The answer is east isnt it?
Answer:
hot spot
Explanation:
There are several different types of plate boundaries, and each boundary type comes with some specific physical geographic feature. The divergent plate plate boundaries have mid-ocean ridges if they are on the ocean floor, or they rifts if they are on land. The transform plate boundaries have faults. The convergent plate boundaries have trenches if they are between oceanic and continental plates, or mountain ranges if they are between two continental plates.
The hot spots though are something that is commonly associated with plate boundaries. The reason for this is that the hot spots can appear anywhere, so they can be near a plate boundary, but they can also be in the interior of an oceanic plate, or in the interior of a continental plate. The hot spots occur because of much more intense activity in the astenosphere, resulting in mantle plumes which manages to break through the crust with ease and manifest themselves on the surface.
Metamorphic rock will form.
Explaination: metamorphic rock is formed under high heat or pressure,causing it's texture or chemical composition to be different from that of the parent rock.
Metamorphism: process of transformation of existing rock
Hope it helps
When volcanoes errupt they can form islands , for example this is how hawaii was formed
Answer:
The Paleozoic Era, which ran from about 542 million years ago to 251 million years ago, was a time of great change on Earth. The era began with the breakup of one supercontinent and the formation of another. Plants became widespread. And the first vertebrate animals colonized land.
Life in the Paleozoic
The Paleozoic began with the Cambrian Period, 53 million years best known for ushering in an explosion of life on Earth. This "Cambrian explosion" included the evolution of arthropods (ancestors of today's insects and crustaceans) and chordates (animals with rudimentary spinal cords).
In the Paleozoic Era, life flourished in the seas. After the Cambrian Period came the 45-million-year Ordovician Period, which is marked in the fossil record by an abundance of marine invertebrates. Perhaps the most famous of these invertebrates was the trilobite, an armored arthropod that scuttled around the seafloor for about 270 million years before going extinct.