 ... rains. By virtue of these films, the sand-grains become separated by elastic cushions of condensed gases, capable of considerable vibration, and whose thickness we have approximately determined. The extent of the vibration and the volume and pitch...  Tales of Travel - Page 392de Marquess George Nathaniel Curzon Curzon of Kedleston - 1923 - 381 pagesAffichage du livre entier - À propos de ce livre
 | American Association for the Advancement of Science - 1891 - 612 pages
...stated In this connection. We believe the sonorousness in sands of sea-beaches and of deserts to be connected with thin pellicles or films of air, or...sand-grains during gradual evaporation after wetting by the seas, lakes or rains. By virtue of these films the sand grains become separated by elastic cushions... | |
 | American Association for the Advancement of Science - 1891 - 616 pages
...the sonorousness in sands of sea-beaches and of deserts to be connected with thin pellicles or lllms of air, or of gases thence derived, deposited and...sand-grains during gradual evaporation after wetting by the seas, lakes or rains. By virtue of these films the sand grains become separated by elastic cushions... | |
 | American Association for the Advancement of Science - 1890 - 610 pages
...evaporation after wetting by the soas, lakes, or by rains. By virtue of these films the sand grains become separated by elastic cushions of condensed gases, capable of considerable vibration, and whose thickness we have approximately determined. The extent of the vibration and the volume and... | |
 | New York Academy of Sciences - 1890 - 254 pages
...upon the surface of the sand-grains during gradual evaporation after wetting by seas and lakes or by rains. By virtue of these films, the sand-grains become...condensed gases, capable of considerable vibration, and whose thickness we have approximately determined. The extent of the vibration and the volume and... | |
 | John Michels (Journalist) - 1920 - 678 pages
...Julien and I believe that the true cause of sonorousness in the sands of singing beaches and of deserts is connected with thin pellicles or films of air,...sand-grains during gradual evaporation after wetting by seas and lakes or by rains. By virtue of these films, the sand-grains become separated by elastic cushions... | |
 | William Shepard Walsh, Henry Collins Walsh, William H. Garrison, Samuel R. Harris - 1890 - 354 pages
...gradual evaporation after wetting by seas, lakes, or rains. By virtue of these films the sand grains become separated by elastic cushions of condensed gases, capable of considerable vibration, and whose thickness we have approximately determined. The extent of the vibration and the volume and... | |
 | 1890 - 674 pages
...stated in this connection. We believe the sonorousness in sands of sea-beaches and of deserts to be connected with thin pellicles or films of air, or...sand-grains during gradual evaporation after wetting by the seas, lakes, or rains. By virtue of these films the sand-grains become separated by elastic cushions... | |
 | 1890 - 1290 pages
...Julien. The cause of sonorousness in the sands of singing beaches and of deserts is believed to be connected with thin pellicles or films of air, or...sand-grains during gradual evaporation after wetting by the seas, lakes, or by rains. By virtue of these films the sand-grains become separated by elastic cushions... | |
 | American Association for the Advancement of Science - 1890 - 612 pages
...and I believe the true cause1 of sonorousness In the sands of singing beaches and of deserts to be connected with thin pellicles or films of air, or...derived, deposited and condensed upon the surface of the sand grains during gradual evaporation after wetting by the seas, Inkes, or by ruins. By virtue of... | |
 | American Association for the Advancement of Science - 1890 - 258 pages
...Julien and I believe the true cause of sonorousness in the sands of singing beaches and of deserts to be connected with thin pellicles or films of air, or...derived, deposited and condensed upon the surface of the sand grains during gradual evaporation after wetting by the seas, lakes, or by rains. By virtue of... | |
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