Page 46 - The Restless Earth Fossils
P. 46

so Many Fossils, so little time  45


                          century that they might be able to determine the age of the Earth
                          if they could figure out how long it would take for a planet-sized
                          blob of matter to cool down from a completely molten state.
                             The right man for this task appeared to be a Scottish math
                          teacher’s son named William Thompson (1824–1907), who later
                          became  Baron  Kelvin  of  Largs,  or  Lord  Kelvin  for  short.  Lord
                          Kelvin became a university freshman in 1834 when he was 10 and
                          had written his first mathematical paper by the age of 17. By the
                          time his career was over, he had written 500 scientific papers, had
                          invented  electrical  meters  and  navigation  aids,  and  had  helped
                          create the transatlantic cable between the United States and Great
                          Britain. In other words, the man had credentials.
                             Lord Kelvin did some math. He made a few general assump-
                          tions about the melting temperature of rock and whether some
                          heat  energy  might  come  from  other  chemical  reactions  as  the
                          Earth  cooled.  He  knew  his  figures  were  somewhat  rough,  but
                          overall he decided the Earth could not be much older than 100
                          million  years.  He  also  figured  the  Earth  would  have  been  cool
                          enough for living things to evolve for perhaps 20 to 25 million
                          years. That is a long time, but was it long enough for the pro-
                          cesses of evolution described by Darwin and supported by Lyell
                          and other scientists of the day? Could the great Lord Kelvin be
                          wrong?  Could  something  else  be  keeping  the  Earth  warm  over
                          much longer stretches of time?
                             In 1898, Marie (1867–1934) and Pierre Curie (1859–1906)
                          discovered radium and polonium in pitchblende, an ore of ura-
                          nium. These new elements gave off unusual amounts of energy in
                          the form of X-rays and subatomic particles, which Marie called
                          radioactivity.  Later,  in  1903,  Pierre  Curie  and  Albert  Laborde
                          found that radium gave off significant amounts of heat.
                             Ernest Rutherford (1871–1937) did further studies on radium
                          and confirmed its heat-generating properties. In a 1905 article in
                          Harper’s Magazine he wrote, “In the course of a year, one pound
                          of radium would emit as much heat as that obtained from the
                          combustion of one hundred pounds of the best coal, but at the









        RE_Fossils2print.indd   45                                                             3/17/09   8:59:34 AM
   41   42   43   44   45   46   47   48   49   50   51