Pockmark (geology)

PockmarkAccording to the 'Glossary of Geology' (Bates and Jackson, 1987): "A concave crater-like depression of the type that occurs in profusion on mud bottoms across Scotian Shelf (King & McLean, 1970). They range in diameter from 15 to 45 meters and in depth from 5 to 10 meters. Pockmarks have also been found in the North Sea (Fannin, 1981) and elsewhere. Their origin is debatable." (Bates and Jackson, 1987, p. 514.

Pockmarks were discovered off the coasts of Nova Scotia, Canada in the late 1960s by Lew King and Brian McLean of the Bedford Institute of Oceanography.They were discovered off Nova Scotia, using a new side scan sonar developed in the late 1960s by Kelvin Hughes. Before the two researchers King and McLean used the side scan sonar, they had noticed 'notches' on echo sounder and shallow seismic records in the seafloor off Nova Scotia. They believed these notches to represent gullies and curvilinear troughs in the muddy seafloor. However, they could never work out how to join these notches from one survey line to the next. It was, therefore, not before they surveyed with the area-coverage system, Side scan sonar, that they realized the notches were in fact closed depressions (craters) and not curvilinear features. This was a great surprise, because there are very few craters on the Earth's surface.

Although pockmarks were first documented and published 50 years ago, they are currently still being discovered on the ocean floor and in many lakes, the world over.

The craters off Nova Scotia are up to 150 m (490 ft) in diameter and 10 m (33 ft) deep. Pockmarks have been found worldwide.[1][2] Discovery was aided by the use of high-resolution multibeam acoustic systems for bathymetric mapping. In these cases, pockmarks have been interpreted as the morphological expression of gas or oil leakage from active hydrocarbon system or a deep overpressured petroleum reservoir.