“The __ is calm tonight”: “Dover Beach” opening

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Possible Answers: SEA.

Last seen on: LA Times Crossword 22 May 2018, Tuesday

Random information on the term ““The __ is calm tonight”: “Dover Beach” opening”:

A diacritic – also diacritical mark, diacritical point, or diacritical sign – is a glyph added to a letter, or basic glyph. The term derives from the Ancient Greek διακριτικός (diakritikós, “distinguishing”), from διακρίνω (diakrī́nō, “to distinguish”). Diacritic is primarily an adjective, though sometimes used as a noun, whereas diacritical is only ever an adjective. Some diacritical marks, such as the acute ( ´ ) and grave ( ` ), are often called accents. Diacritical marks may appear above or below a letter, or in some other position such as within the letter or between two letters.

The main use of diacritical marks in the Latin script is to change the sound-values of the letters to which they are added. Examples are the diaereses in the borrowed French words naïve and Noël, which show that the vowel with the diaeresis mark is pronounced separately from the preceding vowel; the acute and grave accents, which can indicate that a final vowel is to be pronounced, as in saké and poetic breathèd; and the cedilla under the “c” in the borrowed French word façade, which shows it is pronounced /s/ rather than /k/. In other Latin-script alphabets, they may distinguish between homonyms, such as the French là (“there”) versus la (“the”) that are both pronounced /la/. In Gaelic type, a dot over a consonant indicates lenition of the consonant in question.


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“The __ is calm tonight”: “Dover Beach” opening on Wikipedia

Random information on the term “SEA”:

A sea is a large body of salt water that is surrounded in whole or in part by land.[a] More broadly, “the sea” is the interconnected system of Earth’s salty, oceanic waters—considered as one global ocean or as several principal oceanic divisions. The sea moderates Earth’s climate and has important roles in the water cycle, carbon cycle, and nitrogen cycle. Although the sea has been traveled and explored since prehistory, the modern scientific study of the sea—oceanography—dates broadly to the British Challenger expedition of the 1870s. The sea is conventionally divided into up to five large oceanic sections—including the International Hydrographic Organization’s four named oceans (the Atlantic, Pacific, Indian, and Arctic) and the Southern Ocean; smaller, second-order sections, such as the Mediterranean, are known as seas.

Owing to the present state of continental drift, the Northern Hemisphere is now fairly equally divided between land and sea (a ratio of about 2:3) but the South is overwhelmingly oceanic (1:4.7). Salinity in the open ocean is generally in a narrow band around 3.5% by mass, although this can vary in more landlocked waters, near the mouths of large rivers, or at great depths. About 85% of the solids in the open sea are sodium chloride. Deep-sea currents are produced by differences in salinity and temperature. Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun. The direction of all of these is governed by surface and submarine land masses and by the rotation of the Earth (the Coriolis effect).

SEA on Wikipedia