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  • 1
    Book
    Book
    Der pleistozäne Untergrund der Kieler Bucht und angrenzender Gebiete nach reflexionsseismischen Messungen (1995)
    Kiel : Geologisch-Paläontologisches Inst. und Museum
    Details Availability
    Keywords: Dissertation ; Report ; Hochschulschrift ; Forschungsbericht ; Kieler Bucht ; Reflexionsseismik ; Pleistozän ; Angewandte Geophysik ; Kieler Bucht ; Geophysik ; Seismik ; Kieler Bucht ; Sediment ; Pleistozän
    Type of Medium: Book
    Pages: III, 116, VI S , Ill., graph. Darst., Kt , 1 Beil.
    Series Statement: Berichte / Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität Kiel 70
    Language: German
    Note: Zugl.: Kiel, Univ., Diss. : 1994
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  • 2
    Map
    Map
    Geologisk kort over Danmark : Kortbladet Flensborg Fjord ; Sedimentkort = Geologische Karte von Denemark [Dänemark] 1:50.000 (1994)
    København : Geological Survey of Denmark
    Details Availability
    Keywords: Karte
    Type of Medium: Map
    Pages: 7 S. , 1 Kt.
    ISBN: 8789813197
    Series Statement: DGU Kortserie 46
    Language: Danish , German
    Scale: 1:50.000
    Note: Literaturverz. S. 7
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  • 3
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    Paleohydrography of the Baltic since the last glaciation: the Darss Sill gateway (1992)
    In:  [Talk] In: 4. International Conference on Paleoceanography (ICP IV), 21.09.-25.09.1992, Kiel .
    Details
    Publication Date: 2014-04-23
    Type: Conference or Workshop Item , PeerReviewed
    Format: text
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    OceanRep: Talk
  • 4
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    The Darss Sill, hydrographic threshold in southwestern Baltic: Late quaternary geology and recent sediment dynamics (1994)
    Elsevier
    In:  Continental Shelf Research, 14 (7/8). pp. 847-870.
    Details
    Publication Date: 2016-09-20
    Description: About 73% of the water exchange between the Baltic and the North Seas is via the Darss Sill. Joint Danish and German marine geological investigations, including shallow seismic surveys and sediment sampling, have been carried out in the Darss Sill area between 1989 and 1991. Results from these studies and unpublished archive data from the Institute of Baltic Sea Research, Warnemünde, are presented. These show that the entire Quaternary sedimentary sequence in most of the area is at least 40 m thick. A zone of glacial till outcropping between Denmark and Germany belongs to the Late Weichselian ice marginal line G (“Velgaster Staffel”). The formation of this line caused the damming of a pre-existing (sub)glacial meltwater discharge system. At the beginning of the Baltic Ice Lake formation, a deep and presently buried channel incised in this ice marginal line was part of a (glacio)fluvial drainage system with discharge towards the northeast, i.e. into the Baltic Ice Lake. During the Baltic Ice Lake transgression damming of the Darss Sill occurred due to accumulation of sandy sediments within this channel. On the other hand, the recent Kadet Channel was only occasionally overflown during the Baltic Ice Lake highstand maximum, which was 18 m BSL (below present sea level) in the Darss Sill area. The main erosion and deepening of the Kadet Channel began during the Ancylus Lake highstand maximum. At present, sediment transport on the Darss Sill is governed by northeasterly inflow of saline bottom waters in the entire area from the Kadet Channel to the German coast. Baltic outflow affects the seabed at shallower depth in the Danish sector. Large-scale current-induced bedforms in the area include, amongst others, sandwaves with a height of 5 m. Changes of the bedforms observed indicate a maximum bottom flow speed of 70–100 cm s−1, both for inflow and for outflow.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/0278-4343(94)90076-0
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 5
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    Sediment distribution in Flensburg Bay (western Baltic) (1994)
    In:  Report / Geological Survey of Denmark, 1994 . p. 18.
    Details
    Publication Date: 2014-02-18
    Type: Article , NonPeerReviewed
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    OceanRep: Article in a Scientific Journal - without review
  • 6
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    (Table 1) Sea level during storm surges at various sites along the german Baltic Sea coast
    PANGAEA
    In:  Supplement to: Schwarzer, Klaus; Ricklefs, Klaus; Schumacher, Walter; Atzler, Roland (1996): Beobachtungen zur Vorstranddynamik und zum Küstenschutz sowie zum Sturmereignis vom 3./4.11.1995 vor dem Streckelsberg/Usedom. Meyniana, 48, 49-68, https://doi.org/10.2312/meyniana.1996.48.49
    Details
    Publication Date: 2023-05-12
    Description: A seawall was constructed in 1897 along the steep coast of Streckelsberg, Usedom Island to stop the cliff retreat. It was destroyed several times by storm induced sea floods, reconstructed and gradually extended to a length of 450 m. After the severe storm event of 1/2.3.1949, no more repair work was implemented. The ruins were no longer capable of preventing further erosion of the Streckelsberg cliff. A new protective structure became a necessity against ongoing erosion, and to check the lowering of the abrasion platform. The construction of three breakwaters began in 1995. A severe storm occurred on 3/4.11.1995 before their completion. Coastal bottom sediment mapping using a sidescan-sonar carried out two days later showed that a channel system down to a depth of 1.5 m was cut into the sand layer covering the sea floor on both sides of the Koserow Bank. The bottom of these channels was paved with gravel and boulders. This layer was encountered in the whole surveyed area below a mobile sand layer. Discharged bodies of fine sand half a meter high and erosional cavities several m2 in diameter around boulders led to the conclusion that an intensive sediment movement down to a depth of 11 m had taken place during the storm. A storm related direction of sediment discharge could not be identified. The existing section of the breakwaters withstood the severe storm.
    Keywords: Baltic Sea, Germany; Date; DATE/TIME; Event label; Greifswald; KielHarbour; Koserow; Sassnitz; Sea level; Stralsund; TGS; Tide gauge station; Travemuende; Warnemuende; Wismar
    Type: Dataset
    Format: text/tab-separated-values, 112 data points
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  • 7
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    Anhang - Karten und Schnitte der Kieler Bucht = Maps and profiles of Kiel Bight (1994)
    PANGAEA
    In:  Supplement to: Atzler, Roland (1994): Der Pleistozäne Untergrund der Kieler Bucht und angrenzender Gebiete nach reflexionsseismischen Messungen. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 70, 116 pp, https://doi.org/10.2312/reports-gpi.1995.70
    Details
    Publication Date: 2024-02-03
    Description: Ziel der vorliegenden Arbeit war es, mit Hilfe von flachseismischen Messungen den Untergrund der Kieler Bucht in Bezug auf ihre geologische Entwicklung imQuartär zu untersuchen. Es sollten Aufschlüsse über Art und Verbreitung der quartären Sedimente sowie über die Tiefenlage der Quartärbasis gewonnen werden.Verlauf und Internstruktur des pleistozänen Rinnensystems bilden einen weiteren Schwerpunkt der Arbeit, ebenso die Erstellung einer Sedimentkarte der Flensburger Förde. Dazu wurden zusätzlich zu bereits vorhandenen Datenc a. 1200 Profilkilometer seismisch neu aufgenommen.
    Keywords: Bay of Kiel, Baltic Sea; Figure; File name; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; Kiel_Bight; Title; Uniform resource locator/link to image
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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    DATA PANGAEA
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