Not exact matches
We find that many geological and geochemical phenomena
associated with Snowball Earth are consistent with extensive submarine
volcanism along shallow mid-ocean ridges.»
Martian lava tubes are natural sub-surface lava tube caverns on Mars that are believed to form as a result of fast - moving, basaltic lava flows
associated with shield
volcanism.
The island's
volcanism is
associated with the rifting along the Azores Triple Junction; the spread of the crust along the existing faults and fractures has produced many of the active volcanic and seismic events, [22] while supported by buoyant upwelling in the deeper mantle, some
associate with an Azores hotspot.
Martian lava tubes are natural sub-surface lava tube caverns on Mars that are believed to form as a result of fast - moving, basaltic lava flows
associated with shield
volcanism Lava tubes usually form when the external surface of the lava channels cools more quickly and forms a...
Isostatic rebound in response to glacier retreat (unloading), increase in local salinity (i.e., δ18Osw), have been attributed to increased volcanic activity at the onset of Bølling — Allerød, are
associated with the interval of intense volcanic activity, hinting at a interaction between climate and
volcanism - enhanced short - term melting of glaciers, possibly via albedo changes from particle fallout on glacier surfaces.
Release of carbon (as CO2, CO, or CH4 and related compounds), directly from the
volcanism and
associated intrusive magmas, and from heating of carbon - bearing country rocks, doubtless acted as important drivers, but constraining the fluxes and the total amounts released is problematic.