Feeds:
Posts
Comments

Posts Tagged ‘mines’

mining terms

Mining terminology, at the Creede Underground Mining Museum

As mentioned in my last post, I am embarking on a two-week tour of Colorado mining towns. Before I go, there are some basic mining terms that any greenhorn or tenderfoot like me should know before venturing into a mine. Many of these terms come from the Cornish miners who came to America to work when the tin mines in Cornwall played out in the 1800’s.

First, the basic parts of a mine: you always refer to a mine as if you are facing into it. The part of the mine you are working to drill, load, and blast is called the “face.” The left-side wall is the “left rib” and the right-side wall is the “right rib.” The ceiling is the “back” and the floor is the “foot.” The back is also called the “hanging wall” and the floor the “foot wall” depending on the orientation of the ore vein.

Ore body diagram

Diagram of the original ore body.

A “tunnel” is horizontal and must see daylight at both ends. If it only opens to the outside on one end, it is called an “adit.” If it doesn’t connect to the outside at all, it is a “level.” Levels are like the various floors of a building, only underground in a mine, and they provide access to the ore body. A vertical hole that connects with the surface is a “shaft.” If it is a hole that is dug down from a level or an adit, it is a “winze,” and if it is dug upward it is a “raise.” A hole dug to follow a vein horizontally away from a level or an adit is called a “drift” and to dig out a large ore body going up or down is called a “stope.”

The valuable mineral that you are trying to dig out is the “ore,” along with useless rock called “tailings.” Usually the ore is injected as a hydrothermal body along a fault or other natural zone of weakness in the rock, and the entire mineralized zone is called the “ore body” or “lode.” If it is found as a large vertical mass with branches, it is an “ore chimney” and if it is a thin line following any direction it is a “vein.” Sometimes ore is found as crystals deposited along the walls of a natural chamber. This is called a “vug.” When a vein reaches the surface, it is an “outcrop,” and when parts of the outcrop erode away and are carried down into river valleys by water, avalanches, and gravity it will pile up in still areas of the stream, such as the inner parts of meanders along with gravel. These are called “placer” deposits (pronounced “plah-cer” and not “play-cer”).

exploratory mining

Prospectors mine the placers and conduct exploratory mining

The first miners in a new mining district are prospectors, because they are looking to find, develop, and sell a good “prospect.” Typically the first discoveries are placer deposits, because they are easy to find and work using pans, rockers, and sluices. Once the placers are played out, the prospectors head upslope to find the source outcroppings, or the “Mother Lode.” Once they find evidence of ore (such as associated minerals like iron pyrite or chalcopyrite, quartz, etc.) they will “stake a claim” by pounding stakes in the corners of the land and starting to dig exploratory shafts or adits using hand tools such as picks and shovels. They will use a windlass to haul the “muck” or loose rock out of a developing shaft with a bucket. Claims have to be an allowed size (a long, thin swath of land) and registered in the county mine office to be legal. It’s good to set up with a partner so that when one of you leaves to register a claim, the other can guard it from “claim jumpers.”

Samples of the ore are taken to an “assay” office where they are analyzed chemically to see how much valuable metals are actually in the ore. If the ore is rich, or “high grade” or if the vein widens and appears to continue, the prospector will usually sell out to a mining company with the resources and capital needed to further develop the mine.

Once the mining company buys out the prospectors, it starts to build the infrastructure needed to enlarge the mine. The irregular prospector shafts and adits are enlarged and shored up with timbers. The top of a shaft is boxed in with a “collar” and an adit’s entrance is shored up and extended outward to prevent loose rock from falling into it. This becomes a “portal.” At the top of a shaft, a “headframe” or “gallows frame” is erected out of large timbers or steel with pulleys called “sheave wheels” at the top. A braided rope or cable is brought over the sheave wheel and attached to a metal cage called a “skip” which can carry men or ore buckets in and out of the shaft. The other end of the cable is brought to a “hoist,” which is an electric or diesel winch. As the skip is raised and lowered in the mine, a series of electric bell chimes are used to signal the “hoistman” how far to raise and lower the skip. A mark on the cable tells the hoistman when the skip is “on the level.”

mine expands

After a mining company buys the prospect, it expands the mine and adds infrastructure

As the mine deepens, it will usually encounter underground aquifers or water tables which become a major problem as they start to flood the lower mine shafts. The main shaft must be dug lower than the lowest level and a pump installed to remove the water. This low-lying shaft is called a “sump” and the pumps used ran on steam, diesel, electricity, or compressed air. The biggest of these were the famous Cornish pumps found in some mines.

Eventually the shafts are too deep to economically raise all ore cars, sump water, and men to the top of the shaft. A drainage and ore removal adit is sometimes dug at the bottom of the mine that will drain out the waste water and allow easy passage of ore cars out of the side of the mountain. These adits usually have a slight downward slope to the outside so the loaded ore cars can be more easily moved. Waste rock was simply dumped out of the shaft or portal and created a “tailings pile” downslope from the mine or mill.

integrated mine

Integrated mine and mill. As the mine develops, drainage adits, interior shafts, reduction mills, smelters, and other structures are built.

As the mine gets bigger, with additional levels every 100 feet and a complex set of drifts, adits, winzes, raises, interior shafts, stopes, etc. it becomes advantageous for the owners to build their own mill instead of sending their ore elsewhere for processing. A mill is built on the side of the mountain below the lowest portal. It first sorts, then pulverizes the ore into powder, then concentrates the ore mechanically or chemically. The concentrate is then shipped by rail to a smelter for final processing and purification. Sometimes the concentrated ore is heated in a retort or furnace but not separated into its final constituent metals. This combination of metals is poured into bar-shaped or cone-shaped molds and cooled, creating “dore bars” or “buttons” which contain gold, silver, and other metals.

Once the mine is exhausted of ore, or the shaft extends down below where it can be economically drained of groundwater, or the price of the final metal drops so the mine can no longer turn a profit, it is closed down (sometimes temporarily). Today, mines have to post bonds that force them to reclaim the mine and make it safe once mining has concluded. But in the old west, the mines simply shut down and left everything where it was. Tailings piles are the most obvious evidence of mining, and the rocks are often stained a yellow, orange, or reddish brown color from iron sulfides and sulfates. Rotting timbers poke from the ground, and rusted metal scraps adorn the slopes. Drainage water still seeps from adits, often contaminated with metals or other effluents. And the shafts and portals remain, too often a temptation for the unwise to explore. A few people die each year from cave ins while exploring old mines, or get killed by handling old dynamite left in mines. In some states, such as Utah, a concerted effort is underway to close all of these abandoned mines in the name of public safety but at the expense of history. Other states, such as Colorado, seem to strike a better balance between history and safety.

Mining terms B

More mining vocabulary terms. From the Creede Underground Mining Museum.

Now there are many more terms, such as how a typical miner spends his shift to drill, load, shoot, and muck the face. We’ll talk about these later as they come up on my journey. I’m amazed at how many mining terms have made it into general vocabulary, such as “big shot” [blasting out a large section of the face], “hang-up” [when ore is blasted to fall into a lower chute but gets stuck], “getting the shaft” [to buy a worthless mine], etc. For better or worse, hard-rock mining has had a big impact on our history and our culture.

Read Full Post »

Loading chute at Dividend Utah

Ruins at Dividend, Utah

The last few weeks I’ve had to neglect the Elements Unearthed project in order to finish a client video that had a tight deadline. It was uploaded to YouTube Thursday night, so I now have a little bit of a breather before the next project and am back at work on Part 2 of the beryllium video. Winter has finally decided to let go (after one last gasp – we had a snowstorm here just two weeks ago), and already the early summer heat is drying out the cheat grass and turning it a brownish-purple color on the lower south-facing slopes. I decided now was the time to do some exploring and photography while the grass is still green in the mountains.

Belt wheels and Mt. Nebo

Belt Wheels and Mt. Nebo

Over the last two years I’ve visited the Tintic Mining District several times with students and my own children and have collected a considerable amount of photos and video clips, including a tour of the Tintic Mining Museum and an interview with June McNulty, who runs the museum with his wife. But there were several places in the district that I hadn’t visited, including Mammoth and Silver City. So yesterday (Friday, June 4) I packed up the cameras and headed for the hills.

Glory hole at Dividend

Glory hole at Dividend, Utah

Change room stove at Dividend

Change room and stove at Dividend, Utah

I stopped first in the hills above Burgin, the site of the town of Dividend, so called because the mine paid out fairly decent dividends to the miners compared with other mines in the district. I decided to climb up the hill further than before, toward the two large rusty tanks that can be seen from the road. I was surprised to find much more there than I had known about before, including the ruins of miner’s houses (some semi-wild purple irises and lilacs were still alive and blooming). A processing plant once existed here, and the ground is covered with yellowish-stained rocks and pieces of slag and everything smells of sulfides. One ruin 2/3 up the hill still has an old rusted stove for keeping the miners warm in what was probably the change room – the mine portal itself is just above the room, and there are even a few remains of timecards used to clock in and out of the mine. The few I looked at were dated from 1971, which was about the time that the mine at Dividend finally closed down. Mining continued, periodically, further down the slope at Burgin. Almost forty years of weather has taken its toll; all the roofs and any other wooden structures have long since rotted away, leaving old, dry fragments of boards with rusted nails sticking out littering the ground. Most of the equipment is gone, taken by looters and souvenir hunters, but enough of the foundations and structures remain that one can imagine what Dividend looked like in its heyday.

Wild irises at Dividend

Wild irises at Dividend, Utah

The road past Dividend is off the main path of Highway 6. It’s a good road, well maintained and asphalted but not much visited. I only saw two other cars and a motorcycle during the four hours I spent exploring along the road. The East Tintic Mountains between Dividend and Eureka are dotted with old mining ruins and tailings piles, with dirt roads leading off frequently up every side canyon and ridgeline. Most of the area is posted No Trespassing, so I limited myself to taking photos from the main road. It is still late spring up there; the maple trees in the canyons have only just gotten their leaves, and wildflowers including mountain lupine and Indian paintbrush cover the hillsides.

Indian paintbrush

Indian paintbrush near Eureka, Utah

Blue Lupine

Blue Lupine near Eureka, Utah

I traveled through Eureka and saw the continuing cleanup efforts there (more on this in my next post) and drove on to the town of Mammoth. Located in a side box canyon just to the south of Eureka, this was one of the richest areas of the Tintic Mining District. The mines are located ringing the valley – many long since abandoned but several showing recent work. With prices for gold and silver high right now, much exploration is underway to re-work the old claims and tailings piles and to do new exploratory drilling. Again, most of the area is posted and is private property; I limited myself to the main streets of Mammoth to photograph the old buildings and mine dumps.

Mine at Mammoth Utah

Mine at Mammoth, Utah

At one time, when the processing plant was in full operation in the early 1900s, Mammoth boasted a population of about 2000. The people lived in the upper eastern portion of the canyon (Upper Mammoth) while the mill was at the mouth of the canyon lower down the slope (called Robinson after the mill’s foreman and later Lower Mammoth). Once the town was incorporated, public works such as churches and even a hospital (rare for a mining town) were built in the middle, or Midtown. In the early 1930s, my father used to visit his first cousin Ralph Larsen, whose family lived in Mammoth. During the winter the road leading up to town would be covered in packed snow, and the two of them would ride their sleds from Upper Mammoth all the way down to Highway 6, almost two miles, without ever stopping. Then they’d have to wait for someone to give them a lift back to the top.

Miner's shack in Mammoth Utah

Miner's Shack in Mammoth, Utah

Even though the mines had all closed by the 1950s, Mammoth somehow escaped the fate of most boom-and-bust mining towns; it never completely died. A few people hung on. Over the last ten years, since I last drove up here, it even appears to have grown in population. More houses have been fixed up and are occupied than before, and it is becoming an artistic community of sorts. Renewed interest in mining has also given the town a boost.

Lizard

Lizard in the ruins at Dividend, Utah

After Mammoth, I visited the old Jesse Knight smelter at Silver City and drove up the canyon there, but I’ll leave that for next time.

Read Full Post »