The temperature range covers typical values expected in magma chambers.
The main magma chamber was situated under the present lake of Bracciano.
How about in some giant, empty magma chamber, beneath a volcano?
How large is the magma chamber that is currently under Yellowstone?
Instead of photosynthesis, this life depends on hot water rising from the magma chambers as its energy source.
They also show a link between surface behaviour and the size of the deeper magma chamber.
We know the top level of this magma chamber.
Water flowing through the channels is diverted into some sort of magma chamber.
This is commonly known as an inversion of the magma chamber.
As a result, they provide a unique opportunity to study the relationships between magma chambers and their lavas.