Which magma would contain the greatest amount of SiO2?
Which magma would contain the greatest amount of SiO2?
MAGMA COMPOSITION AND ROCK TYPES
SiO2 CONTENT | MAGMA TYPE | VOLCANIC ROCK |
---|---|---|
~50% | Mafic | Basalt |
~60% | Intermediate | Andesite |
~65% | Felsic (low Si) | Dacite |
~70% | Felsic (high Si) | Rhyolite |
Which magma type contains the greatest amount of silica?
Felsic magmas
What type of rock has the greatest silica content?
igneous rocks
Is silica the most abundant compound found in Magma?
Silica (SiO2), is the most abundant compound in magma. Magmas are classified as basaltic, andesitic, and rhyolitic, based on the amount of SiO2 they contain. Different minerals melt and crystallize at different temperatures in the processes of partial melting and fractional crystallization.
What is the most abundant compound in magma?
Oxygen, the most abundant element in magma, comprises a little less than half the total, followed by silicon at just over one-quarter. The remaining elements make up the other one-quarter. Magmas derived from crustal material are dominated by oxygen, silicon, aluminum, sodium, and potassium.
Which magma is the most abundant type erupted at oceanic spreading centers?
Basaltic
How did the ridges around Shiprock form quizlet?
How did the ridges around Shiprock form? The rocks in Shiprock formed when magma solidified in the neck of an old volcano. They are old dikes radiating from the main neck of the volcano. All of the lava and pyroclastic material and some of the volcanic neck were eroded.
What kind of viscosity would basalts have?
Basalt is a hard, black volcanic rock with less than about 52 weight percent silica (SiO2). Because of basalt’s low silica content, it has a low viscosity (resistance to flow). Therefore, basaltic lava can flow quickly and easily move >20 km from a vent.
What is the difference between a dike and a sill?
A sill is a concordant intrusive sheet, meaning that a sill does not cut across preexisting rock beds. In contrast, a dike is a discordant intrusive sheet, which does cut across older rocks. Sills are fed by dikes, except in unusual locations where they form in nearly vertical beds attached directly to a magma source.
What is a dolerite dyke?
The Amata Dolerite is a mafic dyke suite that intruded the late Paleoproterozoic to Mesoproterozoic basement rocks of the Musgrave Province during the early Neoproterozoic at c. 800 Ma. Dykes of the Amata Dolerite occur within the Musgrave Province together with dykes of the older c.