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Discharge rate = 87 m3 /s, R c = 16 m, T = 980°C, n0 = 4.0 wt%, L = 6 km, ω = 3.8, E w = 0. Observation of the co-eruptive ground deformation 6 7 km northwest of Shinmoe-dake's vent, identified it as being the location of the magma chamber, as opposed to being just beneath the vent (Kozono et al., 2013; Nakao et al., 2013; Ueda et al., 2013).
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The relocated hypocenters (98 events) roughly coincide with alignments of eruptive vents identified by remote sensing images obtained by Geospatial Information Authority of Japan (Geospatial Information Authority of Japan 2014) (white masked area in Fig. 4 a).
As noted, the strike direction of the dike is roughly parallel to the alignment of the vents identified from high-resolution imagery (Observations from spaceborne optical and SAR imagers section).
The 2007 eruption was so small that it was not recorded visually; however, it appears that the eruption reactivated a vent of the 1979 eruption because no new vents were identified in the subsequent field survey.
Although small changes (e.g., the appearance of small vents) were identified thereafter, no significant change was detected (Figs. 3 aa)–(ll)).
On 28 December 1963, pyroclastic activity at a new submarine vent Surtla was identified ~2 km to the NE of Surtsey.
A unique thermophilic fermentative hydrogen-producing strain H53214 was isolated from a deep-sea hydrothermal vent environment, and identified as Caloranaerobacter azorensis based on bacterial 16S rRNA gene analysis.
Among the up-regulated genes in mussels collected at the Rainbow vent field, we identified a 60S acidic ribosomal protein and a selenoprotein.
Among the genes significantly up-regulated in mussels collected at the MG vent field, we identified some metabolic genes such as arginine kinase and carbonic anhydrase (CA).
The Auckland Volcanic Field covers 360 km2 and contains 50 identified vents.
The harrat ('volcanic-field') has a total erupted volume of ~2000 km3 (Blank and Sadek 1983) from at least 968 identified vents (Runge et al. 2014, Fig. 1a) and is predominantly basaltic with some more evolved compositions.
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