The elevation of the Ancient Lake Päijänne transgression maximum has been studied with the aid of 27 datable Stone Age shore-side dwelling places. The transition from the Mesolithic Stone Age to the Neolithic Stone Age and the change of the discharge channel of Ancient Päijänne from the Hinkua river to the Kymi river were almost simultaneous occurrences. The absolute age, expressed in C14-years, is in the order of 5 810 + 70 years. The transgression niveau is supposed to be nearly linear
The altitudes of delta plains of the Salpausselkä endmoraines and of eskers, as well as some determi...
The connection between settlement sites and water bodies has been the most prominent characteristic ...
The sediments of Lammaslampi, a small lake situated about 32 m a.s.l. in Vantaa, were studied by mea...
The Holocene development of the Pennala basin, Southern Finland, was studied using lithostratigraphi...
The Holocene development of the Pennala basin, Southern Finland, was stud-ied using lithostratigraph...
Lake Pyhäjärvi is located on Precambrian sandstone bedrock which has been preserved from erosion on ...
Lake Ähtärinjärvi, at the northern end of the River Kokemäenjoki watercourse in northern central Fin...
The twin lakes Etujärvi and Takajärvi in Askola, southern Finland, are closely interconnected mesotr...
Lake Näsijärvi is a body of water of 265 km2 in the northern part of the Kokemäenjoki watercourse, c...
The age of peat on the bottom of palaeochannels (oxbow-lakes) was determined with C14-dating for get...
Abstract Two high-resolution pollen and charcoal analyses were constructed from sediments obtained f...
The Late Weichselian and Holocene emergence history of the Karelian Isthmus and Ladoga Karelia is re...
The Kitka lake complex (Kitkajärvi), some 300 km2 in total area, is located at an altitude of 240.2 ...
The island of Suursaari in the middle of the Gulf of Finland is exceptionally high (175 m a.s.l.). S...
The mid-Holocene Littorina transgression in southern Scandinavia is well documented. Multiple-strati...
The altitudes of delta plains of the Salpausselkä endmoraines and of eskers, as well as some determi...
The connection between settlement sites and water bodies has been the most prominent characteristic ...
The sediments of Lammaslampi, a small lake situated about 32 m a.s.l. in Vantaa, were studied by mea...
The Holocene development of the Pennala basin, Southern Finland, was studied using lithostratigraphi...
The Holocene development of the Pennala basin, Southern Finland, was stud-ied using lithostratigraph...
Lake Pyhäjärvi is located on Precambrian sandstone bedrock which has been preserved from erosion on ...
Lake Ähtärinjärvi, at the northern end of the River Kokemäenjoki watercourse in northern central Fin...
The twin lakes Etujärvi and Takajärvi in Askola, southern Finland, are closely interconnected mesotr...
Lake Näsijärvi is a body of water of 265 km2 in the northern part of the Kokemäenjoki watercourse, c...
The age of peat on the bottom of palaeochannels (oxbow-lakes) was determined with C14-dating for get...
Abstract Two high-resolution pollen and charcoal analyses were constructed from sediments obtained f...
The Late Weichselian and Holocene emergence history of the Karelian Isthmus and Ladoga Karelia is re...
The Kitka lake complex (Kitkajärvi), some 300 km2 in total area, is located at an altitude of 240.2 ...
The island of Suursaari in the middle of the Gulf of Finland is exceptionally high (175 m a.s.l.). S...
The mid-Holocene Littorina transgression in southern Scandinavia is well documented. Multiple-strati...
The altitudes of delta plains of the Salpausselkä endmoraines and of eskers, as well as some determi...
The connection between settlement sites and water bodies has been the most prominent characteristic ...
The sediments of Lammaslampi, a small lake situated about 32 m a.s.l. in Vantaa, were studied by mea...