 Gjas, or chasms, which form its lateral boundaries, to mark the limits of the disruption; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a roof beneath which the molten stream flowed...  A Girl's Ride in Iceland - Seite 108von Mrs. Alec-Tweedie (Ethel) - 1894 - 166 SeitenVollansicht - Über dieses Buch
 | Frederick Temple Blackwood Marquis of Dufferin and Ava - 1857 - 544 Seiten
...side from the adjoining plateau, and sinking down to its present level, left the two parallel Gjas, or chasms, which form its lateral boundaries, to mark the limits of the disruption; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a... | |
 | Wonders - 1866 - 400 Seiten
...side from the adjoining plateau, and, sinking down to its present level, left the two parallel Gjas, or chasms, which form its lateral boundaries, to mark...the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a... | |
 | Georg Hartwig - 1869 - 500 Seiten
...plateau, and sinking down to its present level, left two parallel gjas, FALL OF THE OXERAA. ^ ' . ' rni or chasms, which form its lateral -boundaries, to...the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a... | |
 | Georg Ludwig Hartwig - 1869 - 614 Seiten
...either side from the adjoining plateau, and sinking down to its present level, left two parallel gjas or chasms, which form its lateral boundaries, to mark...the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a... | |
 | Georg Hartwig - 1869 - 602 Seiten
...its lateral boundaries, to mark the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a roof, beneath which the molten stream flowed on to lower levels, leaving a vast cavern into which the upper crust... | |
 | Georg Hartwig - 1872 - 780 Seiten
...either side from the adjoining plateau, and sinking down to its present level, left two parallel gjas, or chasms, which form its lateral boundaries, to mark...the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a... | |
 | Esther Singleton - 1900 - 480 Seiten
...its lateral boundaries, to mark the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a roof beneath which the molten stream flowed on to lower levels, leaving a vast cavern into which the upper crust... | |
 | Esther Singleton - 1900 - 474 Seiten
...from the adjoining plateau, and sinking down to its present level, left the two paralleled Gjas,or chasms, which form its lateral boundaries, to mark the limits of the disruption ; or else, while the pith or marrow of the lava was still in a fluid state, its upper surface became solid, and formed a... | |
| |
