Oregon Gold

Finding Gold in Oregon

Humbug Creek, Jackson County

Humbug Creek

Humbug Creek

 

Humbug Creek is a little known area to gold prospectors in Oregon, but in its day, it was the center of a major gold rush in Jackson County.

Today, one can access this great old gold creek by following Oregon State Highway 238 (The Williams Highway) and following Humbug Creek Road which is located just due east of the community of Applegate, Oregon. (Take note that much of this area is now private property and care should be taken to respect the rights of the property owners along the creek).

Like most creeks in Jackson County, gold was discovered relatively early on in and around Humbug Creek. In fact, enough gold was found by early miners that during the late 1850’s, a small mining camp sprung up along its banks and by March of 1860, the Humbug Mining District was established, using the following camp laws (mostly adopted from those used over the state border in Yreka, California): 

The Mining Laws Of Humbug Creek

Article 1st
Size of Claims

Each man shall hold a claim 100 yards square by preemption and as much by purchase as he represents.

Article 2nd
Priority of Water Rights

The oldest claim shall have the first right to the water but shall run no water by unnecessarily to keep others from using it.

Article 3rd
Necessary Work to Hold Claim

No claim shall be considered forfeited if worked one day in every five during the time there is a good ground sluice head in the creek.

Article 4th
Restriction on Dams, Etc.

No person or company shall put a dam, reservoir or any obstruction in the creek, provided it is a damage to those above said obstruction.

Article 5th
Flood-gate for Dams to Be Kept Open

Any person or company putting in a reservoir shall have a flood gate five feet in breadth and three feet hight [sic] which shall be kept open as long as there is a good sluice head in the creek for washing up.

Article 6th
Recorder; Fee; When Claim Must Be Recorded

There shall be a recorder elected and he shall be allowed One dollar per claim for recording. Any person leaving the Creek to be gone two months shall have their claims recorded.

Article 7th
Judicial Power

Any person or persons violating any of these resolutions or by-laws shall abide the decision of a miners’ meeting.

Article 8th
Chinese Excluded

No Chinaman shall be allowed to purchase or hold any claim on this Creek.

Article 9th
Adoption of Resolutions

Resolved, the foregoing articles shall come into effect as Laws of this Creek on or after and from the twentieth day of March A. D. 1860.

J. F. Headrick, Chairman,
V. P. Comstock,
Jas. W. Mee,
E. Thompson,

Committee on Resolutions
Francis Sackett, Secretary
John Goff, Recorder.

This document was filed and recorded with the Jackson County Clerk in Jacksonville on March 24th, 1860.

 

Several notable mines were located in this district, including:

 

The Wright Mine (Lat. 42.25537, Long. -123.1442) which was a medium sized underground prospect that was active until it was shut down in 1942 by Government Limitation Order 208. In addition to gold, the Wright also yielded silver, zinc and lead.

The Nonesuch (Lat. 42.25037, Long. -123.1394) , which was also a medium sized underground mine. In addition to gold, silver was also mined in the Nonesuch. Like the Wright, it was shut down in 1942.

The Scott (Lat. 42.26117, -123.13), also a prospect of medium size, but unlike the above two, the Scott was a surface mine. Most of its activity was in the 1930’s.

The Victor (Lat. 42.27097, -123.1517), which was a well known and very profitable operation dating from before 1940. Like the Scott, the Victor was a surface mine.

The Broken Heart (Lat. 42.27007, Long. -123.1283), another medium sized underground producer.

The Ace of Hearts (Lat. 42.27757,  Long. -123.1203), which was a medium sized underground operation yielding gold and silver.

The Oregon Belle (Lat. 42.28817, Long. -123.1006), which is a rather famous mine and a fine producer of lode gold. Located due east of Humbug Creek.

The Sundown (Lat. 42.28317, Long. -123.1047),  yet another surface mine, located due south of the Oregon Belle. Also east of Humbug Creek.

The Grange Gulch (Lat. 42.25227, Long. -123.1208), which yielded gold and silver until 1942.

Finally are the Humbug Creek Placers (Lat. 42.26707, Long. -123.1389) which between the 1860’s and the 1940’s had many names, including the Benson Placer, the Johnston Placer, Exter, Pittock and the Kubli Ranch. This last name is attributed to Kaspar Kubli, a very early pioneer in the Applegate Valley. This last operation ran a drag line dredge up Humbug Creek.

Kerby Jackson, Josephine County, Oregon

Galice Creek - Oregon Gold Locations

Galice Creek (located in Josephine County) and its tributaries were important placer gold producers, especially in regard to the “Old Channel” gravels which form a terrace to the west of the creek and 600 feet above it. Placer gold was discovered on Galice Creek in 1854, and significant amounts of gold were produced. The Old Channel hydraulic pit on the high terrace was started in 1860 and ultimately became almost 2,000 feet wide and 100 feet deep, the largest such pit in the State of Oregon. It is reported that over 50,000 ounces of gold were produced from the pit. The gravels averaged about .007 ounce of gold per cubic yard and a lot of good ground remains to be mined.

If you see this sign you will know your in the right place.

If you see this sign you will know your in the right place.

There are a number of old lode gold mines in the Galice district, and those mineralized zones supplied most of the placer gold deposits found in the area. The Galice district, including Mount Reuben, had a total production of around 268,000 gold ounces. The local placer operations include the Ankeny Mine, Courtney Mine, Carnegie Mine, California-Oregon Mine, and Last Chance Mines.

galice-creek-map

The hillside just West of the Galice Range (approximately 1/4 to 1/2 miles wide, extending 4 miles to the Southwest), patches of gravel benches about 500 feet above present day streams as dissected by tributaries of Galice Creek there is placer gold. The “High Bench Gravels” along both sides of the Rogue River are gold bearing, but not much worked at this time. Downstream you will find the Dean and Dean placer Mine, and the Rocky Gulch placer Mine. In Hellgate Canyon, the Hellgate placers, were very productive. Along Galice Creek there are many rich placers. The Chinese also worked in the area.

Near these sites: If you go 21 miles Southwest of Glendale in Douglas County, in section 22, 23, and 27 of Township 33S and Range 8W, you will find the Benton Mine, near Mount Reuben. It was found in 1893 and is the largest underground mine in Oregon. It was closed in 1942. The Almeda Mine, Gold Bug Mine, Oriole Mine, Black Bear Mine, and Robertson (Bunker Hill) Mines, were important producers of lode gold in the area.

The Geology of Gold

by Harold Kirkemo, William L. Newman, and Roger P. Ashley  (Repost from Free Public Information)

Gold is relatively scarce in the earth, but it occurs in many different kinds of rocks and in many different geological environments. Though scarce, gold is concentrated by geologic processes to form commercial deposits of two principal types: lode (primary) deposits and placer (secondary) deposits.

Lode deposits are the targets for the “hardrock” prospector seeking gold at the site of its deposition from mineralizing solutions. Geologists have proposed various hypotheses to explain the source of solutions from which mineral constituents are precipitated in lode deposits.

gold-vein

One widely accepted hypothesis proposes that many gold deposits, especially those found in volcanic and sedimentary rocks, formed from circulating ground waters driven by heat from bodies of magma (molten rock) intruded into the Earth’s crust within about 2 to 5 miles of the surface. Active geothermal systems, which are exploited in parts of the United States for natural hot water and steam, provide a modern analog for these gold-depositing systems. Most of the water in geothermal systems originates as rainfall, which moves downward through fractures and permeable beds in cooler parts of the crust and is drawn laterally into areas heated by magma, where it is driven upward through fractures. As the water is heated, it dissolves metals from the surrounding rocks. When the heated waters reach cooler rocks at shallower depths, metallic minerals precipitate to form veins or blanket-like ore bodies.

Another hypothesis suggests that gold-bearing solutions may be expelled from magma as it cools, precipitating ore materials as they move into cooler surrounding rocks. This hypothesis is applied particularly to gold deposits located in or near masses of granitic rock, which represent solidified magma.

A third hypothesis is applied mainly to gold-bearing veins in metamorphic rocks that occur in mountain belts at continental margins. In the mountain-building process, sedimentary and volcanic rocks may be deeply buried or thrust under the edge of the continent, where they are subjected to high temperatures and pressures resulting in chemical reactions that change the rocks to new mineral assemblages (metamorphism). This hypothesis suggests that water is expelled from the rocks and migrates upwards, precipitating ore materials as pressures and temperatures decrease. The ore metals are thought to originate from the rocks undergoing active metamorphism.

The primary concerns of the prospector or miner interested in a lode deposit of gold are to determine the average gold content (tenor) per ton of mineralized rock and the size of the deposit. From these data, estimates can be made of the deposit’s value. One of the most commonly used methods for determining the gold and silver content of mineralized rocks is the fire assay. The results are reported as troy ounces of gold or silver or both per short avoirdupois ton of ore or as grams per metric ton of ore.

Placer deposits represent concentrations of gold derived from lode deposits by erosion, disintegration or decomposition of the enclosing rock, and subsequent concentration by gravity.

Gold is extremely resistant to weathering and, when freed from enclosing rocks, is carried downstream as metallic particles consisting of “dust,” flakes, grains, or nuggets. Gold particles in stream deposits are often concentrated on or near bedrock, because they move downward during high-water periods when the entire bed load of sand, gravel, and boulders is agitated and is moving downstream. Fine gold particles collect in depressions or in pockets in sand and gravel bars where the stream current slackens. Concentrations of gold in gravel are called “pay streaks.”

In gold-bearing country, prospectors look for gold where coarse sands and gravel have accumulated and where “black sands” have concentrated and settled with the gold. Magnetite is the most common mineral in black sands, but other heavy minerals such as cassiterite, monazite, ilmenite, chromite, platinum-group metals, and some gem stones may be present.

Placer deposits have formed in the same manner throughout the Earth’s history. The processes of weathering and erosion create surface placer deposits that may be buried under rock debris. Although these “fossil” placers are subsequently cemented into hard rocks, the shape and characteristics of old river channels are still recognizable.

The content of recoverable free gold in placer deposits is determined by the free gold assay method, which involves amalgamation of gold-bearing concentrate collected by dredging, hydraulic mining, or other placer mining operations. In the period when the price of gold was fixed, the common practice was to report assay results as the value of gold (in cents or dollars) contained in a cubic yard of material. Now results are reported as grams per cubic yard or grams per cubic meter.

Through laboratory research, the U.S. Geological Survey has developed new methods for determining the gold content of rocks and soils of the Earth’s crust. These methods, which detect and measure the amounts of other elements as well as gold, include atomic absorption spectrometry, neutron activation, and inductively coupled plasma-atomic emission spectrometry. These methods enable rapid and extremely sensitive analyses to be made on large samples.

In the past two decades, low-grade disseminated gold deposits have become increasingly important. More than 75 such deposits have been found in the Western States, mostly in Nevada. The first major producer of this type was the Carlin deposit, which was discovered in 1962 and started production in 1965. Since then many more deposits have been discovered in the vicinity of Carlin, and the Carlin area now comprises a major mining district with seven operating open pits producing more than 1,500,000 troy ounces of gold per year.

About 15 percent of the gold produced in the United States has come from mining other metallic ores. Where base metals- -such as copper, lead, and zinc–are deposited, either in veins or as scattered mineral grains, minor amounts of gold are commonly deposited with them. Deposits of this type are mined for the predominant metals, but the gold is also

recovered as a byproduct during processing of the ore. Most byproduct gold has come from porphyry deposits, which are so large that even though they contain only a small amount of gold per ton of ore, so much rock is mined that a substantial amount of gold is recovered. The largest single source of byproduct gold in the United States is the porphyry deposit at Bingham Canyon, Utah, which has produced about 18 million troy ounces of gold since 1906.

Geologists examine all factors controlling the origin and emplacement of mineral deposits, including those containing gold. Igneous and metamorphic rocks are studied in the field and in the laboratory to gain an understanding of how they came to their present location, how they crystallized to solid rock, and how mineral-bearing solutions formed within them.

Studies of rock structures, such as folds, faults, fractures, and joints, and of the effects of heat and pressure on rocks suggest why and where fractures occurred and where veins might be found. Studies of weathering processes and transportation of rock debris by water enable geologists to predict the most likely places for placer deposits to form. The occurrence of gold is not capricious; its presence in various rocks and its occurrence under differing environmental conditions follow natural laws. As geologists increase their knowledge of the mineralizing processes, they improve their ability to find gold.

Marion County Oregon Gold

A gold belt overlaps from Linn County into Marion County and slightly into Clackamas County. Primary placer gold deposits can be located about 22 miles Southeast of Salem on the Little North Fork of the Santiam River. Gold found from the Capital Mine, Crown Mine, Black Eagle Mine, and the Silver King Group of Mines produced roughly around 1,000 ounces.

Wheeler County Oregon Gold

In the Southwestern part of Wheeler County, gold, silver and galena can be found in Rock Creek and Birch Creek, which run into the John Day River. There is also gold to be found in the Spanish Gulch area. Wheeler County is also home to the John Day Fossil Beds National Monument and Shelton State Park.

Union County Oregon Gold

A boom in population came to Union County in the 1860’s and gold was the reason for it’s initial reason for the boom, mainly because gold was discovered in the Auburn area, what is now known as Baker County. People in hope for riches traveled from the Willamette Valley to Eastern Oregon. Before that, Union County was settled by the Nee Percé Indian tribe for several hundreds of years. Union County did not have the success in mining as other bordering counties, such as Baker County and most people settled for farming and logging in the county instead. When the snow got deep in the high mountains, many miners from Baker traveled to the Grande Ronde Valley in Union County for the winter.

From Starky, go to the Southwest to the North end of the Elkhorn Range. Near the North boundary of Bald Mountain and near the head of the Grande Ronde River, especially in Tanners gulch, is where the Camp Carson Placer mine is located. It was extensively hydraulicked. According to a mining report from 1903, there was a lot of platinum found, in addition to gold, in the area of Camp Carson, especially in Carson Channel.

A Rich Strike at Rich Gulch

 

Cluggage and Poole

Cluggage and Poole

Following the first discovery of gold in Oregon on Josephine Creek, in late December of 1851 or early January of 1852, packers John R. Poole and James Cluggage who owned a company called Jackass Freight, were packing supplies from the Willamette Valley to Sacramento, California. The two men decided to camp near the present site of Jacksonville, Oregon. Needing water for their animals, the two men headed up the gulch (a tributary of Daisy Creek) and choosing a likely looking place, began digging a hole in the hope that it would fill with enough water to give their mules a drink. Having moved a little bit of material, they spotted pieces of color in the hole that were large enough to be visible to the eye. The two men had accidentily stumbled into one of the largest gold strikes in Oregon history.

 

They called their find Rich Gulch and soon extended their search to nearby Jackson Creek, where they found extensive amounts of course placer gold throughout its gravels. With great foresight, the two men filed on the land adjoining their find, laid out a townsite and both became wealthy, influential men in the brand new community of Table Rock City, Oregon Territory. Today, we know the town that they founded by its current name: Jacksonville.

Rich Gulch

Rich Gulch, January 2010

Miners flocked into the area and Jacksonville promptly grew into the largest community north of San Francisco, its size soon exceeding that of Oregon’s Territorial Capital of Salem. Jacksonville was named the county seat of Jackson County. Major gold strikes were made throughout the area surrounding Jacksonville, most notably on Jackson and Daisy Creeks and thousands of ounces of gold, in both nugget and dust form flowed into town, bringing instant wealth to both miners and merchants alike. One resident who became very wealthy indeed was local banker C.C. Beekman, who’s Beekman Bank held the distinction of being the only bank in United States that charged its clients for the privelage of banking and did not pay interest on accounts. It is said, that during their time, Beekman’s scales weighed over ten million dollars worth of gold.

At today’s gold prices, this would be nearly three-quarters of a billion dollars worth of gold!

~ Kerby Jackson, Josephine County, Oregon

102_26211

Plaque at Rich Gulch

Briggs Creek - Oregon Gold Locations

Briggs Creek is not to be confused with the Briggs Pocket Mine, as they are not even close to one another. Briggs Creek is located on the western side of Josephine County. It is located in the Illinois District and had a total production  from 1852 to 1953 of 5,000 to 10,000 ounces of Oregon placer gold. That is a estimate. Upper Briggs Creek Valley, in section 7, of township 36S and range 8W, you will find the Barr Mine. This was a rich placer operation.

Along lower Briggs Creek, in the area of Red Dog Creek and Soldier Creek, there are some very rich placer gold prospecting locations. On the Northwest side of Briggs Creek, in section 24, of township 36S, and range 9W, you will find the Elkhorn placers, which were very productive.

Placer gold was discovered in Briggs Creek and it’s tributaries in 1852 or 1868 (conflicting accounts), and over 5,000 ounces of gold was recovered from the drainage area. This includes Onion Creek, Red Dog Creek, Secret Creek, Swede Creeks, as well as Briggs Creek itself. The upper part of Briggs Creek, below the Barr lode mine, was especially rich with that Oregon Gold.

Applegate River - Oregon Gold Locations

The Applegate River - Oregon Gold Location

The Applegate River - Oregon Gold Location

The Applegate River rises in Jackson County and empties into the Rogue River west of Grants Pass. Most of the placer gold deposits are found in tributaries such as Board Shanty, Caris, Miller, Grays, Oscar, Slate and Williams Creeks. Williams Creek, and it’s tributaries, Bamboo and Whiskey Gulches, were extensively worked. The Layton Hydraulic pit south of Provolt was a important producer. Oscar Creek was worked with a power shovel  and was noted for it’s large Oregon nuggets that it produced. Cans, Miller, Rocky and Slagle Creeks converge to form a rich placer area at Missouri Flat near the Jackson County line. The total placer gold production  along the Applegate River was well over 20,000 ounces.

Many spots on the Applegate River show bedrock exposed.

Many spots on the Applegate River show bedrock exposed.

The Applegate River stretches 51 miles long rising from California and stretches into both Josephine and Jackson Counties in Oregon.

Althouse Creek - Oregon Gold Locations

Althouse Creek is about 13 miles long; is located in Josephine County and feeds into the Illinois River from the Siskiyou Mountains. A section of the creek it is located about 9 miles east of Waldo. Few places in Oregon produced more placer gold than Althouse Creek, as in the early days miners lined the banks and claimed up every inch of the 10 mile stretch that was claimable. Gold was first discovered in 1852 by a man with name Althouse on the east fork, which gave it it’s name.

Althouse Creek

Althouse Creek

Browntown (the original site does not remain) was the mining center for Althouse and the surrounding mining districts in that day. A great number of large nuggets were taken from Althouse Creek as many mines from toiling miners were dug in the adjacent hillsides. So many that the hillside was said to look like a giant woodpecker had swooped down and drilled many holes into the surrounding hillsides. About three miles from Browntown on the Althouse was another town called Grass Flat, which also served as another center for the cattle trade and gold. This area in Josephine county not only had lot’s of miners but had it’s share of farmers and cattle rustlers also. After all the miner’s had to eat, and many found profit in other ways besides a pick, pan and shovel. Before long, power shovels and a dragline excavator were introduced in 1936 and they discovered that the Chinese had drift mined the area in the early days. The dragline could handle 6,000 cubic yards of gravel per day.

Of greater importance in the Althouse drainage area was the Briggs Pocket Mine in the presence of large hydraulic cuts in, or near Allen, Fry, Sailor, Scotch and Waldo Gulches. The Logan Llano de Oro hydraulic cut was opened in 1874 and was worked on and off until 1945. It consumed 30 acres and produced 30,000 ounces of gold, along with some silver, platinum, and osmiridium, from gravels, which contained up to .016 ounce of gold per cubic yard.

The high gravel and deep gravel cuts were made in the same general area during the same time interval. The high gravel cut produced around 5,000 ounces of gold. The deep gravel cut covered 65 acres and produced about 14,000 ounces of gold, from gravels that produced about .0125 ounce per cubic yard. Considerable placer gold remains to be mined in the district. Near Holland, south and half a mile along Althouse Creek, in stream deposits, and in benches you can find gold colors, and nuggets. In the area along Althouse and Sucker Creeks there were extensive placers including the Llano de Oro (Esterly), Deep Gravel, Placerica, and Leonard placers. All of which were very rich, worked by thousands of miners in the 1850’s -60’s.

New Pocket Gold Discovery near Cave Junction, Oregon

Written and submitted by Tom Bohmker

Southern Oregon is famous for it’s pocket gold deposits which are on or near surface enrichments of lode gold. Many of these finds were quickly worked out and few ever developed into any kind of conventional lode mine with sizable tonnages of ore and ore processing mills. Most pocket deposits were shallow holes worked with hand tools, a little dynamite and the gold separated from the country rock in mortal and pestle. Details of pocket mining prospecting and case by case discussion can be found in the book The Elusive Pocket Gold of SW Oregon available from Cascade Mountains Gold.

Some months ago, I receive some emails from a mining acquaintance who reported on a rich recent pocket find in the Hungry Hill Area. A photo sent to me shows the digging at 4 feet down and a large mass high grade about 4 inches across. Another photo shows approximately 20 to 30 ounces of gold that had just been crushed out of the host rock. Initially reports claimed 20 Ibs of gold have been recovered from this pit. A recent photo shows the excavation nearly 8 feet deep and the yield is said now to be much more. If these figures are accurate this could be one of the largest pockets in recent decades.

Geology of pocket deposits in the Hungry Hill Area

This area is on the contact of Meta-volcanic such as greenstone and certain meta-sedimentary rock units with the large serpentine belt that stretches North by Northeast from the Oregon/California border to an area near Canyonville, Oregon. Most of the gold deposits are in the rock units bordering the serpentine . There are a few larger quartz veins exposed on the surface for fractions of a mile and have been worked hundreds of feet deep. However, many of the pocket deposits are broken up tiny veinlets of quartz which may be only followed down a few feet before pinching and losing value. Others may show little quartz but contain gold values in shear zones of localized faulting. Where such gold bearing lodes are on the surface there can be additional concentration of gold values by eroding away of the lighter ingredients of the host rock or from the formation of laterite type soils.

The pocket belt is especially strong from the head waters of Canyon Creek just a couple miles west of Cave Junction . From here the belt heads North by Northeast to Hungry Hill; then the Pocket Knoll and across the Illinois River to the drainages of Briggs Creek. The creeks and gulches that drain this area are famous for rich placer gold deposits. Interestingly only a few of these lode deposits ever developed into large underground mines as the Peck Mine and the Eureka Mine on Soldier Creek a tributary of Briggs Creek Most of these diggings were shallow surface pits quickly worked out and abandoned. On hill sides such as Hungry Hill the slopes still show the out lines of hundreds of shallow pits. The old timers did not find them all!

Gold in Josephine County - 1870

From the archives of Kerby Jackson

Extract from -
Mines & Mining in the States and Territories West of the Rockies
U.S. Commision of mining statistics, 1870

CHAPTER XXX.
JOSEPHINE COUNTY.

Josephine County in 1895

Josephine County in 1895

This county is situated in the southwestern part of the State, and contains about two thousand five hundred square miles. It is bounded north by the Rogue River Mountains, separating it from Douglas County, east by Jackson County, south by California, and west by Curry County. There are about fifteen hundred inhabitants, and five or six thousand acres of land under cultivation. Kerbyville, Leland, Slate Creek, and Waldo are the principal towns. The condition of the placer mining in the county during the past year has been substantially the same as in Jackson County. Josephine suffers somewhat from lack of regular communications. It is perhaps on this account that I have failed to receive the detailed reports promised by letter from Sailor Diggings and other noted localities. The following description, furnished to a committee of the State Agricultural Society in 1869 by Dr. Watkins, a physician long resident in the county, may be relied upon.

Josephine County attracted attention as early as 1852, as a locality for placer gold-mining. The first mining of any importance was on Josephine Creek, which derived its name from a daughter of one of the miners, and afterward gave name to the county. In the spring of 1853 there was a great rush to the mines on Althouse Creek, which rises in the Siskiyou range, and runs in a northerly direction, uniting with other tributaries, forming Illinois River. The diggings on Althouse were very rich, the bed of the stream paying not only heavily but quite uniformly. At one time Adams & Co.’s books had a thousand names to obtain letters for in the different localities, where miners had previously resided. Sailor Diggings was then a famous locality; a ditch was dug some fifteen miles long at a cost of some $75,000 or $80,000 to bring water to the rich placers of this vicinity, and when fairly under way paid for itself the first year. It paid heavy dividends to its stockholders for ten or twelve years, and many parties who live sumptuously every day owe their fortune to their connection with the Sailor Diggings Ditch Company.

Sucker Creek, a tributary of Illinois River, a large turbulent mountain stream, was extensively mined from 1854 to 1860, but the diggings are deep, the boulders are large and unwieldy, the stream an unmanageable one, and, I think, never made an adequate return for the labor expended; but Sucker Creek has not yet had its day, and, with cheaper labor and better facilities, it will yet yield a golden harvest to the hand of adventure.

Canon Creek, Illinois River, and Galice Creek, were mined during these years, and generally with an adequate return for labor expended.

Williams Creek, a tributary of Applegate Creek, has had for the last few years a hardy mining population, who have met with a moderate return. Josephine is a mining county, and has had all the vicissitudes of such a county. Her citizens leading a roving life, and having little to bind them to the soil, mostly left during the Indian war of 1855-’56. Her rich minerals brought back to her a renewed population, however, but the great Fraser River excitement nearly depopulated her, and now she is only the shadow of her former self. But her rich placers are far from being exhausted. There are rich veins of copper running into her hills. The most noticeable one, some eight or tea feet in thickness, is situated in the hills betweeu Waldo and Althouse; but for some reason attempts to work it have failed, although it appears to be of great purity and inexhaustible in quantity. But the copper mines down Illinois River will yet make this locality famous; the copper is found in well defined lodes, and practically inexhaustible. The question is one of transportation.

Platter & Beach have been running a tunnel for the last three years through a heavy divide, to turn the waters of Althouse, so as entirely to drain the bed of Althouse Creek. Hanson & Co. have done the same at another point, and are now ” striking it rich.” These two operations have opened a district of great mineral wealth, which will awaken the old times in placer-gold mining on Althouse. The returns of the Malachi quartz lode have been very heavy ; and it is reported that this property has been purchased by a San Francisco house, who are pursuing the enterprise with vigor.

The county is dependent for supplies upon a slow, laborious and costly transportation over the Coast range.

Notes:

Strangely enough, despite the passing of 140 years, a lot of things have not changed here in Josephine County since 1870. Most of the creeks and rivers which were mentioned by Dr. Watkins are still the centers of what little gold mining still goes on this county. The limited activity is not for the lack of gold, but due to the evergrowing problem of environmentalism all in the name of saving “virgin” waterways that contrary to common knowledge, are not so virgin. Sucker Creek, in particular, has had a lot of exposure in the news due to the prosecution of Cliff Tracey for his challenge against the authority of the USFS. But Sucker Creek, named for the large number of Illinois miners who once worked that creek (so named because Illinois is called “The Sucker State” and they also leant the name of their home state to the nearby river and surrounding valley), was worked so heavily in the old days that every boulder and every piece of gravel was probably overturned by the hands of early miners. Later on, around 1910, dragline dredges worked this waterway. Despite this, Sucker Creek is beautiful and supports a great deal of aquatic life. As Mr. Tracey’s tenacity indicates, there is undoubtedly still a lot of gold in the Sucker Creek watershed. It is reported that even down low in the grassy plain valley where the bedrock runs to depth of seventy five or more feet, that good quantities of course flakes can be recovered by simple panning of this creek’s gravels. Quite a lot of mining claims are still located on the upper end of this creek and its tributaries, mostly worked by individual miners.

Althouse Creek is a neighbor of Sucker Creek, and though it is more famous than the aforementioned waterway, both bring their gold from the same sources, which are largely concentrated in the hills between the East Fork of Althouse and the East Fork of Sucker. The gold in these two creeks originates from both lode deposits, as well as ancient channel gravels which still remain mostly unworked on the Oregon side of the Siskiyous. These two creeks have produced the largest gold nuggets ever located in Oregon history, including the famous Collins Nugget from the East Fork Althouse, as well as several nearly that size from Sucker Creek that were all recovered prior to 1900. Though the gravels of Althouse Creek itself have been heavily worked and the upper reaches are so wild that it is like you’ve stepped back into time, a large amount of activity still takes place in this area, most of which by small suction dredge.

Slightly to the west of Althouse Creek is a tremendous wealth of native copper. In fact, this is the greatest belt of copper on the West Coast and it runs for about 100 miles through Sothern Oregon and Northern California. One copper mine that did exist in this area was the famous Queen of Bronze Mine which was located near Takilma, Oregon and operated between 1862 and the 1930. Durings its heyday (about 1900), this 160 acre operation located at 40S, 8W, Sec 36, NW was the largest copper mine in the United States, consisting of over 7100 feet of tunnels. The Queen of Bronze also yielded gold as by-product, its total production amounting to about 60,000 ounces of gold and over 5 million pounds of copper. Since 1930, the mine has changed hands a number of times and despite housing tremendous mineral reserves, little work has been done since 1930 beyond some basic evaluation.

Seal of the State of Jefferson

Seal of the State of Jefferson

As was mentioned in the article, transportation issues prevented these reserves from being heavily mined. In fact, this condition was such that as late as 1941, the situation finally came to a head when residents of SW Oregon lobbied the State of Oregon to improve transportation into the copper belt. Instead, the state built campgrounds in the Northern Willamette. Meanwhile, California’s government also failed to support mining interests in Northern California. Leading citizens from the counties located on both sides of the California-Oregon border met in Yreka, California on November 17th, 1941 to discuss this issue and emerged with a plan. Their goal was for these counties to secede from Oregon and California and to form a new central government - the State of Jefferson. The state seal and state flag that they adopted reflected the core of the issue. The seal was a gold pan with two X’s emblazoned over top of it, representing “the double-cross” that had been done to the region by the governments of Oregon and California. Ten days later, those involved mounted an organized revolt. Astride horses and armed with rifles, they blocked Highway 199 (now I-5) near Yreka and handed out proclamations of independence to motorists. These read:

“You are now entering Jefferson, the 49th State of the Union. Jefferson is now in patriotic rebellion against the States of California and Oregon. This State has seceded from California and Oregon this Thursday, November 27, 1941. Patriotic Jeffersonians intend to secede each Thursday until further notice.

For the next hundred miles as you drive along Highway 99, you are traveling parallel to the greatest copper belt in the far West, seventy-five miles west of here. The United States government needs this vital mineral. But gross neglect by California and Oregon deprives us of necessary roads to bring out the copper ore. If you don’t believe this, drive down the Klamath River Highway and see for yourself. Take your chains, shovel and dynamite.

Until California and Oregon build a road into the copper country, Jefferson, as a defense minded state, will be forced to rebel each Thursday and act as a separate State.”

Eventually, an officer of the California Highway Patrol stumbled upon the roadblock. The men handed him a flier and told him to “go back to California”, upon which he promptly stepped back into his car, did a U-turn and left the area.

On December 4th, 1941, Judge John L. Childs of Crescent City was elected as Governor of the State of Jefferson and a torchlight parade was held at its Capital of Yreka. Media was present to record the event, which was to broadcasted on December 8th. It seemed the State of Jefferson was off to a grand start.

On the morning of December 7th, 1941, Japan launched a crushing attack on Pearl Harbor. The newsreels of Jefferson’s establishment as a state never appeared and the rebellion of locals ceased as the people went to work to support the war effort.

Eventually, a proper road was built into the copper country. It is called the State of Jefferson Scenic Highway, but most of the copper is still there awaiting some industrious miners to take it out.

One thing that has changed are the communities which Watkins mentioned in the article. Two of the four communities he mentioned no longer exist at all, namely Waldo and Leland. The other two, Kerbyville and Slate Creek barely exist and they are no longer called called by those names. Today, the only substantial community in Josephine County is Grants Pass, which was just a little hole in the road in Watkin’s days.

 

Waldo, Oregon in 1890

Waldo, Oregon in 1890

Waldo was one of the the first communities established in Southern Oregon and was originally called Sailor’s Diggings. This area gave rise to the first organized mining district in Oregon - the Waldo Mining District - which was established in 1852. This district still exists (and actually pre-dates creation of the State of Oregon) and is at the forefront of fighting for the rights of miners in this region. The Waldo Mining District, as the first seat of local government in this area, was instrumental in the formation of Josephine County which was established in January of 1856 when it separated from Jackson County. Waldo became its first county seat. Though popular myth has always claimed that the population of Waldo exceeded 30,000 miners during its heyday, in reality, only about 1500 persons (excluding Indians) lived in Josephine County in those days. Two thirds of these were miners working around the vicinity of Waldo, a small number of which were Chinese. Starting out as a tent city and growing into something more permanent, during its boom, Waldo was a wide open town that often attracted a rough element.

Ferd Patterson

Ferd Patterson

One fella who was attracted to the wealth of the diggings in the area was a young gambler by the name of Ferd Patterson who thought himself as not only a bit of a dandy, but he also thought of himself as a bit of a gunslick. Several years before he made a big name for himself by killing Sumner Pinkham in Idaho and ultimately bit the dust in Eastern Washington, Ferd wound up in an arguement with two local miners in Waldo over a card game and promptly gunned them both down. With the locals hot on his heels, Ferd beat feet for Portland, where he soon got himself into a bunch of trouble when he scalped his mistress and killed a well known riverboat captain whom he thought was shacking up with his girl. Another individual who got himself into trouble in Waldo was the notorious outlaw Boone Helm who later made a name for himself with the Henry Plummer gang, not to mention with his partaking of the flesh of one of his unfortunate partners somewhere in Idaho. In 1858, Boone was on the run from California and headed to The Dalles which widely reputed as a safe haven for criminals. During his stay in Oregon, Boone got himself in all kinds of trouble and killed several other men. One man he didn’t manage to kill was an old farmer living near Waldo. When Helm begged food off the farmer, the old man took pity on him and invited him into his home, where he provided him with food and rest. Illustrating that no good deed should go un-punished, Boone decided that he would kill the old man and steal whatever food and valueables that he had. Upon his attempt to sneak up to the old man while he lay asleep in his bed, instead of an easy victim, Boone soon found himself face to face with the barrel of Fowling shotgun. Upon escaping from the cabin, like Patterson, Boone Helm was chased out of the county. However, like other boom towns, Waldo would not last. By the 1880’s, many miners had left the vicinity and headed to nearby Kerbyville which eventually replaced Waldo as the seat of power in this county. A good many others went to the new strikes on the Frasier River. In December of 1928, Waldo lost its post office. During the 1930’s, it was discovered that Waldo had been built upon a rich gravel bench and the townsite was soon purchased by a local mining company. As also happened with the townsite of nearby Browntown on Althouse Creek, during that decade, the monitors took care of Waldo once and for all as they mined the site out. Today, nothing remains of Waldo but a cemetery.

Fort Leland

Grave Creek House at Leland

Like Waldo, Leland also now no longer exists. This community was located on LeLand Road somewhat past the present community of Sunny Valley, Oregon. Though this was originally the site of Fort LeLand during the 1850’s and the surrounding land was patented in 1859 by James Twogood who operated a stage station nearby called Grave Creek House, the small community that grew up in this area was known by a number of names, namely Maloneyville and Altamont. The town received its first post office in 1884 and served as a supply center for nearby mines, namely that of Criteser and Tast (1/4 mile west of town) which was established in 1878, the Goff Mine that was established a half mile north of town in 1886 and yet another large mine about one mile west of town that was eventually owned by the Lewis Company of Portland. By 1890, a few miles south of Leland, another town also grew up in the form of Placer. Like Leland, that town too no longer exists, both of them going into decline around World War One. By the 1940’s, the name of this area was changed to Sunny Valley. Quite a lot of mining is still done by individual prospectors in this gold rich area, mainly along Grave Creek.

Watkins also mentions the town of Slate Creek. Though now a shadow of its former self, this town still exists only today we call it Wilderville and consists of little more than an old store and a community church. At one time, one of the greatest marble mines in the United States looked down on this community. Nearby Slate Creek runs behind Wilderville and is a tributary of the Applegate River with tremendous reserves of placer gold. Decades ago, when my grandmother first came to Oregon and wished to live a solitary existence, she lived on an old mining claim high up on Slate Creek and made her way with nothing but a gold pan and a rifle.

Kerbyville in 1885

Kerbyville in 1885

As mentioned earlier, Kerbyville replaced Waldo as our local county seat. It still exists today and though little of it remains, it is a great old town with a lot of gold history and a nice musuem. Like Waldo, Kerbyville was a rough place during its heyday where miners often doled out justice at the old hanging tree. According to local legend, Kerbyville was established when a packer by the name of “Tig” Martinez was transporting a pool table from Crescent City, California which he had consigned to a man named Jake Cohen who was a saloonkeeper at Althouse. Tig had the table on the back of his favorite mule, who he called Anita. Suddenly, Anita collapsed from the strain and promptly died. It was believed that there was not another mule in the whole of the valley which could carry the table on to Althouse, so Tig left it atop the mule and went to see Cohen and explained to him that the table was near the farm of James Kerby and that he would have to transport it the rest of the way to Althouse. Tig then asked for his pay, which Cohen refused to give to him for lack of delivery. The end result was that Tig was now the proud owner of one pool table which was currently lying atop the carcass of his favorite mule in the middle of the trail. Not wanting to lose the money that he had invested, Tig soon came up with an idea. After removing his mule from beneath it, Tig erected a tent around the table, set up a bar and advertised the grand opening of a brand new saloon. As it was the only pool table in the area, he soon had a roaring trade and a town grew up around it. At its height, about 500 people lived in Kerby, mostly miners who worked the neighboring creeks and gulches. In the surrounding hillsides, a lot of gold can still be found. As you might have guessed, this writer was named for that town.

~ Kerby Jackson, Josephine County, Oregon

Female Miners in Southern Oregon?

From the archives of Kerby Jackson

When one thinks of the old timers who worked the rivers, creeks, gulches and hills of Oregon in search of illusive riches, we think of the iconic old grizzled prospector. Red shirted and bearded, with a pick over his shoulder, a .45 slung low on his hip and accompanied only by his trusty mule whose back is heaped high with gear, he is the traditional icon of the gold rush era. That image is so powerful and so well known that today, it adorns anything having to do with the word “gold” and like his cousin the cowboy, everyone recognizes him just by his outline. Yet contrary to that traditional image, he wasn’t the only fella who was out there breaking his back for a few bits of color. The patience and hard work of the Chinese and their contribution to the Southern Oregon Gold Rush are legendary, but even lesser known today were the efforts of Pacific Islanders (so-called “Kanakas”), Mexicans, Free Blacks and other groups of men who came to toil in Oregon’s creeks and gulches hoping to strike it rich. And as the following article, originally published over a century ago attests, not every person working in the gold fields of Oregon was necessarily “one of the boys”.

 

Grants Pass, Oregon. May 1904.

The gold fields of Southern Oregon mineral zone appear to be particularly attractive to women; at least this section has its fair share of women miners, and there is no gainsaying that it has profited thereby. A visitor to the Forest Queen hydraulic mine, near Grants Pass, will find a handsome woman busily engaged about the diggings, operating a giant, retorting gold or even “bucking” the boulders on the bedrock. This woman is Mrs. Wisenbacher, but she was formerly Miss Pipes and was one of the stunning “Sadie Girls” with the popular Anna Held company in “The Little Duchess”. Last year, Mrs. Wisenbacher quit the stage and became a full “partner” with her father and brother in the operation of the Forest Queen Mine. With a woman about to assist, the season has been a successful one at the Forest Queen.

“Though I had become fascinated with the life behind the footlights,” said Mrs. Wisenbacher to a Mining Review correspondent, “I am equally so with the life of a gold digger in Southern Oregon. There are few spots anywhere prettier than that where the Forest Queen is located.”

Mrs. Wisenbacher, being a “Sadie Girl” is, of course, handsome. She would have this season been a “La Mode” girl in the same popular company, but she was induced by her father, who is a prominent Colorado and Idaho miner, to give up the stage and live a life of greater ease and freedom in the Southern Oregon Mountains.

The Mining Review correspondent also came unexpectedly upon another woman miner, a woman “piper”, if you please, in a Southern Oregon mine. She is Mrs. M.E. Moore, and this lady, like the other mentioned is a full “partner” in a placer mine. Mrs. Moore is a piper, an expert piper - not the kind the Scotch Highlanders know so much about - but a hydraulic mining piper - the operater of a hydraulic giant. Every day this woman is at her post beside the giant, long before the sun is up, and she remains there throughout her shift. None know better than she how best to swerve the big nozzle to drive an avalanche of boulders down the gulch ahead of the giant’s stream, scattering them like a handfull of bullets shot from a catapult, or how to bring that long and deep growl to the monster as its cuts and gnaws deep at the base of the towering red clay bank till a great slab of a thousand tons topples and falls with a crash from the mountainside.

Mrs. Moore has been a “partner” of her husband in the mining business for nearly twenty years. She has followed the trails through the mining regions of Colorado, Montana, Arizona, California and Oregon, prospecting, pocket-hunting, digging, always on the lookout for a color, a strike, a bonanza. She has traveled hundreds of miles on pack pony and burro, through the snow and over the burning sands. Those twenty years, spent altogether out of doors, have been days of perfect health for her. “Yes,” said she, “mining is the life for me. I love it. I love the freedom of the mountains and the ozone of the pines. There is no other life like it; none as enjoyable for me, at least.”

 

The Mining Review, 5/18/1904
 
Ellen Jack, a female prospector from Colorado at the turn of the 19th century. Courtesy: Kerby Jackson archives

Ellen Jack in 1910

One of the best known female prospectors was Ellen Elliot Jack of Colorado, who is pictured at the left in a photo dated about 1910. Ellen was born in England, but came to the Far West in 1872 after the tragic death of her husband and children. In addition to mining, she was also an early woman business owner. Like her male counterparts who worked the gold fields, Ellen was one tough cookie. Everywhere she went, Ellen carried a pick axe and a six gun in her belt and she knew how to use both of them. She was also said to bear a severe scar that was the result of a tomahawk wound she received during one of the Gunnison Indian Uprisings. At the time this photo was taken, she had just written a semi-autobioghraphical novel entitled “The Fate of A Fairy” which was about a woman who loses her husband and becomes a female prospector.

Another lady prospector was Ferminia Sarras, who was a major mine owner in Nevada and was widely known as the “Nevada Copper Queen”. Ferminia’s story would have been lost to history had it not been for the research of historian Sally Zanjani, the author of “A Mine of Her Own: Women Prospectors in the American West, 1850-1950″

The article above is thought to have been written by Dennis Stovall who was an early author living in Josephine County. Stovall is best known for his novel “Suzanne of Kerbyville” which he wrote the same year as this article. His novel, though fictional, is one of the best sources for information on the early settlement of Kerby, Oregon, as well as the mining that went on in the vicinity of that early gold rush town. Though the novel really focuses on the exploits of a young woman named Suzanne , it is mentioned that Suzanne’s father was a “pocket hunter” and there is quite a good description of his methods.

The Forest Queen Placer, mentioned in this article, was located on Louse Creek, a few miles east of Merlin, Oregon. At the time, it was owned by J.P. Pipes and T. Weisenbacher (or Wisenbacher). The property was originally known as the Lance Placer and at the time of this article it consisted of 212 acres of ground that was worked with the assistance of two miles worth of ditch, 2500 feet of pipe with a pressure of 200 feet, three giants and a Ruble Rock Elevator.

~ Kerby Jackson, Josephine County, Oregon

Gold and Geology of Josephine County

josephine-county-map

Lode Gold

The geology of  Oregon gold locations in the southwestern part of the state is complex and not fully understood, being closely associated with plate tectonics and crustal subduction. Numerous gold-quartz veins can be found in greenstone of the Triassic age (248 - 208 million years ago), which trends in belts from the southwest to the northwest parts of Josephine County. Black slate , peridotite, and serpentine of Jurassic age sometimes contain gold-quartz veins and tend to parallel the greenstone belts. Granite, diorite, and gabbro intrusive bodies can be found in many parts of the county, but are generally devoid of mineralization except where they are in contact with older rocks. Josephine County is noted for past chromium, copper and nickel production as well as gold, and exploratory work for nickel continues to this day.

The most productive lode gold mine was the Greenback Mine, which produced approx. 175,000 ounces of gold from a persistent quartz vein in greenstone. It was sunk to an incline of 1,000 feet on 12 levels. The Benton Mine was developed in gold-quartz veins in greenstone near the contact with intrusive diorite and produced 18,500 ounces of gold. The nearby Gold Bug Mine produced 37,500 ounces. Numerous other lode mines produced  between 1,000 and 13,000 ounces of gold, primarily in the period between 1893 and 1942.

Pocket Gold

Josephine County is noted for rich pockets of gold close to the surface. Some of these pockets were fabulously rich, though they were mined out quickly. The best known pocket diggings was in the Briggs Mine near the California line, where masses of gold totaling 2,000 ounces were taken out in 1904. Slabs of gold up to 3 feet in length were reportedly recovered.

Nuggets

A number of nuggets the size of chicken eggs have been found in placer gravels and pocket deposits. A 17 pound nugget was found in 1859 on the East Fork of Althouse Creek below the Briggs Pocket. Another nugget weighing 15 pounds was found in the gravels near the Esterly hydraulic cut in the early 1860’s. Despite the abundance of nuggets in Josephine County, most gold recovered in placer mining operations is fine flakes.

Placer Gold

Placer gold was discovered in 1850 and simple hand mining methods commenced in 1852. Before long, hydraulic methods were introduced and a number of deep cuts were made in the landscape. Placer gold can be found in stream channels, in bench gravels, and in terrace gravels up to 600 feet above the present stream levels. Old channels can be found in terrace gravels, some of which are rich. Gold is generally found at or near fractured or decomposed bedrock. Some of the bench and terrace gravels are cemented. Boulders are common in many stream gravels, and most gravels range from a few feet to over 50 feet in thickness.

Power shovels, dredges and dragline excavators were introduced around the turn of the century and were used up to 1952. Since 1960, individuals with portable suction dredges have found considerable gold in Josephine County and Jackson County to the east. Most placer work is done between February and September when streams contain sufficient water.


Oregon’s Biggest Gold Nugget: The Collins Nugget

If you trawl the internet for information on gold mining in Oregon, sooner
or later, you’ll find mention of the Armstrong Nugget. This huge lump of
placer gold was discovered near what is today the ghost town of
Susanville, Oregon in 1913 by George Armstrong. This big monster weighed
in at 80.4 ounces. Today, its gold value alone would fetch over $80,000
U.S. dollars. The Armstrong Nugget is currently on display at U.S. Bank in
Baker City in Grant County, Oregon. Most online sources claim that the Armstrong Nugget was the biggest gold
nugget ever discovered in Oregon, but it isn’t so.

In fact, here in Josephine County, on the opposite side of the state, a
number of larger gold nuggets have been discovered near what was refered
to as Sailors Diggings. One of them, pulled out of Sucker Creek, weighed
over 15 pounds. That’s a big chunk of gold, but it’s still not the biggest
nugget that Oregon ever produced.

In 1859, a little Irish fellow by the name of Mattie Collins was mining in
the high bank along the East Fork of Althouse Creek when he uncovered a
huge lump of almost pure gold that became known as the Collins Nugget.
Mattie’s find weighed in at a whopping 204 ounces (approximately 17
pounds. At today’s gold prices, the Collins Nugget would be worth over
$200,000, but typically a nugget will fetch a significantly higher price.

The Collins Nugget is the largest single hunk of gold ever pulled from the
Oregon lands, but unlike the Armstrong Nugget, it doesn’t survive today.

As was always done in those days, Mattie took his find to the smelter at
Jacksonville, sold it for $3500 and then drank himself into poverty.

Copyright 2009 by Kerby Jackson
http://www.western-stories.com/

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