closest point on the seacoast.
Using these points of comparison, Yakutsk is 0.907° of latitude (62.7 miles)
more northerly than Anchorage, and Anchorage is roughly 460 miles closer
to the ocean than Yakutsk is.</span>
Answer:
Explanation:
D. The European Union has a great influence on the world market.
Answer:
Normal fault
Explanation:
Tensional stress occurs as a result of forces which could be wind, water etc pulling the rocks apart and forming faults. Faults are also known as a type of fracture which occurs between rocks.
Tensional stress along a fault can result in a dropped hanging-wall block relative to the footwall side(in a perpendicular position) thereby producing a normal fault.
