Tambora volcano in Indonesia has basaltic andesite lava composition. This type of lava is intermediate in silica content and viscosity, leading to explosive eruptions due to trapped gases.
stratovolcano
yes it is still active
The possessive form of the noun lava is lava's.Example: The lava's heat could be felt at a great distance.
Lava in French is "lave."
Mount Eyjafjallajökull in Iceland has a type of lava known as andesitic lava. Andesitic lava is a viscous lava that can lead to explosive eruptions due to its high silica content.
Mount Tambora typically produces highly viscous lava due to its high silica content. This results in the lava being thick and slow-moving, leading to more explosive eruptions.
No. Tambora is a stratovolcano with a large caldera.
The lava of Mount Tambora covered an estimated area of about 40 square kilometers during its 1815 eruption.
Tambora was a composite cone.
Tambora is a composite volcano (stratovolcano). A stratovolcano/composite volcano is explosive, usually creating large ash clouds, pyroclastic flows and can cause mass destruction for miles and sometimes effect the entire earth for years. *Skylla*
Mount Tambora's lava can reach temperatures of around 1,300 to 1,600 degrees Celsius (2,372 to 2,912 degrees Fahrenheit). This extreme heat allows the lava to flow relatively quickly and efficiently when erupting from the volcano.
Mount Tambora is not a shield volcano; it is a stratovolcano. Stratovolcanoes are characterized by steep slopes and a symmetrical shape due to their alternating layers of lava, ash, and other volcanic materials. Shield volcanoes, on the other hand, have gentle slopes and wide bases formed by successive layers of flowing lava.
During the 1815 eruption of Mount Tambora, materials expelled included ash, volcanic gases such as sulfur dioxide, and lava flows. The eruption was one of the most powerful in recorded history and resulted in global climate impacts.
all lava
Mt. Tambora is a stratovolcano, also known as a composite volcano. Stratovolcanoes are characterized by steep, symmetrical slopes and periodic explosive eruptions. Mt. Tambora famously erupted in 1815, leading to a significant global cooling event known as the "Year Without a Summer."
The eruption of Mount Tambora in 1815 led to a volcanic winter, causing a decrease in global temperatures and disrupting weather patterns. This in turn led to widespread crop failures and food shortages, resulting in famine in many regions around the world, including Europe and North America.
Lava domes usually consist of rhyolite or dacite lava.