When your vacation plans start to dissolve, a little flexibility can go a long way, and may even provide you with the opportunity to see natural wonders rarely witnessed by the majority of travellers. This is the story of how we got to see magnificent wetlands and wildlife as well as the results of a jökulhlaups, and why you might want to consider spending an extra day or more exploring to the west of Anchorage.
We arrived in Anchorage from Gustavus (via Juneau) on our penultimate flight with Alaska Airlines on 3rd August.
After a great week down in south east Alaska, where we’d been extremely lucky with the excellent weather, the skies now decided that ‘blue’ and ‘calm’ were over.
Having reserved a couple of slots with Ellison Air at the end of April, we had hoped to flight-see to the north of Anchorage around Denali (a.k.a. Mt. McKinley, as it was then still officially titled) and Prince William Sound to the south east in whatever order the conditions best suited on the 4th and 5th. As it turned out we wouldn’t get to see either destination on this vacation.
Our scheduled flight departures were both for 08:00 because “the mornings usually have the smoothest air and that is a big deal on a long over land trip like McKinley”, but, when we made the 0.2 mi./3 min. walk from the hotel to Ellison Air’s office on Wisconsin Street at the eastern end of Lake Hood (formerly Lake Spennard until a canal was dug to connect the two water bodies), the weather forecast for the day dictated that flights to Denali and Prince William Sound were untenable.
There was still a window of opportunity to take off to the west of Anchorage, and so, with no knowledge of what lay along the top of Cook Inlet, we agreed to the offer to take us out on a more ‘local’ flight and a landing on Beluga Lake beneath the Triumvirate Glacier. Although we didn’t know it at the time, this flight would take us over the rich wetlands and coastal waters of Matanuska-Susitna (Mat-Su) Borough, and, intermittently, into Kenai Peninsula County as we flew up the Beluga River.
Leaving Anchorage and its Chugach Mountains backdrop, heading across Cook Inlet.
After briefly following a course parallel to the power transmission lines that stretch from the Beluga River Power Plant to supply Anchorage with nearly half of its electricity, we turned towards the lower reaches of the Susitna Flats, spotting our first bull Moose (Alces alces) of the day by the forested banks of one if the myriad of creeks and small rivers flowing down to the sea.
Looking inland from the tidal edge of the Susitna Flats while heading west.Mount Susitna (known as “The Sleeping Lady”) from the Susitna Flats near the Little Susitna River, where a few rays of sunshine tried to pierce the cloud cover.
Perhaps the most spectacular feature of the Susitna Flats State Game Refuge – and certainly the prime reason for its refuge status – is the spring and fall concentration of migrating waterfowl and shorebirds. Usually by mid-April, mallards, pintails, and Canada geese are present in large numbers. Peak densities are reached in early May when as many as 100,000 waterfowl are using the refuge to feed, rest, and conduct their final courtship prior to nesting. The refuge also hosts several thousand lesser sandhill cranes and upwards of 8,000 swans. Northern phalaropes, dowitchers, godwits, whimbrels, snipe, yellowlegs, sandpipers, plovers, and dunlin are among the most abundant of shorebirds. Most of the ducks, geese, and shorebirds move north or west to nest in other areas of the state. About 10,000 ducks -; mostly mallards, pintails, and green-winged teal, remain to nest in the coastal fringe of marsh ponds and sedge meadows found in the refuge. Recently, Tule geese, a subspecies of the greater white-fronted goose, have been discovered to nest and stage on Susitna Flats. In the fall, migrant waterfowl and shorebirds once again arrive in growing numbers to rest and feed on sedge meadows, marshes, and intertidal mud flats.
Mammals
Back from the coast are brushy thickets where moose calve each spring. In the winter, moose from surrounding uplands return to the refuge to find food and relief from deep snow. Both brown and black bears use the refuge, feeding particularly on early spring vegetation near salt marshes and sedge meadows. Beaver, mink, otter, muskrat, coyote, and wolf can also be found. Trapping is a regular winter activity on the refuge.
[…]
Fish
The Susitna River and its tributaries support the second largest salmon-producing system within Cook Inlet. In the summer, set net fishing sites dot the shoreline of the refuge.”
The area covered by the Susitna Flats State Game Refuge. [Source: ADG&F]Looking upstream from the outflow of the mighty Susitna River as we continued flying west.At the mouth of the Susitna River as it flows into Cook Inlet.
Along the shoreline mud bars we started to see increasing numbers of lounging seals, and were also lucky enough to spot the distinct white shapes of Beluga Whales (Delphinapterus leucas) in the grey waters close to shore, which is not a privilege we’d have had around Denali. The resident population of Belugas in Cook Inlet means this is one area where viewing is common, particularly in summer and fall when they congregate between the Little Susitna and Susitna Rivers, before they move to deeper waters slightly further south around Kachemak and the Barren Islands during the winter.
One of the seal banks we saw along the coast of Cook Inlet at Susitna Flats.
Aside from all the wildlife, this area is not always devoid of inhabitants. At the edge of the lake near the center of the image below, a small cabin can just be seen, and, as marked on the earlier map, it’s not the only one in the refuge. This area is prolifically fished and hunted:
“An impressive 40,000 user-days of sport fishing effort are expended on the Little Susitna River each year, reached over land on a rough 4-wheel drive trail. Some hardy fishermen head for the Little Susitna by boat from the mouth of Ship Creek.
The Theodore and Lewis rivers are popular fly-in fishing streams for king salmon from late May through June. Combined, these rivers annually provide approximately 7,000 user-days fishing effort and a harvest of 1,000 king salmon.”
The Susitna Flats SGR continues west of the Susitna River. The sun once again briefly appeared to illuminate the shrouded top of Mt. Susitna.
After a few miles more of the spectacular coastal wetlands we turned inland to the northwest and re-crossed the transmission power lines as we headed to the Beluga River and Lake for our scheduled landing.
The landscape beneath us remained consistently diverse and just as riveting.
Fixed-wing aircraft are ideal for flightseeing across the refuge as they are permitted to travel as low as 500 ft (152m) above ground level during protected wildlife breeding seasons (it’s 1500 ft (457m) for helicopters) which provides some great views of the landscape.
In the open spaces of creek gravel bars we spotted more moose and a bear using the natural highways, but we soon reached our destination
Beluga Lake lies 56 mi. (90km) WNW of Anchorage. It is principally formed by the meltwaters of the Triumvirate Glacier which primarily flow along the northern and southern flanks of a 4.5 mi. (km) bar of land which separates the lake and the glacier’s frontal moraine at the west of the lake. Beluga Lake is approximately 6 mi. (10km) long from east to west, and about 3 mi. (5km) wide. The Beluga River starts at the eastern end of the lake with additional in-flow from the tributary Chichantna River (fed in turn by the Capps Glacier) in the south-eastern corner of Beluga Lake. Coal Creek flows into Beluga Lake from the north just before the start of the river. The relatively isolated location is reflected in the USGS topographical map which dates back to 1958, but it still provides a reasonably accurate impression as can be seen on the CalTopo website.
In a video posted the day before our flight, a landing on Beluga Lake by a 1958 De Havilland Canada Beaver DHC-2 MK.1 floatplane from Rust’s Flying Services shows what the area around the Triumvirate Glacier and a Beluga Lake landing look like in good weather.
As we reached Beluga Lake it became apparent that something strange had recently happened to the landscape below us.
Heading west, looking south. Beluga Lake with the start of the Beluga Rover to the left, with the Chichantna River flowing left to right in the background.The flooded shoreline where Coal Creek enters Beluga Lake.The trees at the periphery of the lake had been inundated by a rapid expansion of the water level and, closer to the land in front of the Glacier, there were boulders of blue ice littering the banks of the principal northern riverine channel and braided streams flowing into the lake.The land below the moraine in front of the Triumvirate Glacier.Following the course of the lateral channel flowing from the edge of the northern edge of the Triumvirate Glacier. Note the blue ice on the over-spill gravels.The water clearly wasn’t flowing in any substantive measure from the frontal tongues of the glacier (although blue ice was once again deposited at the foot of the moraine)……and neither was it flowing over the top of the glacier’s northern-most finger of ice.Flying up above the Triumvirate Glacier the weather was closing in, but our pilot, John Ellison, skilfully managed to get us through the turbulence between the clouds flowing down from the Tordrillo Mountains and the ice below to reveal the source of the flood…Under the impinging cloud layer, Strandline Lake was no longer impounded by the Triumvirate Glacier. Note the stranded glacial ice high on the sides of the lake’s edges. This view of its remaining waters, and the previous images of its continued outflow, show that it wasn’t yet finished draining.
We’d already witnessed the beautiful colour of consolidated glacial ice and the impressive calving of tidewater glaciers in SE Alaska, but the impact of this sight and recognition of the scale of this natural catastrophe was simply awe inspiring.
According to the U.S. Board on Geographic Names the Triumvirate Glacier was so named by S. R. Capps and R. H. Sargent of the U.S. Geological Survey “because this glacier is composed of the joining of three large glaciers.” It flows for over 20 miles in a south easterly direction down towards Beluga Lake, and, near the glacier terminus, a north facing lobe Strandline Lake, forms an ice-dam to the outflow of Strandline Lake in its high-sided narrow valley.
As Strandline Lake backs up and rises against the glacier lobe, calving fills the lake with icebergs that can be 120m in height. Eventually the hydrostatic pressure is sufficient to float the lobe and the water variously forces its way over the ice, down plunge pools, and through old subterranean channels in the bedrock at the northern edge of the ice, whilst also carving its way along new routes and the underside of the glacier.
Point of release.
This type of cataclysmic outflow is known by the Icelandic term ‘jökulhlaups’, which in English means a glacial lake outburst flood (GLOF). We’d never heard of it, let alone witnessed the results of such a catastrophic environmental event.
In the earlier video, Strandline Lake is featured from 4’ 14” to 4’ 57”. At the point when it was filmed the lake was full and the Glacier was displaying characteristic pre-jökulhlaups glacier surface water pools. Shortly before our arrival this condition had dramatically changed, but, if we hadn’t taken the chance to head out in a previously unconsidered direction, we’d probably still know nothing of such events.
The jökulhlaups wrecking ground of the Triumvirate Glacier at the southern end of Strandline Lake.
The month after our visit this video was posted showing a view of the devastation from a R44 helicopter:
A more detailed description of how Strandline Lake is repeatedly blocked and the resulting release and refill mechanisms can be found in the very easily read “A History of Jökulhlaups from Strandline Lake, Alaska, USA” by Matthew Sturm and Carl S. Benson (Journal of Glaciology, Vol.31, No. 109, 1985). Given the publication date, it naturally enough focuses on the September 1982 jökulhlaups when it was calculated that over 95% of Strandline Lake had drained out, releasing about 185 billion gallons (700 million m3) of water, although it is estimated from earlier strandlines that previous releases could have been up to 65% greater by volume.
Other online literature is, unsurprisingly, sparse, but while Sturm and Bensons’ historical (1940 to 1982 (and 1984)) investigations show a release frequency of every 1-5 years, anecdotal and video evidence suggest that an annual release is possibly now more the norm.
In 2013 National Geographic Channel TV viewers might have watched episode 3 of the first series of “Ultimate Survivor Alaska” which was titled “Into the Void” []. It was filmed in the Fall of 2012, and shows that Strandline Lake (see 24’25” to 34’38”) had been recently drained (and why you might not want to be down there crossing it on foot).
The year after our visit Strandline Lake was once again captured on video in a pre-jökulhlaups condition during the flight in a Cessna 180H floatplane into Beluga Lake posted in July 2014:
In a video uploaded in early August 2014, another R44 helicopter flight recorded post-jökulhlaups conditions:
Given the weight of video evidence in this post, travelling to Beluga Lake is clearly not restricted to grey days. Nor is it restricted to summer months and floatplanes, but you might want to consider the following statistics in planning whether your fly-in uses floats, skis or wheels to get down at Beluga Lake:
Year
Freeze Start
Freeze Final
Breakup Start
Breakup Final
2002
26/10/01
01/11/01
30/05/02
30/05/02
2003
Latest – 13/12/02
Latest – 19/12/02
Earliest – 13/05/03
Earliest – 18/05/03
2004
09/11/03
19/11/03
17/05/04
04/06/04
2005
03/11/04
20/11/04
23/05/05
23/05/05
2006
03/11/05
06/11/05
23/05/06
30/05/06
2007
31/10/06
09/11/06
21/05/07
Latest – 08/06/07
2008
08/12/07
08/12/07
Latest – 01/06/08
01/06/08
2009
Earliest – 24/10/08
Earliest – 24/10/08
18/05/09
30/05/09
2010
08/11/09
10/11/09
29/05/10
29/05/10
2011
27/10/10
22/11/10
20/05/11
29/05/11
2012
05/11/11
05/11/11
21/05/12
02/06/12
2014
07/11/13
18/11/13
14/05/14
20/05/14
Freeze Start = first time lake at or greater than 10%. Freeze Final = first time lake greater than 90%.
Breakup Start = last time lake greater than 90%. Breakup Final = last time lake at or greater than 10%.
In addition to a check on the condition of Strandline Lake before landing on Beluga Lake, it’s probably also worth bearing in mind that these jökulhlaups don’t only occur in the fall. Click here for a link to images of the December 1980 Beluga River Outburst Flood, noting how far the destructive force of the water will travel.
A final close up of the shattered edge of the glacial lobe.With buffeting winds propelling the cloud down the glacier it was time to get out.
The journey back was a more direct overland route and took under 40 minutes. Once again, the landscape was a mosaic of waterways and wetlands, with the trees also occasionally revealing cabins and landing strips as we re-crossed the Susitna River, before more managed pastures and small herds of cattle came into view.
Crossing the line of the Lewis River as it flows SW towards the coast.Past the Lewis River and looking SW, on the way down to the Susitna River and flats travelling to the SE.The village of Alexander (population 40) curves around the right bank of Alexander Creek before it flows into the Susitna River. There was a native settlement recorded here in 1898.Over the Susitna on the way back to Anchorage.
Our round trip only took about 1.5 hours, but, when we landed safely back at Lake Hood, we knew that we had made the right decision to fly west that day, and that we’d been spectacularly rewarded with a once in a lifetime experience.
Aside from Ellison Air and Rust’s Flying Service (who don’t list this trip as a regular departure, so prices are on application) there are a number of other Anchorage based operations who offer flightseeing over this fantastic area, including
Regal Air offer a 2 hr “Triumvirate Glacier and Mt. Spurr Volcano Flightseeing Tour” with a Beluga Lake landing and beach walk for $295 p/p . Regal Air operate from Lake Hood using a variety of aircraft equipped depending on the season.
Sound Aviation charge $200 p/p for an approximately 1.5 hr “Volcano/Glaciers” flightseeing experience They operate from Merrill Field airport using asix passenger retractable wheeled landing gear Piper Lance.
Trail Ridge Air offer a 60 min. “Discover Alaska” flight for $150 p/p from Lake Hood in a Dehavilland DHC-3 Beaver floatplane.
It was the 10th August 2013, and we’d almost reached the end of the road when we arrived in the ‘Halibut fishing capital of the world’. If, like us, you’re not into sea fishing, that might not sound like the most attractive destination advertisement, but I don’t mean it to sound like we’d had enough of the 49th state when we drove into Homer, Alaska. We were literally just about to run out of highway (and on the way there had passed by “North America’s most westerly highway point” at Anchor Point).
In good weather you should be able to see all the way across Cook Inlet to Mt Iliamna from here. This was the view on our departure day……but on our arrival day, and a bit further down the road towards Homer, the volcano was revealed through the clouds and haze of the distance.
After a fantastic couple of preceding weeks in Alaska, we were exactly where we wanted to be as we drove down the Sterling Highway (Alaska Route 1, or AK1) and onto Homer Spit (which, with the longest section of road jutting out into an ocean in the world, gives you an extra 10 minutes of driving if you’re so inclined).
We were a mere 4,612 miles (7,422 km) from home as the intercontinental crow flies (and we were clearly tourists in that we were measuring distances in miles first rather than by hours), but we’d travelled considerably further by air and land to get to our final-stay destination of choice in Homer during a three week vacation tour of Alaska in late July to mid-August.
Inspired by our first experience of viewing Brown Bears at Knight Inlet in British Columbia three years earlier, we’d decided to try and end our vacation with a similar highlight, and then have a few days of chilling out with no other trips booked or schedules to meet until it was time to head home.
Back at the start of the previous January we’d booked 3 seats (and by ‘booked’ I mean we’d paid the total amount of $1,950.00* in advance, not a reservation fee with the balance due at a later date or on arrival) with K-Bay Air to fly our family of three out to the Katmai National Park for a bear viewing day trip on the day after our arrival in Homer. As requested, we’d checked-in at their office on the day of our arrival and had been met with a friendly welcome, and instructions where to meet at Homer airport the following morning at 08:00AM…
*I think we probably got the previous season’s rate as our initial enquiry had been in December 2012, which is worth considering if you plan ahead.
…but things didn’t happen quite as planned. Alaskan weather is notoriously changeable – and the second half of August was running true to form in that rainfall often increases then – but that all just serves to emphasise the sense that you’re on the edge of a true wilderness. In Alaska, towns as big as Homer (the name ‘City of Homer’ always makes me smile as it had a population of 5,310 in 2013) don’t really qualify as ‘wilderness’, but you can probably see it from where you’re sitting, and the weather can always bring you back to a healthy sense of your insignificance.
The view over Kachemak Bay late in the afternoon on our arrival day in Homer.
On the morning of our intended departure we rose reasonably early, avoided scented deodorants/perfumes after bathing, dressed in multi layered clothing with hats, gloves and spare socks stowed, and checked each other’s pockets for errant tuna sandwiches. We then made the 4.3 mile (6.9 km)/9 min. drive through the rain and mist down to Homer airport, where we were told we couldn’t fly yet, and that we should come back in an hour.
We drove back to our accommodation at Wild Rose Cottages, kicked our heels for 40 mins. and drove through the rain and mist down to Homer airport, where we were told we couldn’t fly yet, and that we should come back in an hour.
We drove back to our accommodation, kicked our heels for 40 mins. and drove through the rain and mist down to Homer airport, where we were told we wouldn’t be flying that day, and that we should report to the office on the Spit in an hour for a refund.
I totally get it that safety comes first, and that if the weather says you can’t fly, you can’t fly. I accept that if there is no availability to re-schedule in the next few days, it would be unfair to shunt other booked passengers. I really didn’t appreciate the total failure to express even the slightest modicum of regret on behalf of the company, the unwillingness to respond when asked to suggest any other companies who might be able to help out, and to then be presented with a paper cheque refund in US$ which we would be unable to cash until we returned home (even though we’d paid by visa all those months before). However, just because somebody else is having a bad week (and you never know what problems other people might be facing; I later came to understand why there might have been genuine reason in this instance) it doesn’t mean you have to let it affect you, and we suddenly had more important things to do.
You need to have a ‘Plan B’ (and probably a ‘Plan C’) for bear watching in Alaska. Our plan B consisted of having several days still left in Homer and a list of all the other bear watching flight companies in town.
Our first stop was Emerald Air Services on Lakeshore Drive, where, when we explained our predicament, we were kindly and sympathetically told they had no availability for the period of our stay in Homer. Maybe another time guys, looks like a great trip.
I have to admit that by now, and having already noticed a sign from another bear viewing flight company advertising availability after our departure date from Alaska, I had started to privately question whether I was going to be able to deliver on our hopes. A third of a mile further on we turned down Lampert Loop, parked up, and somewhat despondently walked down to the Beluga Lake office of Steller Air, where we were welcomed with smiles from company founder Mark Munro , flight coordinator Olympia Piedra and the rest of the team, and a ‘can do’ attitude that felt like a hug.
Steller Air is a small floatplane charter service based on the 3000 x 600 ft. (914 x 183m) Homer-Beluga Lake Seaplane Base (known by the FAA as the excitingly coded ‘5BL’). Their website, which is linked above, provides pretty comprehensive information about the services they offer – there’s no point in me copying it all here – and allows direct reservation enquiries. You’ll have to visit them in person to get a true grasp of their friendliness and the sense of optimism that this operation inspires.
We were offered a flight to Crescent Lake (not to be confused with the Crescent Lake just north of Kenai Lake on the Peninsula or Lake Crescent in Clallam County in the north of Washington State) in the Lake Clark National Park on the 13th for $1,797 for the three of us, which we of course accepted. For the next 36 or so hours we kept a weather eye on the skies. As we waited through the 12th, we visited the excellent Islands & Oceans Visitor Center of the Alaska Maritime National Wildlife Refuge, ate out at some great places (try the Boardwalk Bakery for breakfast, Maura’s Café for lunch (see below) and either the Fresh Catch Café or Captain Patties Fish House for dinner if you decide to visit Homer), and just relaxed around our rented house. On the afternoon before our intended new flight date the view across Kachemak Bay from the upper balcony of the Kelly House had some sunshine and encouraging streaks of blue in the sky.
By the following morning the world was looking a little too grey again.
Looking east across Kachemak Bay from Homer with a none-too-hopeful amount of light in the sky.
We watched the gulls and a family of Trumpeter Swans down on Homer Spit before driving back to Beluga Lake, and had finished our breakfast burritos before we arrived, but remember that you will need to pre-declare your weight and it may be checked. Take a look at the Stella Air blog for an insight into Alaska floatplane life (and more on what’s available to see and do with Steller). In case it gets deleted in future seasons, I’ve quoted this post for posterity.
“Truth, Lies and Floatplanes in Homer, Alaska
On a floatplane ride, weights are important. We do a weight and balance of the aircraft to make sure that we are in the limits of a gross weight for a safe take off. Because of this, we ask every passenger their weight, or weigh them in the office. We also weigh a lot of gear. Because our flight coordinators ask a lot of people their weights, and then often have to weigh passengers when they come into the office, they have discovered an interesting fact in the course of loading floatplanes. Contrary to popular opinion, men lie about their weight more than women. Sure, a lady will not like to tell you how much she weighs, but she will discreetly whisper something close to the truth. Men, however, seem to boldly shout out a number that is often 30-40 pounds below their actual weight. Now boys, the girls in the office are working hard to get everyone and their gear to their Alaskan destinations—give them a number close to the truth getting everyone in the air will be a lot easier!”
Having arrived promptly at Steller Air for our safety briefing (and credit card payment), we prepared for departure. Our aircraft for the day was N77206, a Cessna U206G Stationair floatplane (the red floatplane that features strongly in many Steller publicity images is Mark’s Cessna TU206A). This was the second time in less than 10 days that we’d flown on exactly the same type of aircraft, attesting to the ubiquity of this type of aircraft in Southcentral Alaska, so we were already confident of the machine’s capabilities.
What really put us at ease was the quietly spoken integrity and professionalism of our pilot, Tom Young, but you can read more about this later, and we were just keen to get into the air and out to some bears. This Cessna 206 configuration has six forward facing seats in rows of two (including the pilot’s seat on the left), so I was seated next to Tom, and my wife and daughter were in the second row. The overhead wings provide for good downward visibility. If there’s something to see.
As we reached the coast on the far side of Cook Inlet we continued flying north west up the line of the Crescent Valley, where we caught occasional glimpses of the Crescent River below and the jagged Chigmit Mountains to either side and ahead of us.
We reached the confluence of the Lake Fork Crescent River and the North Fork Crescent River (not that we could see it) and swung west in the direction of the lake. There was a brief two second sighting of the water ahead, and Tom said that he could probably get us down, and that there were less experienced pilots who would definitely go for it, but if we did go down he couldn’t guarantee we’d get out again. The tone was clear, so this was an easy decision, as we’d signed up to fly with people who know what they’re doing and to respect their advice. We turned back to Homer.
The return flight was a little surreal as we flew back in the narrow space between the cloud above and the fog below:
Strange skies with Steller Air. Well it was for us, as we’re usually way above the cloud level when we fly, but it made for an unusual experience.No photo editing required. This is how it looked as we returned towards the Kenai Peninsula.
We even got in a spot of glacier viewing as we circled by Grewingk Glacier:
A slightly eerie view across the fog-covered Kachemak Bay to Grewingk Glacier with the coast between Fritz Creek and Kachemak/Miller’s Landing just visible along the bottom of the image to the left.
A hole in the fog appeared above Beluga Lake and we circled back for our descent to the water:
Sweeping over Bishops Beach, Beluga Slough (right image) and the AK1 (left image) we made our safe return to Steller Air (spot the red Steller Air floatplane in the left image).
We now only had one day left before we had to start our homeward journey, so we had no hesitation in deciding to see if we could book another flight the following day. We were in for a shock. As we asked the question we were told that as they hadn’t got us onto Crescent Lake, Steller Air would be willing to try again the following day at no extra charge. Forget fancy words on websites and brochures. This is what a real commitment to customer satisfaction looks like.
It also demonstrates Steller Air’s commitment to passenger and pilot safety. Tom must have known what it would cost the company, but he hadn’t hesitated when he advised the return that day.
Olympia recommended Maura’s Café, and after we’d bagged the remains of our huge deli sandwiches – we’d taken the option of a side of soup for just $1 extra, and there was no way we could have finished all of the delicious first choices too – we strolled off down Bishops Beach.
The weather still wasn’t looking too promising at this point, but at least we had renewed hope as we walked, and gradually the fog started to dissipate.
By the late afternoon, as we watched Sea Otters and Bald Eagles around Homer Spit, the sky had turned blue.
From back up on East Hill Road the world suddenly started to look rather different, as we could see the sun shining on Beluga Lake, on houses at the far shore of Kachemak Bay, and glistening on the snow in the peaks above. That night a half-moon shone through thin cloud.
This photo from the following morning’s take off once again shows how quickly the weather can change in Alaska, and although some cloud had returned, this was much more like what we’d been hoping for:
Take off in a north easterly direction from Beluga Lake with a clear view of the line of Homer Spit. At the top end of the Beluga Wetlands Complex is the Homer Airport Critical Habitat Area which can be visited on foot.
Tom was our pilot again, and as we flew across the placid waters of Cook Inlet we could see small drilling rigs, and even smaller private boats leaving distinctive wakes. We apologised to Tom when Rachael decided to take a sleep break, but he just took it as a sign of a confident passenger:
Rachael sporting her then new Alaska Geographic buff which has since become her standard accompaniment to any cold weather.As we approached the land, and turned north east to run up the coast, we got a much closer (if still slightly hazy) view of Mt. Iliamna than we’d seen on our original drive into Homer:
Mt. Iliamna (10,016 ft (3,053m)) is the smaller of the two Pacific ‘Ring of Fire’ Aleutian chain volcanoes in the Lake Clark National Park. A stratovolcano, you can see one of its many glaciers emerging from beneath the cloud band in this image. It hasn’t properly erupted since 1876, but fumaroles are continuously active.
As I get to the bit where we headed inland into the Lake Clark National Park and Preserve (NP&P) again, it’s worth reflecting on the size of the area of which we were about to experience a tiny slice…
Map reproduced from the public domain NPS .pdf file available here.
According to the National Park Service Land Resources Division summary listing of NP acreage (31/12/2015) [see here for statistical sources] Lake Clark NP&P covers a total area of 4,030,130.17 acres (1,630,936 ha) / 6,297 square miles (16,309 km2). Of this area 2,619,836.49 acres (1,060,210 ha) /4,093 square miles (10,600 km2) lie in the park and 1,410,293.68 (570,726 ha) / 2,204 square miles (5,708 km2) in the preserve.
As one of the top 10 US National Parks by size (most of the largest parks are in Alaska), Lake Clark NP&P is larger than the State of Connecticut, and nearly as large as Hawaii. It’s larger than the Everglades, Grand Canyon and Yosemite National Parks combined, but whereas these parks attracted a total of over 9 million visitors in 2014, Lake Clark NP&P saw just 16,100 visitors in the same period (and that was a huge increase over the 2013 figure of 13,000 visitors), so crowded it is not. There is just one residential community within the Park and Preserve, at Port Alsworth (population 159 at the 2010 census), which is located on the eastern shore Clark Lake, about 50 miles (80 km) from Crescent Lake.
The reason for the low visitor numbers is simply down to the fact that, apart from the coast, which can be reached by a comparatively long boat trip (and there are some powerful rips in Cook Inlet), if you’re going to visit the Lake Clark NP&P you’ll have to fly there. You can enlarge the above map as much as you want, but you won’t be able to find a drive-in route because there aren’t any roads there. There are barely even any maintained trails (except around Port Alsworth), and none where we were heading.
The coastal region of the park, in which Crescent Lake is situated, is just outside the officially demarcated “Wilderness Area”, but it all looked pretty isolated to me. There are a few Park Ranger stations (at Chinitna Bay, Port Alsworth, Silver Salmon Creek, Telaquana Lake and Twin Lakes), and, away from Port Alsworth, a few remote cabins and lodges for rent.
As you start to fly up the Crescent River you might notice a few ‘track lines’ in the trees to your left at Squarehead Cove. These are the remnants of a Crescent River logging project which stopped in 2002 after clear cutting about 700 acres of trees between 2000-2001. If you have a low level flight &/or great eyesight (take some binoculars) you might see the properties on the adjacent coastal strip of land first homesteaded by the Kroll family in the 1940’s, and which have been intermittently occupied by their descendants since that time.
As we flew up the course of the Crescent River, the mighty valleys that had only been hinted at the previous day were revealed…
…before we reached Redoubt volcano.
At 10,197 ft (3,108 m) Redoubt volcano is the largest volcano in the Aleutian chain (and more than twice the height of the tallest mountain in my home country). Lying on the Bruin Bay fault, this active stratovolcano last erupted in 2009. At that time the berms of the Drift River Oil Terminal near Redoubt Bay were nearly broached by a giant mudslide (lahar) which partially flooded the complex.
We flew on up the Lake Fork Crescent River and quickly reached Crescent Lake. What a difference a day makes.
From above, the water of Crescent Lake was a distinctly milky blue-grey colour.
The following technical description of Crescent Lake is taken from a USGS document:
“Land cover is primarily alpine tundra and bare soil (44%), spruce forest (31%), and permanent ice and snow (18%). Lake Fork Crescent River drains an area of 125 mi2. Notable features in this watershed are glaciers, which comprise about 16% of the basin and Crescent Lake. Crescent Lake is approximately 6 mi long and slightly more than 1 mi wide. The average depth of the lake is about 75 ft, and the deepest part is about 100 ft. The lake is oligotrophic; its open-water period lasts about 5 months – from June through October. Thermally, Crescent Lake is a dimictic lake – it circulates twice a year – in the spring and the fall. It is directly stratified during summer and inversely stratified during winter. Surface temperatures characteristically reach 10 to 12°C during the open-water period. Annual water-residence time or flushing rate is estimated to be 0.7 to 0.8 years. Most of the inflow comes from overland runoff and snowmelt. Inflow from definable streams consists of meltwater from glaciers on the southwest side of the basin, at mid-lake. The other major tributary is at the upper end of the lake. Because Crescent Lake is glacier-fed, the lake and its outflow have the characteristic turquoise colour. However, Crescent Lake does trap much of the suspended sediment that enters the lake. The North Fork Crescent River drains an area of about 75 mi2. Approximately 23% of the basin consists of glaciers. The North Fork channel is relatively steep, and during open water is characterized by the typical turbid colour of glacier-fed streams. The confluence of the North Fork and Lake Fork Crescent Rivers forms the mainstem of the Crescent River. In this section, the streambed channel becomes braided, and the channels constantly scour and shift.”
The above text reminds how short the floatplane fly-in period is, and how long the icy Alaskan grip on Crescent Lake endures, but it doesn’t describe how beautiful it is up there.
From the surface of the lake there is a greener or more turquoise hue to the water. Our landing was like all our landings with Steller Air. Smooth.
Taxiing over to the landing beach, the Cessna was turned out towards the lake, reverse thrust applied, and the pontoons grounded so that we didn’t even have to wet our feet on disembarking. We had arrived at Redoubt Mountain Lodge (RML) where we were first welcomed by the guard dogs K’eyush and Charlie (lodge security), and then by the friendly staff.
We were introduced to Colleen, our guide for the day, who we later learned was a fairly new and enthusiastic addition to the RML guiding team, having joined a couple of months previously after working as a volunteer with the US Peace Corps in warmer climes.
Boarding a comfortable and stable 4-stroke outboard-powered pontoon, we headed to the nearby southern shore of Crescent Lake, near the point where the lake flows out into the lower Lake Fork Crescent River.
If you fully enlarge the above image RML can just be seen to the left extent of the nearest tree line.
The scenery was captivating, and would be worth visiting even if there weren’t bears along the shores. Around Crescent Lake the forest is mainly composed of Dwarf Birch (Betula nana exilis), Paper Birch (Betula neoalaskana) and White Spruce (Picea glauca) with Feathermoss and lichens.
Manoeuvring backwards and forwards in parallel to the narrow beaches and shoreline scrub vegetation along just a couple of miles, we spent our time in the almost constant sight of bears, and were treated to a great range of their behaviours.
Fortunately for us, as it brings the bears out of the trees and scrub and into the water, Crescent Lake is one of the most productive Sockeye Salmon areas in the park. Between 1979 and 2012 (when they ran out of funding) the Alaska Department of Fisheries and Game used a sonar station located a couple of miles upstream from the Crescent River’s mouth to count returning fish numbers, and a fish wheel to determine the relative proportions of Sockeye to the smaller numbers of Pink, King, Chum and Coho Salmon, and Dolly Varden. Starting as early as the 15th June and ending as late as 12th August, the average count of returning Sockeye in the 33 years data was obtained in this period (no figures for 2009, but there was a small problem with Redoubt volcano erupting earlier that year) was nearly 73,000 fish per year swimming up the Crescent River.
Alaskan Coastal Brown Bear (Ursus arctos horribilis). Don’t expect to get too close to the bears on this trip – we were at the limit of my wife’s 70-300mm telephoto lens in these shots – but you will be close enough to be awed by their size and by the spectacle of these wild creatures acting in a completely natural manner.
“Is it a brown bear or a grizzly? The answer is that all grizzlies are brown bears, but not all brown bears are grizzlies. The grizzly is a North American subspecies of brown bear with the Latin name Ursus arctos horribilis. The correct scientific name for a grizzly is “brown bear,” but only coastal bears in Alaska and Canada are generally referred to as such, while inland and Arctic bears and those found in the lower 48 States are called grizzly bears.” [Source: PBS Nature Brown Bear Fact Sheet]
A sow with two cubs was our main viewing pleasure, as she patrolled the shoreline, taking careful regard and retreat at one point from a potential male bear threat (but ignoring us and anchored anglers), and taught her young how to fish for Sockeye Salmon in the lake’s margins.The only Brown Bear species larger than the Coastal Brown Bear is the genetically distinct subspecies the Kodiac Bear (Ursus arctos middendorffi). The omnivorous Coastal Brown Bears we saw had grown to their huge size due to the protein rich diet provided by this environment.
After about 2.5 hrs watching the bears we returned to the 5-acre bear protected Redoubt Lodge, as not only was our ride home ‘anchored’ there, but our trip also included a delicious lunch of an Alaska sized serving of fresh salmon.
I chatted with Tom about flying as a part of life in life in the Last Frontier “where 82 percent of communities have no road access, airplanes are used like pickup trucks and many young Alaskans learn to fly before they learn to drive”. With a state population of around 710,000 (2010 census) around 1 in every 60 Alaskans is a qualified to fly. He described the need for locals to be versatile in order to survive outside the brief tourist season. He and his wife were just setting up a new aquaponics venture, which it’s good to see seems to be doing pretty well, although I’m somehow not surprised.
It was all very unhurried and relaxed, but eventually it was time to depart. For our return flight there were two extra passengers in the shape of a young couple returning to Homer, and as there was no significant weight imbalances between us all, it was no problem when we volunteered to shunt backwards in the seating plan so that they might fully enjoy the sights we’d had coming in to Crescent Lake. That said, it wasn’t as though we weren’t able to enjoy some amazing views on the way back.
The view at the top of Crescent Lake where the upper Lake Fork Crescent River meanders in multiple streams.Circling at the top of Crescent Lake before heading over its calm surface and back down towards its outlet and the lower section of the Lake Fork Crescent River marked the start of the route back to Homer.We took many photos of the braided course of the Crescent River on our return, but this is one of my favourites. It’s only some light blue water and grey silt banks in a green forest landscape, but I feel that my life is richer for having seen this beautiful wild landscape and shared the view with my family.Returning to Cook Inlet as we left the Lake Clark National Park over the mouth of the Crescent River. Beyond the outflow is Tuxedni Bay.
We flew on with views of Kalgin Island to our left and quickly reached the Kenai Peninsula once again, before travelling down the coast to Homer.
A view of where Deep Creek enters Cook Inlet near Ninilchik.
When we reached Homer, the aerial view was a stark contrast to that of the preceding day:
Homer Spit with the tide out at our return.Our final descent onto Beluga Lake in the opposite direction to our take off.Safe return in the sunshine at the home of Steller Air with courtesy and care as standard operating procedure.
There isn’t much more to say than that we’d primarily travelled to Homer so that we could fly out to see Brown Bears in wild Alaskan territory, and, despite the proverbial weather hitting the propellers, we achieved that aim THANKS TO STELLER AIR!
I’ve saved this sticker from our trip, and if it looks right on my daughter’s first car, she can have it. Maybe I’ll have to make sure we buy her a car that doesn’t suit, so that I can finally put it on my car.
Steller Air currently list two bear viewing day trip options: the trip we took to Crescent Lake, or a flight out to Brooks Camp, each of which is $650 per person.
In case you really can’t get a flight with Stellar Air (or you feel like you want a different type of bear viewing experience), other bear viewing operations flying out of Homer are as follows below. Listed pricing is as per company websites at time of posting, but check directly for updates. Check the minimum passenger numbers, any age limits just in case you’re travelling with young children, and deposit refund periods too. Research the locations used at the dates of your intended travel and look closely at the package details as there are some important differences in the offers, especially in terms of time spent at the destinations. If I were to book another bear viewing trip other than with Steller Air I’d invest in the cost of some international telephone calls to get a feel for the company.
Bald Mountain Air Services fly two 10-passenger DHC3 Turbine Single Otter floatplanes to Katmai coastal river sites, Brooks River Falls, or Moraine Creek (in the north of the Katmai NP) depending on the time of year. Flights cost $675 per person 1st-30th June and 1st-15th It’s $695 per person 1st July-30th August. Again, there’s a small discount if you pay by cash or personal/travellers cheque – $25 per person – but, as you need to get a 50% deposit cheque to them within 30 days of booking, the same limitations as above are effective.
Beluga Air is located next to Steller Air on Beluga Lake and fly with a 7-passenger DHC-2 Beaver floatplane. Most of the year they fly to the Katmai National Park (Brooks Camp, Crosswind Lake, Morraine and Funnel Creeks, Hallo Bay, Geographic Harbor, or Swikshak Lagoon) for bear viewing but also use Chinitna Bay and Crescent Lake. Prices appear to be on application.
Emerald Air Service offer a guided day trip by 7-passenger DHC U-6A Beaver floatplane to an unspecified location which looks like it could be in the Katmai. $675.00 per person (credit card), $650 (cash, cheque or travellers cheque, but that presents the same deposit issue as Bald Mountain Air for non-US visitors). 50% deposit within 10 days of booking, remainder due upon travel. As mentioned near the start of this post, you can find them on Beluga Lake.
Homer Air is the sister company to Smokey Bay Air, and offer bear viewing at either Lake Clark NP or the Katmai for $625 per person. They run 5-passenger wheeled Cessna U206G aircraft for beach landings from Homer airport.
K-Bay Air (also running the same trips under the Alaska Bear Adventures brand [http://alaskabearviewing.com/]) offer three options: a “Short & Sweet Day Trip” at $589 per person, a “Classic Day Trip” at $695 per person ($670 per person for 4 or more), and a tailored Premium Day Trip, POA. There’s a $50 booking deposit and then payment is arranged in full. They run three 5-passenger wheeled Cessna 206 aircraft for beach landings from Homer airport.
Smokey Bay Air offer bear viewing flights to Chinitna Bay, Silver Salmon Creek (Lake Clark NP), or Hallo Bay for $625 per person (min. 2 persons), 30% deposit on booking. Wheeled aircraft for beach landings. They also run 5-passenger wheeled Cessna U206F and U206G aircraft for beach landings from Homer airport.
More online information.
The Summitpost page for the Aleutian Range of mountains.
The US NPS web pages for Crescent Lake and the Brown Bears of the Lake Clark National Park. As is usual with the NPS, there’s lots of information here which is well worth looking at before you travel.
The 1988 NPS Final environmental impact statement: wilderness recommendation : Lake Clark National Park and Preserve, Alaska, with over 200 pages of information on the park’s wilderness designation. A little dated with regard to the then apparently unrecognised value of bear viewing, but lots of good background reading here, especially pages 26-44.
The IUCN Red List entry for global Brown Bear populations.
“Dad’s brought us to the wrong place again” sighed my daughter to her mother after we had pulled up in a car park at the side of the North Douglas Highway, and I had ‘wandered off’ to “ask for directions”. We had only been driving for 10 minutes from where we’d been staying during the first stop in a 3 week tour of Alaska.
The day had started by ‘reminding’ my daughter of the previous day’s tour guide commentary reference to the Alaskan Gold Rush during a boat trip out of Juneau to Tracy Arm Fjord, and my advice to her to dress warmly in layers for a visit to an “old mine” today.
It soon became apparent to my daughter that I had lied (my wife knew, of course) when I returned to the car and escorted everyone to the Era Helicopters’ Juneau base for check in, a safety briefing, and fitting with lifejackets (mandatory for flights over water) and glacier boots (ask for at least one size larger than your regular shoe size).
“Is there anything else you haven’t told me Mum?”
It was the last day of July, three months since I had booked the Juneau Glacier Dog Sled Adventure as a vacation surprise, and the weather gods were with us. In a year of extreme variations across the state of Alaska Juneau experienced a July with an average temperature of 57.6°F (14.2°C), less than 1°F (°C) warmer than the normal mean of 56.9°F (13.8°C). However, during the middle and end of the month there was an upward spike, with the highest temperature for July recorded on the 29th, at 81°F (27.2°C). It was a ‘sucker summer’ up in the 49th.
The sunglasses and shielding of eyes were needed before we got anywhere near the ice, but even on a dull day make sure you pack a decent pair of shades for this trip i.e. 100% protection from both UVA and UVB. Polarised lens are also a good idea; if you’ve paid all that money you might as well be able to see your destination as well as possible. For the relatively short time you’re up there you probably won’t need glacier glasses, but you’ll notice all the camp crew wearing them.
On the subject of UV, don’t forget the reflection of UV from snow can be >80% (compared to snow-free ground which typically reflects only 2-4 percent of UV and surfaces of water bodies which reflect about 5-8 percent), and that you will be at moderate altitude with greater UV levels anyway. We coated up with Riemann P20 sun block before we left. Don’t forget that because of the reflection baseball cap peaks won’t save you, and that even the underside of your chin or nose are at risk of exposure.
Despite the warm weather down at sea level we still dressed in lined hiking trousers (or jeans in my wife’s case), layered up with long sleeved cotton T-shirts under fleeces, and carried our windproof/waterproof overjackets. Hiking boots/shoes with thick hiking socks were donned, hats and gloves stowed in pockets, and we were ready to go…
The helipad is perched on the edge of the Gastineau Channel at 58°19’55” N, 134°29’50” W. The weather is not always this good as you can see from the photos on Google Earth at this location.
Before I continue with the tale of our day out with Era Helicopters, I’m going to get the logistical and financial details out of the way.
For 2016 flights for this trip are currently listed to run from the early afternoon of Monday 9th May until the late afternoon of Tuesday 9th August. Flights run 7 days per week in this period (with the exception of 12th, 15th, and 21st May), with between 3 and 8 flight departure times per day being offered for the Juneau Glacier Dog Sled Adventure. There are over 700 departure slots with starts as early as 7:15AM and as late as 5:15PM. However, at the time of writing, a couple of slots are already sold out and a few only have limited available seats remaining. If you’re going to only be in Juneau for a very specific timeframe get booking now; this may be the one trip of your vacation that you don’t want to miss. We might have just been lucky, as we had no problem when we selected our choice of a specific day and time for our flight, but if I was heading out for next summer I’d be booking now.
In 2016 booking directly with Era will cost you $555.00 per person if you weigh 239lbs (108.4kg) or less, and $655.00 if you weigh 240lbs (108.9kg) or more. Note that the full amount of your booking total will not be charged to your credit card until thirty days prior to your travel date, but, if making reservations within thirty days of your selected date, your card will be charged immediately.
You will need to declare your weight on booking, and if you are just scraping under the threshold it’s worth skipping a couple of meals before you arrive as “Due to [the] length of [the] tour and passenger loads, all passengers will be required to “weigh in” at the heliport. Passengers weighing in excess of 240 lbs. will be subject to a $100.00 surcharge to ensure adequate seating space.” Enough to pay for a blowout meal afterwards!
At the check-in you’ll also need to sign a waiver, and any medical conditions must be disclosed, but don’t worry because this is purely in your interests; Era are, as you’ll read below, a seriously reputable company when it comes to flight safety.
There are no carry-on bags permitted (although cameras are OK), and loose items will be stored securely at the heliport. The list of prohibited items includes drones, iPads, iPad minis, tablets, Go-Pro/selfie sticks and umbrellas.
There’s a minimum number of 4 passengers per flight. We had our family of 3 and 2 additional guests + the pilot, which is the maximum passenger seating in the AStar helicopters (see more below) used for this tour.
The vast majority of passengers come from cruise ships, and are collected from the Juneau dock terminal by personnel from Era’s ground staff operation. It’s only a 5.3 mile (8.5km) journey. If, like us, you drive yourself to the heliport, don’t expect a discount, and, more importantly, don’t be late.
If you book this trip through your cruise provider you can probably expect to pay a premium, but firstly, make sure you are actually getting the trip you want as there are several alternatives in the Juneau area (more on these below). Some examples of cruise ship companies offering this specific tour and their pricing are as follows.
Carnival Cruise Line call the Era trip the “Four Glacier Helicopter & Dogsled Adventure” (not to be confused with the “Dog Sledding on Mendenhall Glacier via Helicopter” shore excursion). Listed at only $549.99 per person, and with their guarantee to offer the best price for this trip – “Find a better price for any excursion we offer and we will refund you 110% of the price difference!” – that’s a whole $5.01 saving over direct booking. Unless you are over 240lbs. Carnival note that “guests weighing over 250 lbs [and this figure should probably be checked if you happily maintain your weight at 245lbs] will be required to purchase 2 seats (1½ tickets) on this excursion. You may acquire the second ½ ticket/seat […] after making your initial online purchase.” If half a ticket comes in at around $275 I think the $100 Era additional charge looks quite attractive by comparison.
Celebrity Cruises offer the Era package as a “Dog Sledding Adventure By Helicopter”. They charge $589.75 per person, and state that “Guests weighing 240 lbs or more will be assessed a weight surcharge” (but not how much this is).
Princess Cruise Line go with “Dog Sled Adventure by Helicopter” and charge $599.95 per person. They also note that “Prices are based on the amount Princess typically charges for each excursion, but your price may vary by voyage date and departure time. Weight surcharge ($130) may apply on this flight. Due to weight and balance limitations, as well as passenger safety and comfort, the helicopter companies have advised that guests weighing 240lbs or more (fully clothed) will be assessed the weight surcharge to reserve adequate space on board the helicopter. Guests weighing 240lbs or more should reserve an extra surcharge ticket and, once on board, go to the Tour Office to have the ticket charge adjusted down to the surcharge amount.”
Disney also go with the name “Dog Sled Adventure by Helicopter” and charge $619 (ages 10 and up), or $479 (ages 2 to 9). For two parents travelling with 3 children under 10 this booking rate would save $100 over direct booking with Era. This figure drops to $24 if they only have 2 young children, and with only 1 child they would need to think about borrowing an extra child, having another child themselves and delaying the cruise until that child was 2 years old (the minimum age for this experience), or just accepting they’re going to take an overall hit of $24. Or they could book direct with Era (especially if their children are over 10 years old). Disney also refer to the ‘half-seat’ surcharge.
If you’ve travelled into Juneau by air rather than by water you may have already had a sneak preview of at least part of the day’s destination. If you’re a) flying in from the south from Seattle, b) doing so in fairly good weather, and c) sitting in a window seat on the right of the aircraft, you’ll probably be admiring the mountainous coastline and several glaciers for much of your descent.
About 10 minutes before you land at Juneau international airport (JNU) you’ll pass Port Snettisham as you fly along Stephens Passage…
Gilbert Bay is the fork to the right and the Whiting River flows in from the NE. The northern fork to the left is the Speel Arm (with Fannie Island in the middle) and River. There’s a runway up there to access the Alaska Electric Light & Power hydroelectric plant which normally provides Juneau with most of its electricity via a 44 mile transmission line.
Around 4 minutes further on you’ll pass Taku Inlet with its amazing water colour variations and spiked promontories.
Look to the shore on your left which will give you a view of the terminus of the Taku glacier, and beyond in the distance, past the Hades Highway, the peaks of the Devil’s Paw (8584 ft/2616m) on the Canadian-U.S. border.
As you start to pass the mainland 5 minutes before landing there is a further brief chance to see the Taku Glacier:
That’s not a lake just above the centre of the image. Welcome to the wild Juneau Icefield.
Returning to the world of rotary aircraft, there’s an interesting article on Era’s roots and development over the years, and the company’s place in the Alaskan landscape here. With regard to Era Helicopters today, you’ll be flying with one of the top four international offshore oil and gas industry helicopter operators in the world. They also operate in the contract Search and Rescue (SAR) and air medical markets, so you can be assured that passenger safety is a critical priority for them.
The helicopter type used for Era’s flightseeing operations is the Airbus Helicopters AS350 (known as the AStar AS350 in the U.S.). It has a strong pedigree of use in inhospitable terrain, including such as decades of service with the Brazilian Navy for Antarctic environmental monitoring., and is also used by the other three helicopter excursion companies in Juneau (see further details towards the end of this post).
Era has a total fleet of 31 AS350 helicopters, 11 of which are based in Alaska and are used for tourist trips out of Juneau and around Denali.
In the AS350 B2 configuration for 5 passengers the pilot sits on the right, slightly forward of the two front seat passengers next to him, and there are three passenger seats behind.
The pilot will allocate the exact seating arrangements for passengers based on a determination of weight and balance, so you fly in and fly out in the same seating position. You will be provided with flight headsets on boarding.
Visibility is pretty good in the AS350, but keep in mind that at certain angles there may be slight reflections from the windows so keep on snapping those extra shots…
…and remember that if, like me, you’re dumb enough to place your coat against the front windshield it’s going to appear in lots of your photos! Zoom in to see my Berghaus jacket logo the Juneau-Douglas bridge.
Our Juneau Glacier Dog Sled Adventure started with a journey heading south down the Gastineau Channel, as per the image above. If you’ve already had time to explore the area this provides a fascinating new perspective. If you only have one day in town it still provides a unique view of the state capital of Alaska (and if you book your trip times wisely you’ll have the chance to squeeze in more opportunities around this tour).
Looking back at the view of Juneau (on the right) and Douglas (on the left) from the other end looked like this:
I’m pretty sure that taking in this view in person will stick with you for a long time… if you’re not overwhelmed by what’s still ahead.
From here we flipped right towards the mainland and climbed up to a hover above Sheep Creek in front of the north-west faces of Hawthorne Peak (4210 ft/1283m), Middle Peak (3722 ft/1134m), and West Peak (3620 ft/1103m):
Turning north-east, we flew up over the ridge to our left which descends from Mt. Roberts (behind us in the above image), following the line of the Sheep Fork between the Hawthorne and Powerline Ridges to its confluence with Carlson Creek, before cresting the rock and snowfields of Annex Ridge to the south-west of Annex Peak (4,170 ft /1,271m). Here we got a closer view of the Taku glacier ahead on the same line of sight as when we’d flown into Juneau a few days earlier:
A view all the way to the Devil’s Paw and Michael’s Sword, about 30 miles (48km) away.
Dropping down into the steep sided valley we flew over the mirror smooth surface of Glory Lake as the enormity of the Taku Glacier ahead began to hit home, but, as we exited over the end of the lake, Norris Glacier suddenly appeared on the left:
Note the trim line evidencing the rapidly receding size of the Norris Glacier.The terminus of the Norris Glacier. Go while it’s there to be seen.
Our pilot then took us down across Norris Lake towards the Taku Glacier:
Looking ENE across the huge expanse of the Taku Glacier terminus, with Grizzly Bar to the centre right and Taku Inlet just visible between the top edge of the glacier and the nearest of the far shore land mass on the right. To the far side of the Taku Glacier (by the small dark spur running down from the Brassiere Hills to Swede Point on the left in this image) is a distance of just over 4 miles (6.5km).
The Taku Glacier (now well over the 1995 calculation of 831 km2 (321 square miles) in size) is the primary outlet of the Juneau Icefield which covers an area of over 1,500 square miles (3885 km2), and stretches nearly 100 miles north to south and 45 miles east to west.
During the variably dated ‘Little Ice Age’ it is believed that the Taku Glacier extended out across the Taku Inlet creating an ice dam that caused the formation of a lake backed up into Canada (although others disagree about this). It has been noted that when Vancouver first visited the inlet in 1794 the Taku Glacier “was in an enlarged state, blocking the headward end of Taku inlet […]. He mentioned that ‘the basin’ was about 13 miles from the mouth of the inlet, indicating that the ice-front was not far from Taku Point. This agrees with the local Thlingit accounts of an ice barrier which prevented access to the interior valley of the Taku River ‘before the White Men came’.” This was contested in 1996 by Arne Friedmann who wrote “A detailed investigation of Taku Point showed, that the Taku Glacier ice front did not reach the eastern shores of Taku Inlet and the Taku River was not ice blocked. No large ice dammed lake reaching into Canada was formed in the 18th century.” Later still, the 1980 USGS Professional Paper 1386-K notes “As recently as about 1750, Taku Glacier was more than 3.5 km beyond its late 20th century position. At that time, it dammed Taku River at Taku Point. A large ice-dammed lake extended northeast into Canada.”
This image was produced from the USGS Professional Paper 1386-K “Satellite Image Atlas of Glaciers of the World, Alaska” (see the link at the end of the post) which in turn was created from a map adapted from Post and Motyka (1995).
Today the size of this ice river, flowing 36 miles (58km) from the north, and approximately 5¾ miles (9.25 km) long around the front of its terminus, is still awe inspiring.
The view up Taku Glacier from the terminus. To the left is Norris Mountain (4,125 ft/1,257m), and to the right the Brassiere Hills. Click on the image to enlarge it and get a better idea of just how striking the crevasses are from above.
This Era trip maintains a tradition of tourists visiting the Taku Glacier that is over 100 years old. For the 1896 edition of “Appletons’ guide-book to Alaska and the northwest coast” (the full title is a tad longer, but it’s still available as a reprint-to-order) author Eliza Ruhamah Scidmore wrote
“It is one of the show places on the Alaska coast, and is regularly visited by excursion steamers. The Taku Glacier was christened the Schulze Glacier in 1883, in honour of Paul Schulze, of Tacoma, and in 1891 was renamed the Foster Glacier, in honour of the then Secretary of the Treasury; but locally to geologists, tourists and navigators it remains Taku. The native Name is Sitth Klunu Gutta, “the spirits’ home.” It is Sitth too Yehk’s, the ice spirit’s, very palace of delight, and the fabled man-faced seals with their human hands live and frolic in its clear blue grottoes and crystal dells. The ice-stream, a mile in width, fills its canons from wall to wall, and is squarely broken front rises from 100 to 200 ft. above the water. It is one of the purest and cleanest glaciers, without medial or apparent lateral moraines, and deeply fissured and crevassed for the 5 miles of its course which is visible from the water. Because of its purity, ships prefer to fill their ice-boxes in this basin, and the process of lassoing the icebergs and hoisting them on board is an interesting feature in ship life.”
From our helicopter seats in 2013 the view of Taku Glacier was no less than amazing, but there was a lot more of it to be seen than in 1896. Extending its length by 4.8 miles (7.3km) between 1890 and 1990, the tidewater Taku Glacier stopped calving into Taku Inlet in 1948 (elsewhere stated as 1953) which allowed it to advance across its own outwash delta.
The amount of sediment deposited into the Taku Inlet by the glacier had eventually stopped steamships and their descendants from getting up to a viewing position, and later prevented even lighter keeled craft from making a reliable viewing journey; these days you need either an airboat, a hovercraft or a kayak to get to the glacier by water (see the airboat trip reference link at the end of this post).
Taku Glacier maintained an extremely positive mass balance between 1948 and 1988, but since then a slightly negative mass balance has been recorded, and between 1990 and 2000 its advance effectively halted, although the terminus height continued to rise at an average rate of 1.4m per year. In the summer of 2001 the Taku Glacier started advancing again at a rate of between 10-30m per year, and it has often been cited by comparison with other significant Juneau Icefield glaciers as being the only one which was still expanding. However, as reported in the Juneau Empire in September 2015, the advance of Taku glacier has stagnated since 2013. No longer constrained by mountainous sides, the broad bulbous terminus means that the glacier has more area to expand across with less mass to drive forward movement.
Eventually, Taku Glacier will withdraw, underlying silt will be washed out, and a mighty 50km fjord will be created in place of the deepest and thickest alpine temperate glacier known on the planet (the Juneau Icefield Research Program (JIRP) which has studied the Taku Glacier since 1946, recorded a maximum measured depth of 4855 ft (1480m)).
With a glacier of this size, that will not be happening anytime soon, and it will remain as a spectacular site to visit for decades. However, whilst no one appears quite sure as to whether the ‘advance’ stage of a tidal glacier’s lifecycle is currently ending for the Taku Glacier, I’m glad we were there to see it at its possible maximal extent for the foreseeable future.
Our view of the Norris Glacier terminus was returned in this shot…
The view looking south-west from the edge of Taku Glacier over Norris Lake to the retreating Norris Glacier terminus and Glory Lake.
Norris Glacier began its retreat prior to 1890, but when it reached its fullest extent in 1911, it still stretched out around the spur descending from Norris Mountain (to the centre right in the above image), across what is now a lake, and onto the northwest shore of Grizzly Bar (the low lying tree clad land in the centre left of this image). As late as 1929 there was still no proglacial lake. Today Norris Glacier has retreated to the extent that it barely scrapes over the rock edge of the lake. For more on the retreat of Norris Glacier see the links at the bottom of this post.
Rather than returning over Norris Lake we hopped up and straight over the Loon Lakes and Oona Lake on the spur of Norris Mountain to view the Dead Branch of Norris Glacier which floats on its own melt water during the summer:
There’s another shot of the Dead Branch further down this post where some of its enormous glacial crevasses can be even more clearly seen.
Turning left into the Middle Branch of Norris Glacier which lies between the Dead Branch and Death Valley, we descended towards our drop off at the Alaska Heli-mush sledding camp:
To give you an impression of the scale of this place, there’s a camp with kennels for about 150 dogs, and tents for staff accommodation, a vet, cooking and eating, etc., right in front of your eyes in this image.
From take-off at the heliport to set-down at the camp had only taken around 18 minutes, but it had felt like a much longer trip with all that we’d had to see and take in.
Leaving our lifejackets in the helicopter, the obligatory family arrival photo was taken (through the fade of memory, I think we were offered to purchase a print on our return to base, which we declined in favour of the image below which the base crew took with our own cameras):
We were then introduced to our guide, who kindly took another family photo for us, explained a little about the rigging, ran through the procedures for controlling a dog sled, and we were nearly ready for the off.
The dogs closest to the sled are the main powerhouse whilst the lead dog is trained as the team direction guide.
The nine dogs were to pull all four of us, with my wife at the front of a two-seater touring sled and our guide driving on the runners, whilst my daughter stood on the runners and I sat in the bucket seat of the lighter sled (as pictured above) coupled a few meters behind. Although it was less about personally mushing a dog team and more about being towed around, the feeling of almost silently speeding across the bleakly beautiful landscape (and in my daughters’ case, also learning how to lean/steer the sled) genuinely made it a memorable experience to have shared together.
The Middle Fork is more than large enough to host several groups of helicopter passengers sledding at the same time, and it took around 20 minutes to complete a large clockwise circuit out across the snow before returning to camp.
A view from a sled. The peak is Split Thumb (4,993 ft/1,522m) at the south-west extreme of the Middle Branch. On the other side is Lemon Creek Glacier
After the sled ride there was a chance to meet some of the dogs up close:
1 hr 10 minutes after landing at the camp we returned to the skies…
…but as the tents and kennels on the Middle Fork of the Norris Glacier shrank in the distance (they’re in the middle of the photo) the trip was far from over.
Bearing in mind that I’d never been to Alaska before, and had very little prior knowledge of the geography of the Juneau Icefield i.e. had no idea where we were going, the following photos are included purely to give you an idea of what you might see on the way back to Juneau (the route will vary according to the prevailing weather, but we were lucky enough to see all of this during our flight). I’d be very happy to see advice in the comments section to better identify specific locations, name peaks, etc.
Heading north out of the Middle Branch of Norris Glacier towards Guardian Mountain (5059 ft/1542m). The gap to the right leads up to the North Branch of Norris Glacier or by turning right to the south-east, back down the glacier to Taku Inlet. The route to the west leads to Death Valley.
We took a route that headed north-west across Death Valley towards Echo Pass and Amherst Peak, climbing and dropping with the landscape, and then followed an anti-clockwise arc around the upper end of the valley and down towards Nugget Mountain. The two Era helicopters in front added some perspective to the raw landscape – you might be able to spot them in some of the other photos if you enlarge the images enough – and later gave me some clues about the direction of our travel over the Juneau Icefield.
Death Valley, Alaska Style, looking north-west. If you draw an imaginary line between the two helicopters ahead (there’s one in the center of the image and another out towards Echo Pass) and carry it on to the peaks on the far horizon, I think you’re looking at the Mendenhall Towers.
Back over the Middle Branch Norris Glacier with a view of the dog camp far below and the Devil’s Paw out on the horizon.Passing by Split Thumb at the upper end of the Middle Branch Norris Glacier.The Dead Branch Norris Glacier showing the crevasse fractures, and a final glimpse down to Taku Glacier.
Heading upwards and over towards Lemon Creek Glacier.Flying over the Lemon Creek Glacier you get a good view of the JIRP Camp 17. On the other side of the nuntak is Ptarmigan Glacier.Flying out of the Juneau Icefield.Heading down past Observation Peak and over Salmon Creek Reservoir. The dam was built in 1914. This is the secondary drinking water supply for Juneau and its hydroelectric generation provides about 10% of the city’s power.Leaving the trees of the valley behind and emerging over the Gastineau Channel.Safe return to the helibase with Era Helicopters.
The question you might still have at this point is whether a 1 hr 35minute trip is worth $555.00 per person. The answer is simple and emphatic. Yes. Would I do it again? Not necessarily.
I wouldn’t want to have missed sharing any of this trip with my family, but the experience also brought the realisation of just how much there is to see around Juneau. A helicopter flight is the perfect (and in some instances the only practical) way to access so much of the Juneau Icefield, and I’d have no hesitation in flying with Era Helicopters again, but I might also look around for a different excursion next time.
Alternative trips
Era Helicopters also offer
An Extended Juneau Glacier Dog Sledding Tour where you get 2.5 hrs at the Alaska Heli-mush camp (and a longer sled ride experience). It is currently booking from 10 May to 2 September 2016 (not every day), departing at 11:15AM only. Booking directly with Era will cost you $735.00 per person if you weigh 239lbs (108.4kg) or less, and $835.00 if you weigh 240lbs (108.9kg) or more.
The Juneau Pinnacle Experience with “up to 65 minutes of flight time and 2 unique landing locations (15-20 minutes each).” It is currently booking from 30 April to 12 August 2016 (not every day), departing at 10:00AM only (most dates). It looks as though there’s just one helicopter currently scheduled to run this service, so advanced booking would be sensible if you want to ensure a seat on a specific date. Booking directly with Era will cost you $650.00 per person if you weigh 239lbs (108.4kg) or less, and $750.00 if you weigh 240lbs (108.9kg) or more.
Taku Glacier Adventure in Juneau with approximately 30-35 minutes flight time (depending upon flight route due to weather) and 15-20 minutes on the glacier (Norris Glacier is an alternative). There are only two currently listed dates for 2016 and they are both sold out, but it would be worth checking back to see if they add more dates later.
There are a number of other providers of helicopter-based tourist excursions from Juneau.
Coastal Helicopters fly out of Juneau International Airport:
The Coastal Helicopters base at JNU. Mt. Mc Ginnis (4228 ft/1289m) and Stroller White Mountain (4833 ft/1473m) rise in the background.
They offer a range of trips including
A 1 hr Icefield Excursion for $290 to walk on either Herbert, Taku, Lemon or Norris Glacier.
A 1.5 hr Dog Sled Tour for $510 on Herbert Glacier. There’s also a 2 hr extended version of this trip with an additional landing elsewhere on Herbert Glacier for $580
NorthStar Trekking fly out of JNU and offer three options on the same model (pricing appears to be on application or check your cruise shore excursions listings) with a c.30 min. helicopter ride out to either Mendenhall, Taku, Norris, Herbert, Gilkey, Battle or Thiel Glaciers, followed by ice field trekking:
Extended Helicopter Glacier Trek. 3 hrs of trekking and climbing on a glacier. There’s a great series of shots to accompany an account of this trip taken in 2015 here.
Temsco Helicopters fly out of JNU to offer several options for tourists (pricing again appears to be on application or check your cruise shore excursions listings) including
A 55 min. Mendenhall Glacier Tour (includes a 20-25 minute landing/guided walk, and flight out to Mendenhall Towers). In 2015 Fodors listed the Temsco flightseeing trip to Mendenhall Glacier as #8 of 22 of the World’s Most Amazing Helicopter Rides.
A 1 hr 30 min. Dog Sled Tour: Juneau on Mendenhall Glacier. 30 min. flight time and 55-60 min. at the dog camp (20-25 min. of dog sledding).
More online information.
Words to learn before you go. A Glossary of Glacier Terminology from the USGS. There are also lots of great pictures, many of which, unsurprisingly, come from Alaska.
Alaska Heli-mush: the people behind the dog sled camp on the Era tour.
The Crevasse Zone contains lots of interesting information and images of the Juneau Icefield.
From Icefield to Ocean neatly summarizes the importance of Alaska’s coastal glaciers in an award-winning poster.
For topographical maps use the USGS Map Locator and Downloader service (also great for the rest of the USA). Norris Glacier mostly falls into the AK Juneau B-1 area. Download the multi-layered .PDF files for later reference, but keep in mind the most recent version is from 1997.
We’ve been lucky enough to stay in some pretty good vacation accommodation over the years, but back in August 2010 we booked a three-night out-of-town stay at a small family-owned riverside property in the U.S. state of Washington (WA), and we’ve tended to compare cabins to this great experience ever since.
The Sol Duc Riverside Cottages lie alongside the eponymous river, downstream of the Sol Duc falls, on Olympic Highway 101 in the north of Washington state between Forks and Port Angeles.
Having travelled over to Clallam County on the ferry from Vancouver Island this was the perfect location for a few days exploring the northwest of the Olympic Peninsula, and we would have booked four nights had there been availability (we started our enquiry and booking process the previous November/December). The first tip for Sol Duc Riverside Cottages is therefore to plan ahead, and check that you can get in. If you can’t, change your vacation dates.
The website also lists the extensive array of amenities that are provided with each cabin, and there’s a good selection of images in the slideshow gallery.
So what else can I tell you…
We arrived from the Forks direction in the late afternoon after a day spent visiting the nearby Hoh River rainforest and First Beach at La Push in the Quileute nation tribal lands. There are three cabins on the property. Cedar Breeze is the original cabin, and the one we stayed in. There’s also the smaller Loft Studio, and the newer Riversong cabin (the family of five from Minnesota who were staying in Riversong at the time of our stay were the first guests to do so. We both eagerly inspected each others cabins, and while I’d stay in either, I still think we picked the best one).
Cedar Breeze and The Loft cabins at Sol Duc Riverside Cottages
We parked up – plenty of space – and entered using a pre-arranged key code…
First view of Cedar Breeze.
…and that was pretty much the end of our travels until it was time to leave. That might sound unremarkable for a vacation. However, we’re a family who might occasionally plan a ‘chill out day’ or two, but we generally tend to find a base and then head off to the surrounding world. “Shall we just stay here instead of going out today?” just doesn’t enter our normal vacation vocabulary. Once my wife and daughter had walked through the door of Cedar Breeze that was it. I was even sent off on my own to buy some steaks for the BBQ from Forks Outfitters.
Don’t get me wrong; the Hoh River and rain forest were great, La Push is worth the effort, and I wouldn’t have wanted to miss our arrival day drive up to Hurricane Ridge or our departure day detour to the Upper Sol Duc and lakes along the 101. They’re all recommended, and places I’d like to see again. I could also imagine spending some future time in the dozens of other places in easy reach of the Sol Duc Riverside Cottages… but I’d make sure that I had enough time to just hang out at the cabin too.
Owners Brenda and Ted Abrams have spared no effort in creating the most comfortable and extraordinarily well equipped vacation retreats at the Sol Duc Riverside Cottages, and the properties are maintained both inside and out with exemplary care.
The interior of the Cedar Breeze cabin from the front doorCedar Breeze cabin interior view from the kitchen area.The separate bedroom in the Cedar Breeze cabin
Cleverly fenced and screened, the Cedar Breeze cabin also appears to be remarkably private whether you’ve retreated to the open-plan interior or are spending your time on the large covered deck.
The view down to the river across the Cedar Breeze cabin deck. The hot tub is to the left. I’ll have to use a wide angle lens next time.
The weather was also a winning factor during our stay . We visited in early August when the temperatures ranged from a maximum high of between 63°F to 66°F (17°C to 19°C) in the day time to a low of between 51°F to 54°F (10.5°C to 12°C) – you might get lucky as for the same date range in 2015 the high was 72°F to 75.9°F (22°C to 24.5°C) while the low was about the same at 48°F to 55.9°F (9°C to 13°C) – and there was a fair bit of fog out on the coast, but the c. 3000ft (900m) coastal strip of the Northwest Olympics rising above the cabins in the valley seemed to hold back the mist, at least for a couple of days…
Looking back from the river, the Sol Duc Riverside Cottages in the August sunshine.There’s a reason these forests are so green and vibrant. The River Song cabin under the mist on our departure day.
We were certainly warm enough whether simmered, toasted or roasted:
The Cedar Breeze hot tub at Sol Duc Riverside Cottages. There are other pictures of me in there with sunglasses on but I’ll spare you those.Toasted toes with wifi in the Cedar Breeze cabin at Sol Duc Riverside CottagesThe fire pit at Sol Duc Riverside Cottages
Maybe it was the rich (and sometimes entertaining) wildlife that kept our company around the cabin. There are several interesting terrestrial mammals in the area worth keeping your eyes and ears open for (see a full list here), including
River Otter (Lutra canadensis) – listen for their barking from the river in the night
Roosevelt Elk (Cervus canadensis roosevelti)
This was a close as we came to a Cougar. They apparently favour raking Maples to mark the limits of their territorial range.Chipmunks were frequent visitors around the cabinMy wife enjoyed playing hide-and-peek with Douglas Squirrels inquisitively running around tree trunks
Birds were also prolific around the Sol Duc Riverside Cottages, and while we were only treated to a couple of brief sightings of American Bald Eagles calling along the river just after our arrival, good numbers of smaller avian species were present throughout our stay. We saw American Dippers (Cinclus mexicanus) on the river, Pine Siskins (Carduelis pinus) on the feeders. and Steller’s Jay (Cyanocitta stelleri) and American Robins (Turdus migratorius) around the lawns.
As for the Sol Duc itself, with a 400 ft (120m) stretch flowing westward along the southern border of the property, it is the jewel in the crown of the natural setting here. The name is derived from the Quileute name which means “sparkling water”…
The river looking upstream at Sol Duc Riverside CottagesLooking downstream, the Sol Duc at low summer levels
Fabulously clear, we found dozens of intricate and varied Caddisfly larvae cases in the river, which were brought back across the lawn to inspect on the deck in the belief they were empty. Once placed on a glass table surface they invariably proved to still be inhabited, prompting a quick dash back to the river.
The crystal clear water of the Sol Duc River teams with tiny lifeWatch where you step! There is an abundance of Caddisfly Larvae in the Sol Duc River attesting to its biological cleanliness
Despite the fact that the Sol Duc is the only river on the Olympic peninsula to support all five species of Pacific Salmon, we didn’t see any of them in the low water conditions. However, this was not a problem as it meant that we could wade across the breadth of the river along the property’s banks without either drowning (although there were a few deep holes avoided) or disturbing any spawning fish.
A stout stick is a good idea to help wading and checking depths even at low levels
This vacation was five years ago, but the memories are undimmed, and the challenge set by our benchmark cabin still stands. Since that summer there have been a few close contenders (and even near equivalents on their own local terms, which I’ll probably post about), some reasonable efforts, and a few places that never stood a chance. All you have to do to match the Sol Duc Riverside Cottages is to be able to write what we put in the guest book before we left: “This place is absolutely perfect.”
More online information.
If you’re there in the fall American Whitewater lists seven sections for kayakers ranging from grade II to IV+. Just scroll down to get to the Sol Duc entries. More on the Sol Duc for paddlers from the Whitewater Guidebook. For rafting (and more) try Rainforest Paddlers Inc.
The Forks Chamber of Commerce website includes a directory of places to eat out locally – if you can drag yourself away from your cabin.
The National Park Service website for the Olympic National Park. There is loads of information here, so hunt around.
![The area of our trip from Anchorage to Beluga Lake [Base terrain map data © 2016 Google].](http://www.afewmilesmore.com/wp-content/uploads/2016/03/Anchorage-to-Beluga-and-Strandline-Lakes-1.png)
![The area covered by the Susitna Flats State Game Refuge. [Source: ADG&F]](http://www.afewmilesmore.com/wp-content/uploads/2016/03/Susitna-Flats-State-Game-Reguge-Matanuska-Susitna-Borough-Mat-Su-Cook-Inlet-Anchorage-Alaska.png)
![Heading west, looking south. Beluga Lake with the start of the Beluga Rover to the left, with the Chichantna River flowing left to right in the background.]](http://www.afewmilesmore.com/wp-content/uploads/2016/03/Beluga-Lake-and-the-Chichantna-River.jpg)
![The flooded shoreline where Coal Creek enters Beluga Lake.]](http://www.afewmilesmore.com/wp-content/uploads/2016/03/New-shoreline-at-Coal-Creek-Beluga-Lake-Alaska.jpg)
![Rachael sporting her then new Alaska Geographic buff which has since become her standard accompaniment to any cold weather.]](http://www.afewmilesmore.com/wp-content/uploads/2016/01/Stella-Air-flights-are-pretty-relaxed.jpg)
