As a geologist he had limitations which he clearly recognised.
Palæontology, petrology, and mineralogy he had a sound working
knowledge of, but he never professed to know them thoroughly, and
much of the teaching of these subjects he left to specially trained
assistants. Had he been better equipped in these respects, he might
have avoided some of the pitfalls into which he stumbled at times.
But in physical and structural geology he took a very high place
among living scientists. The thorough training and natural aptitude
for structural and field geology made him a very shrewd judge of
controversial questions in tectonics, and laid a secure foundation
for his researches in geographical evolution and the origin of the
earth’s surface features. As a geographer, interested especially in the
larger problems of geographical configuration, he earned a world-wide
reputation. His special field of work, however, was the history of the
glacial period in all its aspects, and as time went on he came to be
recognised as the most thorough-going advocate of repeated glacial and
interglacial epochs. The positions he took up at a very early stage
in his scientific career he maintained with little modification till
its close, and in spite of indifference and in the face of severe
criticism he saw his theories more and more completely established year
by year. The subject is one of the most controversial in geological
science at the present day. Very eminent authorities may be found who
deny the validity of nearly every one of Prof. Geikie’s conclusions
about interglacial epochs, but there is a large and increasing body
of supporters of his views, though even now the extreme position he
took up in subdividing the Ice Age into six glacial periods cannot be
said to be generally accepted. But if we compare the text-books of the
present day with those published twenty years ago, we can realise how
great an advance has been made in the direction in which he led; and
there can be no doubt that in the long-run his consistency, courage,
and sagacity will receive full recognition.
The old Scottish school of geology which had numbered so many
famous men among its members found in James Geikie one of its most
distinguished representatives. In science, as in all things, he was
pre-eminently a Scotsman. Ramsay and Croll, two of the most philosophic
geologists of their time, were the men to whom he owed the inspiration
which originally directed him, and he was a true disciple of Playfair,
whose memory he reverenced. In all his writings he places in the
foreground the observations which he and his fellow-workers in Scotland
had made in the field, and the inferences drawn from them; and it was
in no small measure to James Geikie that the high position which the
work of Scottish geologists holds in the estimation of scientific men
is to be ascribed.
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