See stillstand on Wiktionary
Download JSON data for stillstand meaning in All languages combined (9.2kB)
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"text": "A useful exercise may be to calculate the basin-wide deglacial erosion rate for the Jakobshavn catchment area using the volume of glacimarine sediments deposited in front of the fjord-mouth sill (29.2 km3) during an 800 year stillstand (Hogan et al., 2012) and a glacial catchment area derived using the same procedures in this study (33 504 km2; Fig. S1b).",
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"text": "Repeated bathymetric measurements adjacent to the LeConte glacier terminus offer a rare view into the evolution of a morainal bank on interannual time scales during a stillstand, starting immediately after a rapid glacier retreat.",
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"ref": "1977, Peter R. Vail, Robert M. Jr. Mitchum, Steve Thompson, III, “Seismic Stratigraphy and Global Changes of Sea Level, Part 3: Relative Changes of Sea Level from Coastal Onlap” (chapter 5), in Charles E. Payton, editor, Seismic Stratigraphy: Applications to Hydrocarbon Exploration (AAPG Memoirs), volume 26, Tulsa, Oklahoma: American Association of Petroleum Geologists, →DOI, →LCCN, →OCLC, archived from the original on 2021-06-16, Application of Seismic Reflection Configuration to Stratigraphic Interpretation (section 2), page 68",
"text": "A relative stillstand of sea level is an apparently constant position of sea level with respect to the underlying initial surface of deposition, and is indicated by coastal toplap. It may result if both sea level and the underlying initial surface of deposition actually remain stationary, or if both rise or fall at the same rate.",
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"ref": "1978, A. Hallam, “Eustatic cycles in the Jurassic”, in Palaeogeography, Palaeoclimatology, Palaeoecology, volume 23, Amsterdam: Elsevier, →DOI, archived from the original on 2024-04-11, pages 1-32",
"text": "More generally, regressive sedimentary episodes often correlate with widespread stratigraphic gaps implying erosion or non-deposition. Such facts imply a sea-level fall rather than a stillstand combined with sedimentary infill. Without such periodic falls it is difficult to understand why the successive phases of transgression did not extend much further than areal plots of marine deposits indicate.",
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"ref": "2021 December, Paulo Henrique Cetto, Alex Cardoso Bastos, Marco Ianirruberto, “Morphological evidences of eustatic events in the last 14,000 years in a far-field site, East-Southeast Brazilian continental shelf”, in Marine Geology, volume 442, number 106659, Elsevier, →DOI, archived from the original on 2024-05-19, page 14",
"text": "The results show that shelf morphology in a far-field site, such as a South Atlantic continental margin, exhibits morphological evidences indicating a stillstand during YD, characterized by the configuration of distinct coastal systems (lagoons, estuaries, barrier islands and potential fringing reefs), followed by a rapid sea-level rise that drowned and preserved the morphology of these coastal features.",
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"(geology) A period of geologic time during which eustatic sea level stays apparently constant, relative to adjacent periods of geologic time, neither characterized by transgression, nor regression."
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"ref": "2005 October 25, Jeremy Everest, P. Kubik, “The deglaciation of eastern Scotland: cosmogenic ¹⁰Be evidence for a Lateglacial stillstand”, in Journal of Quaternary Science, volume 2, number 1, Wiley, →DOI, archived from the original on 2021-09-06, pages 95-104",
"text": "It is tempting in these circumstances to look for the 'smoking gun'-a mechanism whereby glaciers from both the local Cairngorm ice cap, and the much larger Scottish Ice Sheet could stillstand, or even readvance for a period of 1 kyr, during deglaciation.",
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"ref": "2016 April, Pierre Dietrich, Jean-François Ghienne, Alexandre Normandeau, Patrick Lajeunesse, “Proglacial deltaic landforms and stratigraphic architecture as a proxy for reconstructing past ice-sheet margin positions”, in EGU Geophysical Research Abstracts, volume 18, EGU General Assembly 2016, 17-22 April, 2016, Vienna Austria: European Geosciences Union, EPSC2016-2851, archived from the original on 2023-09-25",
"text": "The base of the stratigraphic successions consists of outwash fan deposits emplaced in the early deglaciation when ice margin stillstanded immediately beyond the depositional area.",
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"ref": "2017 December 5, Pierre Dietrich, Jean-François Ghienne, Alexandre Normandeau, Patrick Lajeunesse, “Reconstructing ice-margin retreat using delta morphostratigraphy”, in Scientific Reports, volume 7, number 16936, Nature Portfolio, →DOI, archived from the original on 2024-05-16",
"text": "Ice-contact depositional systems formed when the LIS was stillstanding along the Québec North Shore.",
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"To cease in either glacial advance or retreat."
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"text": "A useful exercise may be to calculate the basin-wide deglacial erosion rate for the Jakobshavn catchment area using the volume of glacimarine sediments deposited in front of the fjord-mouth sill (29.2 km3) during an 800 year stillstand (Hogan et al., 2012) and a glacial catchment area derived using the same procedures in this study (33 504 km2; Fig. S1b).",
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"text": "Repeated bathymetric measurements adjacent to the LeConte glacier terminus offer a rare view into the evolution of a morainal bank on interannual time scales during a stillstand, starting immediately after a rapid glacier retreat.",
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"text": "A relative stillstand of sea level is an apparently constant position of sea level with respect to the underlying initial surface of deposition, and is indicated by coastal toplap. It may result if both sea level and the underlying initial surface of deposition actually remain stationary, or if both rise or fall at the same rate.",
"type": "quotation"
},
{
"ref": "1978, A. Hallam, “Eustatic cycles in the Jurassic”, in Palaeogeography, Palaeoclimatology, Palaeoecology, volume 23, Amsterdam: Elsevier, →DOI, archived from the original on 2024-04-11, pages 1-32",
"text": "More generally, regressive sedimentary episodes often correlate with widespread stratigraphic gaps implying erosion or non-deposition. Such facts imply a sea-level fall rather than a stillstand combined with sedimentary infill. Without such periodic falls it is difficult to understand why the successive phases of transgression did not extend much further than areal plots of marine deposits indicate.",
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{
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"text": "The results show that shelf morphology in a far-field site, such as a South Atlantic continental margin, exhibits morphological evidences indicating a stillstand during YD, characterized by the configuration of distinct coastal systems (lagoons, estuaries, barrier islands and potential fringing reefs), followed by a rapid sea-level rise that drowned and preserved the morphology of these coastal features.",
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"(geology) A period of geologic time during which eustatic sea level stays apparently constant, relative to adjacent periods of geologic time, neither characterized by transgression, nor regression."
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"ref": "2005 October 25, Jeremy Everest, P. Kubik, “The deglaciation of eastern Scotland: cosmogenic ¹⁰Be evidence for a Lateglacial stillstand”, in Journal of Quaternary Science, volume 2, number 1, Wiley, →DOI, archived from the original on 2021-09-06, pages 95-104",
"text": "It is tempting in these circumstances to look for the 'smoking gun'-a mechanism whereby glaciers from both the local Cairngorm ice cap, and the much larger Scottish Ice Sheet could stillstand, or even readvance for a period of 1 kyr, during deglaciation.",
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"ref": "2016 April, Pierre Dietrich, Jean-François Ghienne, Alexandre Normandeau, Patrick Lajeunesse, “Proglacial deltaic landforms and stratigraphic architecture as a proxy for reconstructing past ice-sheet margin positions”, in EGU Geophysical Research Abstracts, volume 18, EGU General Assembly 2016, 17-22 April, 2016, Vienna Austria: European Geosciences Union, EPSC2016-2851, archived from the original on 2023-09-25",
"text": "The base of the stratigraphic successions consists of outwash fan deposits emplaced in the early deglaciation when ice margin stillstanded immediately beyond the depositional area.",
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{
"ref": "2017 December 5, Pierre Dietrich, Jean-François Ghienne, Alexandre Normandeau, Patrick Lajeunesse, “Reconstructing ice-margin retreat using delta morphostratigraphy”, in Scientific Reports, volume 7, number 16936, Nature Portfolio, →DOI, archived from the original on 2024-05-16",
"text": "Ice-contact depositional systems formed when the LIS was stillstanding along the Québec North Shore.",
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"To cease in either glacial advance or retreat."
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"(geology) To cease in either glacial advance or retreat."
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This page is a part of the kaikki.org machine-readable All languages combined dictionary. This dictionary is based on structured data extracted on 2024-06-23 from the enwiktionary dump dated 2024-06-20 using wiktextract (1b9bfc5 and 0136956). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.
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