Geological Time
Found in 11 Collections and/or Records:
Correspondence: from Duncan M Irvine to Alfred John Jukes-Browne, 1865-1899
The Correspondence: from Duncan M Irvine to Alfred John Jukes-Browne sub-series consists of:
- 44 letters, alphabetically arranged (1865-1899)
Correspondence: John Strong Newberry to John Perry, 1863-1900
The Correspondence: John Strong Newberry to John Perry sub-series consists of:
- 37 letters, alphabetically arranged (1863-1900)
Correspondence: WA Herdman to Joseph Dalton Hooker, 1872-1900
The Correspondence: WA Herdman to Joseph Dalton Hooker sub-series consists of:
- 33 letters, alphabetically arranged (1872-1900)
Lecture on 'The Origin of the Scenery of the British Isles', 1884
Notes for 5 lectures on 'The Origin of the Scenery of the British Isles' given to the Royal Institution in 1884, along with printed abstracts. Sir Archibald Geikie focused on geological formations around the British Isles, with comparisons from European and North American locations, looking at the materials of which they are composed and the processes which went into their creation.
Lecture on the 'Volcanic History of Britain', 1886
Notes for 4 lectures on the 'Volcanic History of Britain', given to the Royal Institution in 1886. Sir Archibald Geikie looked at the emergence of types of geological formations against a geological timeframe and how they have been affected by various processes, especially the action of volcanoes and materials produced by them, within the natural world. He used examples from numerous locations from different parts of the British Isles.
Lectures on American geological history, c1879
Notes and text for seven lectures looking at the geological history of the American continent, looking at specific locations therein, based partly on results from American survey work. These locations were related to to other places around the world, particularly in Britain and Europe. A variety of geological formations were looked at, including that of the continent itself, considering the materials which make them up and the geological timeframe.