Lecture 7 - During the Eruption Flashcards
What are the Products of Effusive Eruptions?
-Lava flows (basaltic or rhyolitic)
-Basaltic comes in two forms; ah ah and pahoehoe (ah ah is hotter and faster flowing, pahoehoe slower and forms a smooth crust)
-Rhyolitic flows are very rare, highly viscous and don’t travel far
What are the Products of Explosive Eruptions?
-Pele’s tears (volcanic glass droplets) low velocity lava
-Pele’s hair (fine strands of volcanic glass) high velocity lava
-Tephra (bombs, scoria, pumice, ash)
What are Volcanic Bombs?
-Large chunks (>64mm) of lava that have been blown into the air
-Big version of Pele’s tears
-Relatively light as they are full of gas
-Pumice: -floats (lots of vesicles)
-felsic composition
-not very dense
What are Lapilli?
-Smaller (2-64mm) fragments of rock
-Basaltic lapilli is called scoria
What are Lithic Fragments and why are they Useful?
-Fragments of bedrock around volcano or within volcanic conduit
-Appearance of them in tuff tells us that the volcano became unstable at this stage during the eruption
-Volcano was torn apart and incorporated these fragments into the ash column
What is the Eruption Column?
-Super-heated cloud of tephra and gas
-Can rise 10s of kilometres into the air
-Rise is generated by heat and pressure from below, generating giant convection currents
-These inject gasses into the stratosphere
What are the Different Types of Lava Structures?
-Pillow lava
-Lava tubes
-Lava tubes
How do Pillow Lavas Form?
-Each pillow forms a glassy crust and expands like a balloon
-This ruptures to form a new pillow
-Top layer of the oceanic crust is made of these
-Piles of them make new landforms
How do Lava Tubes Form?
-Hollow tunnel where lava used to flow
-Form when the top of a low-viscosity lava flow cools forming a thick crust
-Lava moves underneath, draining out and leaving a tunnel
How do Lava Trees Form?
-Lava flows travel through forests at a high level
-When lava meets a tree, the sap creates a protective barrier which preserves and almost fossilises the tree
-Lava eventually drains to a lower level which leaves the cooled margins as fossil remnants of the trees
What are Pyroclastic Density Currents?
-Mixture of super-heated gas and ash (up to 1000C)
-Fast-moving (up to 700km/h)
-Deadliest volcanic hazard
-Burn everything in their path
-Rock deposits from these are called ignimbrites
What are the 3 Different ways in which Pyroclastic Density Currents Form?
-Dome collapse
-Directional blasts
-Column collapse
How does Dome Collapse create a PDC?
-Structure at the top of the volcano collapses under gravity
-This forms an avalanche becoming a pyroclastic density current
How does a Directional Blast create a PDC?
-Caused by a particular side of a volcano collapsing/ exploding
How does Column Collapse create a PDC?
-Eruption column of gas keeps rising due to convection
-If this heat runs out, the column collapses
-Gas and ash roll down the valleys in the form of a PDC