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Microbial life can thus exist in isolated geothermal refuges despite long-term subfreezing surface conditions.
The geothermal gradient data in this study are derived from systematic steady-state measurements, oil and gas testing, and temperature logging.
This section presents some indirect and direct evidence of hydrogen production in the seafloor and in continental geothermal systems.
Often permafrost has disappeared because the geothermal heat flux is slightly greater than elsewhere.
As the authors point out, geothermal energy is, at best, a semi-renewable resource, akin to 'mining' heat from the ground.
Nearisothermal decompression and partial melting indicate a high geothermal gradient.
The trade-off between geothermal gradient and denudation generally means that the two thermal methods may overestimate denudation.
Monitoring is also important in the case of reinjection of cooled geothermal water, which is much preferable to surface disposal on environmental grounds.
A non-volcanic, topographydriven geothermal system, harboring a microbiological community, operates in an extremely cold environment and discharges through solid ice.
The most important temperature data used to characterize the geothermal field of sedimentary basins are those from systematic steady-state temperature measurements and well tests.
This process also increases the depth extent of the high geothermal gradients in the mid-upper crust, potentially promoting conditions for crustal melting.
The rather high geothermal gradients suggested by this calculation may well result from regional magmatism, as discussed above.
Tests on the subsurface would require locating geothermal regions associated with ground ice and sampling the ice for geochemical analysis.
However, three indices lend support to geothermal activity, just not necessarily mantle derived.
It decided to keep the shaft open until it would be possible to organise regular geothermal observations within it.