Кеннекотт: Заброшенный горнодобывающий лагерь на Аляске

Kennecott, also known as Kennicott and Kennecott Mines, is an abandoned mining camp in the Copper River Census Area in the U. S. state of Alaska that was the center of activity for several copper mines. It is located beside the Kennicott Glacier, northeast of Valdez, inside Wrangell St. Elias National Park and Preserve. The camp and mines are now a National Historic Landmark District administered by the National Park Service. It was declared a National Historic Landmark in 1986.

In the summer of 1900, two prospectors, "Tarantula" Jack Smith and Clarence L. Warner, a group of prospectors associated with the McClellan party, spotted "a green patch far above them in an improbable location for a grass green meadow." The green turned out to be malachite, located with chalcocite (aka "copper glance"), and the location of the Bonanza claim. A few days later, Arthur Coe Spencer, U. S. Geological Survey geologist independently found chalcocite at the same location, but was too late to stake any valuable claims. Stephen Birch, a mining engineer just out of school, was in Alaska looking for investment opportunities in minerals. He had the financial backing of the Havemeyer Family, and another investor named James Ralph, from his days in New York. Birch spent the winter of 1901 1902 acquiring the "McClellan group's interests" for the Alaska Copper Company of Birch, Havemeyer, Ralph and Schultz, later to become the Alaska Copper and Coal Company. In the summer of 1901, he visited the property and "spent months mapping and sampling." He confirmed the Bonanza mine and surrounding by deposits were, at the time, the richest known concentration of copper in the world. Kennecott had five mines: Bonanza, Jumbo, Mother Lode, Erie and Glacier. Glacier, which is really an ore extension of the Bonanza, was an open pit mine and was only mined during the summer. Bonanza and Jumbo were on Bonanza Ridge about 3 mile (5 km) from Kennecott. The Mother Lode mine was located on the east side of the ridge from Kennecott. The Bonanza, Jumbo, Mother Lode and Erie mines were connected by tunnels. The Erie mine was perched on the northwest end of Bonanza Ridge overlooking Root Glacier about 3.7 mile (6 km) up a glacial trail from Kennecott. Ore was hoisted to Kennecott via the trams which head ended at Bonanza and Jumbo. From Kennecott the ore was hauled mostly in 140 pound sacks on steel flat cars to Cordova, 196 rail miles away, via the Copper River and Northwestern Railway (CRNW). In 1911 the first shipment of ore by train transpired. Before completion, the steamship Chittyna carried ore to the Abercrombie landing by Miles Glacier. Initial ore shipments contained "72 percent copper and 18 oz. of silver per ton." In 1938, Ernest Gruening proposed Kennecott be preserved as a National Park. A recommendation to President Franklin D. Roosevelt on January 18, 1940, for the establishment of the Kennecott National Monument went nowhere. However, December 2, 1980, saw the establishment of the Wrangell St. Elias National Park and Preserve.

Kennecott first reported on the 1920 U. S. Census as an unincorporated village. It appeared again in 1930 and 1940, and after its abandonment, it has not reported separately since. It is now within the McCarthy CDP.

Copper ore was discovered in a lode on Chief Nikolai's house at the mouth of Dan Creek in July 1899. The geological formations in the area were described and identified by a USGS geologist by the name of Oscar Rohn in 1899. This original copper find became the basis of the Nikolai Mine in 1900. Simultaneously, placer gold was discovered on the Dan and Young Creeks. The Bonanza ore body was discovered in Aug. 1900 by Warner and Smith. Almost simultaneously, another USGS geologist named Arthur Spencer, came across the ore when mapping the area with Frank Schrader. In 1901, the Dan Creek was staked by C. L. Warner and "Dan" L. Kain. Gold was found on Chititu Creek in April 1902 by Frank Kernan and Charles Koppus. Besides placer deposits, copper is found as polymetallic replacement deposits in the fault planes, fractures and joints of the Triassic Nikolai greenstone, which consists of basaltic lava flows, and in the base of the Upper Triassic Chitistone limestone. Minerals include chalcocite, bornite and chalcopyrite, with associated malachite, azurite and cuprite. Native copper can also be found in the greenstone.

Copper extraction was a many step process in an attempt to be as efficient as possible. Chalcocite and covellite were sent directly to the smelting plant in Tacoma. Malachite, azurite, and other forms of copper within the limestone needed separation in the 14 story mill building before shipment. The mill was mainly built between 1909 and 1923. Ore arrived at the mill via aerial tramways, where the high grade portion (approximately 60% copper) was crushed and placed in a chute to carry it directly to the bottom to be placed in burlap sacks. Lower grade ore was further crushed, sized and sorted. The denser ore was separated from the less dense waste via Hancock jigs and shaker tables. The tailings left over after gravity separation were further treated via ammonia leaching, for the coarse material, or via froth flotation for the fine material. The ammonia leaching plant was built in 1915, where ammonia liquefied the copper but kept the limestone in solid form. The ammonia copper solution was heated to drive off the ammonia, which left behind a copper oxide containing 75% copper. This was then sacked for shipment. The flotation plant was built in 1923 to process the "fines", which were less than 0.3 cm in size. These fines were mixed with water, oil, and buffering chemicals, before air was bubbled through the solution. Copper ore attached to the air bubbles, and floated to the top, where it was skimmed off, dried and sacked.

In the 1980s, Kennecott became a popular tourist destination, as people came to see the old mines and buildings. However, the town of Kennecott was never repopulated. Residents involved in the tourism industry often lived in nearby McCarthy or on private land in the surrounding area. The area was designated a National Historic Landmark in 1986 and the National Park Service acquired much of the land within the Kennecott Mill Town in 1998. Popular tourist activities while visiting Kennecott include glacier hiking, ice climbing, and touring the abandoned mill. Visitors may also hike to the abandoned Bonanza, Jumbo and Erie mines, all of which are strenuous full day hikes, with Erie Mine being a somewhat terrifying scramble along cliffs overlooking the Stairway Icefall. Local guide services offer all of these hikes if one would like some route finding assistance.

Kennecott is now accessible by air (McCarthy has a meter gravel runway) or by driving on the Edgerton Highway to the McCarthy Road, an unimproved gravel road. The McCarthy Road ends at the Kennicott River and a footbridge is available for pedestrian traffic to McCarthy. From McCarthy, it is 4.5 mile (7 km) to Kennecott, and shuttles are available.