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Reconstructing a prehistoric topography using legacy point data in a depositional environment
ABSTRACT Reconstruction of past topography is an essential step towards the understanding of past landscapes in terms of biophysical patterns and processes and man–landscape interactions by archaeologists, geomorphologists, geologists and soil scientists. Landscape reconstructions can be based on pr...
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Published in: | Earth surface processes and landforms 2014-04, Vol.39 (5), p.632-645 |
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creator | Vermeer, Julian A. M. Finke, Peter A. Zwertvaegher, Ann Gelorini, Vanessa Bats, Machteld Antrop, Marc Verniers, Jacques Crombé, Philippe |
description | ABSTRACT
Reconstruction of past topography is an essential step towards the understanding of past landscapes in terms of biophysical patterns and processes and man–landscape interactions by archaeologists, geomorphologists, geologists and soil scientists. Landscape reconstructions can be based on process knowledge, on data, or on a combination of both. In this case study we focus on a data‐based approach, where knowledge on the geological history is used to interpret and exploit legacy data. As part of a landscape reconstruction of a large area of 584 km2 a map of the elevation near 10 000 BC was produced. Starting from a present‐day grid digital elevation model (GDEM) that was filtered for human influences, we identified the thickness of accumulated sediments over the Holocene, mapped these and corrected the GDEM. To map the thickness of Holocene sediments we used 72 (OSL and 14C) dated sediment samples, 731 recent profile descriptions and 3288 legacy profile descriptions. Protocols were formulated based on literature and local correlative studies to convert the legacy profile descriptions into estimates of the thickness of Holocene sediments, with an estimate of the precision. The method of Kriging with uncertain data was applied to obtain a map. Validation at 200 independent test locations with certain data showed a mean error of –6 cm and a standard deviation or error of 16 cm, which was in accordance with the estimated precision of 16 cm. The resulting map indicated zones with marked change that could be studied in more detail. Future reconstructions could employ both process knowledge and data by combining landscape genesis models with legacy data to map model errors and thus increase the quality of the reconstruction. Copyright © 2013 John Wiley & Sons, Ltd. |
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Reconstruction of past topography is an essential step towards the understanding of past landscapes in terms of biophysical patterns and processes and man–landscape interactions by archaeologists, geomorphologists, geologists and soil scientists. Landscape reconstructions can be based on process knowledge, on data, or on a combination of both. In this case study we focus on a data‐based approach, where knowledge on the geological history is used to interpret and exploit legacy data. As part of a landscape reconstruction of a large area of 584 km2 a map of the elevation near 10 000 BC was produced. Starting from a present‐day grid digital elevation model (GDEM) that was filtered for human influences, we identified the thickness of accumulated sediments over the Holocene, mapped these and corrected the GDEM. To map the thickness of Holocene sediments we used 72 (OSL and 14C) dated sediment samples, 731 recent profile descriptions and 3288 legacy profile descriptions. Protocols were formulated based on literature and local correlative studies to convert the legacy profile descriptions into estimates of the thickness of Holocene sediments, with an estimate of the precision. The method of Kriging with uncertain data was applied to obtain a map. Validation at 200 independent test locations with certain data showed a mean error of –6 cm and a standard deviation or error of 16 cm, which was in accordance with the estimated precision of 16 cm. The resulting map indicated zones with marked change that could be studied in more detail. Future reconstructions could employ both process knowledge and data by combining landscape genesis models with legacy data to map model errors and thus increase the quality of the reconstruction. Copyright © 2013 John Wiley & Sons, Ltd.</description><identifier>ISSN: 0197-9337</identifier><identifier>EISSN: 1096-9837</identifier><identifier>DOI: 10.1002/esp.3472</identifier><identifier>CODEN: ESPLDB</identifier><language>eng</language><publisher>Chichester: Blackwell Publishing Ltd</publisher><subject>Bgi / Prodig ; Descriptions ; Errors ; Estimates ; geoarchaeology ; Holocene ; landscape reconstruction ; Landscapes ; Legacy ; legacy data ; mapping ; Palaeogeography ; Physical geography ; Quaternary ; Reconstruction ; Sediments ; Topography</subject><ispartof>Earth surface processes and landforms, 2014-04, Vol.39 (5), p.632-645</ispartof><rights>Copyright © 2013 John Wiley & Sons, Ltd.</rights><rights>Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2014</rights><rights>Copyright © 2014 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4502-ed8e8192d7696e6940b1b4829d79ecb4262d3fb016fd9d4714c6bd5f42a28de63</citedby><cites>FETCH-LOGICAL-a4502-ed8e8192d7696e6940b1b4829d79ecb4262d3fb016fd9d4714c6bd5f42a28de63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28518792$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Vermeer, Julian A. M.</creatorcontrib><creatorcontrib>Finke, Peter A.</creatorcontrib><creatorcontrib>Zwertvaegher, Ann</creatorcontrib><creatorcontrib>Gelorini, Vanessa</creatorcontrib><creatorcontrib>Bats, Machteld</creatorcontrib><creatorcontrib>Antrop, Marc</creatorcontrib><creatorcontrib>Verniers, Jacques</creatorcontrib><creatorcontrib>Crombé, Philippe</creatorcontrib><title>Reconstructing a prehistoric topography using legacy point data in a depositional environment</title><title>Earth surface processes and landforms</title><addtitle>Earth Surf. Process. Landforms</addtitle><description>ABSTRACT
Reconstruction of past topography is an essential step towards the understanding of past landscapes in terms of biophysical patterns and processes and man–landscape interactions by archaeologists, geomorphologists, geologists and soil scientists. Landscape reconstructions can be based on process knowledge, on data, or on a combination of both. In this case study we focus on a data‐based approach, where knowledge on the geological history is used to interpret and exploit legacy data. As part of a landscape reconstruction of a large area of 584 km2 a map of the elevation near 10 000 BC was produced. Starting from a present‐day grid digital elevation model (GDEM) that was filtered for human influences, we identified the thickness of accumulated sediments over the Holocene, mapped these and corrected the GDEM. To map the thickness of Holocene sediments we used 72 (OSL and 14C) dated sediment samples, 731 recent profile descriptions and 3288 legacy profile descriptions. Protocols were formulated based on literature and local correlative studies to convert the legacy profile descriptions into estimates of the thickness of Holocene sediments, with an estimate of the precision. The method of Kriging with uncertain data was applied to obtain a map. Validation at 200 independent test locations with certain data showed a mean error of –6 cm and a standard deviation or error of 16 cm, which was in accordance with the estimated precision of 16 cm. The resulting map indicated zones with marked change that could be studied in more detail. Future reconstructions could employ both process knowledge and data by combining landscape genesis models with legacy data to map model errors and thus increase the quality of the reconstruction. Copyright © 2013 John Wiley & Sons, Ltd.</description><subject>Bgi / Prodig</subject><subject>Descriptions</subject><subject>Errors</subject><subject>Estimates</subject><subject>geoarchaeology</subject><subject>Holocene</subject><subject>landscape reconstruction</subject><subject>Landscapes</subject><subject>Legacy</subject><subject>legacy data</subject><subject>mapping</subject><subject>Palaeogeography</subject><subject>Physical geography</subject><subject>Quaternary</subject><subject>Reconstruction</subject><subject>Sediments</subject><subject>Topography</subject><issn>0197-9337</issn><issn>1096-9837</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqF0V1rFDEUBuAgCq5V8CcMiODNtPmafFzK0lah1FKV9qaETHJmmzqbTJMZdf-9M3SpIEivzsV5zguHF6G3BB8SjOkRlOGQcUmfoRXBWtRaMfkcrTDRstaMyZfoVSl3GBPClV6hm0twKZYxT24McVPZashwG8qYcnDVmIa0yXa43VVTWdY9bKzbVUMKcay8HW0V4nzjYUgljCFF21cQf4ac4hbi-Bq96Gxf4M1-HqDvJ8ff1p_qsy-nn9cfz2rLG0xr8AoU0dRLoQUIzXFLWq6o9lKDazkV1LOuxUR0XnsuCXei9U3HqaXKg2AH6MND7pDT_QRlNNtQHPS9jZCmYojglGHMFH-aNpRzzGY703f_0Ls05fnFRRGGOaeY_g10OZWSoTNDDlubd4Zgs1Ri5krMUslM3-8DbXG277KNLpRHT1VDlNSLqx_cr9DD7r955vjrxT537-fe4Pejt_mHEZLJxlydn86nF-r6Wp6YNfsDr-2o0g</recordid><startdate>201404</startdate><enddate>201404</enddate><creator>Vermeer, Julian A. 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M.</creatorcontrib><creatorcontrib>Finke, Peter A.</creatorcontrib><creatorcontrib>Zwertvaegher, Ann</creatorcontrib><creatorcontrib>Gelorini, Vanessa</creatorcontrib><creatorcontrib>Bats, Machteld</creatorcontrib><creatorcontrib>Antrop, Marc</creatorcontrib><creatorcontrib>Verniers, Jacques</creatorcontrib><creatorcontrib>Crombé, Philippe</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Earth surface processes and landforms</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vermeer, Julian A. 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Reconstruction of past topography is an essential step towards the understanding of past landscapes in terms of biophysical patterns and processes and man–landscape interactions by archaeologists, geomorphologists, geologists and soil scientists. Landscape reconstructions can be based on process knowledge, on data, or on a combination of both. In this case study we focus on a data‐based approach, where knowledge on the geological history is used to interpret and exploit legacy data. As part of a landscape reconstruction of a large area of 584 km2 a map of the elevation near 10 000 BC was produced. Starting from a present‐day grid digital elevation model (GDEM) that was filtered for human influences, we identified the thickness of accumulated sediments over the Holocene, mapped these and corrected the GDEM. To map the thickness of Holocene sediments we used 72 (OSL and 14C) dated sediment samples, 731 recent profile descriptions and 3288 legacy profile descriptions. Protocols were formulated based on literature and local correlative studies to convert the legacy profile descriptions into estimates of the thickness of Holocene sediments, with an estimate of the precision. The method of Kriging with uncertain data was applied to obtain a map. Validation at 200 independent test locations with certain data showed a mean error of –6 cm and a standard deviation or error of 16 cm, which was in accordance with the estimated precision of 16 cm. The resulting map indicated zones with marked change that could be studied in more detail. Future reconstructions could employ both process knowledge and data by combining landscape genesis models with legacy data to map model errors and thus increase the quality of the reconstruction. Copyright © 2013 John Wiley & Sons, Ltd.</abstract><cop>Chichester</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/esp.3472</doi><tpages>14</tpages></addata></record> |
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subjects | Bgi / Prodig Descriptions Errors Estimates geoarchaeology Holocene landscape reconstruction Landscapes Legacy legacy data mapping Palaeogeography Physical geography Quaternary Reconstruction Sediments Topography |
title | Reconstructing a prehistoric topography using legacy point data in a depositional environment |
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