Lecture 9 - Volcanic Evolution Flashcards
What does the Melting Point of a Rock Depend on?
-Temperature
-Pressure
-Volatiles (water and gases)
-Composition
What does the Melt Composition depend on?
-What type of rock is melted
-How much of the rock is melted
-Mantle (peridotite) melts at 1200-1300C
-Basalt melts at 900-1100C
-Granite melts at 650-850C
What is the Liquidus?
-The point where a whole rock (all minerals) is molten
What is the Solidus?
-The point where a whole rock (all minerals) is molten
How does the Source Rock affect Magma Composition?
-Mantle is ultramafic
-Oceanic crust is mafic (basalt)
-Continental curst is intermediate/ felsic (granite)
-Most the time, not all of the source rock is melted; only 2-30%
How does Partial Melting affect Magma Composition?
-Rocks are made of different minerals
-Different minerals have different melting points
-Depending on the temperature, only some of the minerals will melt to produce magma
-The lower the % the partial melt, the higher the silica content (felsic minerals have a lower melting point)
How does Magma Mixing affect Magma Composition?
-Two bodies of molten rock mix together
-This changes the melt composition, producing an average of the two
-Injection of new magma from depth tends to make the melt more mafic (higher melting point)
How does Assimilation affect Magma Composition?
-Hot molten rock is injected into cold crustal rock
-Heat transfer from magma to solid means the crustal rock is melted
-This changes the melt composition (tends to make the magma more felsic)
-Xenoliths = blocks of the crustal rock that fall into the magma chamber
How does Fractional Crystalisation affect Magma Composition?
-As magma cools, minerals crystalise faster than others
-This removes elements from the liquid
-The crystals sink/rise taking these elements with them
-The remaining liquid is a different composition (more felsic and volatile-rich)
Why does Magma Explode?
-The lower the temperature, the more viscous and therefore explosive it is
-Presence of water and gas means they expand which causes explosions
-Felsic magmas are more viscous than mafic magmas (because Si bonds together in long chains which are very difficult to break)
Describe the Characteristics of Felsic Melts
-Gasses have low melting points
-Partial melting, assimilation and fractional crystalisation concentrate gasses in the melt (making the melt more felsic and viscous)
-If no new magma is injected into the volcano, it naturally becomes more felsic over time (more gas-rich and more explosive!)
Why do Explosive Eruptions not happen often at the Same Volcano?
-Large explosive eruptions release a lot of gas and pressure from the magma chamber
-Takes time for this to build back up
-Volcano therefore becomes less explosive for some time following an explosive eruption
Describe the Santorini Volcanic Cycle
-Initially mafic intermediate melts producing effusive eruptions
-Fractional crystalisation and assimilation make melt more felsic and gassy
-Explosive Minoan eruption (c1600BC) releases gas
-Santorini returns to effusive behaviour and the cycle begins again!
-Strombolian eruptions are potentially restarting again as cinder cones are forming on the central island as magma is continuing to evolve
Give a Background on Santorini
-Island in Greece
-Active stratovolcano but with elements of others
-Constantly changing
What is the Present-Day Activity on Santorini?
-Basaltic/dacitic composition
-Low gas content and runny lava
-Shield volcano (Hawaiian-type volcanism)