In a new study led by the University of Sussex, geoscientists from the British Geological Survey and the Technical University of Munich reveal that using a micro-seismic technique, which detects tiny earthquakes which cause cracks in the rock, alongside modern electrical imaging technology, which
measures rock mass, would provide scientists with much earlier warnings of potential rock falls.
Not exact matches
What we would like to do is move down to about three, two, and one Earth
mass, and to do that you need to make sure the instrument you're using to
measure those wobbles is
rock steady.
By looking at the ratio of two of these cosmic - ray - made elements — aluminum - 26 and beryllium - 10 caught in crystals of quartz, and
measured in an accelerator
mass spectrometer — the scientists were able to calculate how long the
rocks in their samples had been exposed to the sky versus covered by ice.
Aaron Satkoski, a scientist in the Department of Geoscience at UW — Madison, with the
mass spectrometer used to
measure isotopes in
rocks from South Africa.
Specifically, they
measured hydrogen and its isotope, deuterium (hydrogen with an extra neutron in its nucleus) with ion microprobes, which use a focused beam of ions to sputter ions from a small
rock sample into a
mass spectrometer.