It is quite hard to imagine that this place once used to be a thriving forest.
Until about 180 million years ago when New Zealand was still part of a super continent Gondwana. Massive event of sheet flooding caused by, at that time nearby live volcanoes, flooded the area and almost instantly turned the forest into stone. Stone turning must have happened relatively quickly, in matter of months, as the trees didn’t have time to decay. Thanks to silica minerals not only trees but also ferns were preserved for us to wonder over.
This is a significant coastal location not only for New Zealand but also internationally, as these types of fossilized forests are very rare.
I had this location in my mind for quite some time, as I wanted to get some new photographs of this interesting place so it was for sure that Curio Bay gets included into my Southland trip. I spend a couple of nights her, exploring around and managed to make a few images.
I have quite few interesting frames from here actually, but it was the mood and gloominess of this night photograph which I like and decided to make a post of it.
I hope you’ll like it as well!
Taken with Nikon D800E and Nikkor 16-35 f4 lens.
Photo: ©Petr Hlavacek – www.nzicescapes.com
This image is not online yet, but you can find more of other coastal imagery in our gallery Coastal photos of New Zealand
Thank you and Enjoy!
Despite this place being right on my doorstep, I’m quite ashamed to admit that it’s been a long 10 years since I visited this location last time. But this long gap won’t happen again, I can promise you that!
This said, you can well imagine my excitement planing my trip back into the wilderness of this spectacular western part of the Southern Alps, part of the Westland National Park in New Zealand.
Copland Valley is simply amazing. Jugged skyline of The Sierra Range on southern side of the valley keeps your mind in awe pretty much all along the way toward the first, well known hut – Welcome Flat Hut, which is reached after around 8hrs. A lot of the time you’re hiking along beautiful Copland River as it runs through this valley. River originates in Copland Glacier and gathers its waters from magnificent peaks of the Southern Alps, especially from The Sierra Range. And it is its glacial origins which gives this river stunning turquoise-blue colour of water.
It was late on a summer day when I took this photograph of the Copland River. As the sun went lower and lower, the Copland Valley lost its light completely and the blue chill of river gave the air its coldness. Combination of these qualities, warm sunlight on the peaks, coldness of the river and with addition of the juicy green rainforest made this frame for me.
This panoramic photograph is a merge of six frames, processed using Lightroom 4 and stitched in Photoshop CS6.
I’ve been wondering for quite some time how Franz Josef Glacier looks under the moonlight. As you know, there is only 12 or 13 full moons in a year and not each of moon’s appearance is on a clear sky for maximum light. Also, I might not always be able to chase it…but eventually, I managed.
Couple of days back it looked like its going to be a good full moon and because I was around, I decided to give it a go and hurried up to climb the hill and spent a night under the stars…and what a night it was!
I’ve been just starting and experimenting with night photography so I was very excited to see what can be captured. I managed to get several exposures ranging from 30 to 40 min but I can see that there is much more potential. It was full moon and that’s why I went up – to get well illuminated glacier but next time I might go somewhere in the middle of the moon cycle. That should allow me to add some nice, stronger star trails into the frame, as well, as this time the sky was too bright.
Since this image is not online yet, the link from it will take you to our STOCK galleries where you can explore more on New Zealand’s landscapes!
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…)