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The USGS estimate that the vulcano has been erupting every 6 years on averages over the last 3000 years.

The Mauna Loa is a really high and big hill. Considering that the sides of Mauna Loa lie on a seabed about 5,000 meters below the surface, the "height" of this vulcano in relation to the neighbouring country (seabed) is rather 30,080 feet (9,170 m)! The Mauna Loa is the biggest volcanic activity in the whole wide range.

Indeed, at this last dimension of its altitude, it is one of the highest peaks in the whole wide globe (although many peaks, such as Mount Everest in the Himalayas, are higher in relation to ocean level). So right below Mauna Loa, the seabed on which it lies is pressed through and an extra 26,000 feet (8,000 m).

So, if one wanted to say how thick (in the middle) the heap of Luna Loa is, one would have to increase its altitude above the surface, its seabed to the surface and the depth of its deepening in the Pacific seabed. See the section "How high is the Mauna Loa volcano" on the HVO website for more information on estimating the true depth of the Mauna Loa vulcano.

Awakening Mauna Loa? Mauna Loa peak began to inflate gradually between 2002 and 2005 after a ten-year mild recession after a short flock of long, profound tremors. However, in 2004 and the first half of 2005, after a larger shoal of several thousand low seismic events at the end of 2004, the rate of global warming was fairly stable, suggesting that the magmatic reserve within the volume was rising.

At the end of August 2015, the HVO aging rate at Mauna Loa rose due to the long-term increase in seismic activity and the peak rate of precipitation in terms of precipitation (measured by the cross-caldera difference). That does not mean that an explosion is impending, but the characters are in line with the penetration of magic into the flat part of the igneous system at the vulcan.

Earthquake activities rose at the beginning of July 2004 and persisted until autumn 2004, but then decelerated significantly throughout 2005 and stayed at a rate of around 10 per week. 2.5 % of the earthquake was caused by the earthquake. The peak of the activities was reached in September 2004 (e.g. there were more than 350 "long period" seismic events below the Mauna Loa peak and the south-western trench area in the first weeks of this months, most of them at depths (35 to 50 km) below the earth's surface).

Explorers of High Voltage Vaporization (HVO) are still watching the vulcan. Frank Trusdell, an HVoS surveyor who has been studying the vulcano for almost two dozen years, is cited in a March 26, 2009 U.S. Federal Ordinance news release: "Mauna Loa will break out again, and there is a good possibility that it will be during your life.

The Mauna Loa is a "shield volcano", i.e. a softly descending hill, which is obtained from a multitude of mostly very liquid streams of water. It has erupted for at least 100,000 years (possibly more) from a main centre of the vulcano, which is currently manifesting itself through the Moku'aweoweo cave at the top of the hill.

It is made of a stone known as Tholeiite bass. One of the oldest remains of the Mauna Loa subera is in an interesting cliff formations, the Ninole Volcanic Series. This hill forms the so-called "Ninole Shield", which is said to be either the remains of a pre-Mauna-Loa volume or raised boulders of the old Mauna-Loa from the Honuapo-kaoiki error system.