Title: Definition of Composite Volcanoes
1Definition of Composite Volcanoes
2Composite Volcanoes - Photos
Mt. Taranaki, NZ
Mt. Tongariro, NZ
Mt. Ruapehu, NZ
3General Characteristics - Composite Cones
4Volcanic Deposits
From Academic Press, Composite Volcanoes
5Radial Distribution of Products
6Composite Volcano Lithofacies
7Stage  Geomorphic signature1 Fresh, young
cones, often dark, pristine lava flows and
summit crater visible, sharp profile not
glaciated2 Small gullies on flanks, lavas
visible and crater may exist, but degraded
cone still sharp, dark apron gone moraines
present3 Individual lava flows barely visible,
no crater, well-established gullies, construction
al surfaces dwindling planezes initiated4 No
lava flows visible, deeply incised gullies, large
planezes, little original cone surface left
considerable relief major U-shaped glacial
valleys in glaciated regions5 Barely
recognizable, low relief radial symmetry the
only clue to volcanic origin
Erosional Stages of Volcanoes
8Factors Controlling Volcano Growth
9Volcano Morphology
- Many of the controls on this shape can be
understood by considering the geometry of a cone.
The volume v of a simple cone is given by - v 1/3p r2h
- where r is the radius of the base and h is the
height of the cone. For a typical steady-state
volcano with the concave-upward profile, a more
complex exponential form is needed -
- r BeMh
- where B and M are constants found by integration.