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The length (L) is defined as 96% of the total length on the water-line at 85% of the least molded depth, or as the length measured from the fore side of the stem to the axis of the rudder stock on the water-line, if that is greater.
The dusky dolphins has a long, light-grey patch on its fore side leading to a short, dark-grey beak.
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The gas is trapped between the impellers and the stator wall and transferred from the high vacuum to the fore vacuum side of the pump.
It most likely detonated in the forward engine room, sparking flames, and causing heavy flooding in the magazines of main battery turret number two and the fore port side secondary battery turret, and putting even more pressure upon the previously stressed hull girder.
Positive basin inversion is documented using seismic reflection profiles and seismic data on the fore-arc side of the back-arc rift system of northern Honshu, Japan.
Seismic reflection profiles and Bouguer gravity anomalies along with available surface and subsurface evidence define a >300-km-long normal fault system, formed in Miocene time, that bounds the fore-arc side of the Miocene back-arc basin.
Geothermal gradients on the fore-arc side commonly range ~20 to 40 °C/km (Tanaka et al. 2004).
The mountains on the fore-arc side are relatively wide, have gentle slopes, and low-relief surfaces (Fig. 1b).
In the Abukuma Mountains on the fore-arc side, apatite FT ages of 100.0 46.0 Ma have been reported (Goto 2001; Ohtani et al. 2004) (Fig. 1a).
However, recent dense seismic observations reveal that the σ 1 axes are oblique to plate convergence directions on the fore-arc side (Yoshida et al. 2015a).
AHe ages show obvious contrast among the different morphostructural provinces: 64.3 49.6 Ma in the Abukuma Mountains on the fore-arc side, and 11.4 1.5 Ma in the OBR along the volcanic front and the Asahi Mountains on the back-arc side.
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