Tuesday, December 23, 2014

Barriere BC hasn't changed its name, but Where is Stout's Gulch?

In searching old records we often come across names that we don't recognize, like Eburne aka Marpole.   BC Geo is the site that decipher's old names longitude latitude, like Barriere, BC, which had a gold strike in 1861 on the banks of the North Thompson River.

Once upon a time Deer were more prevalent in British Columbia....... so for today's hunters, here are some old time longitude latitudes.

This document has more to do with Stout's Gulch aka Barkerville...... than Barriere, but the 'theory' of W. H. Mathews is the same for both gold sitings just waiting to be rediscovered.

W. H. Mathews

Lode Gold Deposits sometimes has a file name spelled Load Gold Deposits: eg. South Eastern BC, South Western BC, and Vancouver Island BC.  'Load' will generate three more documents than a search for 'Lode'.

"Drain Lake for Gold" label??? it was!!!
Page 4 of 17 listing of gold camps   1948  Load Gold Deposits South Eastern British Columbia

....... Course of veins Compared with Placer Diggings.

Page 24 of 60: In my topographical examination of the country, I could not help observing that, without exception, your extremely rich placers lay immediately below the quartz veins; as, for instance, if we start at the Lord Dufferin claim and follow the croppings passing the old Prospine, now called the California, and continuing along the vein in a north-west course, you will find, immediately below, or at the base of the mountain to our left, runs Williams Creek, which has yielded many million of gold, much of it extremely coarse, intermingled with quartz; while to our right, at the base of the same mountain, runs the Conklin Gulch, which also yielded large quantities of gold, as, indeed, both places are yet doing.

Continuing along the course of the vein and crossing Williams Creek at the canon until the summit going towards Lowhee is reached, we find Stout's Gulch lying to the left and below the vein.  All know how extremely rich that gulch has been, while it is, even now, being hydrauliced far up the mountain side towards the vein.   Following the vein over the summit dividing Stout's Gulch from Lowhee Creek, we find the latter has been rich; and within a very few days samples of heavy gold have been pounded out of quartz found while sluicing.

In the vicinity of the Pinkerton claim the vein crosses Lowhee Creek and pierces the mountain, continuing towards the Jack of Clubs Lake, taking in the Enterprise, now called the "Senator Jones", and extension, "Governor Perkins".

The vein, extending up and through the mountain, no doubt supplied Lowhee Creek with the coarse gold mentioned above; and as the vein crosses through the mountain, the gold found on teh banks of the lake perhaps came from the same source.

I think I shall warn venturesome spirits from attempting to pump the lake out in their anxiety to find gold.

In continuing my survey, I find no source from which the rich diggings of Mosquito Creek derived their gold except from the large, well -defined, and continuous vein and cross veins passing through Island Mountain.  Returning to Lord Dufferin, I was not surprised to find that Grouse Creek could not possibly have received its bounteous supply of gold fro any other source than from the Bonanza vein, where it crosses Grouse Creek as it passes from the California claim and continues through to Lord Dufferin ground towards Antler Creek; and surely no one will question the source whence that creek derived its gold, when not a dollar is being mined above where the vein crosses either the Grouse or Antler Creeks.

I find it impossible to embrace the Burns Mountain in this report; but from observation and information obtained from P. C. Dunlevy, of Soda Creek --- a disinterested person, I think --- I am led to think that the Burns Mountain veins supplied millions mined from Lightning Creek, no gold being found above a point where Mr. Dunlevy supposed the veins crossed the creek.

While I may seem to have been somewhat exhaustive in my report of the above veins, I will say I have been shown samples of ore from what, at present, may be termed outside veins -- notably the Steadman, Sergeant Lindsay, and other veins reaching so far away as Sugar Creek -- and they, without exception, show well-defined walls, and invariably prospect well in gold.  Those on Sugar Creek, however, carry a higher percentage of silver than gold; and beyond doubt, many veins exist not yet discovered.  The country is thickly covered with wees and moss, which makes prospect in or following veins somewhat difficult; but the day is not far distant, in my judgement, when many prospectors will be found busily engaged in uncovering good paying veins.  Some will meet with success, while the dreams of wealth of others will, unhappily, never be realized.  Such is too often the fate of the prospector, which can, in a measure, be palliated by the Government, as I will explain further on.  (See Mineral Survey.)

I must not neglect to account for supposed veins carrying free gold, in some cases lying higher up the mountains than the true veins, which have but little free gold; notably one which was discovered high up -- in fact, on the summit of the mountain above the B. C. mines.

During the glacial period all was chaos.  The irresistible force did not always choose its course and destroy the tops of veins and carry them down to creeks below.  On the contrary, portions of a vein were in some cases detached and carried many miles and landed on some mountain top hundreds of feet height than its original bed, as in the case mentioned.   Instead of being ground and crumbled sufficiently fine to admit of being gradually washed to the creeks below, it was carried in the case of a jam or drift of timber in a swollen stream, where trees may be seen piled up many feet, and beyond the line of the jam.  In such cases the elements have but little effect on the supposed vein, and it lies there undisturbed, while thousands of tons broken ground fine have at the same time been washed to the creeks below. ...................

Mining operation for Gold, Coal, Company

Google Search Criteria for around Barriere
'Open pit, on the northern slopes of Samatosum Mountain, 25 kilometres east of Barriere and 60 kilometres north of Kamloops (Friesen, 1990).


And, if you're the least bit curious about that there deserted road bed which appears to be a dead end, whether you're there in person, or looking on a map, or in Google Earth, or BC Geo, just pop the longitude latitude coordinates into the programs to find what's nearby, 5, 10, 15 kilometer radius,
from this here novice starter spreadsheet:

Excel Table of Historic Mines

eg.  Drilling Resumes on the Mucho Oro Zone - Barkerville Gold ... Stouts Gulch


This document shows Iceflow routes throughout BC.... which if it's true that GOLD deposits have been hopping from a low hill to the top an adjacent mountain then why not build a database on where that's happened eh.... to find another Barkerville 

Soil Landscapes of British Columbia Page 49 of 196

Kootenay Lake is REALLY deep which means the Mount Polley dam busters deposits will go DEEP too.

No comments: