- baymouth bar
- Макаров: бар устья бухты, устьевой бар
Универсальный англо-русский словарь. Академик.ру. 2011.
baymouth bar
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Baymouth bar — A baymouth bar is a depostional feature as a result of longshore drift. It is a spit that completely closes access to a bay, thus sealing it off from the main body of water. These bars usually consist of accumulated gravel and sand carried by the … Wikipedia
baymouth bar — a bar extending partly or wholly across the mouth of a bay … Dictionary of ichthyology
baymouth bar — ˈbāˌmau̇th noun Etymology: bay (IX) + mouth : bay bar … Useful english dictionary
Mouth bar — A mouth bar is a bar in a river that is typically created in the middle of a channel in a river delta.[1] It is created by a positive feedback between mid channel deposition and flow divergence. As the flow diverges near the ocean, sediment… … Wikipedia
bay bar — noun or bay barrier Etymology: bay (IX) : a bank of sand or of sand and gravel deposited by waves and currents across the mouth of a bay so that the bay is no longer connected or is connected only by a narrow outlet with the main body of water… … Useful english dictionary
Shoal — Bar (landform) redirects here. For other uses, see Bar (disambiguation)#Landforms. Sandbank redirects here. For other uses, see Sandbank (disambiguation). For other uses, see Shoal (disambiguation). Sandbar between St. Agnes and Gugh on the Isles … Wikipedia
River delta — Nile River delta, as seen from Earth orbit. The Nile is an example of a wave dominated delta that has the classic Greek delta (Δ) shape after which river deltas were named. A delta is a landform that is formed at the mouth of a river where that… … Wikipedia
Spit (landform) — For other uses of the term, see Spit (disambiguation). Diagram showing a spit A spit or sandspit is a deposition landform found off coasts. At one end, spits connect to land, and extend into the sea.[1] A spit is a type of bar or beach that … Wikipedia
Avulsion (river) — In sedimentary geology and fluvial geomorphology, avulsion is the rapid abandonment of a river channel and the formation of a new river channel. Avulsions occur as a result of channel slopes that are much lower than the slope that the river could … Wikipedia
Coastal geography — is the study of the dynamic interface between the ocean and the land, incorporating both the physical geography (i.e coastal geomorphology, geology and oceanography) and the human geography (sociology and history) of the coast. It involves an… … Wikipedia
Sand — For other uses, see Sand (disambiguation). Close up of sand from the Gobi Desert, Mongolia, showing a surface area of 1 square centimetres … Wikipedia
