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1. (of a vessel) Floating freely (not aground or sunk). The term may also be used more generally of any floating object or person. 2. In service, even if not currently underway, but not stranded, crewless, in repair, or under construction (e.g. "the company has 10 ships afloat"). afore 1. In, on, or toward the fore or front of a vessel. [3] 2.
The Standard Marine Communication Phrases (SMCP) is a set of key phrases in the English language (which is the internationally recognised language of the sea), supported by the international community for use at sea and developed by the International Maritime Organization (IMO). They aim to explain: 1) external communication phrases – ship to ...
Aweigh: just clear of the sea floor, as with an anchor. [11] Below: a lower deck of the ship. [1] Belowdecks: inside or into a ship, or down to a lower deck. [12] Bilge: the underwater part of a ship between the flat of the bottom and the vertical topsides [13] Bottom: the lowest part of the ship's hull. Bow: front of a ship (opposite of "stern ...
Maskot/Getty Images. 6. Delulu. Short for ‘delusional,’ this word is all about living in a world of pure imagination (and only slightly detached from reality).
A map of a sea or ocean area and adjacent coastal regions, intended specifically for navigation at sea. Nautical charts use map projections designed for easy use with hand instruments, such as the Mercator projection , and indicate depths, hazards, landmarks , aids to navigation such as buoys , and ashore facilities of interest to mariners .
Jeff Williams' song "Bad Luck Charm" contains the line "I'm a cursed black cat, I'm an albatross, I'm a mirror broken, Sad to say, I'm your bad luck charm". Josh Ritter refers to a lingering albatross in his song "Monster Ballad". The characters are lost in the desert after having been lost at sea.
Floating objects may ride gyres (large circulating current systems) that are present in each ocean, and may be transferred from one ocean's gyre to another's. [24] Further, objects may be sidetracked by wind, storms, countercurrents, and ocean current variation. [24]
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