An almost thermally stationary world would finally result, where the only thermal changes would be the slow temperature increase due to the heat flow from the interior of the Earth and the transient effects related to tectonic movements, like earthquakes and volcanic eruptions.
(the transient effects; related; to tectonic movements, like earthquakes and volcanic eruptions) (An almost thermally stationary world; would result; T:finally) Context(An almost thermally stationary world would result,List([0, 57))):(the only thermal changes; would be; the slow temperature increase due to the heat flow from the interior of the Earth and the transient effects)
An almost thermally stationary world would result,List([0, 57))
the transient effects An almost thermally stationary world the only thermal changes
related would result would be
to tectonic movements, like earthquakes and volcanic eruptions
T:finally
the slow temperature increase due to the heat flow from the interior of the Earth and the transient effects