Whittle Rock
Whittle Rock is a granite corestone reef and navigation hazard in False Bay, Western Cape, South Africa.[1][2][3] The reef rises from a sandy bottom at about 40 m, to a minimum depth of 3.2 m, and is a well known fishing site and recreational diving area. It has an area of about 1 km2, and can affect the waves at the shore in Kalk Bay in special conditions of a long southeasterly swell. It is marked by a cardinal east buoy with sound and light signals.
Location and extent[edit]
Whittle Rock is about 8 km to the east of Miller's Point which is on the coast of the Cape Peninsula just south of Simon's Town, on the west side of False Bay, at 34°14.846′S 18°33.714′E / 34.247433°S 18.561900°E[2] The contiguous reef is a bit over 1 km east to west, and a bit under 1 km north to south. There are several outliers in the order of 100 m size range, within 100m of the main reef, and a lot more that are smaller. Several other granite outcrops and clusters of smaller size and greater depth exist in the vicinity. The official depth of the top of the reef is 3.2m below datum.[2]
Bathymetry[edit]
Minimum depth according to the chart is 3.2 m at low tide, and maximum depth at the edge of the reef is about 42 m in the south. Most of the reef is above 30 m, and a fairly large amount above 18 m, the official limit for most entry level scuba certification.
Geology[edit]
Whittle Rock and the other reefs of this part of False Bay are outcrops of the Peninsula Granite, a huge batholith that was intruded into the Malmesbury Group about 630 million years ago as molten rock and crystallised deep in the earth, but has since then been exposed by prolonged erosion. The characteristic spheroidal shapes of granite boulders are a result of preferential weathering along intersecting fractures and are well displayed above sea level around Llandudno and Simonstown. Close up, the granite is a coarse-grained rock consisting of large (2–5 cm) white or pink feldspar crystals, glassy brown quartz and flakes of black mica, and occasionally containing inclusions of dark Malmesbury hornfels.[3]
Though initially intruded at great depth, prolonged erosion eventually exposed the granite at the surface, and it and what remains of the similarly eroded Malmesbury group now form a basement upon which younger sedimentary rocks of the Table Mountain Group were deposited.[4]
Almost all the exposed granite has been extensively weathered and is in the form of rounded corestones. The colour is generally pale to medium grey, and the surface is typically fairly rough, with clearly visible crystals, and no layered structure. The massive rock is cracked on jointing planes, which tend to be characteristic of the location, and weathering has accentuated these joints, in places widening them to form deep gullies. The general direction and spacing of joints in some areas is fairly consistent over quite large areas.
There are areas of rubble, gravel, pebbles, and shell along the edges of the reef, with much of the pebbled area to the north, but the surrounding surficial unconsolidated material is predominantly fine sand at depths from 30 to 42 m. There are also scattered sand patches in locally low areas, and these often have a relatively high shell content.
History[edit]
In 1672 the Dutch warship Goudvinck was stationed at the Cape and was instructed to survey False Bay, but it is not known how much was done before they were recalled. Simon van der Stel, appointed commander of the station in 1679, sailed False Bay in November 1687 on the ship De Noord, took the earliest recorded soundings, and described the islands, reefs and shoreline of the bay. By the end of the 17th century the general bathymetry was known.[5]
The Whittle Rock reef is named after a lieutenant Whittle of the Royal Navy, who surveyed parts of False Bay after HMS Indent was damaged off Miller's Point soon after the first British occupation of the Cape in 1795.[6]
There are two shipwrecks associated with the reef: The British East Indiaman Euphrates, and HMS Trident, both of which are reported to have sunk after striking the reef, but the positions of their wrecks are not recorded, though there are several large anchors of appropriate age known on the reef.[7]
[edit]
Whittle Rock is a significant navigational hazard due to its depth and position, though very few large ships enter the bay, as fishing is limited and it is off the shipping lanes. However False Bay is occasionally used for shelter in storms. The reef is marked by a cardinal east buoy, with sound and light signals. The seas occasionally break over the top of the reef, but the shallow area is small and not easily seen in a rough sea.[2] The reef is marked by a Cardinal East marker moored at S34°14.876' E18°33.709', about 50 m south of the main pinnacle.
Influence on wave propagation[edit]
The reef at Whittle Rock can focus longer period south-easterly waves on Kalk Bay. This is unusual and associated with a cut-off low pressure system causing the south-easterly winds to blow for an unusually long time over enough fetch to develop a sea sufficiently for it to be refracted by the shoal area.[8]: App3
Economic importance[edit]
Whittle Rock is a well known area for artisanal and recreational line fishing, and a moderately popular recreational scuba diving area.
Recreational dive sites[edit]
Most of the recreational dive sites of False Bay, including some on the Whittle Rock reef, are in the Table Mountain National Park Marine Protected Area. A permit is required to scuba dive in any MPA in South Africa. These permits are valid for a year and are available at some branches of the Post Office.[9] Temporary permits, valid for a month, may be available at dive shops or from dive boat operators who operate in an MPA. A personal recreational scuba diving permit is valid in all South African MPAs where recreational diving is allowed. The business permit to operate recreational scuba business operations in an MPA is restricted to a specific MPA. Diving for commercial or scientific purposes is also subject to permit. Whittle Rock has a number of recreational dive sites which have been identified by position and named.[10] Some of them are listed here (north to south):
- North-west Passage: 34°14.650′S 18°33.125′E / 34.244167°S 18.552083°E
- Kelly's Anchor: 34°14.687′S 18°33.612′E / 34.244783°S 18.560200°E
- Shards Cluster: 34°14.704′S 18°33.763′E / 34.245067°S 18.562717°E
- Riaan and Sven's anchor: 34°14.735′S 18°33.590′E / 34.245583°S 18.559833°E
- East Ridge North Pinnacle: 34°14.742′S 18°33.843′E / 34.245700°S 18.564050°E
- Fractal Zones: 34°14.750′S 18°33.200′E / 34.245833°S 18.553333°E
- North-west corner pinnacles: 34°14.750′S 18°33.482′E / 34.245833°S 18.558033°E
- September anchor: 34°14.762′S 18°33.575′E / 34.246033°S 18.559583°E
- Whittle Rock North-west Pinnacle: 34°14.765′S 18°33.622′E / 34.246083°S 18.560367°E
- Euphrates anchors: 34°14.776′S 18°33.801′E / 34.246267°S 18.563350°E, 34°14.783′S 18°33.790′E / 34.246383°S 18.563167°E and 34°14.783′S 18°33.795′E / 34.246383°S 18.563250°E
- Billy's anchor: 34°14.777′S 18°33.734′E / 34.246283°S 18.562233°E
- JJ's anchor: 34°14.781′S 18°33.720′E / 34.246350°S 18.562000°E
- Little anchor: 34°14.785″S 18°33.666′E / 34.00410694°S 18.561100°E
- Peter's Ridge: 34°14.800′S 18°33.160′E / 34.246667°S 18.552667°E
- Criss-cross Cracks: 34°14.830′S 18°33.879′E / 34.247167°S 18.564650°E
- Bruce's Reef: 34°14.824′S 18°33.318′E / 34.247067°S 18.555300°E
- Whittle Rock West Pinnacle: 34°14.844′S 18°33.682′E / 34.247400°S 18.561367°E
- Whittle Rock (Shallowest pinnacle): 34°14.846′S 18°33.714′E / 34.247433°S 18.561900°E, about 8 km offshore
- Whaleback Pinnacles: 34°14.850′S 18°33.508′E / 34.247500°S 18.558467°E
- Whittle Rock Western Reef Pinnacle: 34°14.856′S 18°33.269′E / 34.247600°S 18.554483°E, inside the TMNPMPA
- Marc's anchor: 34°14.856′S 18°33.716′E / 34.247600°S 18.561933°E
- Gullies: 34°14.872′S 18°33.454′E / 34.247867°S 18.557567°E
- Whittle Rock South-east Pinnacle: 34°14.887′S 18°33.775′E / 34.248117°S 18.562917°E
- Whaleback Rock: 34°14.900′S 18°33.635′E / 34.248333°S 18.560583°E
- South east pinnacle chain (Neptune's bath plug): 34°14.917′S 18°33.753′E / 34.248617°S 18.562550°E
- Flash pinnacle: 34°14.931′S 18°33.718′E / 34.248850°S 18.561967°E
- Georgina's anchor: 34°14.935′S 18°33.784′E / 34.248917°S 18.563067°E
- M&M Tower (the Spark plug): 34°14.943′S 18°33.549′E / 34.249050°S 18.559150°E
- Cave Complex reef: 34°14.943′S 18°33.616′E / 34.249050°S 18.560267°E
- Bus Stop (the Gnarly wall): 34°14.945′S 18°33.573′E / 34.249083°S 18.559550°E
- Wreckless Rock and the Little Labyrinth: 34°14.949′S 18°33.707′E / 34.249150°S 18.561783°E
- Table Top pinnacle: 34°14.968′S 18°33.668′E / 34.249467°S 18.561133°E
- Mossie's Cave and pinnacle: 34°14.972′S 18°33.420′E / 34.249533°S 18.557000°E
- Grant's Spike (South-western pinnacles): 34°14.991′S 18°33.450′E / 34.249850°S 18.557500°E
- Grant's Wall: 34°15.003′S 18°33.445′E / 34.250050°S 18.557417°E
- Labyrinth: 34°15.004′S 18°33.580′E / 34.250067°S 18.559667°E
- Labyrinth South Pinnacle: 34°15.048′S 18°33.606′E / 34.250800°S 18.560100°E
- Deep South Pinnacle: 34°15.103′S 18°33.603′E / 34.251717°S 18.560050°E
Ecology and conservation[edit]
False Bay is at the extreme western end of the inshore Agulhas marine ecoregion which extends from Cape Point to the Mbashe river over the continental shelf, in the overlap zone between Cape Agulhas and Cape Point where the warm Agulhas Current and the cooler South Atlantic waters mix. This ecoregion has the highest number of South African endemics, and is a breeding area for many species. The transition between the Agulhas ecoregion and the cooler Benguela ecoregion is at Cape Point, on the western boundary of False Bay.[11]: 103 [12]
The eastern boundary of the controlled area of the Table Mountain National Park Marine Protected Area is at E 018°15.000' which passes through Whittle Rock reef. Extraction and harvesting of marine life, and other activities, are allowed on condition that one has a valid permit allowing one or more of the following specific activities: spear fishing, angling, scuba diving, snorkelling for mollusc extraction, boating, commercial diving, salvage operations, scientific research, commercial fishing, whale watching, shark cage diving or filming.[13]
The benthic habitat types for Whittle Rock according to the National Biodiversity Assessment are hard inner shelf on the reef, and sandy inner shelf on the surrounding sand.[1]
References[edit]
- ^ a b Pfaff, Maya C.; Logston, Renae C.; Raemaekers, Serge J. P. N.; Hermes, Juliet C.; Blamey, Laura K.; Cawthra, Hayley C.; Colenbrander, Darryl R.; Crawford, Robert J. M.; Day, Elizabeth; du Plessis, Nicole; Elwen, Simon H.; Fawcett, Sarah E.; Jury, Mark R.; Karenyi, Natasha; Kerwath, Sven E.; Kock, Alison A.; Krug, Marjolaine; Lamberth, Stephen J.; Omardien, Aaniyah; Pitcher, Grant C.; Rautenbach, Christo; Robinson, Tamara B.; Rouault, Mathieu; Ryan, Peter G.; Shillington, Frank A.; Sowman, Merle; Sparks, Conrad C.; Turpie, Jane K.; van Niekerk, Lara; Waldron, Howard N.; Yeld, Eleanor M.; Kirkman, Stephen P. (2019). "A synthesis of three decades of socio-ecological change in False Bay, South Africa: setting the scene for multidisciplinary research and management". Elementa: Science of the Anthropocene. 7 (32). doi:10.1525/elementa.367. hdl:2263/75633. Creative Commons Attribution 4.0 International License (CC-BY 4.0)
- ^ a b c d SAN 1016 - Valsbaai (Map). Cape Town: SA Navy Hydrographic Office. 1978.
- ^ a b Theron, J.N.; Gresse, P.G.; Siegfried, H.P.; Rogers, J. (1992). Explanation sheet 3318 – The Geology of the Cape Town Area. Pretoria: Geological Survey, Department of Mineral and Energy Affairs, Government Printer. ISBN 978-0-621-14284-6.
- ^ Compton, John S. (2004). The Rocks & Mountains of Cape Town. Cape Town: Double Story. ISBN 978-1-919930-70-1.
- ^ Gründlingh, M.L.; Largier, J.L. (1988). "Fisiese Oseanografie in Valsbaai: 'n Oorsig". South African Journal of Science and Technology (in Afrikaans). 7 (3): 133–143. doi:10.4102/satnt.v7i3.914. ISSN 0254-3486.
- ^ Stibbe, George R.; Moss, Iain (1998). A Traditional Way of Life – The story of the Kalk Bay Fishermen (PDF). Cape Town: G.R. Stibbe. p. 5. ISBN 0-620-22706-0.
- ^ Rawe, J.; Crabtree, A. (1978). Shipwrecks of the Southern Cape. Cape Town: Atlantic Underwater Club. Ref: L.G. Green, 1965, "Almost Fogotten, Never Told" p32, Euphrates, English East India ship, struck Whittle Rock in False Bay and went down. p 31, HMS Trident Struck Whittle Rock in False Bay and went down.
- ^ Brundrit, Geoff (December 2009). Global Climate Change and Adaptation: City of Cape Town sea-level rise risk assessment (PDF) (Report). Vol. Phase 5: Full investigation of alongshore features of vulnerability on the City of Cape Town coastline, and their incorporation into the City of Cape Town Geographic Information System (GIS).
- ^ "Government Notice 695: Marine Living Resources Act (18/1998): Notice declaring the Table Mountain National Park Marine Protected Area under section 43" (PDF). Government Gazette: 3–9. 4 June 2004.
- ^ "Standard positions for SeaKeys dive sites: Dive sites of the Cape Town region". iNaturalist.org. Retrieved 15 August 2023.
- ^ Sink, K.; Harris, J.; Lombard, A. (October 2004). Appendix 1. South African marine bioregions (PDF). South African National Spatial Biodiversity Assessment 2004: Technical Report Vol. 4 Marine Component DRAFT (Report). pp. 97–109.
- ^ Sink, K; Holness, S; Harris, L; Majiedt, P; Atkinson, L; Robinson, T; Kirkman, S; Hutchings, L; Leslie, R; Lamberth, S; Kerwath, S; von der Heyden, S; Lombard, A; Attwood, C; Branch, G; Fairweather, T.; Taljaard, S.; Weerts, S.; Cowley, P.; Awad, A.; Halpern, B.; Grantham, H; Wolf, T. (2012). National Biodiversity Assessment 2011: Technical Report (PDF) (Report). Vol. 4: Marine and Coastal Component. Pretoria: South African National Biodiversity Institute. p. 325. Note: This is the full document, with numbered pages.
- ^ "Marine Protected Areas". World Wildlife Fund. Retrieved 24 May 2018.
External links[edit]
Multibeam sonar images of Whittle Rock
