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mouse from merced

Trad climber
The finger of fate, my friends, is fickle.
May 18, 2016 - 06:21pm PT

White rocks like this abound on the western slope below the Mother Lode.

This is near Catheys Valley on Hwy 140.




wilbeer

Mountain climber
Terence Wilson greeneck alleghenys,ny,
Jun 21, 2016 - 06:30am PT
Sierra Ledge Rat

Mountain climber
Old and Broken Down in Appalachia
Jul 12, 2016 - 07:27pm PT
This rock is nice

mouse from merced

Trad climber
The finger of fate, my friends, is fickle.
Aug 2, 2016 - 04:46pm PT
Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Sep 27, 2016 - 08:30pm PT
Summer is over, & it's time for a few rock posts from this summer.

Back in early June, I had a great time finding garnets & unlisted Vesuvianite. (I think) It's a somewhat rare silicate mineral in Idaho.

I returned back to "the ranchette" after a quick visit to an obscure mine not too far from the Snake River plain, but on top of the high point below.

It was great for me, after our wet April & May. I found "good rocks", took major risks without injury, and got lots of exercise for most of two days. My high point was balancing on a 60 degree dirt slope, while extracting chunks of rock with great garnets.

After climbing up to slightly steeper terrain, and ignoring what might happen to me if I fell, I happened to look down at my right foot, which was covered with Pogos. (large red ants, which bite). I levitated up the remaining 5 feet to flat terrain while shaking my right foot all the way. No bites!

Although my collecting site was about a mile in from the end of a driveable road, I had brought a 9mm rope, jumars, harness, & even a helmet, to help me search for minerals on the steep slopes of an old open-pit mine.


I hauled all the gear up through steep slopes, tightly grown with small pines & brush to the lip of the mine, selected a likly area, tied the rope to a stout tree, tossed it down and descended the 70 to 80 degree slope with the help of the jumars, my feet, & gravity.

I had correctly worried that moving sideways would bring down rockfall, but with the help of a high tie point on my anchor tree and a near verical slope up high, I didn't induce "killer" rockfall.

However, the 60 degree Pogo ant slope had many more garnets than the one I worked with a rope.

Still a good day, and I found one Vesuvianite specimen. (I think). A somewhat rare silicate mineral.


The big garnet of the day is opaque & not very shinny.

I found some other interesting specimens, like this piece with Calcite & garnets.


And another piece with Biotite Mica.


However, unlike last year, I didn't get to share time with cowgirls on the way out.



tuolumne_tradster

Trad climber
Leading Edge of North American Plate
Sep 27, 2016 - 09:52pm PT
Serpentine, Mt Tamalpais...hydrated peridotite from the upper mantle

Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 4, 2016 - 09:16am PT
Nice Rock TT. That stuff is beautiful!


From Wikipedia:

Fulgurites are formed when lightning with a temperature of at least 1,800 °C (3,270 °F) melts silica or other common conductive and semiconductive minerals and substrates, fusing, vitrifying, oxidizing and reducing mineral grains and organic compounds;[6] the fulgurite mass is the rapidly quenched end-product.

The temperature peak within a lightning channel, however, is known to exceed 30,000 K, with sufficient pressure to produce planar deformation features, or "shock lamellae" in SiO2 polymorphs. It is assumed that the process of forming a fulgurite occurs over a timespan of the order of a single second, following the termination of the return stroke.

Fugerites are commonly hollow and/or branching assemblages of glassy, protocrystalline, and heterogeneously microcrystalline tubes, crusts, slags, vesicular masses, and clusters of refractory materials that often form during the discharge phase of lightning strikes propagating into silica-rich quartzose sand, mixed soil, clay, caliche and other carbonate-rich sediments.
Colloquially, they have been referred to as petrified lightning.
https://en.wikipedia.org/wiki/Fulgurite

It also is possible to make “artificial” Fulgurites by discharging electricity into sand, although it is somewhat more complicated than that.

I learned from a mineralogist last week that this curious rock I had found at 10,400’ is a Fulgurite. I found it in a “contact-zone” where hot granite had intruded into limestone, and I had thought it was just some strangely altered rock from that contact.

Nope the mineralogist said, it’s a Fulgurite. From Wikipedia I discover it is a:
“ Type IV - rock fulgurites, which are either crusts on minimally altered rocks, networks of tunneling within rocks, vesicular outgassed rocks (often glazed by a silicide-rich and/or metal oxide crust), or completely vitrified and dense rock material and masses of these forms with little sedimentary groundmass.”
Upon examination of my 2 1/2" X 2" Fulgurite, with a 7-X magnifier, it appears that the host rock is limestone.

Here's some other views of it. The black surface is slick & shiny, with some greenish spots too.


Anyone else have a fulgurite to share?
Jaybro

Social climber
Wolf City, Wyoming
Oct 4, 2016 - 05:25pm PT
Water saturated sandstone. Let the rock dry at least 24 hrs after storms!!

"It'll take your f*#knghead off!" - Bill Murray Ghostbusters(?)
i-b-goB

Social climber
Wise Acres
Oct 4, 2016 - 05:51pm PT
Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 4, 2016 - 07:34pm PT
Jaybro & i-b-Gob! Thanks for posting up your rocks & petroglyphs.

I've never noticed a sheep-schisting petroglyph before, after viewing many a stone sheep. Is that original to the art, or an add-on?
Spider Savage

Mountain climber
The shaggy fringe of Los Angeles
Oct 4, 2016 - 09:43pm PT
Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 4, 2016 - 09:53pm PT
Nice Petroglyhs Spider!

One of these daze, we need to sample more of those Snake River Glyphs.

I've got the insider scoop on them.



WyoRockMan

climber
Grizzlyville, WY
Oct 4, 2016 - 10:51pm PT
Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 5, 2016 - 07:23am PT
WyoRockMan! Nice glyphs. In the long-ago I remember looking at some SE of Dubois, but otherwise, I am clueless on Wyoming Indian rock-art.

Idaho is another matter.





mouse from merced

Trad climber
The finger of fate, my friends, is fickle.
Oct 7, 2016 - 06:30pm PT
Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 7, 2016 - 08:05pm PT
MFM!


LIKE!
Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 11, 2016 - 09:05pm PT
The Euro’s changed it’s name to Baryte in 1978, but in America, we know it as Barite. (BaSO4)

Barite is a “soft-rock” with a hardness of 3 - 3.5. and it is common worldwide.

Per Wikipedia: It commonly occurs in a large number of depositional environments, and is deposited through a large number of processes including biogenic, hydrothermal, and evaporation, among others.[1] Baryte commonly occurs in lead-zinc veins in limestones, in hot spring deposits, and with hematite ore. It is often associated with the minerals anglesite and celestine. It has also been identified in meteorites.


But I’m talking about Barite crystals, which can be beautiful, per these specimens from Nevada’s Elko County Meinke Mine.





Idaho has one location where colorful Barite crystals have been found, near our highest peak, Mt. Borah.





After fruitless searches in that area, I finally broke down and bought some of the above classic specimens, that were found in the 1950’s.


However, in 2015, I found some clear Barite crystals at the edge of the Frank Church/River of No Return Wilderness Area.


This summer I found lots of clear, white & a blend of both color crystals in Spar Canyon, near the East Fork Salmon River.



Sigh. I’m still looking for Barite crystals like those from Nevada.

Mungeclimber

Trad climber
Nothing creative to say
Oct 11, 2016 - 11:00pm PT
nice rocks and glyphs!

greenery...

Fritz

Social climber
Choss Creek, ID
Topic Author's Reply - Oct 18, 2016 - 07:45am PT
Nice rocks folks!


Out in the wilds of SE Oregon, drivers on Hwy 95 whiz by two road signs of interest.

One is a marker for the Grave site of Sacagawea's son, Jean Baptiste Charbonneau. He had quite a life before falling ill on a trip from California to Silver City, Idaho.


The rather weathered sign reads:
Jean Baptiste Charbonneau
1805–1866
This site marks the final resting place of the youngest member of the Lewis and Clark Expedition. Born to Sacagawea and Toussaint Charbonneau at Fort Mandan (North Dakota), on February 11, 1805, Baptiste and his mother symbolized the peaceful nature of the "Corps of Discovery." Educated by Captain William Clark at St. Louis, Baptiste at 18 traveled to Europe where he spent six years becoming fluent in English, German, French and Spanish. Returning to American in 1829, he ranged the far west for nearly four decades as mountain man, guide, interpreter, magistrate, and forty-niner. In 1866, he left the California gold fields for a new strike in Montana, contracted pneumonia en route, reached "Inskips Ranche" here, and died on May 16, 1866.

More details of his life are on Wikipedia https://en.wikipedia.org/wiki/Jean_Baptiste_Charbonneau

However, the chief reason for this posting, is of course Arock.


Arock is three miles (5 km) north of U.S. Route 95 between Jordan Valley and Rome. Arock was supposedly named in 1922 for a large rock bearing Native American petroglyphs in the vicinity. Arock post office was established in 1926.

The oldest building in Malheur County, Sheep Ranch Fort, is near Arock. It was added to the National Register of Historic Places in 1974. Arock is one of several places in southeast Oregon that were settled by Basque herders.

Apparently, not everyone loves Arock, but it seems important to post it up on Tuesday.
mouse from merced

Trad climber
The finger of fate, my friends, is fickle.
Nov 4, 2016 - 07:05pm PT
[Click to View YouTube Video]
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