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As one comment beneath observed, it comes out "super hard as ice!".
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The high aftershock activity observed in the NLDB area is supposed to reflect the volcanic structure beneath Asodani.
In particular, low velocities were observed beneath the central Marmara Sea at 5 km depth.
Voids observed beneath the extrusions, close to the film-substrate interface, contributed significantly to fatigue failure.
The thick mud layers which are regarded as the source of diapiric intrusions are first observed beneath the basin.
Significantly higher soil NO3 supply rates were observed beneath the mulches of non nitrophilous species (white pine and red oak).
Cumulative infiltration in the cover crop strip was intermediate between that observed beneath the trees and bare lanes.
Looking at the distribution of low-velocity anomalies, a large low-velocity pattern is observed beneath the central Marmara Sea region.
At this depth interval, high P- and S-wave velocity values are observed beneath Armutlu Peninsula, Yalova, Gazikoy, and Tekirdağ.
Another low-velocity region is observed beneath northern Kyushu at a depth of 30 km in the V p structure (33.6°N, 130.7°E).
Two distinctive reflectors at depths of 1 2 and 3 4 km were observed beneath the Miyako Saddle, and they are cut by many normal faults.
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