Rocks at Lake Tekapo
Photo Id: JAB_20170415_7DMII_6414-Edit.
Sunrise over Lake Tekapo
Photo Id: JAB_20170416_7DMII_6489-HDR-Edit.
Fishing amongst autumn colour
Photo Id: JAB_20170416_7DMII_6771-Edit.
Lake Alexandrina
Photo Id: JAB_20170416_7DMII_6945-Edit.
View from Mt. John
Transitions of color and landscape from mountains to valleys while watching the sun go down from top of Mt. John at Tekapo. Photo Id: JAB_20170416_7DMII_7231-Edit.
Banner Cloud at Lake Tekapo
Photo Id: JAB_20170416_7DMII_7265-Edit.
Glacier Ice in Hooker Lake
Photo Id: JAB_20170417_7DMII_7448-Edit.
Mt Cook Reflection in Alpine Tarn
Photo Id: JAB_20170417_7DMII_7466-Edit.
Mt Cook Reflection
Photo Id: JAB_20170417_7DMII_7469-HDR-Edit.
JAB_20170417_7DMII_7483-HDR-Edit
Photo Id: JAB_20170417_7DMII_7483-HDR-Edit.
Hooker River and Aoraki / Mount Cook
It's not surprising that the Hooker Valley Track is the most popular short walking track within the Aoraki/Mount Cook National Park in New Zealand. It's only 5km, but the views are simply amazing. Photo Id: JAB_20170417_7DMII_7492-Edit.
Hooker River and Mt. Cook
The milky blue Hooker River winds itself down from Hooker Glacier which is one of several glaciers close to the slopes of Aoraki / Mount Cook in the Southern Alps of New Zealand. The milky blue water flowing from glacial melt is the result of finely ground rock called "rock flour" that pigments the water.
Last light on Aoraki / Mount Cook
Photo Id: JAB_20170417_7DMII_7554-HDR-Edit.
Road to Lindis Pass
Photo Id: JAB_20170418_7DMII_7614-Edit.
First sun on Kelvin Heights, Queenstown
Photo Id: JAB_20170419_7DMII_7907-Edit.
JAB_20170419_7DMII_7946
Arrowtown Goldminer's Cottage
Photo Id: JAB_20170419_7DMII_7991-Edit.
Autumn Colours in Queenstown Gardens
Photo Id: JAB_20170420_7DMII_8070-Edit.
Lake Dunstan
Photo Id: JAB_20170421_7DMII_8315.
Mystical Lake Ruataniwha
A low-key impression of the autumn colours and reflections on this man-made lake just out of Twizel on the boundary between Canterbury and Central Otago. Photo Id: JAB_20170421_7DMII_8352-Edit-2-2.
