Creator

Joseph LeConte

Creator

Joseph Le Conte

Recipient

[John Muir]

Transcription

00611


I find evidences of this also in Lake Valley at the South end of the lake - in the form of sand hills apparently deposited in the lake. Let me hear from you as to the result of your further exami nation of Mt. Lyell Remember me very kindly to Mrs Hutchings. through you I wish to thank her again for her many kindnesses. Mr Clark I also remem- ber with much pleasure. Sincerely your friend, Joseph LeConte P.S. Prof Agassiz is here. I have seem him and will see him again many times. He is very anxious to visit the interior, par- ticularly since I have told him what a glor ious glacial field it is - but he is not strong enough. He will remain here 2 weeks or more. So if you wish to see him you must come soon.





















Oakland Cal. Sept. 7. /72

My Dear Sir

I reached Oakland on the 3rd since that time I have been so sluggish I could do little else than eat & sleep. I am much in the same condition still but I must redeem my promise to write you of my observations about L. Tahoe. We crossed the Sierras by passing westward through Carson Canon into Hope valley. thence over a low ridge which is little else than a pile of debris, into Lake valley (a valley continuation of Lake Tahoe South ward): thence over Johnson's pass into the canyon of the South fork of the American river This canyon carried us entirely out of the Sierras nearly to Placerville. About 15 miles South of L. Tahoe are a cluster of snowy sum- mits (dont know the name) from which issued a grt glacier which flowed northward filled Hope valley







and then turning westward flowed through Car- son Canyon into the great Carson Valley. The evidence is complete and of every kind. From the same snowy summits another grt glacier flowed northward into Lake Valley and onward into L. Tahoe. On both sides of the valley and of the Lake the mountains are high and still snowy. Innumerable tributaries flowed down these into the - main icy stream. These tributaries - continued after the main icy stream had dried up - they have therefore by their debris somewhat obscured the evidences of the main glacier in the lower part of the valley. One of these tributaries I ex amined closely. It came down from John- son's summit. the scoring & polishing is per- fect. From the same summit amother Gl passed westward down the canyon of the Am. River at least 25 miles. Below this for 25 miles more the canyon is equally deep & bold. but ap parently [underlined: water] worn - at lest I could find no evidence of glaciers. This change however is























nearly or quite coincident with the change of the rocks from Granite to Slate. In the glacial region the canyon is broader at bottom with succession of [underline meadows] and other evidences of [illegible] in the lower Gls region V shaped & not a single meadow. As to the question whether L Tahoe was - scooped out by Glaciers - Observe the main Gl did not run at steep incline into it, but through Lake Valley for 15 miles. That L. Tahoe was filled with ice - a true mer de glace, I have no doubt - but that it was scooped out by ice seems more doubtful I do not think it could have been scooped out by what I might call the Lake Glacier But I know not what an universal ice-sheet might have done at a still earlier period. I learn from my brother that the [underline: outlet gorge] is rocky and [underline: very narrow] in some places only 100 or more feet. Nevertheless there are abundant marks of [illegible] as I understand him about the upper margin of the gorge It has probably been deepened by water and the Lake partly drained off. I think



Oakland, Cal.,
Sept.7, '72.

My dear Sir:

I reached Oakland on the 3rd, Since that time I have been so sluggish I could do little else than eat and sleep. I am much in the same condition still, but I must redeem my promise to write you of my observations about L. Tahoe.
We crossed the Sierras by passing westward through Carson Canyon into Hope Valley, thence over a low ridge which is little else than a pile of debris, into Lake Valley (a valley continuation of Lake Tahoe southward); thence over Johnson's pass into the canyon of the South fork of the American river. This canyon carried us entirely out of the Sierras nearly to Placerville. About 15 miles south of L. Tahoe are a cluster of snowy summits (don't know the name) from which issued a great glacier which flowed northward, filled hope Valley, and then turning westward flowed through Carson Canyon into the great Carson Valley. The evidence is complete and of every kind. From the same snowy summits another great glacier flowed northward into Lake Valley and onward into L. Tahoe. On both sides of the valley and of the Lake the mountains are high and still snowy. Innumerable tributaries flowed down these into the main icy stream. These tributaries continued after the main icy stream had dried up - they have therefore by their debris somewhat obscured the evidences of the main glaciers in the lower part of the valley. One of these tributaries I examined closely. It came down from Johnson's summit. The scoring and polishing is perfect. From the same summit another gl[acier] passed westward down the canyon of the Am[erican] River at least 25 miles. Below this for 25 miles more the canyon is equally deep and bold, but apparently water worn. At least I could find no evidence of glaciers. This change, however, is nearly or quite coincident with the change of the rocks from granite to slate. In the glacial region the canyon is broader at bottom with succession of meadows and other evidences of gl[acier]s; in the lower region V shaped and not a single meadow.
As to the question whether L. Tahoe was scooped out by glaciers. Observe the main gl[acier] did not run at steep incline into it, but through Lake Valley for 15 miles. That L. Tahoe was filled with ice - a true mer de glace, I have no doubt -- but that it was scooped out by ice seems more doubtful. I do not think it could have been scooped out by what I might call the Lake Glaciers. But I know not what an universal ice-sheet might have done at a still earlier period. I learn from my brother that the outlet gorge is rocky and very narrow, in some places only 100 or more feet. Nevertheless there are abundant marks of gl[acier]s, as I understand him, about the upper margin of the gorge. It has probably been deepened by water and the Lake partly drained off. I think I find evidences of this also in Lake Valley at the south end of the Lake - in the form of sand hills apparently deposited in the Lake.
Let me hear from you as to the result of your further examination of Mt. Lyell.
Remember me very kindly to Mrs. Hutchings. Through you I wish to thank her again for her many kindnesses. Mr. Clark I also remember with much pleasure.

Sincerely your friend,

Joseph LeConte.

Prof. Agassiz is here. I have seen him and will see him again many times. He is very anxious to visit the interior, particularly since I have told him what a glorious glacial field it is, but he is not strong enough. He will remain here 2 weeks or more, so if you wish to see him you must come down.

[Folder marked by Muir, "Prof. Joseph LeConte on gls., etc., and mention of Agassiz 1872 after 1st visit to Yo. and Sierra."]

Location

Oakland, Cal

Date Original

1872 Sep 7

Source

Original letter dimensions: 20.5 x 25.5 cm.

Resource Identifier

muir02_0887-let.tif

File Identifier

Reel 02, Image 0887

Copyright Statement

Some letters written to John Muir may be protected by the U.S. Copyright Law (Title 17, U.S.C.). Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Responsibility for any use rests exclusively with the user.

Owning Institution

University of the Pacific Library Holt-Atherton Special Collections. Please contact this institution directly to obtain copies of the images or permission to publish or use them beyond educational purposes.

Pages

3 pages

Share

COinS
 
 
 

To view the content in your browser, please download Adobe Reader or, alternately,
you may Download the file to your hard drive.

NOTE: The latest versions of Adobe Reader do not support viewing PDF files within Firefox on Mac OS and if you are using a modern (Intel) Mac, there is no official plugin for viewing PDF files within the browser window.