Showing posts with label British Columbia. Show all posts
Showing posts with label British Columbia. Show all posts

04 December 2010

Minerals, Mining, and Water III: Gold Mining and the Columbia River

Tiffany Mountain (1980 m)
Okanogan County, Washington
©eop

It has been awhile since last I commented on mining, but today I came across several articles in various newspapers and other sources discussing mineral extraction in relation to water resources. A gold mine in Okanogan County, Washington has been a topic of concern for people in the Pacific Northwest for several years. The Canadian mining company operating the mine was recently fined by the State of Washington for filing false reports on water testing. Now that company wants to explore nearby areas for further mining activities, potentially profitable given the recent spikes in the price of gold. Draining into the Columbia River, the streams leading from the highland mining areas could bring arsenic, mercury and other toxic materials into the river. Water from the Columbia is used downstream for drinking water, for irrigation, and for recreation. While quite a distance away, the lower reaches of the river are also important salmon breeding areas.There is a fear of a toxic spill polluting that river in much the same way as smelter tailings and emissions at Trail, BC, just upstream on the Columbia, have contaminated nearby areas and Lake Roosevelt behind Grand Coulee Dam. There is an ongoing large-scale study of the contamination of the river by that smelter just across the international boundary. The Province of British Columbia is also conducting ongoing studies of contamination of air, water, and soil by the emissions from the smelter.


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05 August 2010

Petroleum, Pipelines and Water

Whittier Oil field, wells along property line of Central Oil company and Murphy Oil company. Looking east. Los Angeles County, California. 1905. Plate 13-A in U.S. Geological Survey. Bulletin 309. 1907.

My expectations of more oil flooding out of the breech in the Gulf seem to have been misplaced, and the ongoing process of sealing the well ("static kill" in the lingo of the trade) seems to be working. Moreover, we are told by the EPA that a large fraction of the oil that gushed from the breech has now dissipated. I hope the EPA statement is true, but I fear in the not too distant future oceanographers of various stripes will find it to have been an over rosy evaluation of what future environmental historians are likely to describe as one of the greatest ecological catastrophes since the beginning of the industrial revolution. Anyway, the effects of  the BP spill on fresh water were minimal, and its effects on food supply through the contamination of one of the most important source areas for seafood should be clearer before the food course begins in the Spring.

Petroleum is not out of the water supply picture, however, nor is it likely to be until the age of petroleum ends. A pipeline leak in Michigan has contaminated the Kalamazoo River, a stream flowing into Lake Michigan, the primary water source for Chicago, Milwaukee, and many smaller communities. The Enbridge Spill, named after the pipeline company operating the breeched pipe, has been estimated to have dumped more than 3,755,00 liters (1 million gallons) of crude oil  into the river, causing some nearby residents to be evacuated and restrictions to be placed on the use of the river for water supply and recreation. It is lucky that no nearby large town uses the river as its major source of water!

Enbridge Michigan Pipeline and Spill Location

The Enbridge spill has not, as far as we know, killed or even seriously injured anyone. In 1999 a rupture in a gasoline pipeline sent that flammable liquid downstream in Whatcom Creek in the city of Bellingham, Washington. Three youths were killed, two of them while playing with the matches that ignited an immense explosion. The third victim was a recent high school graduate celebrating the arrival of warm weather with a afternoon of fly fishing downstream from the Olympic Pipeline spill at Whatcom Falls Park, probably killed by the fumes before his body was incinerated by the fire. Whatcom Creek flows, partially underground, near the center of Bellingham enroute to Puget Sound. Gasoline entered the city's sewers, and there was a realistic fear that much of the picturesque center of Bellingham would explode in a huge fireball. A number of structures in Bellingham were damaged, and the pumping plant at a sewage treatment facility on Whatcom Creek was all but completely destroyed. Indeed the Bellingham area, often ranked as one of the most desirable places to live in the United States, has an unfortunate relationship to oil and oil pipelines. Earlier this year 7 workers were killed in an explosion at an oil refinery about 50 km away, and since the events of 1999 the city has been on edge each time a spill has been reported, including a large underground one in 2007. Facing one of the most beautiful but also one of the most heavily utilized portions of Puget Sound, the city is also acutely aware of the possibility of a maritime accident, including one in Canadian waters less than 100 km distant, though a May 2010 article in the major Vancouver, BC newspaper thinks tanker leakage is unlikely.

View of smoke from Whatcom Falls Gasoline Spill, 1999

The old axiom that oil and water do not mix has considerable resonance in any discussion of water supplies. Neither the Gulf nor the Bellingham spills directly impacted on the supply of fresh water, though the Bellingham spill and subsequent explosion and fire did destroy a sewage treatment facility. It seems only a matter of time until an oil pipeline passing across a stream breaks and renders the stream unfit for use in the water system of some large city or another. A break in a pipeline or other large spill involving the Ohio or the Mississippi could render water from those rivers unfit for consumption for hundreds of miles and would all but inevitably affect a large city.

[At home we are suffering a water supply problem! A leaking hot water tank and a malfunctioning shut off valve for that tank means the water to the house is shut off until the plumber can fix it later in the day. Hardly equivalent to even a tiny part of the suffering of that fifth or more of humanity who lack access to adequate water, but it does generate more sympathy for them.]

25 July 2010

Climate Change - Glacial Retreat

Receding glacier, Upper Joffre Lake, British Columbia, Canada
©EOP

Any discussion of world water supplies over the next century must take into account climate change or what is frequently termed "global warming." The scientific consensus has long since concluded that an increase in global temperatures of several degrees over the next century is nearly certain. The only remaining debate is on how great and how fast the warming will be. That is an important debate, but a little outside our purview. What is important is the impact of increased temperatures on world water supplies. The worst case scenarios for that issue are, to use a very bad pun, chilling indeed.

One early sign of the increase in global temperatures is the recession of glacial ice in the Northern Hemisphere and of mountain glaciers in tropical areas. Glaciers are an important part of the water supply equation as well as a key variable in world climates. Glacial ice acts as a natural reservoir helping to keep runoff in streams constant over the year and from wet years to dry ones. Many perennial streams would run dry for several months a year, and for several years in succession in a severe drought, were it not for glacial melt. Exotic rivers in North America and Asia depend on glacial melt for a sizable part of their flow. The disappearing glaciers of the Rockies are major suppliers of water to the great American Rivers of the west. As a sad example, Glacier National Park is rapidly loosing its namesake features and may have no glacial ice in less than a century. In the Coast Range of British Columbia many glaciers are rapidly melting, like the one feeding Joffre Lakes, one of the most stunning sets of glacial lakes in the world. Not long ago that glacier reached the water of the upper lake. Now the melting glacier is more than 100 meters higher than the lake surface.

Highland glaciers are found in several tropical areas where there is clear evidence of rapid melting. Much of highland tropical South America, including populated parts of Ecuador, Peru, and Bolivia, has permanent streams only because of the water released when glaciers in the high mountains melt. Urban water supplies and irrigation are dependent on that water, for the region is characterized by a division between a wet season and a dry season. There is disturbing evidence of glacial retreat in that area as there is in New Guinea. Kilimanjaro has one of the few glaciers in Africa, and the debate is not if the glacier will disappear but when with the best guess being in about 10 years.

Outside the tropics there is rapid glacial melting in the Himalaya. An unfortunate error in a major climate report concerning glacial melting in the Himalayas has been used as "evidence" by those opposed to the idea of global warming, persons who believe, against all evidence, that global warming is a myth being perpetrated by greedy scientists to get more research funding. The elected Attorney General of the antediluvian Commonwealth of ole Virginny is among those anti-scientific Luddites. Almost all of them are slavishly repeating the propaganda generated by the coal and petroleum industry, an industry which does not want to have any limits placed on coal and oil consumption, the major source of the most important greenhouse gas carbon dioxide. It is clear the glaciers are less important as sources of water in major Asian rivers than the report indicated, and the rate of melting is slower than the alarmist information in the report. But glacial melt in the world's highest mountains is crucial to the flow of the Indus and significant in several other streams. The retreat of those glaciers portends catastrophe in an area where water supplies are already seen as inadequate to meet increasing demands.


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