Morphology of Salina offshore (Southern Tyrrhenian Sea)

被引:12
作者
Casalbore, D. [1 ]
Bosman, A. [1 ]
Romagnoli, C. [2 ]
Chiocci, F. L. [1 ,3 ]
机构
[1] CNR Ist Geol Ambientale & Geoingn, Rome, Italy
[2] Univ Bologna, Dipartimento Sci Biol Geol & Ambientali, Bologna, Italy
[3] Sapienza Univ Roma, Dipartimento Sci Terra, Rome, Italy
来源
JOURNAL OF MAPS | 2016年 / 12卷 / 05期
关键词
Multibeam bathymetry; insular volcano; mass-wasting processes; morphometry; wavy bedforms; SUBMARINE; EVOLUTION; ISLANDS; BATHYMETRY; INSIGHTS; CHANNEL; SLOPES; FLANKS;
D O I
10.1080/17445647.2015.1070300
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
In this paper, we present the first complete morphological map of the Salina offshore at a scale of 1: 100,000. The submarine flanks of the Salina edifice extend down to -650 to -1300 m, are steep and characterized by an uneven morphology due to the presence of volcanic and erosive-depositional features. The volcanic features cover similar to 30% of the submarine portion and include volcanic cones and bedrock outcrops. The remaining similar to 70% is affected by a wide series of erosive-depositional features. Among these, features related to Late Quaternary sea level fluctuations comprise the insular shelf surrounding the island and overlying submarine terraced depositional sequences. Mass-wasting features include landslide scars, channels, fan-shaped deposits and waveforms. The presented map provides useful insights for a better understanding of the morphological evolution of the edifice
引用
收藏
页码:725 / 730
页数:6
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