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Endogenous domes

Anticipated collapse modes are examined for contrasting small (200 m) and large (350 m) endogenous dome geometries, for varied inclinations of the detachment plane, and under different conditions of interior water- and gas-pressurization, and for lobe failures resulting from only rainfall induced overpressures [Figure I). [Pg.711]

Endogenous domes-water and rind pressures only... [Pg.711]

Elsworth, D., et al. 2(X)3. Some Models of Rainfall-Triggered Collapse of Endogenous Lava Domes in Potentially Gas-Effusive Environments. To be published. [Pg.714]

See other pages where Endogenous domes is mentioned: [Pg.709]    [Pg.709]    [Pg.712]    [Pg.712]    [Pg.713]    [Pg.709]    [Pg.709]    [Pg.712]    [Pg.712]    [Pg.713]    [Pg.29]    [Pg.55]    [Pg.709]    [Pg.710]    [Pg.710]    [Pg.294]   


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