I can report, yes, the guaifenesin makes a difference. I left it off yesterday in the theory it might be contributing to the sinus congestion: wrong. I coughed. A lot. And by evening I was coughing really badly every few minutes (postnasal drip was bad) —and finally took guaifenisin that evening. Stopped the drip, stopped the cough for the most part, so I actually got some sleep.

Discovery/Science/History2 has a couple of nice programs, btw. One is How the Earth Works: I could do without the cutesy athletics of the hosts, but any program that can tell me or show me things I didn’t know… is a delight. And the athletics may appeal to some who desperately need to understand this stuff. Program #2 is a one-shot called The First Apocalypse, which is a thorough go-over on all the reasons for the demise of the dinosaurs and going back to other events, such as new info on the Deccan Traps eruption, which has long been discounted, and is now being looked at far more seriously.

Which is how I spent the restive bits of last night.

Here’s the interesting bit: the Deccan Traps eruption is now understood to have been more intense and shorter than previously believed. And it coincides with the era of the Chicxulub impact. The measurement of the SIZE of the Chicxulub impactor is due to the thickness of the iridium deposits around the world…ergo, with that much iridium, plus Mexican rock frags in the iridium layer in Colorado, you’re dealing with a 6 mile asteroid impactor. BUT volcanoes also emit iridium from the Earth’s own core/mantle, and the massive Deccan eruption was around the time of the Chicxulub Event.

From Wikipedia: “The Cretaceous–Paleogene boundary of 65 million years ago, marking the temporal border between the Cretaceous and Paleogene periods of geological time, was identified by a thin stratum of iridium-rich clay.[41] A team led by Luis Alvarez proposed in 1980 an extraterrestrial origin for this iridium, attributing it to an asteroid or comet impact.[41] Their theory, known as the Alvarez hypothesis, is now widely accepted to explain the demise of the dinosaurs. A large buried impact crater structure with an estimated age of about 65 million years was later identified under what is now the Yucatán Peninsula (the Chicxulub crater).[42][43] Dewey M. McLean and others argue that the iridium may have been of volcanic origin instead, as the Earth’s core is rich in iridium, and active volcanoes such as Piton de la Fournaise, in the island of Réunion, are still releasing iridium.[44][45]”