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Because Kīlauea lacks a topographical prominence and appears as a bulge on the southeastern flank of Mauna Loa, it was historically interpreted by both native Hawaiians and early geologists to be an active satellite of Mauna Loa.
After publishing a summary paper in 1852, he directed a detailed geological study of the island in 1880 and 1881 but did not consider Kīlauea a separate volcano, instead referring to it as a flank vent of Mauna Loa; it was not until another geologist, C. E. Dutton, had elaborated on Dana's research during an 1884 expedition that Kīlauea came to be generally accepted as a separate entity.
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The date corresponded with a massive flank collapse at the nearby Mauna Loa, and it was theorized that it was a massive tsunami, generated by the landslide, that deposited the fossils.
At 1,247m it's not even the tallest volcano on Hawaii (it's dwarfed by the 4,169m Mauna Loa) but it has been belching out huge quantities of deep crimson, slow-moving lava almost continuously since 1983.
Likewise, a stone in the garden (object c in Figure 4) is absent for both the new and the old LoA, since it satisfies no typed variable of either one.
If it were easier for people to find out whether they're infected with Loa loa worms, it might be easier to convince them that it's safe to take ivermectin, or so the logic goes.
Caused by the Loa loa worm, it is highly endemic in certain rainforest areas across 10 countries in Central and West Africa.
The location of Mauna Loa has made it an important location for atmospheric monitoring by the Global Atmosphere Watch and other scientific observations.
Wilkes sailed to Hilo on the island of Hawaii and decided to climb Mauna Loa first, since it looked easier than Mauna Kea.
Regardless, Kīlauea's lack of a geographic outline and strong volcanic link to Mauna Loa led to it being considered an offshoot of Mauna Loa by the Ancient Hawaiians, meaning much of the mythos now associated with Kīlauea was originally directed at Mauna Loa proper as well.
Mauna Kea is over in volume, so massive that it and its neighbor, Mauna Loa, depress the ocean crust beneath it by 6 km.
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