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Mobile Bay is 413 square miles (1,070 km 2) in area. It is 31 miles (50 km) long by a maximum width of 24 miles (39 km). [ 1 ] The deepest areas of the bay are located within the shipping channel, sometimes in excess of 75 feet (23 m) deep, but the average depth of the bay is 10 feet (3 m).
In 2004, a study conducted by the Geological Society of America analyzed the potential for land subsidence along the Cascadia subduction zone. It postulated that several towns and cities on the west coast of Vancouver Island, such as Tofino and Ucluelet, are at risk for a sudden, earthquake initiated, 1–2 m subsidence. [23]
With a few exceptions, the shelf break is located at a remarkably uniform depth of roughly 140 m (460 ft); this is likely a hallmark of past ice ages, when sea level was lower than it is now. [ 11 ] The continental slope is much steeper than the shelf; the average angle is 3°, but it can be as low as 1° or as high as 10°.
Tectonic subsidence is the sinking of the Earth's crust on a large scale, relative to crustal-scale features or the geoid. [1] The movement of crustal plates and accommodation spaces produced by faulting [2] brought about subsidence on a large scale in a variety of environments, including passive margins, aulacogens, fore-arc basins, foreland basins, intercontinental basins and pull-apart basins.
Table of geography, hydrography, and navigation, from a 1728 Cyclopaedia.. Hydrography is the branch of applied sciences which deals with the measurement and description of the physical features of oceans, seas, coastal areas, lakes and rivers, as well as with the prediction of their change over time, for the primary purpose of safety of navigation and in support of all other marine activities ...
The General Bathymetric Chart of the Oceans (GEBCO) is a publicly available bathymetric chart of the world's oceans. The project was conceived with the aim of preparing a global series of charts showing the general shape of the seafloor. Over the years it has become a reference map of the bathymetry of the world's oceans for scientists and others.
The subsidence resulted from crustal stretching, cooling, and loading. Initially, the crustal stretching and cooling combination caused about 5–7 km (3.1–4.3 miles) of tectonic subsidence of the central thin transitional and oceanic crust. The basin expanded and deepened because subsidence occurred faster than sediment could fill it. [9 ...
Interstate 10 eastbound in downtown entering the Wallace Tunnel. Inside of the tunnel, westbound lane. The George C. Wallace Tunnel, like the Bankhead Tunnel, emerges on the west end under Royal Street, in downtown Mobile (see map); however, whereas the Bankhead Tunnel emerges at street level joining into Government Street, the George C. Wallace Tunnel slopes upward to continue Interstate 10 ...