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Revision as of 14:45, 8 July 2003

Some doubts about recent changes:

• I thought Yellowstone is the first National Park, not Yosemite
• Sequoia and Kings Canyon are two separated national parks though they are neighbors joined by their border. The original text had them separted as two links, the recent change merged the two together into one.

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Yellowstone was the first national park created by that name in roughtly its current form, and the Act of Congress that establishing it set the pattern for the national park system. But the first effort by a modern state to set aside such an natural area was the ceding of Yosemite Valley (a small part of today's park) to the control of the State of California during the Civil War, some years before Yellowstone. Some historical materials seem to indicate that the more sweeping Yellowstone legislation was prompted by the mixed (at best) results of the Yosemite experiment. The Park Service, Smokey Bear hats and all, didn't come into existence until 1916, when there were 14 parks and 21 national monuments. (see http://www.cr.nps.gov/history/hisnps/NPSHistory/npshisto.htm) Some countries have never set up a unform system of parks, even though they do set areas aside.

The relationship between Yellowstone and Yosemite does make for some minor rivalry and a great trivia question or two.

As for Sequoia - Kings Canyon, they were established separately (Sequoia first) but are contiguous and are managed as a single unit. (see http://www.nps.gov/seki/index.htm) ClaudeMuncey, Thursday, April 18, 2002

Mav: interesting stuff about geology of Yosemite. I haven't heard anything at all about the school of geologists who don't think that glaciation and uplift had a major effect. I went to a Open House at the Menlo Park USGS back in 1995 or so and didn't see anything about that. And there is lots of glacial polish well above 5600'... Well, you properly NPOV-ed it.. Is it possible to give sources on it? I'd like to poke around some more...

I think the large amount of uplift of the Sierra is pretty well established --- the faults along the eastern Sierra have undergone a large amount of vertical displacement (the westernmost Basin and Range fault) .. For example, the Alabama hills in the Owens Valley have the same granite as near Mt. Whitney, but are much lower. Anyway, it seems difficult to reconcile with the "glaciation and uplift are unimportant" theory. Say more? -- hike395 00:19 8 Jul 2003 (UTC)

I didn't say that the newer school thought that uplift did not have a major effect. I did say that this newer school has attacked the longstanding idea that rapid uplift over the past 2 million years combined with highly abrasive glaciations has been the major shaping force of the parks topography. They state that the uplift happened much more slowly and much further in the past and that jointing was the major dictator of events (of course all types of erosion will take advantage of weaknesses and joints provide those weaknesses). This new line of thought has been led by Jeffrey P. Schaffer (see cite below). Much of what I read in the cite was statements of fact with little supporting evidence (which in understandable considering the book I read was a natural history guide). But I'm sure his earlier work The Geomorphic Evolution of the Yosemite Valley and the Sierra Nevada Landscapes will have all his evidence. I just report what I read and try to NPOV it - thus the last paragraph was a compromise between Geology of the National Parks and Schaffer's natural history guide.

Yosemite National Park: A Natural History Guide to Yosemite and Its Trails, Jeffrey P. Schaffer, (Wilderness Press, Berkeley; 1999) ISBN 0-89997-244-6

Oh and Schaffer is not arguing that that glaciers did not effect anything above 5600 feet. I know for a fact that glaciers did cover areas well above 9,000 feet in at least the high country since I saw (and photographed) a several ton glacial erratic on top of Lambert Dome. The erratic was unmistakable since the rock type of the boulder was markably different and it still had glacial polish and striations below its base (meaning that it was transported and did not erode in place). Schaffer does disagree with the prevailing view that Lambert Dome is the shape it is because it is a huge roche mountonnee, however. He points out, and I have to somewhat agree, that the cliff face of Lambert (and Liberty Cap for that matter) does not look at all like it was formed by glacial plucking (which would result in a great many concave depressions in the rock face). It looks to me more like a joint plane (very similar to Half Dome's steep face). Of course glaciers would have taken advantage of the joint plane and helped to sheer off large slabs of the face but Shaffer states that without the joint plane there would not have been a vertical cliff (thus Lambert and Liberty Cap are not roche mountonees). His overall theme, I gather, is that the granitic rock of the Yosemite area is very resistant to erosion and when it does erode it almost allways follows major joint planes.

I may have given Schaffer's views more credit than warrented (since I'm not a professional geologist and do not really know what the consensus view on this is) so if that is the case then please attribute those views to just Schaffer. Also, IIRC, Muir and a prominent contemporary geologist (whose name escapes me for the moment) also differed on this exact point; Muir thought that glaciers were the primary shaping force of the valley but this geologist (who was apparently highly respected in his time) thought that major joints where the primary shaping force of the valley. It would be great if we put this argument into its historical context. --mav 02:45 8 Jul 2003 (UTC)

OK.. I'll try and investigate and see if more people than Schaffer believe it. I've found that we have to be careful about those guides, sometimes: the Roadside Geology of Washington had the "asteroid hitting the hot spot causing the Basin and Range" hypothesis that I mentioned in Talk:Basin and Range Province.. I suspect that people use guides as a bully pulpit for their favorite hypothesis. But, you did NPOV it well.

Oh, btw --- The contemporary geologist you are thinking of is Josiah Whitney, the chief geologist of California at the time. Mount Whitney is named after him. -- hike395 14:40 8 Jul 2003 (UTC)