Feb 23, 2007  The Hidden Forest: The Biography of an Ecosystem is a great read on the ecology of a Pacific Northwest old growth forest. How does nitrogen enter the system? One of the main contributors is Lobaria oregana, aka Oregon Lungwort, a lichen that hangs from the branches in the canopy.  Oh, the book is chock full of goodies like that, and I wish I'd taken some notes.  It also gives a rundown of the evolution of American forest science, and a peek at some of the obstacles faced, and methods used, by scientists who want to study and understand forest ecology.  And it goes down easy -- it was my bedtime reading, which generally has to be something that doesn't require undue concentration.  It inspired me to take a drive down the beautiful Columbia Gorge to visit an old growth forest.  I picked the most easily accessible one, according to A Walking Guide to Oregon's Ancient Forest , because my back has restricted my activities considerably in the past year. As an old growth forest, I found this Wauna Viewpoint Trail disappointing - Forest Park, just a few miles from my house, seems to look the part just as much as this did. But it was a lovely outing, anyway, with a view of the Gorge at the top.  Some other time, I must attempt the Herman Creek Ancient Cedar Grove, which involves twelve miles walking, but has a large stand of thousand-year-old western red-cedars.


Nov 26, 2006
  My friend Linnea, whose family we visited in Bellevue last month, mentioned to me that "geological forces" were causing Olympia, the capital of Washington, to sink.  I hunted around a bit to fill in just a little bit of detail on that.

Well, the basic global tectonics story is that the Juan de Fuca Plate, which is in the Pacific off the shore of Washington, is sliding under the North American Plate, and the friction of that movement is causing the North American plate to fold.  Try sliding a piece of cardboard under a flat beadsheet, and you'll see the general effect.  You have your upwardly moving ridges - the Cascade and Olympic mountain ranges - and your downwardly moving troughs - the Puget Sound, at the south end of which is Olympia, destined someday to become part of the Sound.



Nov 12, 2005  We came for the water.  Well, we came for a good public school for Arno, but we also came for the water.  Our skin feels it in the air, or rather, our skin felt its absence in the air in Milpitas.  We see it all year in the greenery.  We see it now in early morning fog, in clouds and rain.

We'd see a lot of it in the Columbia River if we went for a look.  How did the Columbia Gorge form, how did it cut through the Cascades?  I found the story that answers that question at the USGS/Cascades Volcano Observatory website's description of the Columbia River Basin.

"This vast river basin was formed near the end of the last Ice Age, 12,000 to 19,000 years ago, by the Bretz Floods. Immense ice dams half a mile high held back melting ice, creating a huge lake in northwest Montana, called Lake Missoula. Each time the ice gave way, massive walls of water as high as four hundred feet hurled boulders and icebergs seaward with a great destructive force. These floods generally followed the route of the present day Columbia River and came at least 40 times."

400-foot tall tsunamis, 40 of them.  I guess that would do it.