On the Connexion of the Physical SciencesJ. Murray, 1858 - 523 pages |
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Page xi
... Temperature ascribed by Sir John Herschel to the varia- tion in the Excentricity of the Terrestrial Orbit - Difference in the Temperature of the two Hemispheres erroneously ascribed to the Excess in the Length of Spring and Summer in ...
... Temperature ascribed by Sir John Herschel to the varia- tion in the Excentricity of the Terrestrial Orbit - Difference in the Temperature of the two Hemispheres erroneously ascribed to the Excess in the Length of Spring and Summer in ...
Page xiii
... Temperature of Space - Internal Heat of the Earth Zone of constant Temperature Increase of Heat with the Depth Central Heat - Volcanic Action - Quantity of Heat - received from the Sun - Isogeothermal Lines - Line of Perpetual Con ...
... Temperature of Space - Internal Heat of the Earth Zone of constant Temperature Increase of Heat with the Depth Central Heat - Volcanic Action - Quantity of Heat - received from the Sun - Isogeothermal Lines - Line of Perpetual Con ...
Page xiii
... Temperature - Measurement of Heights by the Barometer - Extent of the Atmosphere- Barometrical Variations Oscillations Trade - Winds Cloud - Ring- Monsoons Winds - Laws of Hurricanes Rotation of Page 117 SECTION XVI . -- - - Sound ...
... Temperature - Measurement of Heights by the Barometer - Extent of the Atmosphere- Barometrical Variations Oscillations Trade - Winds Cloud - Ring- Monsoons Winds - Laws of Hurricanes Rotation of Page 117 SECTION XVI . -- - - Sound ...
Page xiii
... Temperature of Space - Internal Heat of the Earth - Zone of constant Temperature - Increase of Heat with the Depth - Central Heat - Volcanic Action - Quantity of Heat received from the Sun - Isogeothermal Lines - Line of Perpetual Con ...
... Temperature of Space - Internal Heat of the Earth - Zone of constant Temperature - Increase of Heat with the Depth - Central Heat - Volcanic Action - Quantity of Heat received from the Sun - Isogeothermal Lines - Line of Perpetual Con ...
Page 71
... Temperature ascribed by Sir John Herschel to the varia- tion in the Excentricity of the Terrestrial Orbit — Difference in the Temperature of the two Hemispheres erroneously ascribed to the Excess in the Length of Spring and Summer in ...
... Temperature ascribed by Sir John Herschel to the varia- tion in the Excentricity of the Terrestrial Orbit — Difference in the Temperature of the two Hemispheres erroneously ascribed to the Excess in the Length of Spring and Summer in ...
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61 Cygni absorbed action appears atmosphere attraction bismuth blue bodies centre centrifugal force chemical circular polarization coloured rings comet consequently copper crystal dark density diamagnetic diameter diminishes direction distance disturbing earth ecliptic effect electricity equal equator ethereal medium excentricity experiments extreme force gravitation greater heat hemisphere increase intensity Jupiter latitude length lines liquid longitude luminous lunar magnetic mass mean meridian metallic miles molecules moon motion move nebula nodal lines nodes NOTE nutation observed optic axis orbit parallax paramagnetic particles passing perihelion period perpendicular phenomena plane polarized light pole position prism produced quantity rays reflected refraction refrangible retrograde motion revolution revolving right angles rotation round satellites Sir John Herschel solar spectrum sound space stars substances sun's surface telescope temperature terrestrial theory tion tourmaline transmitted tricity undulations Uranus vapour velocity vibrations violet visible Voltaic waves wire