Perhaps everyone knows how glaciers work…a lot of snow (and I mean a lot of it, up to 50m to gain a compressing weight of its own) compacting into the ice with gravity pulling this mass down the hill. It may however be a bit harder for everyone to imagine the scale of the area where all this compacting happens.
Franz Josef Glacier is one of the smaller glaciers by world standards but quite a sizeable chunk of ice in New Zealand landscape.
On this photograph I’ve been hoping to show the vastness of the upper parts of this currently about 10km long glacier. With 2 highest peaks of the New Zealand’s Southern Alps dominating the background – Mount Tasman on far top left 3,497m and highest mountain Aoraki/Mount Cook 3,724m next to it on right, the vastness of the Geikie and Davis Snowfields of the Franz Josef Glacier is quite apparent.
This wonderful scene has been photographed just as the sun was dipping over the horizon of the Tasman Sea on right and I love the beautiful light bouncing over about 30 square km large NEVE in wonderful hues of purple, pink and orange. Hope you enjoy this image, too. Thank you.
It’s hard to describe my feelings when I’m at pristine places like Okarito on the West Coast in New Zealand with its surrounding lagoons, wetlands and wild beaches. Without wanting to be too sentimental, I just can’t help it to say that my heart is always up my throat, filled with joy how beautiful this place is.
Regardless of the time of the day, you always can make a wonderful photograph in Okarito. For me though, my time I love to photograph is when the sun is near the horizon and the light orchestrates its play around you. Once the sun dips below horizon, the air fills up with pastel hues of pinks and purples, contrast balances out, remoteness with silence all around makes me feel this place belongs just to me….and it’s then, when photographs like this can be made.
Thank you for checking in and Enjoy!
Image ©Petr Hlavacek – nzicescapes.com
I’m sure that every photographer time time struggles with culling similar images down…which one to keep and which to throw into the bin…especially when each of the frame can stand on its own, has it’s own quality and charm?
I’ve always had problems with this but I think I’m getting better at it now.
Time to time however, I find a nut which is hard to crack…like this one.
When I get to this point where I simply am out of breath, I look at it from a different angle and try to find deliberate use of the images for portraying the scene, usually in a different quality light as it passes through… and I’m finding that this works best with scenes with strong and clear compositions and main subject….like this one.
Taken with Nikon D300 and printed as high quality Fine Poster at 130cm x 60cm approx.
Thank you for visiting and Enjoy!
Yesterday I got back from a tramping trip in the hills.
Partially scouting trip, together with my beautiful model and partner, we hiked up into the Southern Alps in New Zealand to spend a night under the stars…and what a blast we had!
The weather was great but it couldn’t be said about Fox Glacier township below us. The whole time the town was under heavy blanket of clouds while we had blue skies above our heads.
Incredible 360 degree views and vistas from atop of Mt. Fox are truly hard to beat.
Highest peaks of the whole Australo-Asia (Mt. Cook and Mt. Tasman) on one side with Tasman Sea on the other side just take one’s breath away.
These are some of the best locations New Zealand has on offer and I’m always thrilled and shaking by excitement when I plan to venture into these spots.
It won’t be long before I’ll be back here!
Mt. Cook on right (3754m) and Mt. Tasman on left (3497m) from near Mt. Fox in Westland National Park, West Coast, New Zealand.
Love this place – Enjoy!
By the end of the last year’s winter, we had a lot of fun. With our still photography we were covering an exciting promo project of the Glacier Country in New Zealand – Rugby Match on Fox Glacier Neve. This project offers an opportunity to win NZ$50.000 price package in a Glacier Country Rugby Competition. For details please go to – glaciercountry.co.nz
On this project we worked alongside of a great film maker from Auckland, (more…)
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 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 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…)