Hawai'an volcanic islands
Hawai'an volcanic islands is not part of a convergent/subduction plate boundary.
<h3>What kind of plate boundary produces a sequence of volcanic islands?</h3>
- convergent boundary
- Along the convergent boundary, the new magma (molten rock) rises and may erupt violently to form volcanoes, frequently creating arcs of islands.
- Divergent plate boundaries are created when two plates are moving apart.
<h3>Why do volcanic chains and convergent borders coexist?</h3>
- Subduction causes melting that is partially molten.
- Water loss in the plate causes partial melting.
- Mantle material melts as a result and rises to the surface.
<h3>Which are the 4 types of convergent boundries?</h3>
- Divergent Plate Boundary.
- Convergent Plate Boundary.
- Transform Plate Boundary.
- Hotspot.
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A holdfast is a root-like structure that anchors aquatic sessile organisms, such as seaweed, other sessile algae, stalked crinoids, benthic cnidarians, and sponges, to the substrate.
Of poor water hygiene and management
Answer:
There will be NO topography, no ice, no winds, no water, no river, no lakes, no aquifer, no seas, no ocean. Minerals would get scarce, no more will be deposited.
Explanation:
Gamma waves have the highest energy and can be extremely harmful. Hope this helped.
