See also:

• AUGUST (originally Sextilis)

AUGUST See also:

• FRIEDRICH, JOHANN (1836— )

FRIEDRICH See also:

• AUGUST FRIEDRICH GFRORER (1803–1861)

GFRORER (1803–1861)  , See also:

• GERMAN
• GERMAN, DUTCH AND SCANDINAVIAN

German historian, was See also:

• BORN, IGNAZ, EDLER VON (1742–1791)

born at See also:

• CALW

Calw, See also:

• WURTTEMBERG

Wurttemberg, on the 5th of See also:

• MARCH
• MARCH (1) (from Fr. marcher, to walk; the earliest sense in French appears to be " to trample," and the origin has usually been found in the Lat. marcus, hammer; Low Lat. marcare, to hammer; hence to beat the road with the regular tread of a soldier: cf.
• MARCH, AUZIAS (c. "1395-1458)
• MARCH, EARLS OF
• MARCH, FRANCIS ANDREW (1825– )

March ' So written, with a medial mem (re) instead of the final (o) . to See also:

• ACCOUNT
• ACCOUNT (through O. Fr. acont, Late Lat. comptum, cornputare, to calculate)

account for the frequent and periodical See also:

• PRODUCTION (Lat. productionem, from producere, to pro-duce)

production of the necessary See also:

• HEAT (0. E. haktu, which like " hot," Old Eng. hat, is from the Teutonic type haita, hit, to be hot; cf. Ger. hitze, heiss; Dutch, hitte, heet, &c.)

heat ; but he has the See also:

• CREDIT (Lat. credere, to believe)

credit of hitting on what is certainly the proximate cause—the sudden See also:

• EVOLUTION

evolution of See also:

• STEAM
• STEAM (0. Eng. steam, vapour, smoke, cf. Du. steam; the origin is unknown)

steam . By See also:

• BUNSEN, CHRISTIAN CHARLES JOSIAS, BARON VON (1791-186o,)
• BUNSEN, ROBERT WILHELM VON (1811-1899)

Bunsen's theory the whole difficulty is solved, as is beautifully demonstrated by the artificial See also:

• GEYSER, GEISER, or GEISIR

geyser designed by J . H . J . See also:

• MULLER, FERDINAND VON, BARON (1825–1896)
• MULLER, FRIEDRICH (1749-1825)
• MULLER, GEORGE (1805-1898)
• MULLER, JOHANNES PETER (18o1-1858)
• MULLER, JOHANNES VON (1752-1809)
• MULLER, JULIUS (18oi-1878)
• MULLER, KARL OTFRIED (1797-1840)
• MULLER, LUCIAN (1836-1898)
• MULLER, WILHELM (1794-1827)
• MULLER, WILLIAM JAMES (1812-1845)

Muller of See also:

• FREIBURG

Freiburg (fig . 2) . If the See also:

• TUBE (Lat. tuba)

tube ab be filled with See also:

• WATER

water and heated at two points, first at a and then at b, the following See also:

• SUCCESSION (Lat. successio, from succedere, to follow after)

succession of changes is produced . The water at a beginning to See also:

• BOIL

boil, the superincumbent See also:

• COLUMN (Lat. columna)

column is consequently raised, and the stratum of water which was on the point of boiling at b being raised to d is there subjected to a diminished pressure; a sudden evolution of steam accordingly takes See also:

• PLACE (through Fr. from Lat. platea, street; Gr. IrAar6s, wide)

place at d, and the superincumbent water is violently ejected . Received in the See also:

• BASIN, or BASON (the older form bacin is found in many of the Romanic languages, from the Late Lat. baccinus or bacchinus, probably derived from bacca, a bowl)
• BASIN, THOMAS (1412—1491)

basin c, the See also:

• AIR (from an Indo-European root meaning " breathe," " blow ")
• AIR, or ASBEN

air-cooled water sinks back into the tube, and the temperature of the whole column is consequently lowered; but the under strata of water are naturally those which are least affected by the cooling See also:

• PROCESS

process; the boiling begins again at a, and the same succession of events is the result (see R . Bunsen, " Physikalische Beobachtungen fiber See also:

• DIE
• DIE (Fr. de, from Lat. datum, given)

die hauptsachlichsten Geisire Islands," Pogg . See also:

• ANN

Ann., 1847, vol .

72; and Muller, " Uber Bunsen's Geysertheorie," ibid., 185o, vol . 79) . The See also:

• PRINCIPAL

principal difference between the artificial and the natural geyser-tube is that in the latter the effect is not necessarily produced by two distinct See also:

• SOURCES

sources of heat like the two fires of the experimental apparatus, but by the continual influx of heat from the bottom of the See also:

• SHAFT
• SHAFT (O. Eng., sceaft, from scafan, to shave; the word is common to Teutonic languages)

shaft, and the See also:

• DIFFERENCES, CALCULUS OF (Theory of Finite Differences)

differences between the boiling-points of 186° 225° the different parts of the column owing to 230° 241° the different pressures of the superincum- ° See also:

• BENT
• BENT (E1. BENI)
• BENT, JAMES THEODORE (1852–1897)

bent See also:

• MASS (O.E. maesse; Fr. messe; Ger. Messe; Ital. messa; from eccl. Lat. missa)
• MASS, IN

mass . This may be thus illustrated: C 249 AB is the column of water; on the right 255° See also:

• SIDE
• SIDE (mod. Eski Adalia)

side the figures represent approximately the boiling-points (Fahr.) calculated according to the See also:

• ORDINARY (med. Lat. ordinarius, Fr. ordinaire)

ordinary See also:

• LAWS

laws, and the figures on the See also:

• LEFT

left the actual temperature of the same places . Both gradually increase as we descend, but the relation between the two is very different at different heights . At the See also:

• TOP (cf. Dan. top, Ger. Topf, also meaning pot)

top the water is still 39° from its boiling-point, and even at the bottom it is 19°; but at D the deficiency is only 4° . If, then, the-stratum at D be suddenly lifted as high as C, It will be 2° above the boiling-point there, and will consequently expend those 2° in the formation of steam .