Abstract
Pockmarks are seabed depressions that represent primary evidence of
rapid biogenic/thermogenic gas build up and fluid release from seabed
sediments to the water column. We use a Geographical Information System
(GIS) to analyse multibeam echo-sounder bathymetric data and use a range
of semi-automated tools to map seabed pockmarks in fjords and adjacent
coastal waters around western Scotland. We map 1019 individual pockmarks
in 12 different hydrographic areas covering ca. 2019 km2. We
use morphological metrics and statistical procedures to classify and
analyse the variety of pockmark forms. A k-means clustering algorithm
identifies three classes of pockmark morphology: deep, elongate and
regular. The recognition of separate pockmark classes could aid
understanding of their age, activity and origin. This work presents the
first detailed mapping of pockmark fields in Scottish west coast waters
and highlights the use of pockmarks as an indicator of the quantity,
mobility and fate of stored carbon.
Original language | English |
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Pages (from-to) | 807-817 |
Number of pages | 12 |
Journal | Journal of Maps |
Volume | 15 |
Issue number | 2 |
DOIs | |
Publication status | Published - 15 Oct 2019 |
Keywords
- Carbon
- Gas release
- Classification
- GIS
- k-means
- Morphology