Rugged

Plettenberg Bay hosts one of the largest seagull breeding colonies along the South African coast at the mouth of the Keurbooms River, named after the indigenous keurboom tree. There are many pelagic birds in the area as well as the endangered African oystercatcher which live along the shores. The bay falls within the Agulhas Bank ecoregion (bioregion), specifically within the Agulhas inshore ecozone. There has been a long history of sport fishing from the rocks, ski boats launched from Central Beach, or in Keurbooms estuary. The sea life activity both surface and sub-surface varies considerably as either deep water upwelling brings cold water into the Bay, or warm water eddies over from the Agulhas Indian Ocean current offshore. A distinctive flower-shaped sea shell called a pansy shell is endemic to this part of the coast, and is used as the symbol representing the town. Looking for these shells on the beach at low tide is a popular activity amongst visitors and locals alike.

Info source: https://en.wikipedia.org/wiki/Plettenberg_Bay

The photo was taken during October 2016 at Beacon Isle Resort, Plettenberg Bay, Western Cape, South Africa.

Rugged

Break

Surfing is a surface water sport in which the wave rider, referred to as a surfer, rides on the forward or face of a moving wave, which usually carries the surfer towards the shore. Waves suitable for surfing are primarily found in the ocean, but can also be found in lakes or rivers in the form of a standing wave or tidal bore. However, surfers can also utilize artificial waves such as those from boat wakes and the waves created in artificial wave pools. The term surfing refers to the act of riding a wave, regardless of whether the wave is ridden with a board or without a board, and regardless of the stance used. The modern-day definition of surfing, however, most often refers to a surfer riding a wave standing up on a surfboard; this is also referred to as stand-up surfing. Info source: https://en.wikipedia.org/wiki/Surfing
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The photo was taken during June 2016 at Cabana Beach Resort, Umhlanga, Kwazulu-Natal, South Africa.

Mushroom

There are 3 main layers of rock in Golden Gate Highlands National Park, the characteristics of which have lead to the famous cliff formations present in the park today. The red layer was created 200 million years ago when swampy rivers deposited the mud-like sediment. 196 million years ago, the area dried up and became a desert, resulting in the yellow sandstone deposits. From 160-190 million years ago, volcanic activity capped the area with a basalt layer. The rivers and streams in the park have carved the rocks into their present formations. The name ’Golden Gate’ originates from the two cliffs that face each other on either side of the road: at sunset, the yellow sandstone becomes a rich gold colour. And those black marks?All around the park you can see black stripes on the rock, even long after it has rained. These are areas where water seeps out of the rocks. Minerals from the top basalt layer (manganese dioxide) are carried in the water and these stain the rocks black. The water enables organisms like algae and moss to live on the rock as well.
Info source: https://www.sanparks.org/parks/golden_gate/conservation/ff/geology.php
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The photo was taken during December 2015 at Golden Gate National Park, Clarens, Freestate, South Africa.

Mushroom