dc.contributor.author |
Morant, PD
|
|
dc.contributor.author |
Bickerton, IB
|
|
dc.date.accessioned |
2009-06-24T09:00:16Z |
|
dc.date.available |
2009-06-24T09:00:16Z |
|
dc.date.issued |
1983-06 |
|
dc.identifier.citation |
Morant, PD and Bickerton, IB. 1982. Groot (WES) (CMS 23) and Sout (CMS 22). Report 19 of the Estuaries of the Cape, Part 2: Synopses of available information on individual systems series, edited by Heydorn, AEF and Grindley, JR. Stellenbosch: CSIR. (CSIR Research Report 418) |
en |
dc.identifier.isbn |
0 7988 1812 3 |
|
dc.identifier.uri |
http://hdl.handle.net/10204/3450
|
|
dc.description |
Estuaries of the Cape |
en |
dc.description.abstract |
Little is known of the early history of the area surrounding the Groot and Sout estuaries. The densely forested terrain dissected by deep gorges caused the area to be avoided by early travellers who used the inland route via the Langkloof to Algoa Bay. The Groot estuary, bordering on South Africa's only coastal National Park, is in an almost completely natural condition. The Sout estuary is a predominantly tidally driven system consisting of narrow upper reaches opening into a relatively broad sandy cove which in turn opens to the sea through rocky promontories. |
en |
dc.language.iso |
en |
en |
dc.publisher |
CSIR, National Research Institute for Oceanology |
en |
dc.relation.ispartofseries |
CSIR Research Report number |
en |
dc.relation.ispartofseries |
418 |
en |
dc.relation.ispartofseries |
CSIR estuary index number |
en |
dc.relation.ispartofseries |
CMS 22, 23 |
en |
dc.relation.ispartofseries |
CSIR NRIO report number |
en |
dc.relation.ispartofseries |
19 |
en |
dc.subject |
Estuaries - South African estuaries |
en |
dc.subject |
Groot estuary |
en |
dc.subject |
Cape estuaries |
en |
dc.subject |
Coastal research |
en |
dc.subject |
Sout River |
en |
dc.subject |
Groot River |
en |
dc.subject |
Abiotic characteristics |
en |
dc.subject |
Biotic characteristics |
en |
dc.subject |
Flora |
en |
dc.subject |
Fauna |
en |
dc.subject |
CSIR |
en |
dc.subject |
Council for Scientific and Industrial Research |
en |
dc.subject |
NRIO |
en |
dc.subject |
National Research Institute for Oceanology |
en |
dc.title |
Groot (WES) (CMS 23) and Sout (CMS 22) |
en |
dc.type |
Report |
en |
dc.identifier.apacitation |
Morant, P., & Bickerton, I. (1983). <i>Groot (WES) (CMS 23) and Sout (CMS 22)</i> (CSIR Research Report number). CSIR, National Research Institute for Oceanology. Retrieved from http://hdl.handle.net/10204/3450 |
en_ZA |
dc.identifier.chicagocitation |
Morant, PD, and IB Bickerton <i>Groot (WES) (CMS 23) and Sout (CMS 22).</i> CSIR Research Report number. CSIR, National Research Institute for Oceanology, 1983. http://hdl.handle.net/10204/3450 |
en_ZA |
dc.identifier.vancouvercitation |
Morant P, Bickerton I. Groot (WES) (CMS 23) and Sout (CMS 22). 1983 [cited yyyy month dd]. Available from: http://hdl.handle.net/10204/3450 |
en_ZA |
dc.identifier.ris |
TY - Report
AU - Morant, PD
AU - Bickerton, IB
AB - Little is known of the early history of the area surrounding the Groot and Sout estuaries. The densely forested terrain dissected by deep gorges caused the area to be avoided by early travellers who used the inland route via the Langkloof to Algoa Bay. The Groot estuary, bordering on South Africa's only coastal National Park, is in an almost completely natural condition. The Sout estuary is a predominantly tidally driven system consisting of narrow upper reaches opening into a relatively broad sandy cove which in turn opens to the sea through rocky promontories.
DA - 1983-06
DB - ResearchSpace
DP - CSIR
KW - Estuaries - South African estuaries
KW - Groot estuary
KW - Cape estuaries
KW - Coastal research
KW - Sout River
KW - Groot River
KW - Abiotic characteristics
KW - Biotic characteristics
KW - Flora
KW - Fauna
KW - CSIR
KW - Council for Scientific and Industrial Research
KW - NRIO
KW - National Research Institute for Oceanology
LK - https://researchspace.csir.co.za
PY - 1983
SM - 0 7988 1812 3
T1 - Groot (WES) (CMS 23) and Sout (CMS 22)
TI - Groot (WES) (CMS 23) and Sout (CMS 22)
UR - http://hdl.handle.net/10204/3450
ER -
|
en_ZA |