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In 1842 Justus von Liebig had visited England under the guidance of his former student at Giessen, Lyon Playfair, and after ample inspection of cities, and numerous contacts with bigwigs, had con- cluded that England ist nicht das Land des Wissensehaftes.
There is a queer element of the fortuitous in both events.
Even when scientists prepare perfect diets for the inhabitants of towns, there remain the causes which have tended to weaken the stomach.
In the villages, open air, plenty of manual exertion, simple and un- sophisticated food and occasional fasting, with few opportunities for excessive indul- gence, keep the peasantry healthy and robust.
Thus he came to recognise the other volatile possibilities concealed by this unsavoury refuse, and in 1848 patented his naphtha- lamp, long used in gipsy-caravans and country -fairs. Those were empirical days, and Professor Morgan’s picture of Dan Dawson illuminates the period.
Bom in 1809 at Bradford, Eead Holliday began in 1830 to distil ammonia from gas-works liquor, and offered this new wool-cleanser to the manufacturers of Huddersfield, where he bought a strip of land on the river Colne and invited the local gas-works to dump its tar thereon.
Modern civilised man lacks leisure, peace, open air, exercise and appetite.
4 Data on Post-Glacial Climatic Changes in North-West India . Professor Morgan has laid under deep obligation all those to whom the early history and the early chemistry of artificial dye-manufacture appear momentous and engrossing.
The question of nutrition is primarily the problem of the urban population on whom the pressure of all the complicated factors of the civilisa- tion impinges.
The progress * f material civilisation, as it affects the educated communities, seems to be almost in conflict with the physical health, hardihood and efficiency which characterised the generation belonging to the early Christian era.
“CURRENT SCIENCE A MONTHLY JOURNAL OF SCIENCE VOLUME V (JULY 1936— JUNE 1937) BANGALORE CITY: THE BANGALORE PRESS, MYSORE ROAD n ? The terminal moraines of the fourth glacia- tion w r ere observed between 7,500 and 8,500 feet above sea-level, and in most cases the corresponding trough was appreciably smaller than the higher trough scooped out by the third glaciers.
This correlation permits of dating the second Himalayan ice-advance as being of Boulder Conglomerate or Middle Pleistocene age, so that the following third and fourth glacia- tions would fall into the Upper Pleistocene.