VOLCANIC ERUPTIONS MATERIALS ASSOCIATED WITH VOLCANIC
- Factors that determine the violence of an ERUPTIONS
eruption - Pyroclastic materials
o Composition of the magma o “Fire fragments”
o Temperature of the magma o Types of pyroclastic material
o Dissolved gases in the magma Ash and dust – fine, glassy
- Viscosity of magma fragments
o Viscosity – a measure of a material’s
resistance to flow TYPES OF PYROCLASTIC MATERIAL
o Factors affecting viscosity - Pumice – from “frothy” lava
Temperature (hotter magmas - Lapilli – “walnut” size
are less viscous) - Cinders – “pea-sized”
Composition (silica content) - Particles larger than
High silica – high
viscosity (e.g., rhyolitic
lava) VOLCANOES
Low silica – more fluid - General features
(e.g., basaltic lava) o Conduit, or pipe, carries gas-rich
Dissolved gases (volatiles) magma to the surface
Mainly water vapor o Vent, the surface opening (connected
ang carbon dioxide to the magma
Gases expand near the
surface
Provide the force to
extrude lava
Violence of an eruption
is related to how easily
gases escape from
magma
o Easy escape
from fluid
magma
o Viscous magma
produces a
more violent
eruption
o Lava flows
Basaltic lavas are more fluid
Basaltic lavas are more
fluid
Types of lava:
o Pahoehoe lava
(resembles
braids in ropes)
o Aa lava (rough,
jagged, blocks)
Gases
o One to five
percent of
magma by
weight
o Mainly water
vapor and
carbon dioxide