Landform and Geology
The southern Mount Lofty Ranges form a spine to the Fleurieu Peninsula and ridges extending from the range to the south coast make up the landform of Deep Creek Conservation Park. In the northern part of the park, elevations on the range reach 300 metres and numerous streams are fed by springs and soaks.
Flowing south, these creeks carve deep valleys to expose some spectacular rock outcrops before emptying into the Southern Ocean at small, predominantly rocky coves. These coves provide the only breaks in an otherwise imposing line of rugged cliffs that form the coastline. Blowhole Creek, Deep Creek and Boat Harbor Creek Beaches are the most attractive and accessible coves within the park.
The present landform in Deep Creek Conservation Park is the result of a geological history of sedimentation, uplifting, folding, faulting, glaciation and erosion.
The Kanmantoo trough was formed by the collapse along fault lines of the southern and eastern sides of a large undersea basin called the Adelaide Geosyncline. This trough collected a great depth of sediment before uplifting and folding, due to tectonic activity, occurred. The rock outcrop pattern found on the Fleurieu Peninsula today is largely a result of this folding process.
Glaciation followed, which flattened much of the mountain range and gouged valleys including Backstairs Passage. When the glaciers retreated the area was subject to a period of gradual weathering and erosion, leaving a plain of low relief. The remnants of this plain form the laterite hilltops of the Peninsula today.
A period of faulting then uplifted the Fleurieu Peninsula and left it surrounded by the St Vincent and Murray basins. Several fluctuations in sea level occurred before present-day shores developed. Active stream erosion stripped much of the old land surface and exposed the underlying rock which is seen in the landscape today.
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