A Treatise on Attractions, Laplace's Functions and the Figure of the EarthMacmillan, 1865 - 162 páginas |
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Página v
... stations of the Indian Arc , the volume is closed by a summary of the ar- gument regarding the hypothesis of the original fluidity of the earth , an hypothesis which I consider to be established beyond doubt . J. H. PRATT . CALCUTTA ...
... stations of the Indian Arc , the volume is closed by a summary of the ar- gument regarding the hypothesis of the original fluidity of the earth , an hypothesis which I consider to be established beyond doubt . J. H. PRATT . CALCUTTA ...
Página xii
... stations on the Indian Arc 147 · 152. Mean and geodetic arcs of longitude sensibly the same 153. Effect of local attraction in mapping a country 154. On the curvature of particular arcs 150 151 . 152 156. Geodesy gives no evidence ...
... stations on the Indian Arc 147 · 152. Mean and geodetic arcs of longitude sensibly the same 153. Effect of local attraction in mapping a country 154. On the curvature of particular arcs 150 151 . 152 156. Geodesy gives no evidence ...
Página 45
... stations from the point where the axis crosses the meridian are 3 ° 39 ' , 9 ° 23 ' , 15 ° 27 ′ or 219 ' , 563 ' , 927 ' ; in the same proportion are the distances of the stations from the prism or axis . It will be found that the ...
... stations from the point where the axis crosses the meridian are 3 ° 39 ' , 9 ° 23 ' , 15 ° 27 ′ or 219 ' , 563 ' , 927 ' ; in the same proportion are the distances of the stations from the prism or axis . It will be found that the ...
Página 46
... station above its middle point . 51. Let t be the thickness or depth ; h the height of the particle from the nearer ... station above the middle of the attracting mass below , that is , h + t , be so small that it may be neg- lected in ...
... station above its middle point . 51. Let t be the thickness or depth ; h the height of the particle from the nearer ... station above the middle of the attracting mass below , that is , h + t , be so small that it may be neg- lected in ...
Página 47
... station on the continent will be diminished from this cause by the amount 2t a 9 { 1- ( 1 + ) - 9 nearly . But the attraction of the underlying mass of thickness t must be taken into account . Hence the real diminution of gravity by the ...
... station on the continent will be diminished from this cause by the amount 2t a 9 { 1- ( 1 + ) - 9 nearly . But the attraction of the underlying mass of thickness t must be taken into account . Hence the real diminution of gravity by the ...
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Términos y frases comunes
amplitude angle attracted particle axes axis calculation Cape Comorin centre Clairaut's Theorem co-ordinates coefficient compartments cos 2m cos² crust Damargida deduced deflection difference distance earth earth's mass effect ellipticity equal equation equilibrium expansion find the attraction fluid mass fluid theory formula geodesy gravity height Hence Himmalayas hypothesis Indian Arc integration Kaliana Kalianpur Laplace's Equation Laplace's Functions last Article latitude law of attraction length longitude mean arc mean ellipse mean figure measured Mechanical Philosophy meniscus meridian miles nearly spherical ocean Ordnance Survey pendulum experiments plumb-line pole precession prism PROP quantities radius result rigid sea-level semi-axes series of Laplace's shell sin² solid sphere spheroid square station strata suppose T₂ thickness tion δα µ² µ³
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