( an effective ) The brand new geotectonic form off Greece (changed off Reilinger ainsi que al. [ 58 ], and Vott et al. [ 67 ]) portraying the region of one’s investigation urban area and you may ( b ) hill shaded chart of your own investigation town produced from topographic charts at the step one:5000 level of Hellenic Military Geographic Services.
Geological map of studies town modified of Theodoropoulos [ 51 ], IGME [ 68 ], and you can Lekkas ainsi que al. [ 69 ]. Blame kinematics is undifferentiated, and most faults is actually deceased.
Schematic expression of the uncertainties considered into the enough time-title uplift pricing estimations, as well as the fresh relationship of your own aquatic terraces with previous sea-level highstands. Elizabeth ‘s the establish-time elevation of the interior edge of the brand new patio, A ‘s the age the fresh patio, age represents the brand new level of sea level on lifetime of terrace development, and also the delta icons (?) represent the newest estimated suspicion regarding the other variables. The fresh new ple.
Colored arrows (exact same tone as Shape cuatro ) point out terraces T1, T2, T3, T4, T5, T6, T8, and you will T9 ( b ) View of the fresh paleo-shoreline angle out-of terrace T3 (corresponding to MIS 5e ocean-peak highstand) northern away from Cape Punta
Geographical shipment of one’s uplifted marine terraces of one’s wider Neapolis city, southeastern Peloponnese. The region of topographic users, in addition to precise location of the OSL examples, also are illustrated.
( an effective ) View of the airline out-of aquatic terraces northwest of Cape Punta. ( c ) Character view of the newest patio succession towards western element of the latest Elafonissos Area ( d ) View of the inner side of terrace T3 (add up to MIS 5a water-top highstand) at north part of Elafonissos. ( age ) Outcrop regarding Patio T5 caprock, northwest of Cape Punta. View of the inner edge of terrace T3 (corresponding to MIS 5e ocean-level highstand) northeast of Profitis Ilias.
Three topographic profiles constructed dos.3 km northwest out-of Cape Punta (Character An excellent), during the western a portion of the Elafonissos Area (Character B), and you may cuatro.6 kilometer south out-of Neapolis (Profile C). Having towns and cities of pages, look for map during the Profile cuatro . This new marine terraces was designated consecutively, beginning with a reduced you to definitely. The elevations of one’s interior corners into terraces, while the produced by the brand new topographic users, are supplied. The region and the period of the fresh new OSL samples, and the MIS related to each marine patio, also are given.
Correlation diagram of the two OSL dated trials, compiled out of marine terraces T3 and you may T5, respectively, that have late Quaternary MIS. Grey vertical bands match the age the total amount of different sea-height highstands (off Lisiecki and you can Raymo [ 88 ]). Suggest, restrict, and you can minimum uplift pricing out of this correlation also are found.
The position of sedimentary cut off attempt N gathered to possess OSL dating is even portrayed ( f )
( a beneficial , b ) Uplifted scratch networks between Profitis Ilias and Agia Marina, supported by a reduced, high cliff having an effective tidal notch from the cheekylovers yГјkle the foot. ( c , d ) Uplifted scratch networks at Agia Marina.
Relative drawing of your predicted/questioned aquatic terraces’ inner line elevations’ range (marked of the dense black colored lines) additionally the observed interior boundary level range (marked because of the narrow red outlines) for the broader Neapolis area. New forecast height ranges of one’s interior sides (palaeo-shorelines) for every single MIS was indeed determined within the presumption the enough time-term uplift speed (0.36 ± 0.eleven mm a great ?step one ) try constant for the last 401 ± ten ka and you will considering age stretch of each and every MIS highstand (based on Lisiecki and you will Raymo [ 88 ]-marked here just like the grey straight groups), together with restrict and minimal status regarding eustatic ocean-height per MIS highstand (based on water-level curve by the Waelbroeck et al. [ twenty-five ]).