The salter waters apparently tend to make their way westwards close to the African coast, and at the bottom the highest salinities have been observed south of Crete.
Salter and H.
The very dense water of the Red Sea and the Mediterranean makes the column of water salter and heavier and the level lower than in the ocean beyond the straits.
Through the Bosporus and Dardanelles at the entrance of the Black Sea, and through the sound and belts at the entrance of the Baltic, streams of fresh surface-water flow outwards to the salter Mediterranean and North Sea, while salter water enters in each case as an undercurrent.
Bowman, The Administration of Iowa, a Study in Centralization (New York, 1903), an able presentation of the present administrative system in the light of its historical development; William Salter, Iowa, the first Free State in the Louisiana Purchase (Chicago, 1905); B.
It is tidal, spring tides rising about 9 ft.; the water is somewhat salter than the Indian Ocean, and seldom exceeds 10 fathoms in depth; with the exception of the Shatt al `Arab, the Jarrahi and the Hindiyan rivers, which mingle their waters with those of the sea at the W.
Among them were Henry Ward Beecher, pastor of Plymouth church (Congregational) from 1847 to 1887; Lyman Abbott, pastor of the same church from 1887 to 1898; Thomas De Witt Talmage, pastor of the Brooklyn Tabernacle (Presbyterian) from 1869 to 1894; Richard Salter Storrs (1821-1900), pastor of the church of the Pilgrims (Congregational) from 1846 to 1899; and Theodore L.
Salter, the palaeontologist; and in 1852 he included the Llandeilo and Bala beds (Silurian) in the Upper Cambrian.
It was left for the subsequent labours of Salter and H.
This statement holds good for the Gulf of Suez, in which the water is much salter than in the open;sea; but in the Gulf of Akaba the distribution is exceedingly uniform, nowhere differing much from an average of 40.6 per mille.
The great evaporation going on from the surface probably causes a slow vertical circulation in the depth, the salter colder waters sinking, and ultimately escaping to the Indian Ocean.
The water is salter than the sea.
Beneath these layers are masses of salter water, through which a thermal wave of small amplitude is slowly propagated to the bottom by conduction.
Their salter waters must have been originally derived from outside, and must therefore have passed over the plateau between Falster and Mecklenburg, but their horizontal extension is checked by the ridges separating the deep hollows in the Baltic from each other.