Anatomy of the Underground

Copper Falls Mill |

The adit we discovered at Copper Falls in only part of a much larger labyrinth of tunnels and shafts that comprise a Copper Country mine. The copper rich rock that mines sought were localized and concentrated into areas called lodes. Due to the geological forces that shaped the Keweenaw, copper bearing lodes were long and narrow strips of rock - running generally parallel to the shoreline. These lodes are only a couple hundred feet in thickness and extend for miles on a westward dip under Lake Superior. Because of this, mines in the Copper Country are generally very deep and narrow in structure.

this map of the Forest Mine near Rockland, shows all the components of a typical copper country mine. The long vertical line is a shaft, the horizontal lines drifts, and the short vertical line between drifts are winzes.

A mine’s structure can be easily mapped flat along the lode itself. Running along the dip of the lode are inclined shafts. These are deep holes running along the lode itself in which men and materials are transported. Branching off of these shafts are long tunnels running perpendicular to the shafts and along the lode from north to south. These are called drifts, and from these the major mining is done underground. Drifts were driven off of the shafts at regular intervals of depth (about 100 feet at the turn of the century), creating the levels of the mine. Drifts often connected two or more separate shafts along the lode, creating paths for air to enter and exit the mine readily.

As the region matured, shafts became further and further apart along a lode. This often resulted in distances of thousands of feet along drifts between shafts. To facilitate the movement of air underground and to allow for vertical movement of miners and equipment underground between these shafts, winzes were built. These were similar to shafts rising vertically between levels along the dip of a lode but never broke surface. They were usually smaller and more shallow then their shaft brethren, but often served the same purposes.

Underground at a typical copper country mine. Here we are looking down a drift as it intersects the shaft. The shaft is below the rock car and the workers, you can see the rails and stringers along it to the left for the shaft. It runs from the upper left of the picture (to the surface) towards the bottom right (further underground).

Another photo underground, same lode but different mine (the Tamarack). Here we look down a typical drift. Notice the angle of the roof timbers which follow the dip of the lode itself. The stope is to the right.

Copper Country mines usually were mines upward from the drifts - up into the lode from below. This facilitated the removal of waste rock and copper by the use of gravity. The large hallows from which copper and rock had been removed were called stopes. In some copper rich mines, stopes could reach cavernous proportions, sometimes reaching up to the level above. The ceiling along these stopes - called the hanging wall - could become highly unstable. Companies would leave pillars or rock along stopes as supports, or (in the case of C&H) use timber supports in a virtual underground forest to hold up the hanging wall.

a look into a open stope at C&H. The stope is still being mined, as you can see at the left. The stope follows the dip of the lode, running from the upper left of the photo to the lower right. The drift up from which this stope extends would be at the bottom right. The hanging wall at the top of the picture where you can get a glimpse of the “forest” used underground at C&H to hold the hanging wall up.

A map of the underground at C&H showing a close up view of a stope. The shaft on the right of the diagram was protected from collapse by a narrow column of rock known as a shaft pillar. Outside of the shaft pillar stoping of the copper rock proceeded, leaving large areas of open ground as shown here. This diagram does not represent a true vertical, but instead is drawn upon the surface of the lode itself. “UP” in the diagram would be a line intersecting the map at a 45 degree angle

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Been in Copper Falls mine. Lots of cool “archaeology”, if you will.

Mulder | July 24, 2008

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