...K'dsegrotte, Bertrich-Baden, half way between Treves and Coblentz. Height of grotto, from 7 to Sfeet. a small stream of lava, from 30 to 40 feet thick,...represented by a section like that already given at (Fig. 100. p. 184.), if we merely suppose inclined strata of slate and the argillaceous sandstone called...

...Kasegrotte, Bertrich-Badcn, half way between Treves and Coblcntx. Height of grotto, from 7 to Sfeet. a small stream of lava, from 30 to 40 feet thick,...represented by a section like that already given at (Fig. 100. p. 184.), if we merely suppose inclined strata of slate and the argillaceous sandstone called...

...of the Kiiacgrotte, Bertrick-Saden, halfway between CoUentz. Height of grotto from 7 to 8 feet. and basalt, there, is part of a small stream of lava,...be represented by a section like that already given (Fig. 100. p. 112.), if we merely suppose inclined strata of slate and the argillaceous sandstone called...

...a¡ the Kätfgrvttr, Serlricn-Barin, ìiaìf tray and 1'Mtnls. Ufifltl of grolla, from 7 to xjfrl. a small stream of lava, from 30 to 40 feet thick, which has proceeded from one of several vulcanic »ters, still extant, on the neighbouring heights. lie position of the lava bordering the...

...Kisegrotte, Bertrich-Baden, half may between 7V««» and CoUentz. Height of grotto from 1 to 8 feet. basalt, there, is part of a small stream of lava, from 30 to 40 li vt thick, which has proceeded from one of several volcanic craters, still extant, on the neighbouring...

...Käsegrotte, Bertrich-Baden, halfway between Trena and Coblenlz. Height of grotto from 7 io 8 feet. basalt, there, is part of a small stream of lava,...be represented by a section like that already given (Fig- 100. p. 112.), if we merely suppose inclined strata of slate and the argillaceous sandstone called...

...is called the Kasegrotte, or Cheese-cavp. "The basalt is part of a lava-stream, from thirty to forty feet thick, which has proceeded from one of several...volcanic craters still extant on the neighbouring hills ;"t and, having run in the valley, it has since been partially destroyed and excavated by long-continued...

...usually flattened, as in the Cheesegrotto at Bertrich-Baden, in the Eifel, near the Moselle (fig. 690.). The basalt there is part of a small stream of lava, from 30 to 40 feet thiek, which has proceeded from Columnar basalt in the Vicentin. (Forti».) Basaltic pillari of the...

...usually flattened, as in the Cheese-grotto at Bertrich-Badeo, in the Eifel, near the Moselle (fig. 690). The basalt there is part of a small stream of lava,...of several volcanic craters, still extant, on the neighboring heights. The position of the lava bordering the river in this valley might be represented...

...usually flattened, as in the Cheesegrotto at 'Bertrich-Baden, in the Eifel, near the Moselle (fig. 590). The basalt there is part of a small stream of lava,...craters, still extant, on the neighbouring heights. Columnar basnlt in the Vicentin. (Fortis.) In some masses of decomposing greenstone, basalt, and other...