Geographical Notes | Nature

Geographical Notes | Nature

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ABSTRACT M. VIOLET D'AOUEST read a note at a late meeting of the Geographical Society of Paris on aerial formations on the soil. Referring to Richthofen's discovery of a vast aerial formation of loess in China, M. d'Aouest described meteoric formations which he had himself examined in Mexico. In 1857 he made a communication on this subject to the Society; he found in the flanks of the most elevated mountains argillaceous deposits, which could not be attributed to decomposition of the rocks there, or to the alluvion deposited by rivers, or by the rain. He referred them after investigation to atmospheric currents. In the day the winds raised the particles from the plains and carried them at night to the hills, depositing them there. In course of time these deposits had reached a thickness of thirty to fifty and in places a hundred metres. The upper part, which was generally finer, stopped at the limit of herbaceous vegetation, for beyond this there was nothing to retain the particles, which were carried down by rains, glaciers, snow, or winds to the lower part. Fifteen years later he heard of Richthofen's publication on the subject, and Col. Prjevalsky during his late journeys in Thibet states that analogous aerial deposits are now being formed under the influence of powerful winds which prevail at these altitudes. Subsequently M. d'Aouest met Baron Richthofen and discussed the subject with him, when the latter stated that these formations exist in Europe, adding that it was singular how men, unknown to and far removed from each other, could be led to make the same discoveries in wholly different regions. M. d'Aouest now intends publishing a translation of Richthofen's monograph on the subject, with a supplement of his own containing a number of important documents which he has collected on these deposits. He thinks he will be able to explain loess and argillaceous deposits, the origin of which has hitherto been regarded as problematical, by this theory. Access through your institution Buy or subscribe This is a preview of subscription content, access via your institution ACCESS OPTIONS Access through your institution Subscribe to this journal Receive 51 print issues and online access $199.00 per year only $3.90 per issue Learn more Buy this article * Purchase on SpringerLink * Instant access to full article PDF Buy now Prices may be subject to local taxes which are calculated during checkout ADDITIONAL ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE _Geographical Notes_ . _Nature_ 32, 376 (1885). https://doi.org/10.1038/032376a0 Download citation * Issue Date: 20 August 1885 * DOI: https://doi.org/10.1038/032376a0 SHARE THIS ARTICLE Anyone you share the following link with will be able to read this content: Get shareable link Sorry, a shareable link is not currently available for this article. Copy to clipboard Provided by the Springer Nature SharedIt content-sharing initiative

ABSTRACT M. VIOLET D'AOUEST read a note at a late meeting of the Geographical Society of Paris on aerial formations on the soil. Referring to Richthofen's discovery of a vast


aerial formation of loess in China, M. d'Aouest described meteoric formations which he had himself examined in Mexico. In 1857 he made a communication on this subject to the Society; he


found in the flanks of the most elevated mountains argillaceous deposits, which could not be attributed to decomposition of the rocks there, or to the alluvion deposited by rivers, or by


the rain. He referred them after investigation to atmospheric currents. In the day the winds raised the particles from the plains and carried them at night to the hills, depositing them


there. In course of time these deposits had reached a thickness of thirty to fifty and in places a hundred metres. The upper part, which was generally finer, stopped at the limit of


herbaceous vegetation, for beyond this there was nothing to retain the particles, which were carried down by rains, glaciers, snow, or winds to the lower part. Fifteen years later he heard


of Richthofen's publication on the subject, and Col. Prjevalsky during his late journeys in Thibet states that analogous aerial deposits are now being formed under the influence of


powerful winds which prevail at these altitudes. Subsequently M. d'Aouest met Baron Richthofen and discussed the subject with him, when the latter stated that these formations exist in


Europe, adding that it was singular how men, unknown to and far removed from each other, could be led to make the same discoveries in wholly different regions. M. d'Aouest now intends


publishing a translation of Richthofen's monograph on the subject, with a supplement of his own containing a number of important documents which he has collected on these deposits. He


thinks he will be able to explain loess and argillaceous deposits, the origin of which has hitherto been regarded as problematical, by this theory. Access through your institution Buy or


subscribe This is a preview of subscription content, access via your institution ACCESS OPTIONS Access through your institution Subscribe to this journal Receive 51 print issues and online


access $199.00 per year only $3.90 per issue Learn more Buy this article * Purchase on SpringerLink * Instant access to full article PDF Buy now Prices may be subject to local taxes which


are calculated during checkout ADDITIONAL ACCESS OPTIONS: * Log in * Learn about institutional subscriptions * Read our FAQs * Contact customer support RIGHTS AND PERMISSIONS Reprints and


permissions ABOUT THIS ARTICLE CITE THIS ARTICLE _Geographical Notes_ . _Nature_ 32, 376 (1885). https://doi.org/10.1038/032376a0 Download citation * Issue Date: 20 August 1885 * DOI:


https://doi.org/10.1038/032376a0 SHARE THIS ARTICLE Anyone you share the following link with will be able to read this content: Get shareable link Sorry, a shareable link is not currently


available for this article. Copy to clipboard Provided by the Springer Nature SharedIt content-sharing initiative