Titlebook: Atlas of the Deep-Water Seabed; Ireland Boris Dorschel,Andrew J. Wheeler,Koen Verbruggen Book 2010 Springer Science+Business Media B.V. 201

cancellous-bone

新陈代谢

Angiogenesis

Escarpments Escarpments can form as a result of strong, slope-parallel bottom currents, or as the scars left following submarine (land)slides. In addition, they can be associated with morphological features such as canyons and seamounts. Regardless of the formation processes, escarpments are the results of erosive processes active on the continental slope.

发芽

Below the Irish Seabedogical structures of the Irish deep-water seabed developed as a result of a series of rift valleys that formed during the early development of the north Atlantic starting in the Permo-Triassic geological period (around 250 million years ago).

弄脏

Porcupine Seabightat its mouth in the southwest. The northern border of the Porcupine Seabight is difficult to define with no clear break of slope but a gradual transition from the Seabight to the Porcupine Bank and Celtic Shelf. With the borders as presented here, the Porcupine Seabight covers an area of 67,100 km. (Fig. 13.1).

Anal-Canal

Rockall Bankvel. Being separated from the Irish continental margin by the Rockall Trough, the Rockall Bank represents a relatively sediment starved area isolated from the input of terrestrial sediments by rivers and glaciers. Morphologically, the Rockall Bank is characterised by a generally steeper eastern slope and a generally gentler western slope (Fig. ).

dysphagia

Irritate

Fundamentals of Robotic Mechanical Systemsat its mouth in the southwest. The northern border of the Porcupine Seabight is difficult to define with no clear break of slope but a gradual transition from the Seabight to the Porcupine Bank and Celtic Shelf. With the borders as presented here, the Porcupine Seabight covers an area of 67,100 km. (Fig. 13.1).

neuron

Congregate

Fundamentals of Rigid-Body Mechanics,such as cold-water coral carbonate mounds. Even though the mound features have a variety of origins, they all elevate from the seabed and protrude into the water column forming obstacles to bottom currents. Thus, they are often subject to erosion, providing hardgrounds and environmental conditions for organisms to settle and dwell.