The wind was blowing really hard across the navy blue water surface of slacks trapped behind the shingle banks at Rochefort Point. Rochefort Point is a short walk from the Louisbourg Fortress in Cape Breton, Nova Scotia. The ripples were tight packed and narrow, travelling at speed. The water was actually a brackish brown but reflected the clear blue of the sky resulting mostly in dark blue hues. From some angles and in certain lights the sun shone through the ripples revealing the reddish colour of the water. The low standing crests of the waves were so distinct that it seemed as if the water was viscous.
Thames Dock Water Ripples 1 -11: Rippled river water surface pattern and texture in an abstract artistic image derived by digitally altering the colours of a photograph so that the blue represents the reflected light.
The MacIntosh Brook is one of the stopping places along the Cabot Trail in the Cape Breton Highlands National Park in Nova Scotia, Canada. This clear mountain stream flows rapidly via waterfalls and over stones of many colours as it passes through dense old-growth hardwood forest. The water source is high up in the hills at about 430 metres. It starts in Ordovician-Carboniferous granitic plutons, then passes over Ordovician-Silurian meta-igneous rocks (both rock formations belong to the Aspy Terrane). Finally, in the lower reaches it flows over red Horton Group sand stones and conglomerates from the early Carboniferous Period. The torrents of winter storms and spring snow melt bring rocks of all these types tumbling down the ravines to the stream bed where they ‘colour’ the water and create a rapidly transitioning series of riffles, ripples, and water reflections – a kaleidoscope of impressions.
The river flowing down to the seashore meets with waves from the sea at Charmouth in Dorset, England. This somewhat abstract image of the natural patterns generated from the meeting of the two forces shows the freshwater continuing to flow smoothly seawards on the left of the channel (top left) while on the right it rebounds from the curving bank with the ripples moving upstream and towards the middle of the channel. The blue and white are reflected sky, and the yellow is reflection from the shingle beach.