Not exact matches
Using an accelerator mass spectrometer at the Lawrence Livermore National Laboratory, the geologists
measured how much beryllium - 10 was in their samples — giving them a kind of clock to
measure erosion
over long time spans.
Someone actually wants to
measure things
over longer time spans.
But
over that
long span of
time, the ways of
measuring that data have changed dramatically, and differences in data collection mean that temperatures collected by ships in the early 20th century might be different from the data collected today.