scholarly journals I.—The Recent Geological History of the Baltic. Part II: The Ancylus Sea and the Baltic Breach

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:

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 (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:—


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.


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.


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.


2000 ◽  
Vol 30 (3) ◽  
pp. 474-476 ◽  
Author(s):  
LUIZ JOSÉ TOMAZELLI ◽  
SÉRGIO REBELLO DILLENBURG ◽  
JORGE ALBERTO VILLWOCK

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