Cruising the Eastern Arctic – Ilulissat

I have been on safari in Africa; I’ve crossed the Andes and walked the streets of Paris, London, Rome, Athens, Tokyo, Hong Kong, Bangkok and Buenos Aires. But August 2nd was one of the most memorable and magical travel days in my life. It was a glorious morning as we awakened in Disko Bay off the central coast of West Greenland and gazed out at the massive icebergs littering the calm ocean surface. Disko Bay or Qeqertarsuup tunua in Greenlandic, is considered a southeastern inlet of Baffin Bay.

Overnight, we had sailed north from Sisimiut (which was the subject of my last blog) and navigated around Disko Island into this bay or “bugt”, as it’s called in Danish.  That massive white expanse covering most of Greenland (the largest island in the world) on the Google Earth photo map below is ice, some 1.71 million km² or 660,000 square miles. Greenland’s ice sheet (also known as Inland Ice) covers 79% of the country and is second only to the Antarctic ice sheet, which is ten times as big. Together, Greenland and Antarctica contain almost three-quarters of the world’s fresh water. At its thickest point, Greenland’s ice sheet is 3 km (1.79 mi) thick with a volume estimated at 2.85 million km3 (684,000 mi3).  Greenland has more than 100 glaciers (e.g. Kangerlussuaq, Helheim, Petermann, Hiawatha, Kong Oscar, Midgard) that flow out through its rocky margins each summer and send icebergs into the sea, but the Jakobshavn Icefjord or Isbrae (Danish) – Sermeq Kujalleq (Greenlandic) is the biggest, and the one we were here to see.

Fishboats were out in the bay, its waters rich in halibut, cod, Atlantic redfish, Arctic char and wolffish.

These guys just heading out were as curious about us as we were about them.

I loved the cheerful colours of this little fishing boat….

….. and the contented look of the fisherman about to head to work.

Turning towards shore, we saw the village of Ilulissat with its colourful houses arrayed up the rocky hillside under a massive mountain wall. (Greenland has myriad mountain ranges, many still unnamed). Established as a trading post by Danish merchant Jakob Severin in 1741, it was originally known as Jakobshavn. The third-largest city in Greenland after Nuuk and Sisimiut, Ilulissat has a population of 4,670 (2020).

Kalaallisut is the Greenlandic language of West Greenland (East Greenland has its own) and the Kalaallisut word for “icebergs” is Ilulissat! So there was no question why we were here; indeed, this is the town closest to the Ilulissat Icefjord UNESCO World Heritage Site that we were about to visit.

The hotel in the distance is one of three in town catering to tourists and scientists. In 2015, there were 22,000 international tourists and 15,000 local tourists, with the majority coming in July and August.

A plane passed overhead bringing passengers from Iceland as part of a seasonal schedule.

When Zion Church (Zion’s Kirke) was dedicated as a Lutheran church in 1779, it was the largest man-made building in Greenland. According to the Geological Survey of Denmark website, “During the Napoleonic Wars supplies from Denmark were limited, and the time from 1807 to 1814 in particular was a period of great hardship. In Jakobshavn, the hunters were forced to re-melt the lead from the roof and windows of the Zion Church in order to make rifle bullets.” It was moved to this location from lower ground in 1929, and services continue there today.

I admired these rocks at the shoreline, below. According to Canadian geologist, Dr. Marc St-Onge, Senior Emeritus Scientist at the Geological Survey of Canada, who has worked throughout the Arctic: “The bedrock geology of the Ilulissat region comprises dominantly 2.84–2.76 billion years old Archean orthogneiss (gneiss derived from a plutonic precursor), reworked and metamorphosed 1.88 billion years ago by the Nagssugtoqidian orogenic belt.”  In fact, Greenland has some of the oldest known Archean rocks on the planet, with a zircon crystal from the tonalitic gneiss protolith (the original rock before being metamorphosed) at Amîtsoq near Nuuk U/Pb-dated to 3.872 Ga (Giga annum or billion years ago). Incidentally, the Greenland rock is younger than the oldest-known exposed rock in the world, the Acasta Gneiss dated at 4.02 Ga and found in 1983 by Dr. St-Onge and his geologist wife Dr. Janet King 300 km north of Yellowknife, in Canada’s Northwest Territories. 

Once docked, we set off on foot to the outskirts of Ilulissat, passing the inevitable sled dogs on the way.

Before long, we arrived at the boardwalk leading to the edge of the icefjord.  The boardwalk passes through the Sermermiut Valley, which was once an Inuit settlement. At 1.4 k (.87 mile) in length, it is a pleasant, easy hike, but one with a spectacular terminus that showcases one of the planet’s most awe-inspiring phenomena.

I marked the Google Earth map below with yellow arrows to show the boardwalk and its relationship to town.

It is simply impossible to describe how thrilling it was to walk through this gentle meadow with its delicate little ecosystems of plants and ancient rock toward this massive parade of glacial ice slipping, sliding and booming towards the ocean.

In 2004, as it was creating the International Heritage Site designation, UNESCO described the site and determined that it met two criteria:

The combination of a huge ice sheet and a fast-moving glacial ice-stream calving into a fjord covered by icebergs is a phenomenon only seen in Greenland and Antarctica. Ilulissat offers both scientists and visitors easy access for close view of the calving glacier front as it cascades down the ice sheet and into the ice-choked fjord. The wild and highly scenic combination of rock, ice and sea, along with the dramatic sounds produced by the moving ice combine to present a memorable natural spectacle.

The Ilulissat Icefjord is an outstanding example of a stage in the Earth’s history:  the last ice age of the Quaternary Period. The ice-stream is one of the fastest (40 m per day) and most active in the world. Its annual calving of over 46 km3 of ice accounts for 10% of the production of all Greenland calf ice, more than any other glacier outside Antarctica. The glacier has been the object of scientific attention for 250 years and, along with its relative ease of accessibility, has significantly added to the understanding of ice-cap glaciology, climate change and related geomorphic processes.”

As usual, I was distracted with all the photography opportunities in the meadows flanking the boardwalk, and had to hurry along to catch up.  (Thankfully, my friend Anne snapped this photo of me, something that rarely happens when I travel.) It was so warm that lovely day in the Arctic, I didn’t need the jacket I’d brought along. However, according to the World Metereological Organization, Greenland also boasts the lowest temperature ever recorded in the Northern Hemisphere, -69.6 C (-93.3 F) on December 22, 1991 at Klinck, with an elevation of 3,105 metres near the topographic summit of the Greenland Ice Sheet.

The calved ice loomed ahead, but I also loved seeing all the plants, like ubiquitous Scheuchzer’s cotton grass (Eriophorum scheuchzeri)…..

….. with its fluffy white fruiting heads.

The meadow was a tapestry of heath plants, blueberries, mouse-ear chickweed, willow and….

…. dwarf birch (Betula glandulosa).

In the damper spots, mushrooms emerged from luxuriant carpets of moss.

Greenland bellflower grew in drier places, (Campanula rotundifolia subsp. gieseckiana).  

Alpine catchfly (Viscaria alpina) showed off its magenta flowers.

A little Lapland longspur (Calcarius laponicus) eyed me as it ate a seed.

Nearby, creeping crowberry (Empetrum nigrum) was exhibiting serious browning, a result of warm weather.

Tufted saxifrage (Saxifraga caespitosa) is one of ten saxifrage species that grow in the meadows, according to the UNESCO list of flora.

Everyone had their cameras out.

The boardwalk took us down near the meadow’s edge, where the sheer majesty of the icefjiord was on display.

You could view it from there….

….. or from the top of the rocky cliff overlooking the fjord. This was one of my favourite photos from the entire trip, simply showing the scale of the massive icebergs clogging the fjord.

Sometimes the word “spectacular” is just not descriptive enough.

There were stairs to a higher location for those who wanted a different vantage point. In fact, there are a few marked trails for those who want to venture further on the site.

From up there, I looked down on Adventure Canada’s intrepid photographer, Dennis Minty, whose photos from the various expeditions are simply beautiful.

If we ventured too far down on the rocks, someone would yell: “Move up further. If one of those icebergs cracks and breaks away, the tsunami would wash you away.”

Visitors are also warned not to stand on the rocky beach along the fjord.

To get an idea of how daunting the tsunami waves can be, have a look at this video showing a massive iceberg cracking, then turning over: 

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According to Wikipedia, “Some 35 billion tonnes of icebergs calve off and pass out of the fjord each year. Icebergs breaking from the glacier are often so large (up to a kilometer in height) that they are too tall to float down the fjord and lie stuck on the bottom of its shallower areas, sometimes for years, until they are broken up by the force of the glacier and icebergs further up the fjord.” 

What we were looking at from our vantage point was the mouth of the glacier with its iceberg-clogged fjord. We couldn’t actually see the ice sheet itself, but it must be something to fly above its massive expanse and gaze down in summer at the meltwater lakes and rivers, as shown in the NASA photo below. Research on the ice sheet takes many forms, from Landsat and Grace Satellites with radar probing imagery to determine ice loss to long-range high-tech-equipped flights over its surface.  A project called GreenDrill planned for an area near the Hiawatha Glacier in north Greenland aims to drill down into bedrock to determine the last time the ice disappeared. Last year, researchers discovered that, rather than retreating as it had done for the past few decades, Jakobshavn Icefjord had actually slowed, re-advanced and thickened for three consecutive years, mainly due to colder ocean temperatures at the outlet in Disko Bay.

Photo by Maria-José Viñas-NASA Earth Science News Team

The photo below shows Swiss Camp, run by the Cooperative Institute for Research in Environmental Sciences at the University of Colorado Boulder and set up to study the Jakobshavn glacier. Tragically, its long-time director Konrad Steffen fell into a crevasse on the ice sheet and drowned on August 8, 2020.  

Photo by Lino Schmid & Moira Prati – Licensed under
Creative Commons Attribution-Share Alike 4.0 International

Operation Ice Bridge has collected data from Jakobshavn Glacier itself for many years. In the video below, you can see the actual calving front.

I love this photo because it contrasts two different planetary timescales:  Archaean rock that is more than 1.8 billion years old and icebergs containing frozen water that might be tens of thousands years old.   

To view a truly stunning gallery of images from Ilulissat, have a look at this site featuring the work of photographer Kristjan Fridriksson.

Returning from the icefjord to town was a little anticlimactic, to say the least, but it was lovely to come down to earth at the museum that was the home of famous Greenland explorer Knud Rasmussen (1879-1933).

The son of a Danish missionary and his Danish-Inuit wife, Rasmussen became an explorer and anthropologist, making seven expeditions between 1912-33 throughout Greenland and Arctic Canada as far west as Nome, Alaska.

Rasmussen was the first European to cross the Northwest Passage via dog sled.

The front door of the Rasmussen museum opens onto a spectacular view of Disko Bay – a view that likely remains mostly unchanged from his days in the house.

We inspected a typical Greenland sod house at the front of the Rasmussen museum.

Then we walked to the top of Ilulissat for a good view of the bay and a quick stroll through the residential neighbourhoods.

This house might have won the Greenland colour prize, but all the houses seemed to celebrate brilliant colour – not surprising in a place where winter lasts most of the year.

The ubiquitous false mayweed (Tripleurospermum maritimum) was in full bloom. Such a lovely native, adapted to growing in the salty air and soil of the far north seaside.

After lunch on the ship, it was time to head out on a Disko Bay zodiac excursion. The captain in this zodiac was marine biologist Deanna Leonard-Spitzer, who did the whale-spotting on our expedition.

We got as close as we could to the big calved icebergs. Given that only 10% of an iceberg is above the water surface, you get an idea here of the size of these monsters.

Photographing icebergs is a little addictive.

Although I had been warm enough to take off my coat walking down the icefjord boardwalk, being out on the water was definitely cooler.

Seagulls enjoyed perching on the icebergs as they fished. I think these are Iceland gulls (Larus glaucoides glaucoides).

For the most part, icebergs are sparkling white with the accumulated snow from… who knows how many winters?  Icebergs, after all, are just massive aggregations of winter snow that has fallen on the ice sheet – packed, condensed, frozen, surface melted, refrozen, repeat, repeat, repeat – before finally calving off from glaciers in chunks and floating away in the ocean While 96.5% of earth’s water is saline, ice sheets, glaciers and permanent snow account for 1.7% (the balance is groundwater and lakes, etc.) with the Greenland and Antarctic ice sheets accounting for 68.7% of earth’s freshwater. That massive volume combined with an increase in global warming  resulting in melting of the ice sheets leading to sea level rise is one of the major focuses of climate scientists today.

We cruised past an iceberg beginning to melt and noticed the soot embedded in the snow. Scientists have noticed an increase in darkened snow on the ice sheets (and even in the snow atop the Himalayas) due to soot from forest fires and pollution; that darkness becomes a positive feedback loop by reducing the albedo in the ice sheet and absorbing more solar radiation, resulting in faster melting.

At the base of the iceberg, you could see the air bubbles that form part of the iceberg’s structure. These bubbles, trapped between snow layers year after year become part of the ice. When cored as part of ice sheet research, they give scientists many clues as to the composition of the atmosphere at the time they were formed, and now.

For an excellent article on The Secrets in Greenland’s Ice Sheet, read Jon Gertner’s masterful 2015 story in the New York Times Magazine. He has also written a book called The Ice at the End of the World, available in paperback from Penguin Random House.

After our zodiac tour and dinner on the ship, we were treated to a dance party by Adventure Canada’s entertainer, Thomas Kovacs.  These social events were such fun and the resource staff participated on each occasion….

…. including photographer Dennis Minty, left, and now-retired Adventure Canada founder Matthew Swan, right, whose daughter Cedar Swan is now CEO of the company

While I loved hearing them sing, as the skies darkened I found myself drawn to the quiet of the nearby deck where I was transfixed by the icebergs, now dark mauve in the golden twilight, the seabirds wheeling, the Greenland coastal mountains hulking behind.

I felt so privileged to have seen this remarkable place, to have the opportunity to glimpse the setting for one of earth’s most critical and endangered systems, and to expand in a small way my understanding of the Arctic.

*******

This is the 6th in my Eastern Arctic blog series. Be sure to read about:

Iqaluit

Butterfly Bay and the Waters off Baffin Island

Pangnirtung

Sunneshine Fjord

Sisimiut

Hiking Under Aoraki Mount Cook

Of the three January 2018 weeks we spent touring New Zealand on the American Horticultural Society’s “Gardens, Wine & Wilderness” tour, without a doubt my two favourite outings were our overnight voyage on Doubtful Sound in Fiordland and the day we hiked the Hooker Valley Track under the country’s tallest mountain, Aoraki Mount Cook.  That’s not to say I don’t love gardens, but for me there is simply no garden that compares with the one that nature conjures in places that we have not disturbed. So it was with great excitement, a few hours after lunching at Ann & Jim Jerram’s lovely Ostler Wine vineyard in the Waitaki Valley that we found ourselves standing beside Highway 80 on the shores of Lake Pukaki, staring in awe at the majestic mountain in the distance.  Every camera and cellphone came out.

You can see why the Māori of the South Island called their sacred mountain Aoraki, or “cloud piercer”.  (I’ll tell you more of their founding legend later.)

We continued driving Highway 80 (aka Mount Cook Road) along the shore of Lake Pukaki on our way into Aoraki Mount Cook National Park. As at Queenstown, we saw invasive “wilding conifers” along the shore – in this case, lodgepole pines (Pinus contorta), left, from western North America. Introduced into New Zealand in 1880, the trees were intended to “beautify” the lakeshore but have invaded throughout the Mackenzie Basin.

Like Lake Louise in Canada’s Banff National Park, Lake Pukaki appears turquoise because its waters consist of glacial melt from the mountains we’ll see over the next 36 hours. In the meltwater is superfine “rock flour” or “glacial milk” consisting of rock that has been pulverized into fine powder by the grinding action of ice as the glaciers melt and retreat.

Though I wouldn’t really understand the hydrology here until I came home and studied maps, we then drove over a small stream wending its way out into Lake Pukaki’s northern shore.  This, I would learn, is a channel of the Tasman River, which empties both the Hooker glacier and massive Tasman glaciers in adjacent mountain valleys in the park. Now at the height of New Zealand summer, it was not a big flow, but I imagine these braided channels roar in springtime when the gravel floodplain accepts the snowmelt.

Moments later, we arrived at the 164-room Hermitage Aoraki Mount Cook Hotel that would be our home for the next two nights. Built in 1958 and extended several times, this is the third incarnation of the mountainside hotel.  The original, built in 1884 by surveyor and Mount Cook ranger Frank Huddlestone, was sited further into the valley near the Mueller Glacier. It was taken over by the New Zealand government in 1895. As visitors started pouring into the region, the hotel could not keep up with the demand for rooms, and was also subject to seasonal flooding, which ultimately destroyed it. In 1914, a second hotel was erected; it would host four decades of guests, including a young Edmund Hillary and his climbing mates who bunked here during their 1948 ascent of Mount Cook. Five years later, he and Sherpa Tenzing Norguay would be the first to summit Mount Everest. After a 1957 fire destroyed the second Hermitage, the current one was built by the New Zealand government, under the aegis of its Tourist Hotel Corporation (THC) which also owned other tourist properties. In 1990 the THC was sold to a private corporation.  Our room was on the 5th floor of the rear wing and had a floor-to-ceiling view of Aoraki Mount Cook.

It had been a long Day 12 of our tour, starting in Dunedin with a morning stop in Oamaru before our wine lunch in the Waitaki. After a delicious dinner (appetizer below), shared with hundreds of other mountain tourists, we hit the sack. Tomorrow there would be a valley hike – and plants!

My Hooker Valley Track Hiking Journal

10:00 – The next morning, we left The Hermitage (roughly the red square), cheating a little by getting a lift in our tour bus (which cuts off the first few miles and at least a half-hour walk) to the campground, shown at the first yellow arrow, below. Our destination, Hooker Lake – the second yellow arrow – didn’t seem far on the map, but it’s a good hike, as you’ll see.

10:17 –  Armed with a lunch we’d scrounged from our breakfast buffet, off we went in the fine, mid-January summer weather on the Hooker Valley Track (Kiwi for “trail”).

10: 21 – Soon we were passing through matagouri shrubland. Dark and prickly, the other name for this riparian native is wild Irishman (Discaria toumatou).

10:26 – Through the thorny matagouri branches, the massive southeast flank of Mount Sefton appeared. Called Maukatua by the Māori, it’s the 13th tallest mountain in the Southern Alps at 3,151 metres (10,338 feet).

10:28 –  Look at all these amazing golden Spaniards! What? You don’t see any Spanish tourists? No, golden Spaniard or spear grass (Aciphylla aurea) is the name for the sharp-leaved plants stretching across this meadow. Now we could clearly see Mount Sefton and its neighbour to the right, The Footstool (2,764 metres – 9,068 feet).

10:30 – The meadows were spangled with snow totara (Podocarpus nivalis), also called mountain totara. A much-hybridized evergreen, its progeny appears in  temperate gardens throughout the world.

10: 32 – The track features three suspension bridges, two of which were rebuilt in 2015 to divert them from areas prone to flooding or avalanches. This was the first bridge. From here, you could just spot……

10:34 –  …..Mueller Lake as it spilled its own meltwater from the Mueller Glacier just beyond into Hooker River below the bridge.

I walked (bounced?) across the bridge behind my husband who was holding onto his Tilley hat in the fierce valley wind. I was very proud of him. He is not a gardener, and a 3-week garden-wilderness tour of New Zealand might not have been the first item on his bucket list when we contemplated this trip in 2017, but he was enjoying it very much – provided the wine flowed at dinnertime!

10:39 – Here was Griselinia littoralis, aka kapuka or New Zealand broadleaf, an evergreen that normally grows as a tree. Though its Latin name indicates a preference for the seashore (littoral), we are really not far from the Tasman Sea in this mountain valley. (And here I must offer my thanks to New Zealand plant wizard Steve Newall, who helped me identify many of these endemic treasures. Have a read about Steve in this piece by my Facebook friend Kate Bryant).

10:41 – That long berm at left, below, is the moraine wall of Mueller Glacier.

10:44 – We passed a few invasive plants in the first meadows, like foxglove (Digitalis purpurea), below.

10:50 – I passed my phone to my husband and asked for a portrait….of my best side. Like some 70,000 other New Zealand tourists, I wanted to have a record that I actually made this hike.

It was much warmer than I thought it would be, and I adopted my customary “I thought this was a glacier hike?” clothing modification, the same strategy used a few years ago in Greenland to hike the boardwalk through the alpine meadows to the UNESCO   Ilulissat Icefjord site.

11:01 – Okay, back to New Zealand. Forty minutes after we began our hike, we crossed the second suspension bridge, known as the Hooker Bluff bridge. The scenery here can only be described as spectacular.

11:02 – Now we saw the Hooker River spilling into Mueller Lake.

11:05 – After crossing the bridge, the river was on our right side. Though small, it was powerful, its crashing cascades seeming to echo off the nearby mountain walls.

11:06 – I was so transfixed, I stopped for a few minutes to make a recording.

11:07 – Along the path, one of the golden Spaniards (Aciphylla aurea) had toppled over under its own weight. You can see the umbellifer flowers and strange leaves against the stem

11:08 – A moment later, I saw one pointing towards Mount Sefton’s lofty glaciers.  

11:11 – And three minutes after that, I stopped to mourn that I had not been here a month earlier to see the flowering of the iconic Mount Cook lily, Ranunculus lyallii, the world’s largest buttercup, below. It was collected by and named for Scottish botanist David Lyall (1817-1895) who had travelled as ship surgeon around New Zealand and the Antarctic from 1839-41 on HMS Terror. (Terror was later lost with all hands, along with HMS Erebus, in Canada’s Arctic during Captain John Franklin’s ill-fated 1845 expedition to find a shortcut from Europe to Asia.  After years of searching, both shipwrecks were found in 2014 and 2016.)  In assembling Flora Antarctica containing Lyall’s plant collections, his friend, English botanist Joseph Hooker (1817-1911), noted that the New Zealand shepherds called it the ‘water-lily’, an appropriate name since it is the only known ranunculus with peltate leaves.  (It was Joseph Hooker’s father, William Hooker, for whom this valley and glacier were named by Julius von Haast in his geological survey of the Southern Alps in 1863.)

But the Māori of the South Island – the ancient Waitaha, then the Ngāti Māmoe, then the present-day Ngāi Tahu – had known the flower for hundreds of years before David Lyall arrived to botanize. They called it “kōpukupuku”. It has even been featured on postage stamps.

11:13 – A few minutes later, I felt somewhat mollified to come upon a few pristine specimens of Gentianella divisa.

11-17 – Unlike a Canadian alpine meadow in, say, Alberta, there is little bright colour in these tussock meadows under Aoraki Mount Cook.  Many of the herbaceous plants tend to have white flowers, like Lobelia angulata, below.

11:19 – You can barely see the tiny white flowers of inaka (Dracophyllum longifolium), one of the common native shrubs in the Hooker Valley.

11:24 – So far, we’d been walking on crushed gravel. But now we set off across the meadow on a beautiful boardwalk. As it began, it pointed us at Mount Sefton and The Footstool, but a few minutes later, it….


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11:26 –  …… veered to the right and gave us the full valley view of Aoraki Mount Cook.

11:30 – The shimmering meadow here was mostly mid-ribbed snow tussock (Chionochloa pallens).

11:32 – I was happy that I was able to identify mountain cottonwood (Ozothamnus vauvilliersii), which I had also seen in flower on Ben Lomond in Queenstown.

11:36 – Steve Newall helped me identify this lovely little community: the silver leaves of mountain daisy (Celmisia semicordata), its flowers already past, sitting in a bed of Gaultheria crassa to the left, with creeping wire vine (Muehlenbeckia axillaris)  up against the rock. The tussock grass is mid-ribbed snow tussock (Chionochloa pallens).

11:37 – A minute later, we were crossing the third bridge, called the Upper Hooker Suspension Bridge. This one seemed to catch the wind and the vibrations, especially near the river banks, were very strong!

11:43 – I stopped on the path for a few minutes to absorb the sight of these wonderful meadows and shoot a short video. Here’s how they looked:

11:54 – As we approached the end of the track, I found a stand of creeping wire vine (Muehlenbackia axillaris) in flower…..

11:54 – and Raoulia glabra with its little pompom flowers.

11:55 – When I looked up from the tiny alpine plants nestled in these rocks, I couldn’t help but notice the massive boulders lying in the meadow. The one below looked like it had sheared clean off the mountain and tumbled down the scree slope. But of course it might have happened dozens or hundreds of years ago. Unless one was actually there…….

11:56 – A minute later, we arrived at our destination. Hooker Lake lay before us – a body of water that hadn’t been there at all before the late 1970s, when Hooker Glacier began its retreat. In geological terms, it’s referred to as a “proglacial” lake.   It had taken us an hour and 39 minutes. We celebrated by walking along the path to a little picnic area and eating our lunch.

12:12 – With our picnic finished, I headed down to join the tourists posing for photos on the lake’s shore.

12:19 – My arthritic knee was not going to keep me from kneeling on the glacial till to capture a souvenir image of this little iceberg – aka “bergy bit” – washed up on shore.  As I looked up from this little lake – melted from a glacier named for an English botanist by a German geologist – at a towering mountain – named for an English sea captain by another English sea captain – I was unaware of the sacred nature of this park.

Long before Captain John Lort Stokes decided in 1851, while surveying New Zealand, to honour his predecessor, Captain James Cook, by naming the country’s highest peak after him, the Māori of the South Island knew it as Aoraki, or “cloud piercer”. The Ngāi Tahu do not see the mountain merely as the result of millions of years of tectonic uplift as the Pacific and Indo-Australian Plates collide far beneath the surface along the island’s western coast  For them it is the core of their creation myth: the mountain possesses sacred mauri. They say that long before there was an island called Aotearoa (New Zealand), there was no sign of land in the great ocean. When the sky father Raki wed the earth mother Papa-tui-nuku, Raki’s four celestial sons came down to greet their father’s new wife. They were Ao-raki (Cloud in the Sky), Raki-ora (Long Raki), Raki-rua (Raki the Second) and Raraki-roa (Long Unbroken Line). They arrived in their waka (canoe) and sailed the sea, but could not find land. When they attempted to return to the heavens, their song of incantation failed and their waka fell into the sea and turned to stone as it listed, forming the south island. The brothers climbed onto the high side of their waka and were also turned to stone. They exist today as the four tallest peaks in the area: Aoraki is the highest (Mount Cook); the other brothers are Rakiora (Mount Dampier), Rakirua (Mount Teichelmann) and Rarakiroa (Mount Tasman).

When title to the park was vested to the Ngāi Tahu in 1998, the mountain’s name was formally changed to recognize Aoraki, and all management decisions are made in concert with them to respect the environment as their sacred place. This remarkable carving by the late Cliff Whiting hangs in the park’s Visitor Centre. It depicts a fierce Aoraki and the four brothers/mountains.

Moments after kneeling at the shore of Hooker Lake, I gazed up at the sky and saw a cloud. People who study clouds call this an orographic cloud – its shape distorted by air currents that must lift in response to tall mountain peaks. But when I looked later at the photo I’d made, all I could see was the face of a fierce ancient god gazing across the sky.

12:20 – Okay, back to earth now. I didn’t bring my ultra-zoom camera with me on the hike or I could have captured the front wall of Hooker Glacier.  As it is, I enlarged one of my images to show the glacier and its calving wall.  If you’re looking to see sparkly-white, gleaming glaciers, you’re in for a shock here. As my friend Andy Fyon, retired head of the Ontario Geological Survey, says: “Active alpine glaciers can be a bit like a child. They revel in the rough and tumble life and in getting dirty! That is not the same for continental glaciers, which enjoy staying clean.”

12:30 – Looking at the upper part of Aoraki Mount Cook, below, you can see the summit partly obscured by a cloud.  I’ve also drawn in the south ridge that was recently renamed the Hillary Ridge. The closest of the mountain’s three peaks, Low Peak (3599 metre – 11,808 ft) was first summited in 1948 via the southern ridge by a foursome that included Edmund Hillary, Mick Sullivan and Ruth Adams and their guide Harry Ayres, Three years later, Hillary, along with Tenzing Norgay, would become the first person to summit Mount Everest. But that 1948 ascent of Mount Cook came with attendant drama, for when the foursome went on to attempt the nearby peak La Perouse (out of my photo to the left or west), Ruth Adams’s rope broke and her 50-foot slide down the slope left her unconscious with several fractures.  Hillary would contribute the first chapter to the gripping account of that rescue.

In fact, some 248 climbers have died attempting to climb Aoraki Mount Cook. Summiting is a considerable achievement in the world of couloirs and cirques and belays. I enclose the following video to demonstrate the skill needed. I estimate that I screamed “Oh, my god” or words  to that effect a dozen times and averted my eyes at least 20 times. Put on your crampons and fasten your carabiner…..

12:38 – Heading back to the hotel now, we took a little side detour up to a few small tarns, which is alpine for glacial pond.

12:46 – The Upper Hooker Suspension Bridge was just as bouncy and windy on the return trip.

12:55 – We walked at the base of Mount Wakefield, which separates Hooker Valley from the Tasman Valley to the east.

12:59 – A small footbridge at the Stocking Stream Shelter took us over the Hooker River with its milky rock flour.

1:20 – Looking down a little later, I saw a drift of Parahebe lyallii.

1:35 – And creeping over a rock was one of the “bidibids”, Acaena saccaticupula.

1:53 – I saw my only Hooker Valley butterfly, the common copper, foraging on New Zealand harebell (Wahlenbergia albomarginata).

2:12 – Coming towards the end of the hike, I made a critical mistake. Weary now and gazing across the meadows at what looked to be a direct route back to the Hermitage, I said, “Why don’t we get off this winding path and go straight back across the meadow?”  My husband, trusting soul that he is, reluctantly agreed.  Neither of us knew that the only people who ventured this way were mountain bikers.  With our tired legs, the spongy soil and long grass of the meadows made the last stretch seem never-ending.

2:14 – In the meadows in front of the hotel were a few lupines. Despite now being on the noxious aliens list, these invaders are quite famous for their massive spring show in the park.

2:19 – Parts of the meadow turned into dried-up gravel stream beds that are clearly part of the seasonal drainage patterns of the rivers here.

2:21 – I found another famous New Zealand mat plant, scabweed (Raoulia australis), growing here.

2:37 – And finally, 4 hours and 20 minutes after we began our hike, we arrived back at the sign-post near the hotel.

3:00 – As we kicked off our hiking shoes and collapsed  onto our beds in the 5th floor room with the great view of the mountains, we cracked open a bottle of the Gëwurztraminer we’d bought at Ostler Vineyard the previous day. A glass of chilled wine never tasted so good.

9:30 – And later, after dinner, as the light dimmed in the sky, I looked out on Aoraki Mount Cook with something akin to affection. Like the Māori, I sensed its spirit infusing this spectacular landscape.

9:43 – And as the sun shed its last rays on its snowy peak, I gave thanks for the pilgrimage we had made to be close to it.