| 000 -LEADER |
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| fixed length control field |
02195nab a2200181 4500 |
| 003 - CONTROL NUMBER IDENTIFIER |
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| control field |
GSMBLIc |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION |
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| fixed length control field |
230522b ||||| |||| 00| 0 eng d |
| 041 ## - LANGUAGE CODE |
|---|
| Language code of text/sound track or separate title |
Einglish Language |
| 100 ## - MAIN ENTRY--PERSONAL NAME |
|---|
| Personal name |
Lewis, R.G. |
| 9 (RLIN) |
22838 |
| 245 ## - TITLE STATEMENT |
|---|
| Title |
The influence of earth movements on climate |
| 300 ## - PHYSICAL DESCRIPTION |
|---|
| Extent |
64-73p. |
| 520 ## - SUMMARY, ETC. |
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| Summary, etc. |
Extract<br/>In the early days of the study of glaciation the problem appeared to be a simple one: we are used to an ice-bound North Pole, and it was natural to assume that the boundary for some reason spread southwards to cover Scandinavia, Scotland, and even some of England. When it was further learnt that North America showed signs of extensive glaciation, this news fell naturally into place and scientists began to form hypotheses to account for a worldwide refrigeration. Quite soon, however, investigators in the countries concerned began to disagree as to the phases, and even the number, of glaciations: the centre of dispersal of the Scandinavian ice was found to be near the head of the Gulf of Bothnia; English geologists were inclined to favour only one glaciation, with certain retreats and advances; Boule would allow three glaciations, while Penck and Bruckner in their classical work on the Alps proved four in their region; Günz, Mindel, Riss, and Würm (with a short climatic improvement at the maximum); followed by the Bühl advance, Gschnitz Stadium and Daun readvance. But these Alpine phases cannot be followed into Italy. Gortani says (1): “Among us, too, Penck had disciples; and we, too, sought all means of adapting his system to the observed facts. But all attempts are vain because (a) nowhere are Günzian moraines to be found; (b) nowhere are to be found traces of more than one true interglacial with a warm climate and (c) the last two advances of the glaciers, where they have left separable traces, show themselves as two principal phases of one glaciation of medium intensity.” |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
|---|
| Topical term or geographic name entry element |
Influence of climate - For earth movement |
| 9 (RLIN) |
22839 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
|---|
| Topical term or geographic name entry element |
Glaciation |
| 9 (RLIN) |
8961 |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
|---|
| Topical term or geographic name entry element |
Earth movement |
| 9 (RLIN) |
1906 |
| 773 0# - HOST ITEM ENTRY |
|---|
| Host Biblionumber |
1913 |
| Host Itemnumber |
2201 |
| Place, publisher, and date of publication |
London Dulau & Co, Ltd 1935 |
| Other item identifier |
002562 |
| Title |
Geological magazine : Vol. 72 Iss. 1-12 Year. 1935 |
| International Standard Serial Number |
00167568 |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) |
|---|
| Source of classification or shelving scheme |
|
| Call number suffix |
{082b} |
| Koha item type |
Article |
