...Mr. Clifton Sorby, in his microscopical researches into the composition of meteorites, states, that "some isolated portions of meteorites have also a structure very similar to stony lavas " ; and again : " this sometimes gives rise to a structure remarkably like that of consolidated...

...mineral was at one time in a state of igneous fusion. The olivin also contains 'gas cavities' like thoee so common in volcanic minerals, thus indicating the...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity...

...met with outside and amongst the crystals, in such a manner as to show that it is the incrystalline residue of the material in which they were formed...glasses. Some isolated portions of meteorites have \lso a structure very similar to that of stony lavas, where the shape and mutual relations of the crystals...

...uncrystalline residue of the material in which they were formed. It is of a claret or brownish color, and possesses the characteristic structure and optical...and mutual relations of the crystals to each other proved that they were formed in situ on solidification. A structure is also found so remarkably like...

...show that it is the uncrystalline residue of the material in which they were formed ( Mezb'-Madaras, Parnallee). It is of a claret or brownish colour,...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity...

...show that it is the uncrystalline residue of the material in which they were formed (Mezö-Madaras, Parnallee). It is of a claret or brownish colour,...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity...

...The vitreous substance found in the cavities is also met with outside and amongst the crysstals, in such a manner as to show that it is the uncrystalline...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity...

...material in which they were formed (Mezo-Madaras, Parnallee). It is of a claret or brownish color, and possesses the characteristic structure and optical...crystals to each other prove that they were formed in situ, on solidification. Possibly some entire meteorites should be considered to possess this peculiarity...