| 作曲 : Dreijer & Dreijer Andersson (S | |
| 作词 : Dreijer & Dreijer Andersson (S | |
| White sand made up of shells upon which rests carious rock, | |
| then prismatic feldspar between these and former ones, hard white rock with | |
| yellow spots. A heap of white balls beneath white sand. | |
| Same process now going on shore, living iron found in it. | |
| Sand white from decomposition of feldspar. In places | |
| every rock is covered with pistiform concretions. In places impossible to tell | |
| whether it is Breccia of modern or older days. Lower | |
| beds of white sand become filled with large boulders of lower rocks. | |
| Beneath this comes a line of another stratum, more | |
| soily and contains large and more numerous shells. | |
| A regular bed of oysters remains attached to the rocks. |
| zuo qu : Dreijer Dreijer Andersson S | |
| zuo ci : Dreijer Dreijer Andersson S | |
| White sand made up of shells upon which rests carious rock, | |
| then prismatic feldspar between these and former ones, hard white rock with | |
| yellow spots. A heap of white balls beneath white sand. | |
| Same process now going on shore, living iron found in it. | |
| Sand white from decomposition of feldspar. In places | |
| every rock is covered with pistiform concretions. In places impossible to tell | |
| whether it is Breccia of modern or older days. Lower | |
| beds of white sand become filled with large boulders of lower rocks. | |
| Beneath this comes a line of another stratum, more | |
| soily and contains large and more numerous shells. | |
| A regular bed of oysters remains attached to the rocks. |
| zuò qǔ : Dreijer Dreijer Andersson S | |
| zuò cí : Dreijer Dreijer Andersson S | |
| White sand made up of shells upon which rests carious rock, | |
| then prismatic feldspar between these and former ones, hard white rock with | |
| yellow spots. A heap of white balls beneath white sand. | |
| Same process now going on shore, living iron found in it. | |
| Sand white from decomposition of feldspar. In places | |
| every rock is covered with pistiform concretions. In places impossible to tell | |
| whether it is Breccia of modern or older days. Lower | |
| beds of white sand become filled with large boulders of lower rocks. | |
| Beneath this comes a line of another stratum, more | |
| soily and contains large and more numerous shells. | |
| A regular bed of oysters remains attached to the rocks. |
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