Archive for Lovelock Cave

Composition Analysis of Michigan Copper

Michigan Copper in the Mediterranean,

The Shipping of Michigan Copper across the Atlantic in the Bronze Age


(Isle Royale and Keweenaw Peninsula, c. 2400BC-1200 BC)

J.S. Wakefield,


Photos coming soon for the article. Apologies from the AA staff.



Recent scientific literature has come to the conclusion that the major source of the copper that swept through the European Bronze Age after 2500 BC is unknown. However, these studies claim that the 10 tons of copper oxhide ingots recovered from the late Bronze Age (1300 BC) Uluburun shipwreck off the coast of Turkey was “extraordinarily pure” (more than 99.5% pure), and that it was not the product of smelting from ore. The oxhides are all brittle “blister copper”, with voids, slag bits, and oxides, created when the oxhides were made in multiple pourings outdoors over wood fires. Only Michigan Copper is of this purity, and it is known to have been mined in enormous quantities during the Bronze Age.


The Geology of Copper

Copper is said to be the most common metal on the face of the Earth with the exception of iron. However, most of it is in the form of low-grade ores that require a sequence of concentration mechanisms to upgrade it to exploitable ore through a series of proto-ores. Copper ores of the “oxidized type”, including the oxide cuprite, and carbonates (malachite) are generally green or blue, and reducible to copper metal by simple heating with charcoal. Ores of the “reduced type” are sulfides or sulfosalts (chalcocite, chalcopyrite, tetrahedrite), and are not readily identified in outcrops as ores; they require roasting to convert them to oxides, then reduction of the oxides to produce metal. There are a number of places in the world where copper can be found in small deposits in the pure state, but it is usually embedded in a rock matrix, from which it must be freed by intensive labor, or, today, crushed in huge volumes, and treated to obtain the metal.


The Unique Geology of Michigan Copper

Early in Earth’s history, there were huge volcanic outflows over the Great Lakes area. As new sediments overlaid these flows, copper solutions were crystallizing in the Precambrian flood basalts of the lava layers. The copper had been crystallized in nodules and irregular masses along fracture zones a few inches, to many feet wide. After a billion years, about a quarter of the age of the Earth, four major glaciations ground upon the edges of the old layered basalt lava beds, and exposed some of the embedded copper (Fig.2, top drawing). Isle Royale and the Keweenaw Peninsula remained high ridges of volcanic basalt. The scraping and digging by the glaciers, followed by surface exposure of the hardest material, the metal, was followed by sluicing of the land by glacial meltwaters. This left many mineral nodules of all sizes on the surface, in the huge pine forests. This was called “float copper”, as it appeared that it had “floated” to the surface. Nodules of copper were discovered shining in the surf along the shores of Isle Royale. The prolonged crystallization, followed by glacial exposure, was a unique sequence of events. When exploited, it took man from the stone age to an industrial world. The half billion pounds mined in prehistory were followed by six and a half billion pounds mined in the “industrial age” in America, starting in the late 1800s

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