II.—The Recent Geological History of the Baltic and Scandinavia and its importance in the Post-Tertiary History of Western Europe

1918 ◽  
Vol 5 (10) ◽  
pp. 451-461
Author(s):  
Henry H. Howorth

Let us now turn to the lessons presented by the Mollusca found in the raised beaches of Norway and Western Sweden.

1905 ◽  
Vol 2 (7) ◽  
pp. 311-320
Author(s):  
Sir H. H. Howorth

The recent history of the Baltic involves problems of great interest and importance, and promises to afford considerable help in solving the mysteries of the later geological changes in Western Europe. It is therefore worth a closer study than has been extended to it in this country. Perhaps I may be permitted to condense in the Geological Magazine what has been written about it in late years by the Scandinavian geologists, and to add some inferences of my own. I am especially indebted to De Geers and Munthe, the latter of whom has written quite an ideal monograph on one section of the story in the Bulletin of the Geological Institution of the University of Upsala, vol. ii.


1918 ◽  
Vol 5 (8) ◽  
pp. 354-367 ◽  
Author(s):  
Henry H. Howorth

Some years ago I was allowed to publish in the Geological Magazine some papers on the recent geological history of the Baltic, in which I tried to bring before English readers the very important discoveries of the Northern geologists as affecting the general geology of the north-west of Europe and to extend their deductions. I was obliged to interrupt them for other work. Perhaps you will allow me to continue them some steps further, as we had reached a stage of some interest.


1905 ◽  
Vol 2 (8) ◽  
pp. 337-353 ◽  
Author(s):  
H. H. Howorth

In the previous paper I ventured to trace the history of the Baltic back to the time when the latest of its raised beaches were laid down, and to show that it was then considerably larger in size, and that its waters were more salt than they are now, although they were even then brackish (see Map I, Pl. XIX).This conclusion was derived mainly from an examination of the molluscan remains in the more recent shell-beds. It is confirmed by other evidence; thus, Munthe mentions the occurrence in the so-called Litorina beds of three species of Rhizopods, whose present and former distribution in the Baltic is shown in the following table:


2012 ◽  
Vol 21 (2) ◽  
pp. 133-143
Author(s):  
THOMAS KÜHNE

Scholarship is not only about gaining new insights or establishing accurate knowledge but also about struggling for political impact and for market shares – shares of public or private funds, of academic jobs, of quotations by peers, and of media performances. Timothy Snyder's Bloodlands fights for recentring contemporary European history.1 No longer, his new book implies, should the centre of that history be Germany, which initiated two world wars and engaged with three genocides; even less should the centre be Western Europe, which historians for long have glorified as the trendsetter of modernity; and the Soviet Union, or Russia, does not qualify as ‘centre’ anyway. Introducing ‘to European history its central event’ (p. 380) means to focus on the eastern territories of Europe, the lands between Germany and Russia, which, according to Snyder, suffered more than any other part from systematic, politically motivated, mass murder in the twentieth century. The superior victimhood of the ‘bloodlands’ is a numerical one. Fourteen million people, Jewish and non-Jewish, in the territories of what is today most of Poland, the Ukraine, Belarus, western Russia, and the Baltic States did not become just casualties of war but victims of deliberate mass murder. Indeed, this is ‘a very large number’ (p. 411), one that stands many comparisons: ten million people perished in Soviet and German concentration camps (as opposed to the Nazi death camps, which were located within the ‘bloodlands’), 165,000 German Jews died during the Holocaust (p. ix), and even the number of war casualties most single countries or territories counted in the Second World War was smaller.


2010 ◽  
Vol 3 (3) ◽  
pp. 350-373 ◽  
Author(s):  
Göran Larsson ◽  
Egdūnas Račius

AbstractWhile the ever more strongly felt presence of Muslims in western Europe has already stimulated numerous scholars of various social sciences to embark upon research on issues related to that presence, it is apparent that just a few studies and introductory text books have so far dealt with the evolution of Muslim communities in other parts of Europe, especially in countries of central, eastern, and northern Europe. Without appreciation of and comprehensive research into the more than six-hundred-year-long Muslim presence in the eastern Baltic rim the picture of the development of Islam and Muslim-Christian relations in Europe remains incomplete and even distorted. Therefore, this article argues for the necessity of approaching the history of Islam and Muslims in Europe from a different and ultimately more encompassing angle by including the minorities of Muslim cultural background that reside in the countries of the European part of the former Soviet Union—the Baltic states and Belarus. Besides arguing that it is necessary to reconsider and expand the research field in order to develop more profound studies of Islam and Muslims in Europe, the article also outlines suggestions as to why the Muslim history in the eastern Baltic rim has been generally excluded from the history of Islam in Europe.


1905 ◽  
Vol 2 (9) ◽  
pp. 407-413
Author(s):  
H. H. Howorth

In two previous papers I have set out the conclusions generally held by Northern geologists in regard to the more recent history of the Eastern Baltic, according to which it was once a great enclosed fresh-water lake or sea, the Ancylus lake, which by the breach in the land-bridge connecting Skäne and Denmark was converted into a brackish-water sea, the Litorina sea, which has in turn become less and less saline until it has reached its present condition.


1905 ◽  
Vol 2 (12) ◽  
pp. 550-562
Author(s):  
H. H. Howorth

In the first part of this series, p. 313, I referred to the recent invasion of the Eastern Baltic by the Mya arenaria, as first pointed out by Dr. Nathorst. Dr. Petersen has called my attention to an important paper by A. S. Jensen, which has apparently been overlooked by English conchologists, and I propose to condense his results, as they are very noteworthy from their geological lessons.The shell has hitherto been treated as a typical Arctic shell. Thus Crosse and Debeaux write of its original home: “De l'océan Glacial arctique, qui parait être sa véritable patrie, elle est descendue dans les mers du nord de l'Europe, jusques et y compris la Manche etune partie de nos côtes de l'Océan” (Journ. de Conchologie, ser. III, iii, 254, 1863). Gwyn Jeffreys, in describing the shell, says, “The occurrence of this circumpolar shell-fish so near the tropic of Cancer probably indicates the most southern limit in space of the glacial epoch” (Brit, Conch., iii, 65, 66).


1905 ◽  
Vol 2 (10) ◽  
pp. 454-462
Author(s):  
H. H. Howorth

Proceeding westward, the fauna again increases in richness. The molluscan fauna of the Gulf of Kiel has been elaborately described by Meyer and Möbius in their well-known work entitled “Fauna der Kieler Bucht.” They thus enumerate the shells found there:—


Author(s):  
J. D. Peacock

SynopsisThe Quaternary features and deposits provide a record of the geological history of the past 18,000 years and only a few elements of the landscape, such as the glaciated rock platforms and cliffs of marine origin, can be ascribed to earlier times. Mainland ice almost certainly covered the islands during the last glaciation, its retreat being temporarily reversed or halted perhaps more than once. There was a final well-marked, but short-lived episode of valley glaciation some 10,000 to 11,000 years ago. Glacial deposits, raised beaches, periglacial features, landslips and the post-glacial accumulations of peat, shell sand and diatomite are discussed briefly.


1997 ◽  
Vol 31 (3) ◽  
pp. 583-601 ◽  
Author(s):  
R. I. Moore

Although they still differ considerably in their willingness to acknowledge it, specialists in the history of north-western Europe in the eleventh and twelfth centuries CE are increasingly treating it as that of the emergence of a new civilization in what had previously been a peripheral region of the Mediterranean-based civilization of the classical west, rather than as a continuation or revival of that civilization itself. In this light Europe, or Latin Christendom as it saw itself, offers a number of striking resemblances to the developments which Lieberman discusses. The most dynamic regions of the new Europe—north-western France, Flanders and lowland England, north-eastern Spain, northern Italy, southern Italy and Sicily—were all peripheral, though in various senses, both to the long-defunct classical civilization and its direct successors, the Byzantine and Abbasid Empires, and to the transitional and much more loosely based ninth-and tenth-century empires of the Franks and Saxons (Ottonians). To this one might add that by the end of the twelfth century the remaining rimlands of the Eurasian continent in a purely geographical sense—Scandinavia, including Iceland, and still more the southern coast of the Baltic and the areas dominated by the rivers which drained into it—were developing very rapidly indeed.


Sign in / Sign up

Export Citation Format

Share Document