This is for a planned wide-audience writing project on evolution, in which I pre-empt (rather than respond to) creationists’ counter-arguments, such as their downplaying of historical science. I would greatly value comments on this approach.
There are sciences, such as physics and chemistry, where we can perform experiments. There are other sciences, such as the science of planetary motion (and astronomy in general) where we cannot do this, but we can still carry out repeated observations in well-controlled circumstances, and devise theories with whose help we can make definite predictions. All of these are what I will call rule-seeking sciences. At the other extreme, we have sciences such as palaeontology and much of geology, which one might call historical sciences.1 With these, the aim is not so much to establish general rules, as to unravel and explain the specifics of what happened in the past. It is usual to regard the rule-seeking sciences as the most rigorous, to which the others should defer. This shows a deep misunderstanding of how science works, and, time and time again, when historical and rule-seeking sciences have come into conflict, it is historical science that has triumphed.
From my friend the Rev Michael Roberts. How Buckland and then Darwin, exploring in Wales, came to accept Agassiz’ Ice Age theory, with Michael’s own stunning images of locales. And no kittens, I’m afraid, but a field assistant [sic] dog
In June 1842 Charles Darwin undertook his last geological field trip. He was at his father’s house, The Mount in Shrewsbury, that month and after a winter of sickness, he felt somewhat better. Thus, he went in his gig to Snowdonia to assess whether Buckland was correct in identifying proof of a former Ice Age. In October 1841 William Buckland travelled to Wales with Thomas Sopwith (his grandson designed the Sopwith Camel, a WW1 fighter plane) to see whether Agassiz could be right about a former Ice Age. In a few days of horrendous Welsh weather Buckland identified all the main glacial troughs
Buckland dressed for Welsh Glaciers by Thomas Sopwith
View from top of Y Garn 3104ft showing the Llugwy trough leading to Capel Curig, Llyn Idwal, a morainic lake.
To the left is Nant Francon, viewed below – with embellishments.
In 1831 de la Beche painted this watercolour…
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