-
referred to as cryolava; it
originates from a
reservoir of
subsurface cryomagma.
Cryovolcanic eruptions can take many forms, such as
fissure and curtain...
- in cryovolcanism, the
water (
cryomagmas tend to be
water based) is
denser than the ice
above it. One way to
allow cryomagma to
reach the
surface is to make...
-
outer layers of the
crust and
triggering the
movement of high-viscosity
cryomagma (muddy
water ice
softened by its
content of salts) onto the surface. Kerwan...
-
eruption which does not. One
mechanism for
explosive cryovolcanism is
cryomagma making contact with
clathrate hydrates.
Clathrate hydrates, if exposed...
-
outer layers of the
crust and
facilitating the
movement of high-viscosity
cryomagma (consisting of
muddy water ice
softened by its
content of salts) onto...
- to 10000
times more quickly. The
subsurface reservoir from
which this
cryomagma emerged may have been
separate from Pluto's
subsurface ocean.
Pluto -...
- than explosive. This
means that
there was a low-viscosity
fluid known as
cryomagma that
flowed down the mountain.
Before the
discovery of
Piccard Mons, it...
- Castillo‐Rogez, J. C. (8
February 2019). "Thermal
Evolution of the Impact‐Induced
Cryomagma Chamber Beneath Occator Crater on Ceres".
Geophysical Research Letters...
-
widespread cryovolcanism, resurfacing, and tectonics,
acting as
reservoirs of '
cryomagma'
which can be
erupted onto a moon's surface. Io is unusual, as in contrast...
-
Lynnae C.; Marsh,
Bruce D. (2016-06-01). "Heat
Transfer of
Ascending Cryomagma on Europa".
Journal of
Volcanology and
Geothermal Research. 319: 66–77...
