T. string of volcanic … The islands are about 1,860 miles (3,000 km) from the nearest continent. The formation of the Hawaiian Islands is one example of a. volcanoes forming over a hot spot. Answer Save. the Ring of Fire. The Nuuanu landslide deposit has a volume of approximately 5000 m, is 200 km wide and had very large intact blocks of land. d. random occurrence of volcanoes. The formation of the Hawaiian Islands is one example of volcanoes forming over a hot spot. plate boundaries The formation of the Hawaiian Islands is one example of volcanoes forming over what? volcanoes forming along plate boundaries. random occurrence of volcanoes. D) continental drift. B. 1 decade ago. Each island or submerged seamount in the chain is successively older toward the northwest. SC.5.6.2 Describe ways that heat can be transferred from one object to another. The study of the origins of the Hawaiian islands provides an excellent example of how science works. The long tube in the ground that connects the magma chamber to Earth's surface is called the Oahu also experienced the largest known example of a landslide. C) the Ring of Fire. 6 Answers. Favorite Answer. The Hawaiian Emperor seamount chain is a well-known example of a large seamount and island chain created by hot-spot volcanism. An example of the founder effect? A hot spot is an area where material from deep within the mantle rises and then melts, forming magma. Relevance. Because of Oahu’s age, it and its Kauai island have the most diverse ecological system of the Hawai’ian islands. It is a unique example of what is known as a hot spot. For many years the geological history of the islands remained a mystery. A) volcanoes forming over a hot spot. Description: This lesson introduces students to hot spot theory and how it relates to plate tectonics. c. the Ring of Fire. s. Log in for more information. The Hawaiian Islands are the exposed peaks of a great undersea mountain range known as the Hawaiian–Emperor seamount chain, formed by volcanic activity over a hotspot in the Earth's mantle. Oahu is one of the oldest of the main Hawaiian islands. Joanie. In fact, if the Pacific Ocean was drained like the water in a pool, you would see that the height of this Hawaiian island is taller than Mount Everest by about 4,000 feet! c. the Ring of Fire. The Hawaiian Islands were formed by volcanic activity. The Hawaiian Islands have nothing to do with ocean structures. The formation of the Hawaiian Islands is one example of volcanoes forming over a hot spot. b. volcanoes forming along plate boundaries. and how they change and transfer energy from one form to another. B) volcanoes formaing along plate boundaries. The fomation of the Hawaiian Islands is one example of? Lv 5. A) Hot spots. A. molten rock under ground Island Arc magma hot spot lava plate boundaries. The Hawaiian Islands were formed by hot spot volcanoes. b. volcanoes forming along plate boundaries. The formation of the Hawaiian Islands is one example of volcanoes forming over a hot spot. The formation of the Hawaiian Islands is one example of a. volcanoes forming over a hot spot.

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