Please use this identifier to cite or link to this item: https://www.um.edu.mt/library/oar/handle/123456789/64238
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dc.contributor.authorHunt, Chris O.-
dc.contributor.authorFarrell, Michelle-
dc.contributor.authorFenech, Katrin-
dc.contributor.authorFrench, Charles-
dc.contributor.authorMcLaughlin, Rowan-
dc.contributor.authorBlaauw, Maarten-
dc.contributor.authorBennett, Jeremy-
dc.contributor.authorFlood, Rory P.-
dc.contributor.authorPyne-O’Donnell, Sean D. F.-
dc.contributor.authorReimer, Paula J.-
dc.contributor.authorRuffell, Alastair-
dc.contributor.authorCresswell, Alan J.-
dc.contributor.authorKinnaird, Timothy C.-
dc.contributor.authorSanderson, David C. W.-
dc.contributor.authorTaylor, Sean-
dc.contributor.authorMalone, Caroline-
dc.contributor.authorStoddart, Simon-
dc.contributor.authorVella, Nicholas C.-
dc.date.accessioned2020-11-20T07:46:21Z-
dc.date.available2020-11-20T07:46:21Z-
dc.date.issued2020-
dc.identifier.citationHunt, C. O., Farrell, M., Fenech, K., French, C., McLaughlin, R., Blaauw, M., ...Vella, N. C. (2020). Chapter 2 : chronology and stratigraphy of the valley systems. In: C. French, C. O. Hunt, R. Grima, R. McLaughlin, S. Stoddart & C. Malone, Temple landscapes : fragility, change and resilience of Holocene environments in the Maltese Islands. Cambridge: McDonald Institute for Archaeological Research. 35-71.en_GB
dc.identifier.urihttps://www.um.edu.mt/library/oar/handle/123456789/64238-
dc.description.abstractAdequate absolute dating is critical to understanding the past, especially where data concerning environmental changes from different sites are being compared, as chronology is often the only reliable way to compare evidence from multiple contexts. The archaeological chronology of Malta is becoming increasingly well resolved and this sets up a challenge – how can we obtain comparable high-resolution chronologies of environmental change in the Maltese Islands? The Maltese landforms pose significant barriers to achieving this goal, as much of the available palaeoenvironmental evidence is limited to cores in alluvial or shallow-marine sediments, which contain materials that have been subject to much re-working through time. In this chapter, we introduce and discuss the various techniques that the FRAGSUS Project has brought to bear on this problem, and review the main approaches used. [excerpt]en_GB
dc.description.sponsorshipThis project has received funding from the European Research Council (ERC) under the European Union’s Seventh Framework Programme (FP7-2007-2013) (Grant agreement No. 323727).en_GB
dc.language.isoenen_GB
dc.publisherMcDonald Institute for Archaeological Researchen_GB
dc.rightsinfo:eu-repo/semantics/openAccessen_GB
dc.subjectGeology, Stratigraphicen_GB
dc.subjectEvent stratigraphy -- Maltaen_GB
dc.subjectClimatic changes -- Malta -- Historyen_GB
dc.subjectChronologyen_GB
dc.titleChapter 2 : chronology and stratigraphy of the valley systemsen_GB
dc.title.alternativeTemple landscapes : fragility, change and resilience of Holocene environments in the Maltese Islandsen_GB
dc.typebookParten_GB
dc.rights.holderThe copyright of this work belongs to the author(s)/publisher. The rights of this work are as defined by the appropriate Copyright Legislation or as modified by any successive legislation. Users may access this work and can make use of the information contained in accordance with the Copyright Legislation provided that the author must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the prior permission of the copyright holder.en_GB
dc.description.reviewedpeer-revieweden_GB
dc.identifier.doi10.17863/CAM.59608-
Appears in Collections:Temple landscapes: Fragility, change and resilience of Holocene environments in the Maltese Islands

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