The Puu Oo eruption of Kilauea Volcano, Hawaii; episodes 1 through 20, January 3, 1983, through June 8, 1984

@inproceedings{Wolfe1988ThePO,
  title={The Puu Oo eruption of Kilauea Volcano, Hawaii; episodes 1 through 20, January 3, 1983, through June 8, 1984},
  author={Edward W. Wolfe},
  year={1988}
}
-------------------------99 Introduction ------------------------99 Methods --------------------------99 Lava temperatures -------------------99 Sampling ------------------------102 Chemical analyses---------------------102 Results -------------------------102 Explanation of tables --------------------102 Vent nomenclature -------------------103 References cited ----------------------103 

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Calculations based on the volume of extruded lava support this inferred increase in supply rate

Puu Oo eruption
  • (Wolfe and others,
  • 1987
VIEW 5 EXCERPTS
HIGHLY INFLUENTIAL

Additional variation results from mixing of such differentiated magma with new magma intruded from the summit reservoir. [In this report, we adopt the terminology of Wright and Fiske

Wright, Fiske
  • 1971
VIEW 8 EXCERPTS
HIGHLY INFLUENTIAL

If magma is injected into the conduit only sporadically, the only source of continuous motion in the conduit during repose periods is the rise and escape of gas bubbles from the magma

Dvorak, Okamura
  • 1984
VIEW 4 EXCERPTS
HIGHLY INFLUENTIAL

were probably eliminated by the short immersion times (generally several minutes for the V4-in.-diameter thermocouple but less than 1 minute for the %6-in.-diameter thermocouple)

Wright, Okamura
  • 1977
VIEW 5 EXCERPTS
HIGHLY INFLUENTIAL

The increasing gravitational load and southward widening with depth to about

Crosson, Endo
  • 1982
VIEW 3 EXCERPTS
HIGHLY INFLUENTIAL

Lengths of Hawaiian lava flows

VIEW 3 EXCERPTS
HIGHLY INFLUENTIAL