Proceedings of the Royal Society of Edinburgh, Том 9The Society, 1878 Obituary notices are included in many of the volumes. |
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Результати 1-5 із 46
Сторінка 50
... centre of eruption ; the aneroid stood at 25 · 05 ( = 5000 feet in round num- bers , whilst the northern plain is about 1000 feet lower . Various angles to Herðubreið ( 80 ° to 40 ° for mag . var . , west 40 ) , and the Skjaldbreið ...
... centre of eruption ; the aneroid stood at 25 · 05 ( = 5000 feet in round num- bers , whilst the northern plain is about 1000 feet lower . Various angles to Herðubreið ( 80 ° to 40 ° for mag . var . , west 40 ) , and the Skjaldbreið ...
Сторінка 59
... centre of gravity , and left free , performs steady motion . Not so a body having three unequal principal moments of inertia . ( 2. ) A rigid body of any shape , in an infinite homogeneous liquid , rotating uniformly round any , always ...
... centre of gravity , and left free , performs steady motion . Not so a body having three unequal principal moments of inertia . ( 2. ) A rigid body of any shape , in an infinite homogeneous liquid , rotating uniformly round any , always ...
Сторінка 67
... centre of the diagram , and perpendicular to the plane in each of the cases represented by the preceding diagrams . The whole motion of the fluid , rotational and irrotational , is so related in its different parts to one another , and ...
... centre of the diagram , and perpendicular to the plane in each of the cases represented by the preceding diagrams . The whole motion of the fluid , rotational and irrotational , is so related in its different parts to one another , and ...
Сторінка 71
... centre of gravity of the areas of these three sets of projections . Find , according to Poinsot's method , the resultant axis , force , and couple of the three forces equal respectively to 1 n of the sums of the areas , and acting in ...
... centre of gravity of the areas of these three sets of projections . Find , according to Poinsot's method , the resultant axis , force , and couple of the three forces equal respectively to 1 n of the sums of the areas , and acting in ...
Сторінка 72
... centre of gravity . Definition V. - The area of the projection of a closed curve on the plane for which the area of projection is a maximum will be called the area of the curve , or simply the area of the curve . The area of the ...
... centre of gravity . Definition V. - The area of the projection of a closed curve on the plane for which the area of projection is a maximum will be called the area of the curve , or simply the area of the curve . The area of the ...
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Інші видання - Показати все
Proceedings of the Royal Society of Edinburgh, Том 23 Royal Society of Edinburgh Повний перегляд - 1902 |
Proceedings of the Royal Society of Edinburgh, Том 8 Royal Society of Edinburgh Повний перегляд - 1875 |
Proceedings of the Royal Society of Edinburgh, Том 6 Royal Society of Edinburgh Повний перегляд - 1869 |
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8vo.-From the Author 8vo.-From the Society Academy acid alum angle appears arrangement axis boulder clay Campsie Carboniferous chrome alum coil colour Convener copper curve deposits diameter didymium direction disc Dissert distance Dorpat Dorpat Univ dorsal dorsal fin Edinburgh Erlangen Erlangen Univ experiments Fasnacloich feet fish fungus Geological Glen granite Heft height Herðubreið hill horizontal hypoderm Inaug inches intersections iron knot length Loch Loch Creran Loch Etive magnetic marcasite miles motion neural canal nodules Observatory observed obtained occurs paper passed plate position present Proceedings produced Professor Tait pumice rays Report resistance ridges Robert Christison rocks rotation round Royal Society salt sandstone scales Scotland side solution sound species specimens striæ surface telephone terminal velocity terraces tion tube Ueber valley ventral vertical vibrations vortex vowel wire
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