Since volcanic emissions are brought about by magma (a combination of fluid stone, gems, and disintegrated gas) removed onto the Earth's surface, we'll initially audit the qualities of magma that we covered beforehand.
Three fundamental kinds of magma includes Mafic or Basaltic (SiO2 45-55 wt%, high in Fe, Mg, Ca, low in K, Na), Moderate or Andesitic (SiO2 55-65 wt%, transitional. in Fe, Mg, Ca, Na, K) and Felsic or Rhyolitic (SiO2 65-75%, low in Fe, Mg, Ca, high in K, Na.)
Gases - At profundity in the Earth essentially all magmas contain gas. Gas gives magmas their unstable person, on the grounds that the gas extends as pressing factor is diminished.
Generally H2O with some CO2
Minor measures of Sulfur, Cl , and F
Felsic magmas ordinarily have higher gas substance than mafic magmas.
Temperature of Magmas includes Mafic/Basaltic (1000-1200oC), Transitional/Andesitic (800-1000oC) and Felsic/Rhyolitic (650-800oC).
Explanation:
Thickness is the protection from stream (inverse of ease). Relies upon sythesis, temperature, and gas content. Higher SiO2 content magmas have higher consistency than lower SiO2 content magmas withlower Temperature magmas have higher thickness than higher temperature magmas.
even if you check if it's plagiarized, nah its not.
Answers & Comments
Answer:
magmas and Lava
Since volcanic emissions are brought about by magma (a combination of fluid stone, gems, and disintegrated gas) removed onto the Earth's surface, we'll initially audit the qualities of magma that we covered beforehand.
Three fundamental kinds of magma includes Mafic or Basaltic (SiO2 45-55 wt%, high in Fe, Mg, Ca, low in K, Na), Moderate or Andesitic (SiO2 55-65 wt%, transitional. in Fe, Mg, Ca, Na, K) and Felsic or Rhyolitic (SiO2 65-75%, low in Fe, Mg, Ca, high in K, Na.)
Gases - At profundity in the Earth essentially all magmas contain gas. Gas gives magmas their unstable person, on the grounds that the gas extends as pressing factor is diminished.
Generally H2O with some CO2
Minor measures of Sulfur, Cl , and F
Felsic magmas ordinarily have higher gas substance than mafic magmas.
Temperature of Magmas includes Mafic/Basaltic (1000-1200oC), Transitional/Andesitic (800-1000oC) and Felsic/Rhyolitic (650-800oC).
Explanation:
Thickness is the protection from stream (inverse of ease). Relies upon sythesis, temperature, and gas content. Higher SiO2 content magmas have higher consistency than lower SiO2 content magmas with lower Temperature magmas have higher thickness than higher temperature magmas.
even if you check if it's plagiarized, nah its not.
Answer:
Magmas and lava
Explanation:
Trust me its the write answer