This shot is from last winter on Franz Josef Glacier in New Zealand.
It was a beautiful day, as it always is on the West Coast and which is why you wanna be on ice, right?
I was on one of my explorations of this glacier. Since the glacier’s changing literally every day, you can keep coming back all the time and always see some new magic.
On this day, it was these turquoise fringes of the crevasses which caught my attention, as they were shining from a distance at me.
I love these ice colours but it is not easy to get around locations like this, especially in winter when every crack, deep crevasse or whole is covered with snow. These adventures can truly be deadly if you don’t know what you’re doing. I’ve been tip toeing around these crevasses, poking the ground in front of me before I put my next step down. I wanted to get as close as I could to get a nice wide angle shot with a lot of detail.
Standing on the slippery edge of the crevasse I made this exposure with my 12-24 mm wide angle lens at 12mm and with +1.3 EV exposure compensation.
Only very little of touch up on this RAW file in Lightroom was required to finalize the frame.
I hope you’ll like it as I do.
Franz Josef Glacier is hugely popular to all kinds of visitors. And that’s no wonder, when one realizes the facets this stunning piece of Mother Nature’s work has on offer.
Besides its pure, mesmerizing blue, translucent beauty hitting us from every direction, Franz Josef Glacier has also its rough face, challenging many people with its ice climbing opportunities.
The characteristics of this icy beast, combined with comfortable access, make this very easily possible. The steep and narrow valley works as a funnel into which Franz Josef slides from almost 3.000m above sea level. Once the body of ice gets into lower, steep and uneven valley floor, massive waves of ice are formed. These waves can be as high as 15-20 m and just scream to be climbed…and there is always plenty of those who can hear the call!
When do we call a chunk of ice a glacier? Usually, the ice mass has to be at least 100m x 100m in size and needs to show some signs of a present or past movement.
Generally, glaciers are divided into two main groups – Ice Sheets and Valley Glaciers, each with several sub-types.
Ice Sheets or Continental Glaciers are the largest masses of ice on Earth spreading over 50,000 square kilometres with the depth of ice sometimes more than 4,200m. They are only found in Antarctica and Greenland. Ice Shelves are floating extensions (more…)
The most destructive and powerful hand of Mother Nature lies, arguably, in the cryosphere. We may not see it doing much immediate damage, but by observing the landscape we can see enormous changes in our environment caused by glaciers. One of the very typical and most visible footprints glaciers leave behind are our, often ice free, valleys. Entire mountainsides were remodeled by
As with all the rest of the glaciated world, New Zealand is also losing ice mass at a rapid rate, with 61% lost since 1850 (Hoelzle et al. 2007), and 11% in the last 30 years (T. Chinn, pers. comm.).
Most of this loss is from the large glaciers calving into pro-glacial lakes, such as the Tasman Glacier. This lake formation is the result of glacier thinning in response to climatic warming in the 20th century. As well as these large dynamic changes in glacier volume, there are smaller annual changes in volume due to changes in the amount of snow accumulation and snow and ice melt. An idea of how much mass is lost or gained each year throughout the Southern Alps is given by measurements of the end-of-summer snowlines since 1977. These measurement indicate that there have been positive mass balances at times during this period balance (Chinn et al. 2008) and the very sensitive and responsive Franz Josef and Fox Glaciers have advanced as a result.
The advance of Ka Roimata o Hine Hukatere Franz Josef Glacier since 1984 has been extraordinary given the global pattern of receeding glaciers during this period. Recent work (more…)
The ice flow of a glacier is divided into two types, internal deformation and basal sliding. Internal deformation is movement of parts of the glacier relative to itself. Throughout the descent of the glacier, the ice at the sides and bottom side of the glacier are subject to more friction from the valley floor and walls, and therefore forced to move at a slower rate than the ice in the centre of the glacier. As a result (more…)
The Franz Josef Glacier is one of the fastest moving glaciers on Earth. Unlike most of glacier in the world the Franz Josef Glacier travels down very steep slopes of the Southern Alps. In the upper and very steep parts of the glacier, where the ice in the huge neve is squeezed into a narrow valley, the ice can move up to 5m each day during period of advance. (more…)
New Zealand owes its stunning beauty to its location on Earth. This applies particularly well to the West Coast of the South Island. Due to the predominant weather patterns in this part of the globe, the South Island faces the weather sweeping in as a persistent westerly airstream from the Tasman Sea. Moisture laden clouds brought in by these westerly winds have a gigantic barrier in their way – The Southern Alps. The Alps force the clouds to climb into higher and colder altitudes so the clouds finally give up and release the moisture in form of rain, and around the Main Divide as snow. The annual precipitation on the West Coast reaches 16 meters in places, making the West Coast one of the wettest places on Earth.
One of the most striking forms of evidence of glacial erosion is the colour of rivers like the Waiho River in Franz Josef. The melt water of the river gains a characteristic greyish colour, sometimes known as glacier milk. This is the result of the suspension of very fine grains of rock <0.002mm in size. These particles are called glacial flour and are the result of a type of glacial erosion known as abrasion. The abrasion occurs where the glacier slides over bedrock and works much like sandpaper, as rock fragments meet at the boundary of rock and ice they grind and smooth the surface below. If a large rock is trapped, large grooves or glacial striations are engraved into valley walls and bedrock.
Another major type of erosion is known as plucking. When the ice slides over the downstream side of the bedrock, it can freeze loosened rocks from the bottom into itself and rips the rocks out from the valley floor and walls, changing its shape forever.
One of the attractions of the glacier is the beautiful blue colour of its ice. In the upper reaches of the glacier the ice can be up to 300m thick. The upper layer is snow. When this reaches about 16 – 20m deep the snow compresses under its own weight and all the air is squeezed from between the snow crystals, forming glacial ice. (more…)
The unique environment of Westland National Park is responsible for the formation of the local glaciers. These powerful remnants of an ice age manage to survive warming temperatures due to the very special weather conditions on the West Coast of the South Island. Up to 16 metres of precipitation falls on the tops of the Southern Alps every year, most of it falling as snow. This massive amount of snow (more…)