Thirteen Mountain Months

Truly knowing a place might be a capacity only of the omniscient or for earthly beings, perhaps, something gained through multi-generational experience. Lacking omniscience, living in an area far from where I was raised, and having lived in my home only for a few years, I’m forced to make do as best I can. I’ll never know a place in its totality, but I’ve come to realize that I can get closer if I experience it in every season, which is how I found myself trekking to the top of Mount Chase, Maine during every month of the year. 

December 11, 2022 
The first trip in the journey and the most treacherous. Snow has yet to establish itself for the winter and ice covers many sections of trail. The summit is frosty. The hike down is much slower than the hike up.

A trail ascends through a thick forest. The trees are generally less than 6 inches in diameter and grow closely together. The trail is covered in ice like a steep stream that has frozen. About 30-40 feet of the trail is visible before it disappears at center.
Ice covers the Mount Chase Trail on Dec. 11, 2022.

View of forested landscape. Lightly frosted spruce and fir fill the foreground. A lake is visible at center in the lower elevation forest. A ridge of mountains forms the horizon at left center.
Looking west from the Mount Chase summit toward Upper Shin Pond, Sugarloaf Mountain, and Traveler Mountain.

January 8, 2023
With snow now covering the ice, the trip is far easier than last month and the snow is not yet thick enough that I have to ski to the trailhead. My trusty fat tire bike, Large Marge, gets me there. At the summit, visibility is exceptional and perhaps only limited on this day by the curvature of the Earth. On the way down, I hear a raspy-sounding chickadee. A boreal? Yes. I see it fluttering from branch to branch in the spruce-fir forest maybe 200 – 300 feet in elevation below the summit.

View from a mountain of a forested landscape. A ridge of large mountains form the horizon, although they appear small in the photo. Snow covered trees form the foreground just above windswept rock. Frozen ponds and forest sit in between the
The view to the west-southwest from the Mount Chase summit on Jan. 8, 2023. The mountains of Baxter State Park including Katahdin form the horizon.

A boreal chickadee perches in a frost covered dead spruce tree. The bird is at left center. It has a brown cap with is diagnostic of boreal chickadees.
A boreal chickadee perches in a dead spruce.

February 12
Peak winter. Minus 60˚ F wind chills during the week prior and low air temps approaching -30˚ F at home. I know arctic peoples cope with those temperatures routinely, but I’m too poorly prepared to survive those conditions. Thankfully, this day is warmer, so much so that snow fleas are active on the snow surface. I ski as far as I can up the trail. Eventually, I abandon my skis and walk the rest of the way when the trail steepness beyond my comfort level. The trail is also too narrow to ski down safely and I don’t own the the right style of skis or the skills to do that anyway. On the way up, though, I miss their floatation. The snow pack on the upper mountain must be at least 36 inches. I post-hole to my waist on two occasions.

View of mountain from a low elevation. The mountain is covered in trees that transition from deciduous to coniferous from low to high. The foreground is snow covered.
The destination: Mount Chase on Feb. 12, 2023.

View from a mountain of a forested landscape. Only a sliver of the lowlands are visible. Snow and trees fill the fore and middle ground. The trees are snow covered, especially on their left side.
The view looking south from the Mount Chase summit on Feb. 12, 2023.

March 11
The snow seems deeper than February, but maybe this will be the last deep snow trip of the year? Along an alternative route I like to take to the main trail, I find a set of lynx prints in the snow. Farther up the mountain I ditch my skis again at a point above the abandoned fire warden’s cabin where the slope gets too steep. A few snowmobiles have made the trip, though, and I continue with relative ease in their trackways.

A single lynx track. Photo is taken from directly above it. The notebook at bottom is about 7 inches long.
A single lynx track. The feline was traveling from right to left.
The 3x4 gait of a lynx in snow. Photo is taken from directly above tracks looking down. The tracks are several inches in width and length.
Although these lynx tracks aren’t well defined, the size and shape are distinctive. I find one set of these tracks per winter on average. Lynx are rare in Maine and have large territories.
Portrait view of forest. Spruce and fir trees fill the scene with spruce growing the tallest. A narrow trail is visible at bottom center.
The coniferous forest on the upper slopes of Mount Chase.

April 22
A difficult trip to the top and back (the hardest of them all, in hindsight). Mud season has fully enveloped the region. The dirt roads that approach the trailhead are slop. Large Marge gets me to the trailhead but not without extra effort from my legs. The trail remains almost wholly snow-covered above the abandoned fire warden’s cabin and the remaining snow is soft. Still, I’m thankful winter’s dormancy is broken. Near the trailhead, I hear wood frogs looking for love in a nearby a vernal pool. The calls of juncos, robins, and sapsuckers—birds that do not overwinter here—fill the deciduous forest nearby.

Two trails intersect at lower right. Both have water flowing on them. A sign at left points to the center of the photo. The sign is mounted on a post has a homemade look. It says "trail." An arrow points to the right toward the trail. Both "trail" and the arrow are outlined in permanent marker.
The official Mount Chase trailhead.

A derelict cabin in a forest. Wet, late season snow covered the bare area in front of the cabin. A mixed forest surround the cabin. The windows and door of the cabin is missing and the brick red lead paint is peeling from the outside.
The abandoned fire warden’s cabin on Mount Chase.
View from a mountain of a forested landscape. A ridge of large snow capped mountains form the horizon, although they appear small in the photo. Snow covered trees form the foreground just above windswept rock. Frozen ponds and forest fill the middle ground.
Looking west-southwest toward Katahdin and Baxter State Park from the Mount Chase summit on April 22, 2023.

May 17
I thought I’d be done with snow on the mountain by now. I was wrong. It falls on the way up and on the summit. Some small patches linger in the shadiest areas among the spruce and fir. Bud break might be advancing fast at lower elevations, but the plant phenology seems at least a week delayed on the mountain’s mid elevations and maybe two weeks behind in the summit area.

GIF of landscape view from a mountain top. Stunted spruce and fir fill the foreground. Forested lowlands fill the middle ground to the cloud obscured horizon. Snow flakes fall in the air.

Close up photo of flower in deciduous forest. The flower petals face the camera. The three petals are maroon.
Trillium erectum on the lower slopes of Mount Chase.

June 19 
A busy day on the trail with a whopping three cars at the trailhead! Large Marge, as usual, doesn’t have any other bicycles to keep her company. The forest has come to life. I note more than 20 plant species blooming. Biting insects are surprisingly few in contrast to home where the abundance of mosquitoes and black flies force me to don long sleeves, long pants, and a headnet almost anytime I intend to spend more than a few minutes outside. In the spruce-fir forest, I enjoy listening to the songs of blackpoll warbler. Sadly, they are categorized as a threatened species in the state.

A rocky trail disappears into a green forest. Trees with bright green leaves obscure the sky. The understory is also thick with green plants.
Late spring on the Mount Chase Trail.

This is the song of a blackpoll warbler recorded in the spruce-fir forest of Mount Chase. The song is a rapid series of high-pitched notes near the beginning of the track. The audio also captures part of the songs of Swainson’s thrush and winter wren.

July 21
The air feels and looks heavy due to high humidity and hazy, smoke-filled skies. This isn’t the first day of the summer with these conditions, and the past two summers had days like this too. Is the presence of smoke becoming the new normal for summertime Maine? I concentrate on observing the trees, which are in “peak green,” a phase in summer when the foliage has reached its max yet still retains some of the freshness of spring. Fledgling birds are the latest addition to the animal community. Golden-crowned kinglets and red-eyed vireos feed noisy babies. On the summit, hundreds of dragonflies zip between the stunted trees.

Portrait view of rocky trail through a green forest. The trail starts at lower right and disappears at center.Trees with bright green leaves obscure the sky. The understory is also thick with green plants.
Peak green on Mount Chase trail. July 21, 2023.

View of forested landscape from mountain summit. Bare rock covers the ground at bottom while spruce and fir trees slope off the mountain. The lowlands and horizon are obscured by haze in the air.
Looking west-southwest through smoky haze toward Katahdin and Baxter State Park from the Mount Chase summit on July 21, 2023.

Close up view of a dragonfly. The insect rests on rock speckled with small crusty lichens. It has a blue-spotted abdomen and holds its wings flat parallel with the rock.
A darner dragonfly of genus Aeshna rests on at the summit of Mount Chase. If you know what species it is, please identify it on iNaturalist.

August 20 
A quiet hike now that songbird nesting season is done. Only white-crowned sparrows sing in the summit area. The summer foliage has reached “tired green.” The work of photosynthesis as well as insect attacks have rendered the previously vibrant leaves a darker, less vibrant hue. I experienced a stressful week. Yet, I’m fortunate to have an escape for some brief solace.

View of forest that is a mix of young and old spruce and fir trees. Dead standing trees are among them. A large trunk is at left.
A section of old growth forest on upper Mount Chase.

View of forested landscape from mountain summit. Bare rock covers the ground at bottom while spruce and fir trees cover the near slopes. The skies are mostly cloudy. Forest fills the lowlands. A pond and mountains can be seen near the horizon at center left.
Looking west-southwest toward Katahdin and Baxter State Park from the Mount Chase summit on August 20, 2023.

September 24 
I discover (for myself) the remnants of a long abandoned cabin maybe 20 yards off the trail. It’s collapsed to its foundation. Still, I’m surprised by its presence. I walked by it many times previously without seeing it. The forest tends to make things disappear. Hazy conditions have returned to the area. A thick band of wildfire smoke clouds the north horizon and the mountains of Baxter State Park are mostly obscured. A few red-tailed hawks ride the thermals on the mountainside on their migration south. A raven family doesn’t tolerate their presence. They move to chase one of the soaring hawks. We’re approaching peak fall colors, although the colors are quite muted compared to normal.

A collapsed cabin rests in the forest. Vegetation has yet to grow over the structure but the wood at the base in the foreground is rotted and moss covered. The rest of the structure forms a pyramid shape.
The forest and weather will soon consume this collapsed cabin.

The Mount Chase Trail on Sept. 24, 2023.

View of forested landscape from mountain summit. Bare rock covers the ground at bottom while spruce and fir trees cover the slopes. A pond is visible at center left. Haze obscures the horizon. The low elevation forest is speckled with yellow foliage.
Looking west-northwest from the Mount Chase summit on Sept. 24, 2023.

October 18
The forest trends brown. A solid layer of newly fallen leaves cloaks the forest floor. I somehow sleepwalk most of the way to the summit, a habit I’ve been trying to break for years with greater mindfulness. I find myself stopping to focus on my breath and immediate surroundings. Something distracted me, probably precipitated by a media culture that profits from distraction and rage-inducing social networks. It is possible to walk through a forest and not see it at all.

Landscape view of rocky trail through a forest. The trail starts at bottom center and disappears at left of center. The canopy is mostly bare of leaves. The leaves that remain are mostly yellow. A larger tree bisects the image from top to bottom.
The Mount Chase Trail on October 18, 2023.

View of forested landscape from mountain summit. Bare rock covers the ground at bottom while spruce and fir trees cover the upper slopes. The lowland forest is mostly brown and bare of leaves. Tall mountains form the horizon although they look small due to the perspective. A pond is visible in the forest at center right.
Looking west-southwest toward Katahdin and Baxter State Park from the Mount Chase summit on October 18, 2023.

November 16
I begin at an alternative trailhead that I’ve used a few times this year. The route isn’t maintained. It’s nothing more than a decades-old skidder trail, but it is a quicker and more secluded course than the main trailhead. The year has been wetter than average, so water has consistently flowed over parts of the trail. Mid fall brought a prolonged stretch of dry weather though, and the trail is drier than it has been over the entire year. Winter will soon be here. The canopy is bare. Patchy snow sits in the shady areas of the mountain’s spruce-fir forest.

View of forest that is a mix of young and old spruce and fir trees. Dead standing trees are among them. A large trunk is at left. Tiny patches of snow sit on fallen tree trunks.
The old growth forest on upper Mount Chase on November 16, 2023.

View of forested landscape from mountain summit. Bare rock with some patchy snow covers the ground at bottom while spruce and fir trees cover the upper slopes. The lowland forest is bare of leaves. Tall mountains form the horizon although they look small due to the perspective. A pond is visible in the forest at center right.
Looking west-southwest toward Katahdin and Baxter State Park from the Mount Chase summit on November 16, 2023.

December 8, 2023
Winter is a time of dormancy for many life forms, although it brings vibrancy in other ways. None of the previous trips were as beautiful or as quiet. Several inches of snow coat the ground at low elevations and about 12 inches linger higher on the mountain. No human footprints are discernible on the trail. Snow and hoarfrost cover the conifers like cake icing. The landscape appears clean in a way that I don’t find in spring, summer, and fall.

A fat tire bicycle rests against a snow covered bank. Trees fill the background at top. The bike has a rear pannier and bar mitts.
Large Marge

view of snowy forest. The trees are mostly deciduous and bare of leaves. Snow covered the ground.
The Mount Chase Trail on December 8, 2023.
The final approach to the Mount Chase summit on December 8, 2023.

View of snowy conifer trees looking toward mountains on a far horizon. The trees are pyramidal in shape and their branches are covered in thick snow. The ground is fully snow covered. A blue sky fills the upper half of the photo.
Looking down the Mount Chase Trail near the summit on December 8, 2023.

View of forested landscape from mountain summit. Snow covers ground at bottom. A single set of human footprints cross them toward the perspective of the camera. Snow-covered spruce and fir trees cover the near slopes. Ice covered ponds and forest fill the lowlands. A line of mountains forms the horizon.
Looking west-southwest toward Katahdin and Baxter State Park from the Mount Chase summit on December 8, 2023.

Time spent in the forest is never wasted and every moment offers the potential to discover new perspectives. I’m no closer to profound insights after thirteen trips to the summit of Mount Chase, although I’ve walked away with a greater appreciation for the mountain’s rhythms. The experience is both the same and vastly different every time. 

My Pebble Mine Draft EIS Comments

As I’ve written before (here, here, and here) and commented on (here and here), Pebble Mine represents an unacceptable threat to Bristol Bay, home to the last great salmon run left on Earth. Through June 29, you can submit comments on the Army Corps of Engineers draft Pebble Mine environmental impact statement. I encourage everyone who cares about wildlife and wild places to comment. Tell the Army Corps of Engineers that this mine is unacceptable.

I also realize that not everyone has the time to read the draft EIS, which is huge, containing about 1,400 pages. So, I’ve copied my comments on the draft EIS verbatim below. You can also download a rich text file of the comments. I hope they inform your comments about Pebble Mine, the development of which would be a grievous mistake.

red salmon swimming in shallow water

Draft Pebble Mine Environmental Impact Statement Comments

I firmly oppose the development of Pebble Mine. The draft EIS (DEIS) fails to adequately address the mine’s short-term and long-term impacts. Additionally, its development would create several permanent hazards to the watershed, and the mine merely represents the first of many potential large-scale developments that will continually degrade salmon habitat in Bristol Bay. After reviewing the DEIS, I urge the Army Corps of Engineers to reject the permit application for Pebble Mine and select the no action alternative.

Permanent Mine Hazards

The mine and its infrastructure create several permanent environmental hazards. Two of these hazards, the open pit lake and tailings storage areas, are particularly concerning, because the DEIS does not provide adequate or convincing information on how these hazards can be contained indefinitely. For example, page 8 of the executive summary states,

“Pyritic tailings and PAG waste rock would be placed into the open pit for long-term storage below the pit lake water level. Once the material has been transferred to the open pit, the pit lake (i.e., the water that would accumulate in the open pit as a lake at closure) would continue to fill, and would be allowed to rise to the pre-determined control elevation threshold (about 890 feet). Once the level of the open pit lake rises to the control elevation, water would be pumped from the open pit, treated as required to meet State water quality standards, and discharged to the environment.”

This final stage of the open pit requires indefinite water treatment and discharge of water from the open pit. This is neither acceptable nor feasible in perpetuity since treatment facilities must be funded and maintained forever. Even if Pebble Limited Partnership is required to establish a bond to fund treatment, government solvency cannot be guaranteed over time spans necessary to treat wastewater from the open pit. Additionally, if costs to treat wastewater exceed the money available in the bond, then the burden to prevent contamination to the watershed will fall to taxpayers.

Page 8 of the executive summary also states,

“The bulk TSF would be closed by grading its surface so that all drainage would be directed off the TSF, and then the tailings surface would be covered with soil and/or rock and possibly a geomembrane or other synthetic material. This would prevent water from ponding on the TSF surface, and is known as a dry closure. Once this surface runoff from the bulk TSF is demonstrated to meet water quality criteria, it would be directly discharged to the environment.”

Since geomembranes have only been in use for 30 to 40 years, we lack adequate information on how they perform over the time span (essentially forever) necessary to keep the bulk tailings storage facility dry and prevent groundwater from leaching in or out. Simply covering it with soil, rock, and a synthetic membrane only delays groundwater contamination. It will not prevent it. The impacts of a degraded geomembrane leading to groundwater contamination are reasonably foreseeable but are currently unevaluated in the DEIS. The EIS needs to evaluate the impacts and timeline of a degraded geomembrane, not just presume that it will protect groundwater forever. It won’t.

Importantly, it is also completely unethical for a private corporation to create permanent hazards of this type. The mine has the potential to become another superfund site. If the Corps is to evaluate whether this project is in the public’s best interest, then it cannot ethically allow the creation of these hazards.

Scope of DEIS

The DEIS repeatedly presents information on best-case scenarios or merely states that something is “expected to happen” in an ideal way. For example, page 39 of the executive summary states,

“Water extraction activities would be required to meet the requirements of the Alaska Department of Natural Resources for temporary water use authorizations, and the Alaska Department of Fish and Game (ADF&G) for fish habitat permits (if issued). The rate and volume of water withdrawals would be monitored at each source to ensure permit requirements are met (as per permit stipulations). Therefore, the magnitude of the impacts to surface water resources is generally expected to result in changes in water quantity likely within the limits of historic and seasonal variation. The duration of the impacts is likely to be the life of the road, and the geographic extent of the impacts is likely to be relatively close to the road.”

Page 41 of the executive summary states,

“Overall, downstream impacts from pit lake level management during post-closure would not be expected.”

For another example, page 43 of the executive summary states,

“Under Action Alternative 1, impacts to water quality would generally be limited to the mine site area, within the zone of contact water capture and treatment, with potential minor exceptions of temperature and turbidity effects. Potential effects of contact and runoff water during construction of downstream water and sediment quality would be minimized through treatment prior to discharge, and would be expected to be minor.”

Statements such as these presuppose nothing will go wrong, ever, not with water treatment, not with the tailings storage areas, not with the fuel or the natural gas pipeline, not with the water extraction sites along the road. It downplays potentially significant risks. The DEIS does not adequately evaluate cumulative, foreseeable, long-term impacts.

Problems maintaining water quality can be expected over the life of the mine and are likely to increase after the mine is decommissioned. The mine will result in a net loss of spawning and rearing areas for salmon, and the habitat cannot be reclaimed. Throughout the DIES, the text downplays the ultimate impacts of the project. To gloss over impacts to the watershed in this manner represents a lack of due diligence on the part of Army Corps of Engineers and Pebble Limited Partnership.

Potential for Catastrophic Mine Impacts

While a credible worst-case spill from the mine, such as a tailings dam failure, is not likely in 20 years, if it were to occur the environmental effects would be devastating. The DEIS, again, neglects to include the possibility of unlikely–but foreseeable–catastrophic events. The agency’s review does not analyze a full breach of the tailings dams. It instead looks at a much smaller partial breach suggesting, “Action Alternative 1 and variants would not be expected to result in a longterm change in the health of the commercial fisheries in Bristol Bay or Cook Inlet.” (DEIS Executive Summary, page 54)

The potential for a tailings dam failure might have been calculated to be small (DEIS K4.15-16) over the near term, for example, but the risk cannot be eliminated and it will increase over time without additional mitigation measures. What is the likelihood of dam failure (large or small) over the next several hundred years? How would a catastrophic tailings dam failure impact the watershed, salmon, other wildlife, and the people who rely on Bristol Bay? This must be evaluated in the EIS. It is a reasonably foreseeable impact for this type of development since tailings dams fail frequently in the United States.

Impacts to Fish and Wildlife

The DEIS does not adequately evaluate the direct or otherwise foreseeable impacts on waters accessible to anadromous fish. As an example,

“The magnitude and extent of impacts, when compared to the total mileage of currently documented anadromous waters in the three tributaries associated with the mine site (i.e., the NFK, SFK, and the UTC), the loss of Tributary 1.19 habitat would represent 4 percent and 3 percent of spawning and rearing habitat for coho salmon, respectively; and 3 percent of Chinook salmon rearing habitat in these tributaries. In the context of the entire Bristol Bay drainage, with its 9,816 miles of currently documented anadromous waters, the loss of Tributary 1.19 represents an 0.08 percent reduction of documented anadromous stream habitat.” (Executive Summary, pg. 49)

Fish populations fluctuate significantly over many years and Pacific salmon utilize different habitats during different life stages. Some places in a creek are good for spawning but not rearing, for example. These habitats do not necessarily occur along a stream’s entire distance, nor do streams support salmon at the same rates consistently. Productivity within a watershed can fluctuate greatly over annual and decadal scales. As recent research1 on the Nushagak watershed demonstrated, entire landscapes stabilize biological production. Patterns of high and low production shift among locations throughout time. Simply acknowledging a stream supports anadromous fish does not adequately acknowledge the complexity of salmon habitat. Subsequent chapters in the DEIS do not present information on the type and relative importance of the habitat that will be lost. Therefore, the DEIS’ conclusions may not reflect the true importance of the stream miles impacted by the mine.

The quoted text is also written in a manner that minimizes the mine’s impact on fish (“In the context of the entire Bristol Bay drainage…the loss of Tributary 1.19 represents an 0.08 percent reduction of documented anadromous stream habitat.”). A more ecologically accurate measure would be to calculate this statistic as a percentage of the North Fork Koktuli River watershed. As I note above, not all anadromous streams are created equal. The North Fork Koktuli River watershed likely supports unique stocks of anadromous fish. Sacrificing .08% of Bristol Bay is not inconsequential and should not be written in a manner that suggests as much.

Regarding the transportation corridor, each of the DEIS alternatives are flawed due to the lack of information on the infrastructure impacts on fish and wildlife. For example, the DEIS does not address whether shipping across Lake Iliamna will impact harbor seals. The seals who live in Lake Iliamna are a unique population2. They live their entire lives in freshwater and have never experienced consistent shipping traffic on the scale proposed. The DEIS, therefore, needs to evaluate the impacts of shipping on wildlife in Lake Iliamna.

Water Extraction

At the mine and along the proposed transportation corridor, dozens of “water extraction sites” are proposed, pumping hundreds of millions of gallons of combined from surface features such as ponds, lakes, and streams (DEIS 2-58, 2-59, 2-96, 2-111). The pumping will continue year-round for the lifespan of the mine, and potentially longer as long as the infrastructure exists. However, I was unable to locate information in the DEIS on the impact of water extraction. Text on water extraction cites Appendix K2, which only includes a table about the estimated extraction rate per year.

There is no analysis of the impact of removing 500-1000 gallons per minute from dozens of surface water features. Are the streams identified for water extraction included in Alaska’s anadromous fish catalog? How will each stream react to that level of water removal? Flow rates in Bristol Bay streams vary greatly across seasons. Can the proposed extraction rates be maintained during years of drought or during winter when flow rates are low with no significant impact on aquatic habitat?

Each water feature is hydrologically unique and should be evaluated separately. A lack of evaluation on water extraction on fisheries and wildlife is a major flaw in the DEIS.

Long-term infrastructure use by communities

The DEIS states in several places that mine infrastructure will improve the quality of life for some communities.

“As described in Section 4.12, Transportation and Navigation, Alternative 1 would result in the construction of roads and ports. Although the road and port would have limited access, PLP has stated that they would work with all local communities to identify the best solutions for controlled-access use of the road and ferry for community transportation. Communities adjacent to the natural gas pipeline (Kokhanok, Newhalen, and Iliamna) would have the opportunity to connect to the pipeline. During operations, PLP would work with local communities to identify safe, practicable ways for residents to use the access roads, such as scheduled, escorted convoys for private vehicle transport.” (4.4)

“Communities adjacent to the natural gas pipeline (Kokhanok, Newhalen, and Iliamna) would have the opportunity to connect to the pipeline. Natural gas would likely be less expensive than diesel heating oil, which could lower the cost of living once equipment (e.g., furnace, water heater) is converted to natural gas” (4.4-5)

However, the DEIS repeatedly states that infrastructure will be abandoned or removed after 20 years.

“If no longer required at closure, the pipeline would be cleaned and either abandoned in place or removed, subject to state and federal regulatory review and approval at the decommissioning stage of the project. Surface utilities associated with the pipeline would be removed and reclaimed.” (Executive Summary, pg. 13)

Due to the high cost of living in the area, communities along the infrastructure corridor are likely to use the access road and the natural gas pipeline as soon as they are permitted to do so. These same communities wouldn’t want to give it up that access after 20 years. Therefore, the likely impacts of a natural gas pipeline and roads are not limited to 20 years. Impacts extend indefinitely. The DEIS should be revised so that it evaluates the impacts of a potentially permanent pipeline and road corridor.

Potential for Larger Mine

The DEIS is a rough evaluation of a mine with a 20-year lifespan, but that is one of the least likely development scenarios. If Pebble Mine is permitted to be developed, then it will open the door for an expanded and much larger mine that will operate for nearly 80 years as well as several other large-scale mineral prospects. The DEIS acknowledges this on page 4.1-8 when it states the Pebble Project Expansion is “reasonably foreseeable” and “would develop an additional 58% of mineral deposits”. The impacts of a much larger Pebble mine and a mining district in the headwaters of Bristol Bay are potentially exponentially greater compared to the mine proposed in the DEIS. This will cause irreparable harm to Bristol Bay’s fishery.

The potential for an expanded mine also increases the likelihood that the Pebble’s supporting infrastructure will remain in place indefinitely. The infrastructure is unlikely to be reclaimed as outlined in the DEIS. It will be used to service not only the larger Pebble Mine but others as well. This will lead to a cumulative degradation of salmon habitat, greater impacts to other species of wildlife, and greater risk for Bristol Bay’s fishing industry and culture. Although it’s not possible for the DEIS to evaluate the impacts of all foreseeable project expansions and other mines, the likelihood of this should at least be acknowledged more prominently, ideally in the executive summary. As currently written it is buried in Chapter 4 and easy to overlook.

In support of the No Action Alternative

Large scale development, especially open-pit mining, is incompatible with salmon habitat. We know this because large scale development has significantly degraded salmon runs and salmon habitat across much of the North Pacific and North Atlantic. Bristol Bay harbors the last great salmon run on Earth. If Pebble Mine is developed, then we will have acknowledged we have learned nothing from the collapse of salmon runs in New England, California, Oregon, or Washington.

The DEIS is largely based on Pebble Limited Partnership’s data. With so many flaws in the DEIS, it’s clear that the applicant’s plan is inadequate and has not met the burden of information necessary to justify their plans.

The cheapest, most feasible, and most environmentally ethical decision is to conclude this mine poses unacceptable risks to Bristol Bay—specifically the Nushagak and Kvichak watersheds—reject the mine alternatives, and choose the no action alternative for the final EIS. This is well within the Corps’ legal authority: “No Action Alternative could be selected if USACE determines during its Public Interest Review (33 CFR Part 320.4[A]) that it is in the best interest of the public, based on an evaluation of the probable impacts of the proposed activity and its intended use on the public interest.” (Ch. 2-8)

Although modern society uses rare earth minerals like gold and copper in many ways, civilization will not collapse if Pebble Mine is not developed. We won’t even be inconvenienced. If developed though, Pebble Mine represents the beginning of the end of Bristol Bay’s salmon. Mining impacts won’t cease after 20 years, and the hazards cannot be mitigated in perpetuity. The infrastructure is a beachhead for a larger scale Pebble Mine as well as many others in the region. The cumulative impacts of each mine will result in the net loss of larger and larger percentages of available anadromous fish habitat. On no metric does the value ore at Pebble exceed the value a healthy Bristol Bay watershed, its tens of millions of spawning salmon, and the economy and culture based on it.

There is no doubt the no action alternative is in the best interest to the public. We have so little to lose by leaving the ore at Pebble Mine in the ground and so much to gain by protecting it for current and future generations. The decision is clear.

The only acceptable alternative proposed in the DEIS is the no-action alternative. Do not permit this mine to be developed. If you do, it will become one of the greatest environmental tragedies of the 21st century, representative of our failure to do what is right by the land, the fish, and the people of Bristol Bay. It will become a monument to human greed and hubris.

Sincerely,
Michael Fitz
Concrete, WA
May 24, 2019

  1. Brennan, S. R., et al. Shifting habitat mosaics and fish production across river basins. Science. Vol. 364. Issue 6442. 24 May 2019
  2. Brennan, S. R., et al. Isotopes in teeth and a cryptic population of coastal freshwater seals. Conservation Biology. Accepted Author Manuscript. 2019. https://doi.org/10.1111/cobi.13303

 

 

 

Bristol Bay at Risk

Imagine a place where the watershed is un-engineered, where the ecosystem’s productivity and potential is fully realized. It produces half the world’s wild sockeye salmon and is home to more brown bears than people. Then imagine that greed for minerals, driven by mass consumption, threatens it.

Alaska’s Bristol Bay is that place.

GIF of underwater footage of adult coho salmon

Bristol Bay is a 42,000 square mile (1.87 million hectare) watershed that encompasses the southeast corner of the Bering Sea. Ringed by the Kuskokwim Mountains to the north and the Aleutian Range to the south and east, the area is almost wholly undeveloped. The watershed includes two of the nation’s largest national parks (Katmai and Lake Clark), three giant national wildlife refuges (Alaska Peninsula, Becharof, and Togiak), the nation’s largest state park (Wood-Tikchik), as well as millions of acres of undeveloped lands and waters. In short, it is one of the most spectacular and wildest landscapes on the continent.

Wildness, however, doesn’t equate unpeopled. Humans have lived in the Bristol Bay region for at least 9,000 years and likely longer (the oldest human habitation sites were probably flooded by rising sea levels at the end of the last ice age).  Bristol Bay’s Yupik, Alutiiq, and Dena’ina developed a complex relationship with the resources they used to survive, especially salmon. Today, salmon remain the cultural, economic, ecological heartbeat of the region.

Born in freshwater and grown large in the sea, salmon are a conveyor of energy and nutrients. Their upriver migration feeds everything from mink, otter, eagles, and brown bears to 30 inch-long rainbow trout and 10-pound char. After spawning, they die and their decomposing bodies distribute millions of pounds of fertilizer, substantially increasing the productivity of an otherwise nutrient poor freshwater system. Salmon even help plants grow faster.

The area’s abundance isn’t fantasy either. Bristol Bay’s 2018 salmon run was the largest on record, with over 62 million wild salmon returning. Of that run, 21 million sockeye went uncaught and escaped upstream to spawn. 2018 was the fourth consecutive year that sockeye salmon runs exceeded 50 million fish. Exvessel value, the activities that occur when a commercial fishing boat lands or unloads a catch, was worth $281 million dollars. In 2010, during a much smaller run compared to 2018, harvesting, processing, and retailing Bristol Bay salmon created $1.5 billion in sales across the U.S. The value of salmon is even higher when all salmon related jobs—fishing, processing, tourism, supplies, services, and government—are taken into account.

Pebble Mine puts all that at risk.

GIF of underwater footage of sockeye salmon

Pebble Mine is a proposed open pit copper and gold mine at the northern headwaters of Bristol Bay. The fully developed mine site would encompass over 8,000 acres. Tailings ponds and an open pit would straddle two incredibly productive salmon producing watersheds—the Kvichak and Nushagak. Supporting infrastructure would include a 270-megawatt power generating plant, a 188-mile natural gas pipeline, dozens of miles of roads, and up to three new ports where no development currently exists.

As part of the required permitting process, the Army Corps of Engineers is currently soliciting comments on its draft Pebble Mine Environmental Impact Statement (DEIS). Comments will be accepted until May 30. I’m working on my comments now and plan to share them in another post, but the draft is huge, over a thousand pages long, so it’s taking me some time to read. However, my initial evaluation of the document has revealed major concerns.

  • The DEIS evaluates the mine’s active phase (20 years), but pays little attention to the true lifespan of the mine’s footprint, which will extend for hundreds, even thousands of years and create a permanent hazard to the watershed. After the mine’s proposed 20-year operation phase is complete, the landscape is supposed to be reclaimed. Tailings and waste rock will be stored underground or underwater in the former open pit. The open pit will be allowed to fill with water. Once the open pit lake rises high enough, water would be pumped from it, treated to meet water quality standards, and discharged into the watershed. This must happen forever to prevent groundwater contamination.
  • The DEIS does not evaluate the effects of a catastrophic tailings dam failure, which would release a toxic slurry of material into the Kvickchak and Nushagak watersheds. The risk of this is low, but that’s beside the point. The risk still exists and cannot be eliminated.
  • The DEIS does not evaluate who will pay for and maintain permanent water treatment in the open pit.* There is currently no financial plan to fund wastewater treatment after the 20-year operational phase when the mine is to be “reclaimed.” Who’s to pick up the tab when the Pebble Partnership, the mining consortium owned by Northern Dynasty Minerals, decides to walk away? The partnership claims financial assurance for site closure and monitoring is required before construction, but this does not assure funding for perpetual waste-water treatment. Since the corporation cannot guarantee financial solvency forever, it should not be allowed to create hazards that last forever.
  • The DEIS does not sufficiently evaluate the cultural impact the loss of salmon would represent to local residents, especially Native Alaskans. I’ve never been to any place where a single group of animals means as much to a regional culture as salmon do for the residents of Bristol Bay. For them, loss of salmon would be equivalent to the loss of bison for American Indians across the Great Plains.
  • Supporting roads, ports, and other infrastructure have the potential to disrupt some the best, untrammeled bear habitat in the region, especially for bears that use the McNeil River area just north of Katmai National Park.

Pebble’s proponents argue that the mine and salmon can coexist, but the two are at fundamental odds and always will be. Mike Heatwole, president of Public Affairs at the Pebble Partnership, told Mashable that the mine will cause no “population-level challenges to fish and wildlife resources.”

Screen shot from Pebble Partnership website. Text says, "Where is Pebble? Despite what you may have heard, Pebble is not at the headwaters of Bristol Bay. It is located at the upper reaches of three small tributaries — out of more than 50,000 in the Kvichak and Nushagak watersheds."

Pebble Partnership also claims the mine isn’t at the headwaters of Bristol Bay, which is blatantly false. This screen shot is taken directly from their website.

Despite talk that the salmon “population” won’t be affected, the mine reduces spawning and rearing habitat no matter what. Even under a best-case scenario where Pebble Partnership keeps its word, this is still precisely how we begin to lose salmon—one impassible culvert, one dam, one mine at a time. A few yards of stream here, a little more there. Does that matter? It sure does, as the story of salmon in the contiguous 48 states illustrates.

When Lewis and Clark explored the lower Columbia, they found the riverbanks lined with people, and a regional subsistence and trade economy based on the river’s salmon. In less than 150 years, it was gone. Farther upstream at Spokane Falls, people once gathered for thousands of years to catch 60 – 80 pound chinook. Those runs too are nothing more than memory.

In Washington State today, we bicker over the last of the wild salmon, considering whether to cull sea lions to help save an endangered population of starving orcas. Not far from where I live, Baker River sockeye are completely dependent on human intervention for their survival, because dams now completely block access to their spawning grounds. The outlook for salmon isn’t good on the rest of the west coast either. By 1999, wild salmon had disappeared from about 40 percent of their historic range in Oregon, Washington, Idaho, and California. Across the continent in Maine, where people have taken great strides to clean up rivers and remove some barriers to salmon migration, almost no wild Atlantic salmon remain. Twelve Atlantic salmon returned to Maine’s second and third largest rivers, the Androscoggin and Kennebec, respectively, in 2018. Twelve.

No single factor caused the collapse of salmon runs in New England or the west coast. It was death by a thousand cuts. They were treated as an afterthought at best, undervalued and willingly sacrificed for “progress.” Similarly, if developed, Pebble Mine probably won’t be the end to salmon in Bristol Bay, but it could certainly be the beginning of the end. As Van Victor, president of the Bristol Bay Economic Development Corporation, rhetorically asked, “At the end of the day, do we really want to risk what is truly one of mother nature’s wonders of the world for copper and gold?”

GIF of underwater footage of salmon fry

Young salmon fry feed in one of Bristol Bay untarnished rivers.

If you haven’t seen Bristol Bay, if you haven’t experienced what a truly wild and healthy ecosystem is like, then it might be easy to dismiss my concerns. It can be hard to imagine rivers and streams flooded with fish, where wildlife and people flourish on the seasonal treasure. That dynamic simply no longer exists in most of the rest of North America and we, unfortunately, consider it normal. In conservation biology, this generational amnesia is called shifting baseline syndrome: Every generation sees nature through a different lens and what we view as normal is actually degraded. Our threshold for acceptable environmental conditions is continually being lowered.

Thankfully, we don’t have imagine or scour history books to understand what Bristol Bay’s fishery and ecosystem was once like because it is what it has been since the last of the Ice Age glaciers melted from the landscape. We can still experience it at its full potential. It’s a treasure to savor and protect.

But we could lose it, quite easily in fact. Pebble Mine represents greed over sustainability. If developed, it provides clear evidence we won’t stop till the entire world is consumed. Future generations will judge us poorly if we take everything and leave nothing. It takes a special kind of naiveté to believe otherwise.

 

*I’d like to add a correction on this point. According to James Fueg of the Pebble Partnership, a closure bond would have to be in place before construction can begin, with the bond’s purpose to fund perpetual wastewater treatment by the state. This is good and something I didn’t know about. However, this is of little consolation. It is unethical for a private corporation to create a permanent hazard that the government then must forever ensure is contained. It’s not in the public’s best interest, and shouldn’t be allowed.

Fishers Return to North Cascades

On an uncommonly sunny day in early February, I stood in a tract of old-growth forest not far from the Suiattle River to watch a missing mammal return to the North Cascades. With the return of the fisher, this area is one step closer to whole.

The fisher (Pekania pennanti) is one of the largest North American weasels. Adult females weigh four to six pounds and measure about 30 to 36 inches long, including tail, when fully grown. Males are about 20% larger, growing upwards of 13 pounds and nearly four feet long. Despite the name, fish are not a primary prey. Instead, fishers are wolverines of the forest. Highly arboreal, cylindrical in shape, and agile in motion, they are formidable predators of rodents, rabbits, hares, grouse, and other small to medium-sized animals.

fisher running to escape a box, people standing behind it

One of the first fishers to be released on February 6. The common name, fisher, is probably a modern English language corruption of “fitch,” a Middle English term for the pelt of the European polecat (Mustela putorius), also known as the common ferret. Not coincidentally, the colonial Dutch fisse and visse as well as the French fiche and fichet, all words for the polecat, sound quite similar to fisher. (NPS Photo)

Fishers were functionally extirpated from Washington by the mid 20th century due to habitat fragmentation and, especially, unregulated trapping. Surveys in the 1990s and early 2000s failed to find evidence of any viable fisher populations. As a first step to recover the species in the state, a coalition of public agencies, tribes, and private organizations released fishers in Olympic National Park from 2008-2010. This was followed by similar efforts in Gifford Pinchot National Forest and Mount Rainier National Park from 2015-2017. The North Cascades National Park Service Complex and Mount Baker-Snoqualmie National Forest began to host the fisher’s return last fall, which is how I found myself standing in the woods with about twenty other people on February 6.

Fishers prefer mature forests with a high canopy, relatively large diameter trees, and an abundance of downed trees. Dead standing trees are particularly important to fishers, as they den exclusively in tree cavities. The release site for the fishers this day seemed particularly well suited to their needs.

forest and stream

Fortunately and conveniently, healthy populations of fishers remain in British Columbia and Alberta and they serve as the source for the restoration effort. Fishers from western Canada are also genetically similar to those that used to inhabit Washington. Canadian trappers were paid to capture live, healthy animals. The Calgary Zoo temporarily housed the fishers while veterinarians evaluated their health and surgically implanted tiny radio transmitters to assist biologists in tracking them.

Twelve hours before release, these particular animals were still in Calgary. At 1 a.m., the fishers were flown to Abbotsford, British Columbia where they were picked up by biologists and driven into Washington. By early afternoon, a gang of biologists and a few interested souls like me were unloading the cargo and carrying the fishers a short distance to the release site.

Fisher release, Buck Creek Campground, Mount Baker-Snoqualmie National Forest_02062019_4

Fishers were transported in specially designed crates. Two fishers, separated by a partition, are in each crate.

view through screened hole of fisher in a box

A fisher peeks through a window toward the outside world.

people carrying wooden crates on forested path

Our group formed a semi-circle around the crates to watch the release. Conversations quieted to a whisper or died in anticipation as the crates were opened one at a time. To coax them out, a screened vent was opened at the top and a volunteer blew a puff of air into the container. I’m unsure if this was as annoying as someone blowing air into my ear, but the trick worked. The fishers shot out like a flash and bolted into the forest.

Six fishers were released that day bringing the total number currently released in the area to 24. The release efforts will continue until about 80 fishers are reintroduced to the area. Biologists will track, monitor, and study the animals to assess survival rates, identify where they go after release and where they establish home ranges, the types of foods they eat, and the diseases and parasites they suffer from.

The effort has a high chance of success. Reintroductions, however, are rarely so simple. Fishers, although not well known among the general public, are relatively non-controversial animals. They don’t evoke the same emotional reactions in people as grizzly bears or wolves, for example.

More than that, however, the forested habitats along the core and margins of the North Cascades are largely intact. Land managers needn’t take extreme, expensive, time-consuming measures to restore the ecosystem to a point where it could support fishers again. It could always support them. We just didn’t allow fishers to survive here.

Because prior generations had the foresight to protect places like North Cascades National Park and Glacier Peak Wilderness, we have the opportunity to restore fishers to land they once knew as home. Situations like these are becoming increasingly uncommon. People have fundamentally altered so much of the Earth to preclude the reintroduction of many extirpated species into their historic ranges. (There’s no substantial habitat available for bison in Iowa, for example.)

view of old growth forest with large coniferous trees

Potential future fisher habitat along Stetattle Creek in North Cascades National Park.

As humanity’s footprint grows, undeveloped landscapes are increasingly valuable, not for the resources we can exploit within them (including supposedly non-consumptive uses like solitude), but as repositories of biodiversity and ecosystem health. To adapt an idea from Thoreau, future generations, I believe, will measure our legacy not by what we invented and consumed, not by our material wealth, but by what we can afford to let alone.

I’ll probably never see any of these fishers ever again. Even if the population increases to hundreds of individuals, they’ll remain reclusive neighbors. If I’m lucky, I may find a track in fresh snow or its scat on a log. But even that doesn’t matter. I’ll know they are there and I’ll know the landscape is healthier because of it. The return of the fisher represents, at least in one small way, the success of our ability to let one place—North Cascades—alone.

Vote on Climate

In my last post, I explored the origins of an alpine lake in North Cascades. The news cycle was especially terrible the day I wrote it, so I decided to leave out details about the causes and consequences of glacial retreat in North Cascades. But honestly, the causes and consequences are too great to ignore. It is no small irony that my insight and enjoyment into the formation of an alpine lake was inadvertently provided by people through human-caused climate change.

All glaciers in North Cascades are retreating and they’ve collectively lost over 50% of their mass during the last 100 years. This is directly due to a warming climate, a product of burning fossil fuels like coal and oil.

before and after photos of glacier.

Banded Glacier in 1960 (left) and 2016 (right) in North Cascades National Park.

Unless you’ve been living under one of those glaciers for the past century, you might’ve heard there’s an election next week and voting has begun in many states. While casting our votes, we have an opportunity to elect representatives who will work to mitigate climate change. But, we shouldn’t vote to combat climate change just because glaciers are receding in North Cascades National Park.

We should act on climate, because glacial melt water moderates summertime drought. Millions of people depend on glaciers for drinking water.

We should act on climate to lessen the risk from extreme weather events like drought, hurricanes, floods, and heat waves.

We should act on climate to ensure supplies of fresh water are not overly taxed by humanity’s increasing demands. Who wants reliable access to clean fresh water? All of us.

We should act on climate to help reduce the spread of invasive species, many of which are finding easier footholds where ecosystems are already stressed and fragmented.

We should act on climate to prevent the loss of arctic sea ice, a habitat that helps cool the planet by reflecting sunlight into space, forms the basis of a complex polar food web, and is one necessary for the survival of polar bears.

We should act on climate so coastlines aren’t flooded by sea level rise.

We should act on climate to mitigate ocean acidification, which can impact marine food chains. A lot of us eat seafood and even if we don’t, we like animals that eat seafood (whales, bears, etc.). What would Katmai National Park, my favorite place, be without abundant salmon? An impoverished place, that’s what.

I could go on, but I think you get the point.

We have a moral responsibility to stave off the worst climate change impacts, because this is a human-caused issue. Collectively we can do it, but we have to take the threat seriously. We, as a nation, didn’t vote to combat climate change during the 2016 election. Thankfully, we have another chance now, but time is running out to slow and eventually halt what is one of the most pressing issues facing humanity. That’s why I’m voting for initiatives to mitigate climate change and only for candidates who take climate change seriously.

photo of Washington State ballot showing yes selected for Initiative 1631

In Washington, Initiative 1631 would authorize the first carbon tax in the U.S. This is my ballot.

I’ve been fortunate enough in my life to explore active glacial environments in many parts of North America. In Katmai, I’ve walked on pumice-covered glaciers to reach volcanic calderas, numbed my feet in icy glacial runoff, and eaten freshly calved ice (if you’re wondering, it was clean tasting but a little gritty). In the North Cascades I explored the margins of the region’s still active ice. To find an advancing glacier in modern times, however, is rare. Melting glaciers are one of our most conspicuous symbols of global warming.

Glaciers have come and gone in the past, of course. I grew up in a region of Pennsylvania where Ice Age glaciers terminated their last advance, leaving behind eskers and sand quarries. I lived near Lake Chelan, a remarkable inland fjord carved by glaciers. Katmai was also completely overrun by ice. Modern glacial retreat is different though, because we’re the primary cause. Climate change isn’t a hoax or some deep-state conspiracy. It’s real, it’s here, and humans are causing it. There is no scientifically plausible alternative theory that explains the changes to Earth’s climate observed since the Industrial Revolution.

I still find beauty in the ice, but each time I see a glacier I also am reminded of one of Aldo Leopold’s many maxims,

“One of the penalties of an ecological education is that one lives alone in a world of wounds. An ecologist must either harden his shell and make believe that the consequences of science are none of his business, or he must be the doctor who sees the marks of death in a community that believes itself well and does not want to be told otherwise.”

The community is not well, because we’ve wounded it. Let’s step up and act. When you vote, only vote for those who take climate change seriously and, more importantly, will actively work to reduce its impact. The status quo got us here, but the status quo is no longer good enough.

Pebble Mine Scoping Comments

Recently, I wrote about an impending threat to Bristol Bay’s salmon: Pebble Mine. The mine, if developed, will have significant effects across some the richest salmon and brown bear habitat left on Earth.

Salmon remain the ecological and cultural heartbeat of Bristol Bay. This mine will create billions of tons of semi-fluid toxic waste, which must be treated and prevented from entering the watershed indefinitely. Impacts from development are never completely restricted to the development’s footprint either. Roads fragment habitat and vehicle traffic displaces wildlife.

When I was born, Pacific and Atlantic salmon fisheries in the Lower 48 states were already significantly degraded. Nearly 40 years later, many salmon stocks in New England, California, Oregon, and Washington remain threatened or endangered. Only a small fraction of fish return to these areas compared to historic levels. I’m not about to let this story repeat itself in Alaska, nor should you. If the mine is developed, future generations will inherit its legacy, and I predict they won’t look upon us fondly for repeating the same mistakes that killed salmon runs in the past.

Please comment during the scoping period on the Army Corps of Engineers’ Pebble Mine Environmental Impact Statement (EIS) and send those comments to your congressional representatives as well. Below you’ll find my scoping comments for the proposed mine. Feel free to copy and personalize them as you see fit. State your concerns now, so when the Army Corps of Engineers writes the EIS it will fully evaluate the mine’s impacts. Don’t let Bristol Bay’s salmon disappear because of our lust for copper and money.

The Corps is accepting comments through June 29, 2018.

salmon jumping at waterfall

Comment to the U.S. Army Corps of Engineers (submitted May 23, 2018):

The proposed Pebble Mine and its associated infrastructure poses a substantial threat to salmon and wildlife across the Bristol Bay region. Pebble Mine will straddle the watershed divide between two of Bristol Bay’s most important salmon spawning and rearing areas. I remain very concerned with the mine’s potential to negatively impact the area’s fisheries and wildlife through its wastewater, tailings, and infrastructure.

The EIS must answer one question: can Pebble Mine be developed without significantly degrading water quality and fisheries? The Corps’ has authority to deny permits under section 404 of the Clean Water Act if a proposed action will significantly degrade water quality and fisheries. This EIS should evaluate and quantify, not just identify, the mine’s potential to significantly degrade water quality and fisheries over short and long-term timespans. The EIS can begin this evaluation by appropriately defining its purpose.

A recent environmental impact statement from the Army Corps of Engineers, the Donlin Mine EIS, merely stated the purpose of the mine and the Corps’ authority to permit it (Donlin Mine Final Environmental Impact Statement – Chapter 1, pg. 1-4, 1-6). The purpose and need of the Pebble Mine EIS should be not be to simply define the project’s purpose (to mine ore) and define the Corps’ regulatory authority. It should be, as I propose, to:

  • Identify the short-term and long-term ecological effects of the proposed Pebble Mine,
  • Evaluate the mine’s and its infrastructure’s impacts on wildlife, including fish, in order to
  • Determine whether the mine’s safeguard can prevent all degradation to water quality, salmon habitat, and wildlife habitat indefinitely.

Even at very low concentrations, dissolved copper is particularly toxic to salmon, interfering with their ability to navigate and avoid predators. Its effects can manifest over minutes or hours and persist for weeks (Hecht 2007). Can the mine’s wastewater treatment plan adequately remove dissolved copper and prevent it from entering the watershed?

The mine’s tailings also pose a great risk to fish. Any accidental discharge from the pyritic tailings ponds will significantly degrade salmon habitat. Open pit mines, even within the United States, have a poor record containing their toxic tailings. Most tailings dam failures occur at operating mines and 39 percent of such failures worldwide occur in the United States, significantly more than in any other country (Rico 2008). Earthquakes and flooding hazards increase the risk of a tailings pond dam failure in the Bristol Bay region, and tailings ponds cannot be drained in the event of flooding or dam failure due to their toxic contents. The probability of a M8+ earthquake, for example, is low from year to year but remains real at any given time. Therefore, the EIS must also evaluate whether the tailings ponds can be engineered to withstand the greatest potential earthquakes and floods expected over the next several thousand years.

After the mine’s 20-year active phase, the mining company proposes to store toxic pyritic tailings indefinitely under water in the former open pit. This seems to create the potential for acid mine drainage to leach into the watershed over hundreds or thousands of years. What geologic studies suggest this is a feasible long-term plan to store the tailings? Even if subaqueous storage in the former open pit prevents the tailings from oxidizing, what safeguards will prevent dissolved copper and other toxic metals from entering groundwater to eventually oxidize and acidify as it nears the surface in a different part of the watershed?

The mine’s supporting infrastructure also creates risks for salmon and wildlife. Although salmon can navigate and migrate through streams with high sediment loads, they do not spawn in these habitats. Erosion of sediments into streams can irritate the gills of fish, smother eggs, alter feeding habitat for salmon fry, and bury spawning habitat. The effects of road construction and vehicle traffic (estimated by the mining partnership to be 35 round-trip truck trips per day) on wetlands and fisheries should also be evaluated.

The road servicing the proposed Amakdedori Port and the port itself will fragment what is now an unspoiled region of coastline on Cook Inlet. McNeil River State Game Sanctuary is one of the most important brown bear refuges on Earth, home to the largest annual congregation of bears yet observed. The road and port have the potential to displace bears moving to and from the McNeil River and Katmai National Preserve areas. Frequent work and dredging at the port area will also displace wildlife in an area that now experiences very little human activity. Other alternatives to transport ore should be evaluated.

Finally, the EIS needs to address more than the 20-year operational phase, because the mine’s waste legacy will threaten salmon for thousands of years. Tailings stored in the former open pit won’t become benign in the near future and wastewater must be treated indefinitely. Also, the possibility of an expanded mine operating over a long time frame increases the threat to salmon, other wildlife, and clean water.

Combined, the Nushagak and Kvichak rivers support about 40% of Bristol Bay’s sockeye salmon. In 2017 alone, over 56 million sockeye salmon returned to Bristol Bay and over 19 million returning to Nushagak River, the largest in the river’s history. Salmon fishing in Bristol Bay is a billion dollar industry. While commercial fisheries generate the bulk of the salmon’s economic value, the area’s tourism is almost entirely based on salmon as well. Bristol Bay is home to dozens of premier sport fishing destinations, which harbor abundant populations of rainbow trout, Dolly Varden, arctic char, northern pike, lake trout, and grayling. The Bristol Bay area also hosts some of the densest populations of brown bears ever measured. Salmon are the most important food source for these animals, and the vast majority of people who visit Katmai National Park come to watch brown bears (Strawn 2015). After spawning, dead salmon fertilize the ecosystem with nutrients derived from the ocean, boosting the productivity of otherwise nutrient-poor area.

Considering the overwhelming economic and ecological value of salmon to the Bristol Bay region, Pebble Mine could displace thousands of workers and tourists if its safeguards fail to protect salmon. Without the energy and nutrients provided by consistently large runs of anadromous salmon, Bristol Bay’s freshwater and terrestrial ecosystems will quickly transition from one of richness to poverty. In many ways, this cycle is a positive feedback loop. The productivity of the area is reliant on large runs of salmon.

We’ve seen, repeatedly, salmon populations in the Pacific Northwest and New England decimated by habitat loss and pollution. Now we’re on the brink of repeating the same mistake in Bristol Bay. Pebble Mine should not be developed. It’s in the greatest interest of Bristol Bay’s fishing industry and culture, watersheds, salmon, and wildlife for the Corps’ EIS to fully evaluate the mine’s near and long-term effects. A failure to contain the mine’s toxic tailings and wastewater would directly impact two of Earth’s most productive salmon producing watersheds. The EIS must address potential groundwater exchange in the abandoned open pit, and whether the mining company can eliminate the risk of acid mine drainage. It must address whether the embankments for tailings ponds can withstand high magnitude earthquakes. It must address whether it’s even appropriate to build a mine whose wastewater will need to be treated indefinitely. It also must critically evaluate the mine’s supporting infrastructure, as it will potentially disrupt the world’s largest seasonal congregation of brown bears. In sum, the EIS must evaluate a worst-case scenario for salmon and other wildlife, since the possibility can’t be completely, or even reasonably, eliminated.

References:

Hecht, S. A., et al. March 2007. An overview of sensory effects on juvenile salmonids exposed to dissolved copper: Applying a benchmark concentration approach to evaluate sub-lethal neurobehavioral toxicity. National Marine Fisheries Service.

Rico, M., et al. 2008. Reported tailings dam failures: A review of the European incidents in the worldwide context. Journal of Hazardous Materials 152: 846–852.

Schindler D. E., et al. 2003. Pacific salmon and the ecology of coastal ecosystems. Frontiers in Ecology and the Environment. 1(1): 31–37.

Strawn, M. and Y. Le. 2015. Katmai National Park & Preserve Visitor Study: Summer 2014. Social and Economic Sciences Research Center, Washington State University, Pullman, WA.

 

Addendum: My comment was apparently too long for the Corps’ comment portal on the Pebble EIS website. So if you use my comment in full, you might receive an error message. To work around it, you can attach the full comment as a PDF or Word document.

The Worst Place in the World for a Mine

“This is the jewel in the crown of America’s fisheries resources – these salmon. If you don’t think this is worth saving, what is? To me, if you don’t draw a line in the sand here, there’s none to be drawn anywhere.”

Thomas Quinn
Professor, University of Washington and author of The Behavior and Ecology of Pacific Salmon and Trout

After more than a decade of controversy, Pebble Mine is inching closer to reality, and from the perspective of salmon, we couldn’t choose a worse place for an open pit mine.

red salmon swimming in shallow water

If you’re unfamiliar with Bristol Bay, its salmon, or Pebble Mine, please watch this 2012 overview on the Pebble Mine controversy, keeping in mind the mine’s currently proposed size and mineral processing plans are different than those outlined in the video.

Pebble Mine is a proposed open-pit copper, gold, and molybdenum mine at the headwaters of some of the last intact and most productive salmon habitat on Earth. Before any development of the mine can begin however, it must be permitted, and before it can be permitted, it must undergo an extensive environmental review. This is where we stand currently: the environmental impact statement (EIS) process for Pebble Mine has begun.

An EIS goes through several stages before a “record of decision” is finalized. Right now, the Pebble EIS is only at the scoping level. If you’re unfamiliar with the EIS process, public scoping is basically a brainstorming step. It’s the public’s opportunity to help define the breadth of the EIS to the lead agency, which in this case is the Army Corps of Engineers. (Read more about the scoping process.) During public scoping, if people don’t express concerns for the ecosystem-wide impacts of Pebble Mine and its infrastructure then the Corps’ EIS will not address them. Therefore, we must comment during the scoping period and demand that the alternatives in the EIS address the mine’s full environmental impact—which will sprawl across southwest Alaska and threaten the last great sockeye salmon run in North America.

The Bristol Bay area is exceptionally special and unique. Its landscape remains largely undeveloped and un-engineered. The major factors that decimated salmon elsewhere—habitat loss, dams, and pollution—are absent and salmon runs reach tens of millions of fish annually. Bristol Bay is where we can imagine the richness of fish that used to flood into the Columbia River or New England. It remains home to one of the most valuable and sustainable fisheries on Earth, one of the few remaining places where the full potential of the ecosystem is realized.

salmon jumping at waterfall

Salmon fishing boats in Naknek

Salmon fishing boats sit idle on a late winter day in Naknek, Alaska. The 2017 Bristol Bay salmon harvest was worth $670 million.

The Pebble EIS must address the mine’s potential, worst-case scenario effects on Bristol Bay’s salmon. A failure to contain the mine’s toxic tailings and wastewater would directly impact two of Earth’s most productive salmon producing watersheds. (The Kvichak River watershed, where part of the mine will be located, is home to the single largest salmon run in the world.) It must address potential groundwater exchange in the abandoned open pit, and whether the mining company can eliminate the risk of acid mine drainage. It must address whether the embankments for tailings ponds can withstand high magnitude earthquakes. It must address whether it’s even appropriate to build a mine whose wastewater will need to be treated indefinitely. It also must critically evaluate the mine’s supporting infrastructure, as it will potentially disrupt the world’s largest seasonal congregation of brown bears.

Map outlining Nushagak and Kvichak watersheds. Red star marks location of Pebble Mine.

Pebble Mine will straddle the divide between the Nushagak and Kvichak watersheds, two of Bristol Bay’s riches salmon producing areas.

By law, the EIS process must identify the least environmentally damaging practicable alternative. Common sense implies the least damaging alternative in this case is no mine at all, but the National Environmental Policy Act does not require agencies implement it. If we don’t demand the Corps critically evaluate the myriad impacts from the mine, then the Corps will merely focus on holes in the ground, “alternatives” of natural gas versus diesel to power the mine, how wide the service roads will be, and the size of the ports. The scope of the EIS will be so narrow to be useless for the protection of salmon. (For an idea of what this might be, look no further than the Donlin Mine Final EIS, whose purpose and need is: “produce gold from ore reserves from the Donlin deposit using mining processes, infrastructure, logistics, and energy supplies that are economical and feasible for application in remote western Alaska. The applicant’s stated need for the project is to provide economic benefits to Donlin Gold, Calista, and TKC shareholders; and to produce gold to meet worldwide demand.”)

I recognize a sad irony—or hypocrisy, if you prefer—of using a computer, which contains gold and copper, to type this post. I understand there’s a hole in the Earth, perhaps filled now with toxic water, where the metals in my machine were once trapped in rock. If you, like me, think Pebble Mine is irresponsible, then voice your opposition not only through the EIS process and with your votes at the ballot box (politicians who support Pebble Mine will not receive my vote), but also by reducing your consumption of products that use gold and copper. We, as consumers, need to say enough is enough. Our addiction to ever-higher levels of consumption brought us here. It’s not really sufficient to say “I’m opposed to Pebble Mine” then go out and buy the newest iPhone even though your old phone works just fine.

Everything we use, everything we make, has a cost. We’re at a point in history when surging human population growth and mass consumption are pushing ecosystems and species to their breaking point, creating an ecologically impoverished planet. In New England, wild Atlantic salmon are nearly extinct, and on the U.S. west coast only a tiny fraction of Pacific salmon return compared to historic levels. Don’t kid yourself: This sad story can repeat itself in Alaska.

We lose salmon one impassible culvert, one dam, one levee, one mine at a time, leaving us to suddenly wonder, where did all the fish go? In Bristol Bay we have a chance, maybe our last chance, to save large runs of wild salmon. If the mine is built and its proposed safeguards fail, we risk losing a significant portion one of the world’s last great sustainable fisheries. Future generations won’t be celebrating our decision if we develop this mine. They’ll criticize us for not learning from the mistakes of the past. Are we really willing to let hyper-consumerism and the promise of short-term profits potentially destroy the last great salmon run?

It looks like we’re on track to do so, unless enough people step up and say no.

Through June 29, 2018, you can submit scoping comments on the Pebble Mine EIS. I’ll share my scoping comments in a forthcoming post when they are finished.

Update May 23, 2018: My scoping comments can be found here.