Consider the age of the various Hawaiian Islands given below in millions of years. Remember, the formation of the Hawaiian Islands reflects: 1) the movement of the Pacific plate, and 2) stationary volcanic hotspot activity over time. Which direction is the Pacific plate currently moving? Maps are plan or bird's eye views of the earth's surface. Here, the top of the figure is north, and the bottom of the figure is south. The left side of the figure is west, and the right side is east.
Select one: a. Southwest b. South c. Northeast d. Northwest e.
Southeast f. North
Last years eruptions emerged from fissures in the East Rift Zone (ERZ) on the big island of Hawaii. This zone is not located at the peak of Kilauea, but instead, near the base. Choose the statement that most accurately describes the tectonic setting of the East Rift Zone (ERZ) on the big island of Hawaii. Hint: To remind yourself the details of the tectonic setting, refer to your Hazard Explorations... Also, it is recommended that you consult a plate tectonic map of the earth (in your text!) to identify the plate tectonic setting at each of the following locations. The figure of Hawaii below shows the shape of the East Rift Zone, which consists of fissures, and the locations of craters that formed along it.
Select one: a. The ERZ is most similar to the East African rift zone, where fissures surrounding Mt. Nyiragongo erupt basaltic lava.
b. The ERZ is most similar to the Mid Atlantic Ridge which erupts basaltic lava from fissures.
c. The ERZ is most similar to mid oceanic rifts on Iceland, which erupt curtains of basaltic lava.
d. The ERZ is most similar to fissures along the mid oceanic East Pacific Rise which erupt basaltic lava. e. The ERZ is most similar to fissures in the Snake River plain of Idaho, which erupted basaltic lava.
The direction of motion of pacific plate is Northwest as shown in the above figure.
The answer is "ERZ is the most similar to mid oceanic ridge on the Iceland, which erupt curtains of basaltic lava.
Because the it is also an oceanic hotspot that has similar to Hawaiian hotspot. Both are oceanic hotspots in which magma erupts from deep mantle plumes.
Consider the age of the various Hawaiian Islands given below in millions of years. Remember, the...
KAUAI (5.1 MYA) AGES ARE MILLIONS OF YEARS AGO OAHU (3.2 MYA) SUIKO SEAMOUNT (59.6 MYA < YA MOLOKAI (2 MYA) ALA MAUI (1 MYA) NINTOKU SEAMQUNT (56.2 MYA) 400 e so 100 #0 km HAWAII (O MYA) KOKO GUYOT (48.1 MYA) SY 6 / MIDWAY (27.2 MYA) YURYAKU SEAMOUNT (43.4 MYA) LAYSAN (19.9 MYA) MAP SCALE 300 600 900 KM dos NECKER (10.3 MYA) 0 20 170 160 Hawaii Homework The diagram represents islands created by the Hawaiian hot...
Volcanic Hotspots and Seafloor Spreading The figure below is a map of the volcanic islands and seamounts (submerged volcanoes) that form the Hawaiian Islands and the Hawaiian-Emperor Chain. These were formed by a "hot spot" - a relatively stationary hot plume that rises through the earth's mantle and melts part of the overriding plate. Table 1 shows a selection of some of these volcanoes with regard to their age and distance from the active hot spot location. The change in...