Question

The image here depicts a convection current below the Earth's surface. The type of boundary shown here is a Response area boundary that results in Response area. The magma reaches the surface because Response area rises and as the magma breaches the crust, Response area emerges.
seafloor spreadingheatlavatransformdivergentmantle

Answer 1

The image you are referencing likely illustrates convection currents in the mantle and their relationship to tectonic plate boundaries. Here's how to fill in the blanks based on terms associated with these geological processes:

"The image here depicts a convection current below the Earth's surface. The type of boundary shown here is a **divergent** boundary that results in **seafloor spreading**. The magma reaches the surface because **heat** causes it to rise, and as the magma breaches the crust, **lava** emerges."

In this context:
- **Divergent boundary**: A type of boundary where two tectonic plates move away from each other, often resulting in the formation of new oceanic crust.
- **Seafloor spreading**: The process by which new oceanic crust is created at divergent boundaries as magma rises and solidifies.
- **Heat**: The driving force behind the movement of magma within the Earth's mantle.
- **Lava**: The molten rock that reaches the Earth's surface during volcanic activity.