Analyze the interactions of the sphere's after the onslaught of taal volcano
Answers
Answer:
Taal volcano belongs to the geosphere. When it erupts, it releases materials like carbon dioxide to the atmosphere. It also releases ashes which spreads all through out the surrounding area. The interaction of those materials released in the atmosphere would result to acid rain ( hydrosphere ).This
eruption will also damage the life forms surround the volcano like the fish of the lake will die, the trees and in worst case scenario it cost the lives of animals, plants, and humans ( biosphere ).
There are four system of the Earth:
Hydrosphere - This correspond to the water layer of the Earth
• Biosphere - This correspond to the living organism found on Earth.
Atmosphere This correspond to the gas layer of the Earth
. Geosphere - This correspond to the rock layer of the Earth.
Each Earth system plays a vital role on the existence of Earth and its life forms. They are constantly coordinating and interacting to support each other. If one system fails to carry out its function, then the rest of the system will also be affected particularly the biosphere which all depends on hydrosphere, atmosphere and geosphere. Life forms may not exist if this happen.
Answer:
Taal Volcano is one of the most active volcanoes in the Philippines. The first recorded eruption was in 1573. Since then it has erupted 33 times resulting in thousands of casualties and large damages to property. In 1995, it was declared as one of the 15 Decade Volcanoes. Beginning in the early 1990s it has experienced several phases of abnormal activity, including seismic swarms, episodes of ground deformation, ground fissuring and hydrothermal activities, which continues up to the present. However, it has been noted that past historical eruptions of Taal Volcano may be divided into 2 distinct cycles, depending on the location of the eruption center, either at Main Crater or at the flanks. Between 1572-1645, eruptions occurred at the Main Crater, in 1707 to 1731, they occurred at the flanks. In 1749, eruptions moved back to the Main Crater until 1911. During the 1965 and until the end of the 1977 eruptions, eruptive activity once again shifted to the flanks. As part of the PHIVOLCS-JICA-SATREPS Project magnetotelluric and audio-magnetotelluric surveys were conducted on Volcano Island in March 2011 and March 2012. Two-dimensional (2-D) inversion and 3-D forward modeling reveals a prominent and large zone of relatively high resistivity between 1 to 4 kilometers beneath the volcano almost directly beneath the Main Crater, surrounded by zones of relatively low resistivity. This anomalous zone of high resistivity is hypothesized to be a large hydrothermal reservoir filled with volcanic fluids. The presence of this large hydrothermal reservoir could be related to past activities of Taal Volcano. In particular we believe that the catastrophic explosion described during the 1911 eruption was the result of the hydrothermal reservoir collapsing. During the cycle of Main Crater eruptions, this hydrothermal reservoir is depleted, while during a cycle of flank eruptions this reservoir is replenished with hydrothermal fluids.