Bob:

I think plains have to be evaluated separately from mountains--at least 
until they erode like the Catskills and turn back into mountains.

Lee

[email protected] wrote:
>
> Lee,
>
>  
>
>      You have presented me with a way to think about mountains, young 
> and old, andtheir climates that I could have never achieved on my own. 
> Should I conclude that the most pleasing mountains of all are those 
> that have eroded to flat plains - the ultimate old growth mountain 
> state? Just wondering.
>
>  
>
> Bob
>
>  
>
>
> ----- Original Message -----
> From: "Lee Frelich" <[email protected]>
> To: [email protected]
> Sent: Thursday, July 16, 2009 9:32:18 AM GMT -05:00 US/Canada Eastern
> Subject: [ENTS] Re: Catskills
>
>
> Bob:
>
> When I saw your pictures of the Catskills, I thought, there are
> mountains with real character and elegant rounded shapes resulting from
> a few hundred million years of graceful aging. They have not quite
> reached the dignified state of the Porcupine Mountains in Michigan and
> Sawtooth Mountains in Minnesota, that used to rival the Himalayas, but
> have undergone a billion years of erosion to end up being about 1500
> feet higher than their base, but the Catskills are almost there.
> Old-growth mountains such as the Porkies have a lot of character, and
> they don't block the view of the sky (and approaching tornadoes) like
> juvenile mountains such as the Rockies. Besides that, in the northern
> Midwest we can get 20 feet of snow in the winter and Siberian
> temperatures without resorting to excessive elevation.
>
> Lee
>
> PS--speaking of approaching tornadoes, the Kandiyohi Elm forest in
> Minnesota narrowly escaped being leveled by a tornado AGAIN on Tuesday.  
> They sure get a lot of tornadoes west of Minneapolis. No wonder the
> first settlers out there lived in dugout houses with sod roofs.
>
>
> [email protected] wrote:
> >
> > Robert,
> >
> >  
> >
> >       Glad you enjoyed the photos. There will be more as I discipline
> > myself to take my camera on tree and mountain ventures. In the past I
> > relied on friends to do what I should have also been doing. I'm
> > finally getting my act together. I have a lot of photographic
> > documentation to catch up on.
> >
> >       With respect to vertical relief of mountains, over the years
> > I've done dozens of analyses on East versus West, mountain range
> > versus mountain range, and peak versus peak. I am as big of a nut on
> > mountains as trees. I would agree that the East does has some big
> > climbs that can go unappreciated by westerners. The west side of the
> > Great Smokies in eastern Tennesse and the White Mountains in New
> > Hampshire have the biggest climbs in terms of vertical relief.
> > They are followed by the isolated summit points of Mount Kathadin in
> > Maine and Giant Mountain in the Adirondacks. The Blacks and Balsams of
> > North Carolina and Adiriondack High Peaks come next. There are a few
> > large elevation gains (3,000 feet) in the Green Mountains and Taconics
> > of Vermont. The Blue Ridge of North Carolina, Virgina, and Georgia,
> > the Greens and Taconics in Vermont, the Catskills of New York, and
> > some of the other Maine Appalachians form a large area of mountains
> > where vertical relief can reach 3,000 feet and slightly more in the
> > case of the highest peaks. The Burroughs range in the Catskills comes
> > to mind. But these latter mountain regions are roughly comparable. To
> > be fair, we'd also need to include some areas in West Virginia, but
> > I'm less familiar with West Virginia's 'tall' peaks.
> >
> >      The lack of understanding and appreciation for eastern summits
> > often stems from invalid comparisons. But, this occurs for western
> > summits as well. Trails to the tops of well known summits can begin
> > half way up the mountain, allowing a hiker or climber to claim that
> > he/she climbed the mountain when he/she climbed half the mountain - or
> > less. Establishing the base of a mountain at the bottom of the final
> > rise is a ridiculous practice of some hikers and writers - very, very
> > misleading. The Peak Baggers have devised a system of peak by peak
> > comparison for vertical relief. They are the reaal experts.
> >
> >       Different methods of comparison can be applied to judge the
> > vertical relief of mountains. For me, I like to use the visual
> > impressiveness of a mountain or mountain range as seen from different
> > distances. I especially enjoy viewing the vertical relief that a
> > mountain or range attains from the surrounding lowlands so that I see
> > the full vertical sweep of the peaks.  However, lots of foot hills
> > stretched over a long horizontal distance can reduce the visual
> > impressiveness of a range. Conversely, some foothills can set the
> > stage, so to speak, for the bigger peaks beyond.
> >
> >       The western side of the Great Smokies rise from foothills that
> > are between 1,500 and 2,000 feet above sea level. Spots along the
> > water courses are even lower.  The tops of the Smokies reach to a
> > maximum height of 6,643 feet at Clingman's Dome. Mt. Guyot is second
> > at 6,621 feet. Mt Leconte is third at 6,593 feet. These peaks and
> > other 6,000-footers along the crest of the Smokies rise between 4,500
> > and 5,000 feet above the basal foothills. They are western-sized
> > mountains. The highest peaks of the Whites in New Hampshire provide
> > almost as much relief and are generally steeper sided, giving the
> > appearance of being higher.
> >
> >      The high peaks of the Rockies generally rise from 4,000 to 7,000
> > feet above their basal lowlands. In terms of vertical relief as seen
> > at a distance, the Front Range in Colorado, the Bighorns in Wyoming,
> > and the Wasatch in Utah have impressive base to summit rises, with
> > about a thousand foot difference between each, i.e. 9,000 feet for the
> > Front Range's highest summits, 8,000 feet for the Bighorn high
> > summits, and 7,000 for the Wasatch. The Tetons in Wyoming and the
> > Sangre de Cristo,  La Platas, San Juans, and Sawatch in Colorado are
> > more more on the order of 6,000 to 6,500 feet.
> >
> >        In judging impressiveness, the Tetons and Sangres haved no
> > foothills. They are really 'in your face' mountains and can through
> > you off in judging what you have to climb. The eye and brain do a lot
> > of work to bring the proportions together and make them understandable.
> >
> >       As Don Bertolette has pointed out in his examples, the peaks of
> > California and the volcanoes of the Pacific NW go off the charts in
> > terms of vertical relief. San Jacinto in southern California rises
> > very abruptly 10,800 feet above the desert floor. When I spent several
> > months at March AFB in 1966, I viisted those huge mountains. The
> > enormous vertical relief initially confused me until I realized how
> > much mountain I was looking at and got my brain to assess the
> > proportions better.
> >
> >       Of course, visual appeal of mountains is in the eyes of the
> > beholder. A beautifully contoured mountain rising abruptly 2,000 feet
> > above its base can be as attractive as much larger mountains. I like
> > them all.
> >
> >     BTW, congrats on the movie deal.
> >
> >  
> >
> > Bob
> >
> >
> > ----- Original Message -----
> > From: "JamesRobertSmith" <[email protected]>
> > To: "ENTSTrees" <[email protected]>
> > Sent: Wednesday, July 15, 2009 4:22:18 PM GMT -05:00 US/Canada Eastern
> > Subject: [ENTS] Re: Catskills
> >
> >
> > Absolutely gorgeous photos!
> >
> > I love our eastern peaks. I meet up with a lot of hikers from out west
> > that I call "mountain snobs". They don't consider our mountains to be
> > anything other than hills. I point out to them that the 13K-foot peak
> > they climbed only has 2500 feet of relief, but this matters not at all
> > to them. I've stood on many mountains in Virginia that have as much
> > vertical relief as Half Dome in Yosemite. But they wouldn't admit that
> > those Virgina summits are mountains.
> >
> > Alas.
> >
> > At any rate, those are great photos. One of these days I hope to hike
> > in the Catskills, too.
> >
> >
> >
> >
> > >
>
>
>
>
> >

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