Multi-resolution morpho-bathymetric survey results at the Pozzuoli-Baia underwater archaeological site (Naples, Italy)

被引:62
作者
Passaro, Salvatore [1 ]
Barra, Marco [1 ]
Saggiomo, Roberto [2 ]
Di Giacomo, Simone [3 ]
Leotta, Antonio [3 ]
Uhlen, Helge [4 ]
Mazzola, Salvatore [1 ]
机构
[1] CNR, IAMC, I-80133 Naples, Italy
[2] Enviroconsult Srl, I-80122 Naples, Italy
[3] Kongsberg Maritime Srl, Hydrog Dept, I-00166 Rome, Italy
[4] Kongsberg Maritime AS, Horten, Norway
关键词
DTM; Bradyseism; Campi Flegrei; Underwater archaeology; GIS; SEA-LEVEL CHANGE; ERUPTION CAMPI-FLEGREI; MEDITERRANEAN SEA; SWATH BATHYMETRY; CALDERA; HOLOCENE; HISTORY; FIELDS;
D O I
10.1016/j.jas.2012.09.035
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
Here we show the results of two morpho-bathymetric surveys carried out on the underwater archaeological area of the Pozzuoli Bay (Naples, Italy). Such area is enclosed in the Campi Flegrei active volcanic complex, where bradyseism and recent volcanic activity strongly influenced the coastline shape over the last 2 Ka. The Digital Elevation Model (DTM) of the seafloor allowed to draw the main archaeological features of the Bay, that also include the military complex of Portus lulius and the ancient thermal and villa complex of Baianus Lacus. The extraction of archaeological features from DTM was achieved thanks to the use of a GIS-derived tool based on the profile curvature algorithm. Thus, the Villa dei Pisoni (1st Century B.C.) and the thermal complex of Secca delle Fumose were investigated by using ultra-high resolution DTMs, that show the presence of Roman pilae for the protection of coastal buildings and also the inner planimetry of the Villa dei Pisoni complex. The observation of coastal engineering structures give also the opportunity to formulate some hypothesis on the evolution of morphology and of the sedimentary pattern of the area, while depth of archaeological remains allowed a rough computation of the rate of subsidence, resulted to be 2.55 (+/- 0.5) mm/y for the Eastern sector (Pozzuoli) and 2.90 (+/- 0.5) mm/y for the western (Baia). (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1268 / 1278
页数:11
相关论文
共 61 条
[1]   UNIVERSITY-OF-ROME CARBON-14 DATES IX [J].
ALESSIO, M ;
BELLA, F ;
IMPROTA, S ;
BELLUOMI.G ;
CORTESI, C ;
TURI, B .
RADIOCARBON, 1971, 13 (02) :395-&
[2]   ISOTOPIC STUDY OF THE ORIGIN OF SULFUR AND CARBON IN SOLFATARA FUMAROLES, CAMPI FLEGREI CALDERA [J].
ALLARD, P ;
MAIORANI, A ;
TEDESCO, D ;
CORTECCI, G ;
TURI, B .
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1991, 48 (1-2) :139-159
[3]  
[Anonymous], 1998, INT HYDR ORG SPEC PU
[4]   Sea-level change during the Holocene in Sardinia and in the northeastern Adriatic (central Mediterranean Sea) from archaeological and geomorphological data [J].
Antonioli, F. ;
Anzidei, M. ;
Lambeck, K. ;
Auriemma, R. ;
Gaddi, D. ;
Furlani, S. ;
Orru, P. ;
Solinas, E. ;
Gaspari, A. ;
Karinja, S. ;
Kovacic, V. ;
Surace, L. .
QUATERNARY SCIENCE REVIEWS, 2007, 26 (19-21) :2463-2486
[5]   New insights on the relative sea level change during Holocene along the coasts of Tunisia and western Libya from archaeological and geomorphological markers [J].
Anzidei, M. ;
Antonioli, F. ;
Lambeck, K. ;
Benini, A. ;
Soussi, M. ;
Lakhdar, R. .
QUATERNARY INTERNATIONAL, 2011, 232 :5-12
[6]   Archaeological remains as sea level change markers: A review [J].
Auriemma, Rita ;
Solinas, Emanuela .
QUATERNARY INTERNATIONAL, 2009, 206 :134-146
[7]  
Benini A., 2006, RIV TOPOGRAFIA ANTIC, VXVI, P85
[8]  
Berrino G., 1984, B VOLCANOL, V44, P187, DOI [DOI 10.1007/BF01961548, 10.1007/BF01961548]
[9]   Evaluation of the modern submarine landscape off southwestern Turkey through the documentation of ancient shipwreck sites [J].
Brennan, Michael L. ;
Ballard, Robert D. ;
Roman, Chris ;
Bell, Katherine L. C. ;
Buxton, Bridget ;
Coleman, Dwight F. ;
Inglis, Gabrielle ;
Koyagasioklu, Orkan ;
Turanli, Tufan .
CONTINENTAL SHELF RESEARCH, 2012, 43 :55-70
[10]  
Cinque A., 1985, B SOC GEOL ITAL, V104, P327