|
|
|
|
|
Also look at Mobility as
defined by A (area inundated) - how far it is able to spread.
|
|
|
|
1. Dome collapse pfs
consistent with debris avalanches
|
|
2. Pumice flows - spread
thinner than Dome collapse flows and cold debris avalanches
|
|
3. AV2/3 = geometric
mobility parameter suggested by this analyses where resisting shear stress is
assumed as ~ constant.
|
|
4. This is independent of
volume, large scatter.
|
|
5. Pumice flows are almost
are an order of magnitude more mobile than dome collapse flows of a
|
|
similar volume
|
|
|