ⓘ Baltic Ice Lake

                                     

ⓘ Baltic Ice Lake

The Baltic Ice Lake is a name given by geologists to a freshwater lake that gradually formed in the Baltic Sea basin as glaciation retreated from that region at the end of the Pleistocene. The lake, dated to 12.600-10.300 BP, is roughly contemporaneous with the three Pleistocene Blytt-Sernander periods. The lake followed a period of massive glaciation in the region, which followed the end of the Eemian Sea. The post-glacial Yoldia Sea was immediately subsequent to the Baltic Ice Lake.

                                     

1. Phenomena related to ice lake and sea formation

The term lake is used to mean a body of primarily fresh water. A sea is filled with brackish or salt water. In the history of the Baltic Sea, the distinction is not always clear. Salinity has varied with location, depth and time.

The main factors are the advance or recession of the Scandinavian glacier and the isostatic sinking of the landforms due to the weight of ice or isostatic rebound springing back when relieved of it. The glacier provides a massive flow of fresh water. Salt water enters from the North Sea through straits when the sea level is high enough to allow reverse flow over the sill. When the straits are above sea level or close to sea level, fresh water will accumulate and a lake forms. Fresh water will accumulate to levels substantially higher than sea level when the sills are substantially above sea level. The release of fresh water from the glaciers depends on climate; the presence or absence of entrances to the ocean depends on land rise and oceanic water level; the latter of course is also affected by the amount of ice held in glaciers worldwide.

Several methods are used to determine the quality of ancient sea water. The main one is the type of diatoms found in the sediment. Some species require salt water, while others require fresh. Other invertebrates serve as marker species as well. Also, periods of maximum supply from melt water are marked by low organic carbon in the sediment. Higher carbon content causes greater deposition of iron sulfide, which appears as a black varve.

                                     

2. Formation

The edge of the retreating Weichselian glacier departed from the Lake Gardno end-moraines of Pomerania in present-day northern Poland at around 14.000 BP and reached the southern shore of the Baltic Sea in the time window 13.500/13.000 BP. In the next several hundred years, closed fresh-water pools formed in the southern Baltic region from melt water as the ice retreated northward. These were about 40 m 130 ft above the current sea level.

By 12.000 BP the edge of the glacier was at a line across southern Sweden to the northern shore of the Baltic countries. A connected body of water, the Ramsay Sea, stretched from the Danish islands region to the shores of Estonia. The Gulfs of Bothnia and Finland were still glaciated, as well as nearly all of Sweden north of Scania. In the Allerod warm-period, rising land in the Denmark region created the Baltic Ice Lake. It egressed through a small channel in the Strait of Oresund. The lake was higher than sea level which itself was lower than the present-day sea level by some tens of metres. Lake Ladoga formed part of the Baltic Ice Lake.

Emergence of the land then closed the channel through the Strait of Oresund. The lake rose until at about 11.200 BP it broke through a narrow corridor in the region of Mount Billingen in present-day south-west Sweden; Quaternary geologists used to describe the break-through as a massive, single tap of Niagara-like force, but it is now considered more likely that it happened in several steps over a limited period, perhaps a century, and along different local troughs and passages. By 10.800 BP the lake had dropped 55 m 180 ft. At that point the climate reverted into cooling, and during a cold-climate period the glacier advanced again over the central Swedish exit. The lake became blocked again, rose about 25 m 82 ft, and broke through the Strait of Oresund. By this time the Gulf of Finland had been deglaciated.

At the peak of this high-water phase, most of Finland was under water, including present-day Helsinki at a depth of 115 m 377 ft; only southern Sweden was both free of ice and above the waterline. The Danish Islands were all connected west of the Strait of Oresund. Around 10.500 BP the climate became warmer, the ice retreated to the north of Mount Billingen, and the waters broke through central Sweden again, providing a second egress. Water level dropped 25 m 82 ft to the sea level of that time.

                                     

3. Summary

At about 16.000 BP the retreating ice had reached the southern shores of the present Baltic. Melt water formed extensive lacustrine systems still visible today in north Russia, Poland and Germany. By 14.600 BP the Baltic Ice Lake had come into existence. Beyond it only southern Sweden was habitable, and it was an island. Scandinavia means "the island of Scandza" or "Scandia", which cannot be accounted for by todays map, and is generally assumed to be an inadvertent misrepresentation by ancient geographers. However, the first Scandinavia was an island, and was identical to southern Sweden.

Several carbon-dated sites in Estonia indicate that human habitation of the shores of the Baltic Ice Lake began in the Boreal period, in the time window 11.200-10.200 BP. Charcoal, animal bones, and artefacts from Mesolithic temporary settlements have been found at Pulli and in the Lake Ladoga region. The diet included roe deer, red deer, marten, otter, wolf, bear and ringed seal. An open pine-birch forest covered the region. Pollen from Pinus, Betula, Alnus, Rosaceae, Cyperaceae and Artemisia have been found.

Around 10.300 BP, the ice lake discharged through channels that opened in central Sweden near Mount Billingen until it reached the ocean level. The Yoldia Sea phase began 10.300-9.500 BP.



                                     
  • the ice sheet and the southern shores that were free of glacier ice This accumulation of freshwater constituted a lake known as the Baltic Ice Lake This
  • Washington state Ice Lake microprocessor Ice Lake a novel by Trevor Ferguson Lake ice ice on lakes Lake ice in the cryosphere Baltic Ice Lake retreated
  • what are now the large lakes of Sweden, and the White Sea - Arctic Sea. Eemian Sea, 130, 000 115, 000 years ago Baltic Ice Lake 12, 600 10, 300 Yoldia Sea
  • geologists to a variable brackish - water stage in the Baltic Sea basin that prevailed after the Baltic ice lake was drained to sea level during the Weichsel glaciation
  • The Baltic Sea Campaigns were conducted by Axis and Allied naval forces in the Baltic Sea, its coastal regions, and the Gulf of Finland during World War
  • its recession, the Baltic Ice Lake appeared. Baltic Ice Lake 12, 600 10, 300 years before present Yoldia Sea, 10, 300 9500 Ancylus Lake 9, 500 8, 000 Mastogloia
  • took place in the Lake Ladoga basin between 12, 500 and 11, 500 radiocarbon years BP. Lake Ladoga was initially part of the Baltic Ice Lake 70 80 m. above
  • P. being in effect one of various predecessors to the modern Baltic Sea. The Ancylus Lake replaced the Yoldia Sea after the latter had been severed from
  • Fennoscandian Ice Sheet. In Gotland 20th century cliff retreat rates have been estimated at 0.15 to 0.78 cm year. Retreat of the Baltic Klint in Gotland
  • freshwater taxa such as Mysis and Salvelinus to lakes like Sommen that were never connected to the Baltic Ice Lake The survival of these cold - water taxa into
  • struggle on the slippery surface of the frozen lake The Crusaders started to retreat in disarray deeper onto the ice and the appearance of the fresh Novgorod
  • sand dunes were formed from sediments from the Baltic Ice Lake and Ancylus Lake i.e. after the last Ice Age. Species in the nature reserve includes white - tailed