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Mountain peaks cal maxima ) , valley bottoms ( local mini1 ) , and passes ( saddle points representing a nimum in one direction and a maximum in second , independent direction ) are critical ints where the gradient vanishes .
Mountain peaks cal maxima ) , valley bottoms ( local mini1 ) , and passes ( saddle points representing a nimum in one direction and a maximum in second , independent direction ) are critical ints where the gradient vanishes .
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A C a Bob : What keeps these rotations aimed in the right direction ? Isn't it possible to make mistakes ? ... Its state can be in one of two transverse oscillation ( polarization ) directions ( Fig . 2C ) .
A C a Bob : What keeps these rotations aimed in the right direction ? Isn't it possible to make mistakes ? ... Its state can be in one of two transverse oscillation ( polarization ) directions ( Fig . 2C ) .
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Pre - eruption Local Fast direction 800 0 0 Overpressured dike Regional Fast direction turing the 1994 deployment , however , have verage similar to the shallow results . The ges in cannot be due to an alignment in seismometer ...
Pre - eruption Local Fast direction 800 0 0 Overpressured dike Regional Fast direction turing the 1994 deployment , however , have verage similar to the shallow results . The ges in cannot be due to an alignment in seismometer ...
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1772 | 1749 |
Cosmology and 21stCentury Culture | 1769 |
1842 | 1775 |
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