Sentence examples for continuing fault from inspiring English sources

Exact(1)

Both amendments were overwhelmingly defeated in subcommittee votes, and later by the full committee, in a debate that highlighted the party's continuing fault lines.

Similar(57)

Although non-volumetric faulting can generate crustal deformation, it is unlikely to continue fault motion up to a few minutes at a shallow depth of a volcano.

5) Continued faulting along the outer rise will further reduce continuous reflections from the TIC.

Many continued to fault the Securities and Exchange Commission and other regulators for not catching the scheme earlier.

Mr. Romney continues to fault Mr. Obama for not leading on Syria, where thousands have died at the hands of President Bashar al-Assad's forces.

Federal regulators have continued to fault the McNeil unit for failing to identify and address systemic problems at its plants, and consumers remain mystified about why simple products like O.B. tampons can disappear from drugstore shelves.

As critics continue to fault Mr. Obama less for his administration's overall response to the spill than for what they say has been his own slow and reactive leadership style, the ultimatum to BP and the president's use of the solemn setting of the Oval Office escalate his personal engagement to a new level.

The BBB continues to fault the coalition for making misleading fund-raising appeals and having too small a board of directors.

F5 and F4 cutting the horizon Open image in new window Fig. 8 Travel time of horizon H5 at 23.55 s., with master faults continue, continuous to discontinuous reflection with high and low amplitudes and chaotic area.

"What's absolutely stunning is that we see the fault continuing to slowly creep at the surface - by up to 10 cm over a couple of months," explained Prof Tim Wright from the UK's Nerc Centre for the Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET).

The highest horsts (Osogovo, Rila, Pirin, and Belasitsa) experienced additional uplift in the Pleistocene, in part as a result of regional uplift and in part through continued normal faulting.

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