Confederate Gulch and Diamond City
Confederate Gulch is a steeply incised valley on the west facing slopes of the Big Belt Mountains. Its small stream drains westward into Canyon Ferry Lake, on the upper Missouri River Valley near present day Townsend, Montana. In 1864 Confederate soldiers on parole from the American Civil War made a minor gold discovery in the gulch, but in 1865 the discovery of the sensationally rich Montana Bar—one of the richest placer strikes per acre ever made—led to other rich gold strikes up and down the gulch, and touched off a frantic boom period of placer gold mining that extended through 1869. From 1866 to 1869 the gulch equaled or outstripped all other Montana Territory mining camps in gold production, producing an estimated $19 to $30 million in gold—late 1860s money. For a time, the gulch became the largest community in Montana—in 1866 Montana had a total population of 28,000, and of these, about 10,000 (35%) were working in Confederate Gulch. The main community was Diamond City , and while gold production was at its height, Diamond City roared along both night and day. During its heyday, Diamond City was the county seat of Montana's Meagher County, although today the area has become part of Broadwater County. In their frantic efforts to get at more gold, the miners built ditches and flumes that extended for miles, and employed high pressure hydraulic mining methods which washed down whole hillsides and ate up the gulch floor. The hydraulic mining process stripped the gulch and left huge spoil banks—hydraulic mining even consumed the site of Diamond City, which had to be moved to a new location. Then the gold ran out, the boom was over and the population simply picked up and left. In 1870 there were only 255 people left and a year later only about 60. Today hardly a trace remains of Diamond City or the other gulch communities. The gulch is quiet and empty, with only an occasional summer prospector, or a rare traveler using the unimproved road that still winds up the gulch from the Missouri Valley and crosses the top of the Big Belts on its way down to the Smith River Valley. Diamond City, Confederate Gulch and the Montana Bar were spectacular examples of the flash-in-the pan Montana placer gold mining camps, but what a flash.
- 1 The initial discovery in Confederate Gulch by paroled Confederate soldiers
- 2 The discovery of the fabulous Montana Bar in Confederate Gulch in 1865
- 3 History of gold production in Confederate Gulch after the seminal Montana Bar strike of 1865
- 3.1 Rich strikes on Confederate Gulch, and its tributaries—at Boulder Bar, Diamond Bar, Gold Hill, Cement Gulch, Montana Gulch, and Greenhorn Gulch
- 3.2 Gold production 1866 to 1869
- 3.3 Technical problems from 1866 to 1869
- 3.4 Hydraulic mining in Confederate Gulch
- 3.5 Mining operations 1870 to the mid-1940s
- 3.6 Lode mining in Confederate Gulch - the search for the mother lode
- 4 Diamond City: "The Most Spectacular of Montana's Boom and Bust Gold Towns"
- 5 The geology of Confederate Gulch
- 6 Confederate Gulch in the present
- 7 Visiting Confederate Gulch
- 8 See also
- 9 References
- 10 External links
The initial discovery in Confederate Gulch by paroled Confederate soldiers
Confederate soldiers arrive in the Montana territory, during the Civil War, in 1864 and 1865
In 1864 and 1865, before the end of the American Civil War, Confederate soldiers arrived in Montana, prospecting for gold. The soldiers had been part of General Sterling Price's Confederate army, which had invaded Missouri from Arkansas in 1864. The army disintegrated after several defeats. However, the remnants of the defeated army remained in quasi-official units of a couple-of-hundred to a thousand-or-so.
Hunting these scattered units was very dangerous business. After pondering the situation the Union commander in the area, General Alfred Pleasonton, instituted the policy of amnesty, offering parole to the Confederates captured during the 1864 campaign if they would leave the combat area and go up the Missouri River into the west. Pleasanton hoped that his policy for captured Confederates would also convince the remaining free roving units to disband, and prevent them from becoming bushrangers living off the country like Quantrill and the James Boys.
Fighting and perhaps dying for a lost cause was discouraging. The offered parole seemed to be the better choice. Additional motivation came from rumors of rich new gold discoveries up in the Montana Territory. Whether due to General Pleasanton's policy or despite it, in 1864 and 1865 these rag tag Confederate units faded away, and a tough breed of Missourians began to show up in the Montana Territory.
Paroled Confederate soldiers make a minor strike in the Big Belt Mountains
In 1864 two Confederate prisoners, Wash (Washington) Barker and Pomp Dennis, were paroled and released at Liberty, Missouri to the owner of a steamboat bound up the Missouri for the Montana goldfields. Steamboats had to make frequent refueling stops for wood to heat the boilers, but from Yankton, Dakota Territory to Fort Benton, Montana Territory (a distance of well over a thousand river miles), hostile Indians controlled most of the country. The Indians had burned the few existing wood yards and steamboats had to stop and cut wood as they went. Rebel soldiers like Barker and Dennis could work their way to the Montana Territory, by chopping fuel along the way.
The Missouri river was low in 1864 and Barker and Dennis only made it as far as Cow Island, before low water forced the steamboat to unload passengers and freight. The freight and paying passengers were carted by team and wagon the rest of the way to Fort Benton, but the former Confederates were on their own. News had come down the river that a new gold strike had been made at Last Chance Gulch (present day Helena), at the foot of Mullan Pass, but by the time Barker and Dennis walked there from Cow Island, the good ground was taken, no jobs were to be had, and the price of everything was high.
Smoke from prospectors' camps could be seen all along the foothills and so Barker and Dennis set out up the Missouri from Last Chance Gulch, (present day Helena Montana), prospecting here and there, living off the country. Here the Missouri was a large mountain river, cold and clear, bordered on each side by high ranges, with vast alluvial fans running out from steep gulches down to the river. Good color could be found in these gravels, but so far there were no rich strikes.
While prospecting and living off the country Barker and Dennis were joined by Jack Thompson, and John Wells, who had also been rebel soldiers. They eventually wandered into a gulch on the west side of the Big Belt Mountains. Late fall was at hand, and they determined to stay for the winter—there was a good creek, and wild game. At one place near the mouth of the Gulch, east of the creek, Thompson sunk a hole and found the first pay dirt, a piece of gold about the size of a grain of wheat. Prospecting up the canyon they found more gold in small quantities. Eventually they established a modest discovery of placer gold in gravels of the little creek, where a day’s hard work could produce enough to pay for a few pounds of beans.
Naming Confederate Gulch and Diamond City in the winter of 1864-65
The initial strike of Barker, Dennis and Thompson on the gulch in the Big Belt Mountains was small, but hard work produced enough gold so that word spread. Other southern sympathizers showed up in late 1864, and the area became known as Confederate Gulch.
During the winter of 1864-65 four log cabins were built equidistant around a large rock obstruction on the narrow floor of the gulch. The paths from cabin to cabin made a perfect diamond in the snow, as seen from the slopes above, and so the cabins in the gulch were named Diamond City. The "city" part of the name was a joke, comparing this poor settlement of southern sympathizers to the booming mining camps of Helena and Virginia City.
The discovery of the fabulous Montana Bar in Confederate Gulch in 1865
Diamond City and the associated prospecting camp grew slowly. In the winter/spring of 1865, many prospectors passed through Confederate Gulch, since it was on one of the few trails that led from the Missouri Valley up over the Big Belt Mountains to the Smith River Valley, where game was abundant and there was available land that could be farmed.
In late 1865 a group of newcomers arrived, referred to as "The Germans". They were led by an old time Colorado prospector named Charles Fredericks. He liked the looks of things and prospected up the stream in an area that later became known as Cement Gulch. Cement Gulch area later became one of the richest discoveries of Confederate Gulch, but the Germans didn't get down to bedrock and so they decided to move on to look elsewhere.
Fredericks led his group back down the main gulch, through timber and sank a prospect hole in a clearing on a shelf up from the gulch floor, at the foot of a small tributary. In the prospect hole, the group literally "struck it rich". The tributary became famed as Montana Gulch, and the shelf became doubly famed as the Montana Bar of the Montana Gulch.
The Montana Bar was only about two to 3 acres (12,000 m2) in extent, but it was one of the truly spectacular placer gold discoveries in terms of yield per unit area. The Bar was also unique in that the gold wasn't located on bedrock at the bottom of the gulch, but was in a shelf of gravel located up on the side of the gulch.
The Montana Bar gravels were saturated with gold from the surface down to the bedrock, which was a dense blue gray limestone. Depressions in the bedrock trapped gold, and when washed over by water, the gold in these depressions was so thick it could be seen from a distance as glowing metal. The gold bearing gravel deposit was about 8 feet (2.4 m) deep in most places, but thickened to thirty or forty feet against the mountain.
The few acres of the Montana Bar were freakishly rich in gold. It was claimed that the gravels of the Montana Bar were some of the richest ever washed, anywhere. It was not uncommon to get $1,000.00 of gold from a pan of gravel and dirt, and this was at a time when gold was worth less than $20.00 an ounce. The record pan, according to witnesses, was $1,400.00, or roughly 7 pounds of gold in 15 pounds (two shovelfuls) of gravel. At the first cleanup of the sluice boxes on the Bar, the riffles were clogged with gold. One week’s production of gold on Montana Bar was $115,000.00.
A popular legend grew up around the discovery of the Montana Bar. According to popular account, the Germans were greenhorns, and did not know the habits of gold to sink to the lowest levels of bedrock in a gulch, due to the forces of erosion and gravity. In response to their earnest, repeated (and annoying) requests to the more experienced Confederate boys for directions to "the good claims", they were told (with a wave of the hand at the sides of the gulch) to "go up yonder". According to legend, they dutifully went "up yonder" and discovered the Montana Bar.
History of gold production in Confederate Gulch after the seminal Montana Bar strike of 1865
Rich strikes on Confederate Gulch, and its tributaries—at Boulder Bar, Diamond Bar, Gold Hill, Cement Gulch, Montana Gulch, and Greenhorn Gulch
The discovery of the fabulous Montana Bar immediately generated frantic prospecting throughout Confederate Gulch and its tributaries. This rapidly led to a multitude of strikes.
Rich finds were developed along Confederate Gulch proper. Two miles up Confederate Gulch, claims in Cement Gulch proved very rich and productive. Prospecting up Montana Gulch new discoveries were made. Good placer deposits were found along Greenhorn Gulch and Boulder Gulch.
The Montana Bar strike motivated prospectors to prospect the sides of Confederate Gulch mining district. Gold is heavy, and the sorting process from water and glacier flow usually results in concentrations of gold down on bedrock along the gulch bottom. Confederate Gulch was the exception. Some of the richest gold concentrations were found in benches of gravel along the hillsides.
On the same hillside level as the Montana Bar the Diamond Bar was discovered. It was as rich in yield per acre as the Montana Bar, though not as extensive. Gold Hill and other gravel shelves at the same level along the gulch and its tributatries yielded good gold production.
The Boulder Bars were in Boulder Gulch. These benches rested on shelves of bedrock. They posed a special problem. The surface of these hillside benches were littered with large boulders even though underneath were well sorted stream gravels with streaks and pockets of gold. The underlying gravels were hard to work because the surface boulders settled in heaps as the underlying lighter gravel was carted away or washed away by hydraulic methods.
Within a few months after the Montana Bar strike of 1865 Confederate Gulch and its tributaries were an antihill of activity with gold miners swarming over the ground, digging and working on their claims.
Gold production 1866 to 1869
For a few years Confederate Gulch boomed. From 1866 to 1869, Confederate Gulch probably equaled or outstripped other Montana Camps in gold production, chiefly because (a) the gold was course and easy to get at, (b) water was close and (c) gradients were favorable to create sluice currents and dump disposal. These conditions also allowed the transition from simpler placer operations to more efficient hydraulic mining.
The initial strike on Montana Bar set records for gold production. The best of the 200-foot-wide (61 m) claims along the shelf yielded $180,000.00, or about $900 per running foot of width. The total production from the Montana Bar alone is estimated at $1 million to $1.5 million.
Confederate Gulch proper was mined for a distance of five miles (8 km). When properly worked the Confederate Gulch claims were all rich. The rich stretches along the bottom of the Gulch were very rich. The gold production ran from $100.00 to $500.00 per running foot, and produced $20,000 to $100,000 per claim.
Cement Gulch and Montana Gulch were highly productive, but Cement Gulch was in a class by itself. Some of the claims in Confederate Gulch were true bonanzas. They produced more gold than comparable claims of the fabulous Montana Bar, though requiring movement of a much larger tonnage of gravel, boulders and dirt.
No one knows how much gold was taken from the Boulder Bars. Because of the boulders strewn across the surface of the bars, they were worked by many different operators, some mere pocket hunters and others operating with teams of men and equipment.
The gold production of Confederate Gulch created massive gold shipments from the gulch, starting with the spectacular production of Montana Bar. A single shipment of gold in 1866, representing a short run of gold bearing gravel through the sluice boxes weighed two tons and was valued at $900,000.00. In the late 1860s two and a half tons of gold were produced in a final clean up of the sluice boxes.
In September 1866 the steamboat Luella piloted by Captain Grant Marsh took 230 miners back down the Missouri River to the states. Between the gold carried by individual miners and consigned gold shipments, the Luella had a cumulative two and a half tons of gold on board, conservatively valued at $1,250,000. This was the richest cargo ever carried down the Missouri River by steamboat. The bulk of this gold reputedly represented production in 1866 from the Confederate Gulch area.
There are varying estimates of the total gold production from the Confederate Gulch Mining District during the boom years—1866 to 1869. The estimates run from $16 million to an estimate of $10 to $30 million. These estimates could fall far short of the total gold volume that was actually produced. The total production will never be known. Businesses which transported gold, as well as individual miners took out their gold secretly, in order to mislead highwaymen and prevent robbery.
All of the estimates of gold production are in 1860's dollars. In addition, this is when gold was worth less than $20 an ounce. Were the values of total production be stated in today's dollars, the figures would be much higher than the estimates.
A feature of Confederate Gulch is the abrupt jump into high production of gold in 1866, the continued intensity of the production through 1867 and 1868, and its abrupt end in 1869/70. Gold production from the Confederate Gulch mining district started at a high level in 1866 because of the sheer opulence of the Montana Bar strike. Production was maintained at a high level as numerous fresh strikes were made and brought on line. The intense utilization of hydraulic mining kept the production levels high from 1866 onward until the gold ran out in 1869/70.
Technical problems from 1866 to 1869
Along Confederate Gulch and on Cement Gulch the gold claims were rich, but they demanded a great deal of labor. There were large boulders mixed with gravel along the gulch bottoms. These boulders had to be moved. Cold water would flood the shafts and trenches. The hillside shelves, like Montana Bar and Diamond Bar were easier to mine, but even some of the hillside shelves had technical problems. Along the various Boulder Bars, the large boulders that littered the surface had to be drilled and blasted, or lifted and moved by rope tackle. These were dangerous projects.
Hydraulic mining in Confederate Gulch
Confederate Gulch saw large scale hydraulic mining. Hydraulic mining methods in Confederate Gulch used the force of water to wash down banks of gravel bars and terraces located on the sides of the gulches, as well as the beds of gravel on the gulch floor. The earth and fine gravel was then flushed through sluice boxes where the heavier gold was extracted from the lighter gravel.
Hydraulic mining was particularly applicable in Confederate Gulch because gold bearing gravels lay on terraces high up on the hillsides above the gulch. In addition, the water sources and gradients supported the development of hydraulic mining.
Water from sources high up the gulch were tapped and fed into flumes or ditches that ran along the sides of the gulch. The ditch/flume was kept at a much shallower gradient than the floor of the gulch. Eventually the water in the flumes and ditches was high above the mining sites down on the floor of the gulch. The water was then released from the high ditch down through several hundred feet of pipe, and emerged through huge nozzles that resembled small cannon. The massive jets of water from these nozzles reputedly had such force that they could smash down a brick building in one pass. The most powerful hydraulic hoses required six men to control.
Building the ditches and flumes that hydraulic methods required large amounts of capitol. This brought outside investors into the business of removing gold from the gulch. They wanted the quickest return possible on their investment and they encouraged unrestricted use of hydraulic methods.
The powerful jets of water used in hydraulic mining washed down whole hillsides and simply ate up the floor of the gulch. The dirt and fine gravel was then washed through the sluices, and the silt was carried off down the gulch. The gravel tailings produced by hydraulic mining were left behind as spoil banks, piled along the bottom of the gulch for long intervals. Hydraulic mining methods and the resulting spoil banks obliterated all the remains of the original Diamond City, as well as the other small communities in the gulches. Hydraulic mining was very damaging to the environment on the gulch. It changed the appearance, geography and ecosystem of Confederate Gulch.
Mining operations 1870 to the mid-1940s
From 1866 to 1869 the miners swarmed over the Confederate Gulch area and skimmed the cream as well as took the milk. They got it all, or most of all. Nothing after that—neither the placer mining operations or the lode mining operations even came close to the production in the boom years.
After 1870 some sporadic hydraulic operations continued in Confederate Gulch and its tributaries for many years. A company based in Milwaukee worked some old ground briefly in 1899. About nine years later, a company worked gravels in the lower end of the gulch using a Risdon dredge, but it shut down operations after three months when it found no values in the gravels. Placering continued off and on during the late 1910s and 1920s, with at least two operations in 1928; lack of water frequently hampered success.
Gold activity often works inversely to economic health. In the booming 1920's mining activity fell off. As a worldwide depression developed after 1928, gold production increased. The federal government moved to establish the price of gold, which rose to about $35.00 per ounce. The increased price of gold, combined with lower wages and material costs prevailing during the Depression, caused gold mining to become attractive again.
Dredging companies moved into Confederate Gulch in a big way in the 1930s, using power shovels and a variety of other equipment, including a stationary washing plant, dry-land dredge, and drag-line dredge. The best returns came in 1939 when two dredging operations recovered 2,357 fine ounces of gold. One company had 16 to 18 men on the payroll that season. A single dry-land dredge worked the ground in 1942, after which operations shut down for the duration of World War II.
The reported 1939 year's production of 2,357 ounces of gold was worth $82,495.00 at the then current price of $35.00 per ounce. This is but a small patch on the boom days of 1866 to 1869, when tons of gold were produced yearly from Confederate Gulch, and one week on the legendary Montana Bar produced $115,000.00 of gold at under $20.00 per ounce.
Lode mining in Confederate Gulch - the search for the mother lode
Even before the placer deposits began to run out, miners were combing the Big Belts for the "mother lode"—that is, the rich emplacement of gold in bedrock which had, through erosion, produced all the placer gold found in the Confederate Gulch gravels. No rich "mother lode" was ever found. The general theory is that the mother lode was consumed by erosion and the gold was distributed into the gravels that lay along the sides and bottom of Confederate Gulch and adjacent gulches in the Big Belt Mountains.
Though no mother lode was found, there were some lode operations in the Confederate Gulch district but they never measured up to the standard set by the rich placer mines. The most important mines, including the Hummingbird, Slim Jim, Schabert, Baker Group, and Three Sisters, are all located along the divide between Confederate Gulch and White Creek, principally on Miller Mountain. Lode mines produced only $100,000 in gold, while the placers of Confederate Gulch yielded this sum one hundred and fifty times over. The Philadelphia Mill, with a capacity of 15 tons per day, operated briefly at Diamond City around 1889.
Diamond City: "The Most Spectacular of Montana's Boom and Bust Gold Towns"
Confederate Gulch and Diamond City were transformed by the discovery of the amazing Montana Bar, followed closely by the discovery of the almost equally astounding Diamond Bar. Gold was being generated and shipped in record volumes. Word flashed across the territory and miners poured into the diggings.
From a small collection of cabins and shacks Diamond City was instantly transformed into a crowded boom town that roared along both night and day. Satellite communities sprouted up on the Gulch—El Dorado, Boulder, Jim Town, and Cement Gulch City. At the crest of the boom ten thousand people lived and worked in Confederate Gulch, but Diamond City dominated the area, and when Meagher County was formed Diamond City was named the county seat.
Between 1866 and 1869, when Diamond City and Confederate Gulch had ten thousand people grubbing for gold, federal estimates put Montana's total population at twenty eight thousand. In these years, roughly 35% of Montana's population was working in Confederate Gulch.
Placer gold discoveries, like Confederate Gulch, attracted a diverse and cosmopolitan population. While many came from the Midwest and border states like Missouri, many also came from mining areas in California, Idaho and Nevada. Because they moved about so constantly, they cared little about background or status. The use of casual nicknames predominated over proper names. A roster of Confederate Gulch citizens could include names like Wild Goose Bill, Black Jack, Nubbins, Roachy, Steady Tom, Workhorse George, Dirty Mary, Whiskey Mike, and Lonesome Larry.
Placer gold strikes were "poor man's diggings". Placer gold is formed by erosion forces which slowly break down gold veins embedded in bed rock and over geologic time leave the gold in the gravels and sands of ancient or presently flowing river beds. The gold is in a natural state in the form of gold dust, flakes or nuggets. Such deposits required no special processing, except the hard grueling work to dig out and sort through tons of gravel, dirt, sand and boulders. Newly discovered deposits like Confederate Gulch attracted young footloose men, motivated by a desire to get rich quickly.
Towns that sprang up at placer gold strikes were jerry built, ephemeral and hectic places and Diamond City and the other Confederate Gulch communities were no exception. As long as gold was produced they boomed along. When the mining stopped, the prospectors left as suddenly as they came.
During the boom years, Diamond City seethed with excitement and activity. It provided entertainment and commercial goods for the miners and for the crews that labored night and day to build a 7-mile-long (11 km) ditch/flume for hydraulic work. When the ditch/flume was completed, full scale hydraulic mining began. At the height of the mining activity, between 1866 and 1869, hydraulic mining led to the displacement of Diamond City. The approaching hydraulic mining undercut the town, and spoil banks began to pile up against buildings. The merchants first propped their buildings on stilts. Eventually the stilts reached fifteen feet, and finally the town was simply removed to a nearby location in Confederate Gulch where it roared on with business as usual. Meanwhile the hydraulic mining process ate its way through the former town site.
Mining production from 1866 through 1869 was intense—the rich deposits encouraged quick exploitation, and the shift to hydraulic mining kept production in high gear. This led to record production, but it also shortened the life expectancy of the community. In 1869 and 1870 the gold ran out and so did the population. They simply picked up and left. By 1870 the population of Diamond city was down to 225 people, and a year later only about 64 people remained; by the 1880s 4 families were left.
From nothing in 1864, and from a few cabins in 1865, Diamond City became the county seat of Meagher County and the center of most populous camp in Montana in 1866. Diamond City boomed along for 3 years until 1869. Then the party was over, almost everyone left and Diamond City sank not just into obscurity but into oblivion. Unlike other boom-bust areas, Diamond City did not even remain as a picturesque ghost town. The rapacious search for gold consumed Diamond City, and hardly a trace now remains. Reflecting this meteoric rise and fall, Diamond City has been aptly described as "the most spectacular of Montana's boom and bust gold towns" by the authoritative text, "Montana: A History of Two Centuries", by Michael P. Malone, Richard B. Roeder, William L. Lang, 1991, University of Washington Press, p. 67.
The geology of Confederate Gulch
Confederate Gulch is considered a separate mining district. The district includes the length of the gulch, along with the upper tributaries of Boulder Creek, Montana Gulch, and Cement Gulch.".
The principal rocks underlying the placer gold deposits of the Confederate Gulch district are the shales of the Spokane and Greyson formations, as well as limestones of the Newland formation. These are cut by diorite and quartz diorite dikes, stocks, and sills. Narrow quartz veins, found along fractures in the diorite and along bedding planes in the shale, contain most of the high grade gold ore. Ore values decrease with depth, and few mines have been developed deeper than 150 feet. In addition to the quartz veins in the shales, the diorite contains "low grade mineralized shear zones".
These Spokane, Greyson and Newland formations have been uniformly considered to be in the Middle Proterozoic Belt Supergroup. In this classification these formations would be much older than the overlying Flathead sandstone from the Middle Cambrian Period, and the division between the older Proterozoic rocks, and the newer Cambrian rocks was considered to be a significant disconformity. New field work in the Big Belt Mountains, suggests that some rocks mapped as the Spokane Formation are conformable with overlying Middle Cambrian strata, and are not part of the Middle Proterozoic Belt Supergroup, but are part of strata that may be younger Late Neoproterozoic.
The rich placer gravels of the drainages were deposited during the interglacial stages of the Pleistocene epoch. Confirmation of concentration of the placer gold deposits in relatively recent times is indicated by the bones of mastodons and elephants that were dug out of the gravels.
The distribution of the placer gold concentrations suggests that the common source of most of the placer gold in Confederate Gulch and White Creek was a series of quartz lodes on Miller Mountain on the divide between the two drainages. These gold bearing quartz lodes were consumed by the erosion that produced the placer gold deposits in Confederate and White Gulch.
Confederate Gulch in the present
Today a passable but unimproved road goes up the gulch from Townsend and over the crest of the Big Belts from the Missouri River to the Smith River Valley. In the winter the road is closed by snow. In the summer individual gold prospectors can still be seen, trying their luck up and down the gulch. They dig on the sides of the gulch and bring the gravels down to the stream.
Confederate Gulch is unlike other boom and bust mining districts in Montana, because no ghost town was left at the site. The hydraulic mining during the boom years, and the reworking of the site since has obliterated the sites of the earlier mining communities. Along the bottom of the gulch are spoil banks overgrown with brush. Occasional pieces of timber appear in these areas to show that once there were towns and buildings in the gulch.
One thing alone remains. On a cliff overlooking the Confederate Gulch and Boulder Gulch from the south is the graveyard for Diamond City and Confederate Gulch. About 65 people are reportedly buried there. This site is marked on Wikimapia.
Visiting Confederate Gulch
Confederate Gulch runs out of western slopes of the Big Belt Mountains to the lake that is formed behind the Canyon Ferry Dam. The dam and lake are part of the Missouri River drainage. Across the Missouri River valley from the Big Belts are Townsend and U.S. Highways 12 and 284.
One can drive to and through Confederate Gulch. Go east on U.S. Highway 12 from Townsend for about 3 miles (4.8 km). Turn north on Montana county road 284. After about 16 miles (26 km) a dirt road goes up Confederate Gulch. In good weather this road can be followed over the Big Belts into the Smith River valley where improved roads lead on to White Sulphur Springs, Montana. It would be best to travel in a vehicle with high clearance, but the grades do not require four wheel drive. Do not try this road in winter or in bad weather.
- Sterling Price
- Alfred Pleasonton
- Thomas Francis Meagher
- Fort Benton, Montana
- Helena, Montana
- Virginia City, Montana
- Alder Gulch
- Big Belt Mountains
- Placer mining
- Gold prospecting
- Gold Prospectors Association of America
- Gold Rush
- The Gold Frontier, Dan Cushman, Stay Away Joe Publishers, 1973, pp. 172–179.
- The "color" referred to is the heavy black mineral Magnetite, which is more common than gold, and is often associated with gold, so it is used as an indicator or marker of potential gold strikes.
- Roadside History of Montana, Don Spritzer, Montana Press Publishing Company, Missoula, Montana, 1999, ISBN 0-87842-395-8, p. 252.
- "Roadside Geology of Montana", David Alt, and Donald W. Hyndman, Mountain Press Publishing Company, Missoula, 1986, 1990, ISBN 0-87842-202-1 (pbk), pp. 276, 277, 296.
- "Montana: A History of Two Centuries" By Michael P. Malone, Richard B. Roeder, William L. Lang, 1991, University of Washington Press, ISBN 0-295-97129-0, pp. 67, 68, 71. Can be accessed at Google Books 
- Pardee, Joseph Thomas and F. C. Schrader, 1933 "Metalliferous Deposits of the Greater Helena Mining Region, Montana", U. S. Geological Survey Bulletin #842, reprint of article in Mining Truth, Vol. 14, No. 10, cited by Montana Department of Environmental Quality Report on Confederate Gulch Mining District .
- "Conquest of the Missouri", Joseph Mills Hanson, 1909, A.C.McClurg and Co., p. 80-88.
- U.S. Department of Interior, Bureau of Land Management website for Upper Missouri Breaks National Monument, with sub site on Missouri Breaks History 
- Fort Benton Blog
- Lyden, Charles J., 1948 The Gold Placers of Montana. Memoir No. 26. Montana Bureau of Mines and Geology, Butte, Montana; Calderhead, J. H., and Oliver M. Holmes, 1900 Seventh Report of the Bureau of Agriculture, Labor, and Industry of the State of Montana for the Year Ending November 30, 1900;Work Projects Administration (WPA), Mineral Resources Survey, 1940 Directory of Montana Mining Properties. Memoir No. 20. Montana School of Mines, Butte, cited by Montana Department of Environmental Quality Report on Confederate Gulch Mining District 
- Lyden, Charles J., 1948 The Gold Placers of Montana. Memoir No. 26. Montana Bureau of Mines and Geology, Butte, Montana; Work Projects Administration (WPA), Mineral Resources Survey, 1940 Directory of Montana Mining Properties. Memoir No. 20. Montana School of Mines, Butte, cited by Montana Department of Environmental Quality Report on Confederate Gulch Mining District 
- Sahinen, Uuno Mathias.\, 1935 Mining Districts of Montana. Unpublished Master's thesis, Department of Geology, Montana School of Mines, Butte; Pardee, Joseph Thomas and F. C. Schrader, 1933 "Metalliferous Deposits of the Greater Helena Mining Region, Montana", U. S. Geological Survey Bulletin #842, reprint of article in Mining Truth, Vol. 14, No. 10; Swallow, G. C. and J. B. Trevarthen, 1889 Reports of the Inspector of Mines and Deputy Inspector of Mines for the Six Months Ending November 30, 1888. Journal Publishing Company, Helena. 1890 Reports of the Inspector of Mines and Deputy Inspector of Mines for the Six Months Ending November 30th, 1889. Journal Publishing Company, Helena, cited by Montana Department of Environmental Quality Report on Confederate Gulch Mining District 
- "Montana, A State Guide Book" Federal Writers' Project, American Guide Series, Hastings House, New York, 1939, reprinted 1955, p. 219
- Wolle, Muriel Sibell, "1963 Montana Pay Dirt: A Guide to the Mining Camps of the Treasure State", Sage Books, Denver; Pardee, Joseph Thomas and F. C. Schrader, 1933 "Metalliferous Deposits of the Greater Helena Mining Region, Montana", U. S. Geological Survey Bulletin #842, reprint of article in Mining Truth, Vol. 14, No. 10, cited by Montana Department of Environmental Quality Report on Confederate Gulch Mining District 
- Lyden, Charles J., 1948 The Gold Placers of Montana. Memoir No. 26. Montana Bureau of Mines and Geology, Butte, Montana, cited in Montana Department of Environmental Quality Report on Confederate Gulch Mining District 
- Sahinen, Uuno Mathias, 1935 Mining Districts of Montana. Unpublished Master's thesis, Department of Geology, Montana School of Mines, Butte; Pardee, Joseph Thomas and F. C. Schrader, 1933 "Metalliferous Deposits of the Greater Helena Mining Region, Montana", U. S. Geological Survey Bulletin #842, reprint of article in Mining Truth, Vol. 14, No. 10; Reed, Glenn C., 1951 Mines and Mineral Deposits (Except Fuels), Broadwater County, Mont. Information Circular 7592. United States Department of the Interior, Bureau of Mines), cited by Montana Department of Environmental Quality Report on Confederate Gulch .
- DETRITAL ZIRCON EVIDENCE REQUIRES REVISION OF BELT STRATIGRAPHY IN SOUTHWESTERN MONTANA, BALGORD, Elizabeth, MAHONEY, J. Brian, Department of Geology, GINGRAS, Murray K., 2009 Portland GSA Annual Meeting (18–21 October 2009), Paper No. 232-1
- Montana Department of Environmental Quality Report on Confederate Gulch Mining District  citing Pardee, Joseph Thomas and F. C. Schrader, 1933 "Metalliferous Deposits of the Greater Helena Mining Region, Montana", U. S. Geological Survey Bulletin #842, reprint of article in Mining Truth, Vol. 14, No. 10, and Reed, Glenn C. 1951 Mines and Mineral Deposits (Except Fuels), Broadwater County, Mont. Information Circular 7592. United States Department of the Interior, Bureau of Mines.
- Broadwater County Cemeteries
- Wikimapia Confederate Gulch Graveyard
- "Montana Atlas and Gazetteer", DeLorme, 2001, Plates 40 and 56.
- Department of Environmental Quality, State of Montana, Report on the Confederate Gulch Mining District.
- "Montana, a Tale of Two Centuries" Google book results
- Confederate Gulch, Diamond City and the Montana Bar in Wikimapia
- MTLinks Diamond City
- Western Mining History, Broadwater County, Gold Production