Abstract
THE appearance noted in NATURE this week (p. 268) by Prof. O'Reilly must surely have been a case of the rayons du crépuscule that are frequently visible near sundown in the eastern sky. East-south-east cannot at this season be very far from opposite the setting sun. Prof. O'Reilly does not mention, though probably it was the case, that the point of convergence of the “beams” which he saw was diametrically opposite the sun's position. That these beams appeared dark is probably merely caused by the real “rayons” being wide, with narrow, darker interspaces between. I have several times (see Phil. Mag., 1877) called attention to the existence of similar rays crossing the rainbow radially; indeed, it is seldom that a rainbow occurs when the sun is low in the sky, without one or more such rays being visible within the are. Two such rays, for example, were visible in a bow seen here at sunset two evenings ago. This bow was interesting in another way also; for, like the “pink” rainbows about which there was some correspondence in NATURE last year, the only colours visible (in the primary are) were red and yellow, the red being of a pinkish rather than a crimson hue.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to the full article PDF.
USD 39.95
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
THOMPSON, S. “Halo”: Pink Rainbow. Nature 26, 293 (1882). https://doi.org/10.1038/026293b0
Issue date:
DOI: https://doi.org/10.1038/026293b0


