Volcanoes Flashcards
(43 cards)
How are volcanoes measured and when was this measurement installed?
Logarithmic scale called the Volcano Explosivity Index (VEI) from 0-8 formed in1982
1 = gentle
4 = cataclysmic
8 = mega colossal
Features of an Icelandic volcano
Type of magma: basaltic
Characteristics: lava flows gently from fissures
Features of a Hawaiian volcano
Type of magma: basaltic
Characteristics: lava flows gently from a central vent
Features of a Strombolian volcano
Type of magma: thicker basaltic
Characteristics: frequent, explosive eruptions of tephra and steam. Occasional, short lava streams
Features of a Vulcanian volcano
Type of magma: thicker basaltic, andesitic, rhyolitic
Characteristics: less frequent but more violent eruptions of gases, ash and tephra including lapilli
Features of a Vesuvian volcano
Type of magma: thicker basaltic, andesitic, rhyolitic
Characteristics: following long periods of inactivity, very violent gas explosions blast ash high into the sky
Features of a Peléean volcano
Type of magma: andesitic and rhyolitic
Characteristics: very violent eruptions of nuées ardentes
Features of a plinian volcano
Type of magma: rhyolitic
Characteristics: exceptionally violent eruptions of gases, ash and pumice. Torrential rainstorms cause devastating lahars.
What is material ejected from a volcano usually known as and what does it mean
Tephra - all pieces of fragments of rock ejected into the air by an erupting volcano
What typically happens with tephra?
Most tephra falls back onto the slopes of the volcano, enlarging it. But, billions of smaller and lighter pieces less than 2 mm diameter (less than one tenth of an inch), termed ash, are carried by winds for thousands of miles.
What is a plume?
A column of hot volcanic ash that has emitted into the atmosphere during an eruption
What are the factors that determine the viscosity of magma?
Temperature, dissolved gases and chemistry
How does temperature determine the viscosity of magma?
the higher the temperature, the lower the density of the magma and the more easily it will flow
How do dissolved gases determine the viscosity of magma?
the greater the amount of dissolved gases, the more fluid the magma. Gases remain dissolved in high temperature conditions.
How does chemistry determine the viscosity of magma?
the higher the silica content, the more viscous the magma.
What is basic magma?
- rich in iron, aluminium and magnesium.
- sometimes referred to as Basaltic. - It is high temperature magma (1000-1200 degrees C)
- has a high proportion of dissolved gases (4-6%)
- low silica content (44-52%).
- It is very fluid and has a low viscosity
What is acid magma?
- very rich in silica (66%+).
- It is a relatively low-temperature magma (800-1000 degrees C)
- much lower proportion of dissolved gases than basic magma
- It is very thick and has a high viscosity
There are 2 types - Andesitic and Rhyolitic magma both have a higher silica content and so have a higher viscosity. They flow less easily and often form blockages in volcanic vents. Also volcanic gases can’t escape easily from viscous lava so pressure builds up until the blockages are cleared by a violent eruption.
What creates more explosive eruptions
The more viscous the magma, the more explosive the eruption
What types of eruptions occur at destructive boundaries?
As one plate is subducted below another, intense pressures and heat cause melting of the rocks and sediments, which can result in the formation of an acidic magma chamber. Very viscous and resistant to flow, there is often a huge build-up of gas which results in very violent and dangerous eruptions involving ash and pyroclastics.
What types of eruptions occur at constructive plate boundaries?
where oceanic plates are moving away from each other, the magma is produced by the partial melting of the mantle deep below the surface. It is a basic-type of magma and therefore has a low viscosity enabling it to flow easily. Volcanoes at constructive margins, for example along the Mid-Atlantic Ridge erupt frequently, but not usually violently and are associated with lava flows and ash.
What types of eruptions occur at constructive plate boundaries - continental plates?
At constructive margins where continental plates are moving apart, such as the East African Rift Valley, the situation is more complex in relation to volcanic features and magma type. Often the volcanic rocks show a diversity ranging from basic to acid and there can be a variety of features from small fissure eruptions, to larger volcanoes, such as Mt Kilimanjaro.
Where do most of the worlds volcanoes occur?
Whilst 75% of all volcanic material is erupted at constructive margins, most of the world’s active volcanoes (over 80%) occur at destructive margins. It is these that are generally considered to be the most hazardous.
Do all volcanoes occur at plate margins?
No - those volcanoes not directly associated with plate margins, such as those on the Hawaiian Islands, result from isolated plumes of rising magma. The magma is basic in nature and these volcanoes are similar to those associated with constructive margins.
What do the frequency of eruptions depend on?
The frequency of volcanic eruptions depends largely on their type. Kilauea, on the island of Hawaii, is an active shield volcano which has erupted basaltic lava continuously since 1983. In contrast many volcanoes that erupt rhyolitic lava, erupt very infrequently. The Yellowstone caldera has erupted 3 times in the last 2.1 million years, with an interval of between 600 000 and 800 000 years between each.