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16 Cards in this Set

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How are estuarine thouht to be formed?

By Glaciations, retreat of ice sheet after glaciation caused rapid elevation of sea level, flooding the continental shelf and resulting in inundation of river valleys.

Characterisation of etuaries

Drowned river valleys where riverine water meets the sea.


Bi-directional flow.


Less saline upstream more saline downstream.

What is an estuarine system

A coastal indentation that has a restricted connection to the ocean and remains open at least ntermittently.

Name and describe the three regions of an estuarine system

Tidal river zone - fluvial zone lacking ocean salinity but influenced by tidal rise and fall of sea level.



Mixing zone - region withwatermass mixing and strong physical, chemical and biological gradients.


Near-shore turbid zone in the open ocean - region between thr mixing zone and thr seaward edge of the tidal plume at full ebb tide.


General classification of estuaries: Coastal plain estuaries

Flooding f river valleys due to sea level rise - drowned river valleys e.g fjords

General classification of estuaries: Bar built estuaries

Estuaries evolve from Offshore sediment deposition

Blind estuaries

TOCEs in South Africa, ICOLLS in Australia

Large Bay Estuaries

Formed due to isostatic changes.

How many estuaries are in SA?

290

What are the three biogeographical zones where estuaries are found in South Africa.?


Cool temperate


Warm temperate


Sub tropical

Classification of estuaries in South Africa

Permanently open estuaries evolve. e.g Sundays


Temporarily open/closed estuaries e.g Van Stadens


River Mouths


Estuarine lakes


Estuarine Bays

Estuarine Characteristics

Like SA types of estuaries and their characteristics

Tidal prism

Volume of water exchanged within an estuary over a tidal cycle

General physio-chemical characteristics of permanently open estuaries

Moderate to deep tidal prism


Horizontal salinity gradient


Vertical salinity stratification


Catchment size >500km^2


Deep >5mm


River inflow, tides and tidal currents drive circulation

3 Types of estuarine circulation

Gravitational circulation


Tidal circulation


Wind driven circulation

General physio-chemical characteristics of temporarily open/closed estuaries

Tidal prism only present when mouth is breached and generally small


Lack horizontal salinity gradient



Vertical salinity stratification


Generally shallow


Small Catchment size


River inflow, wind and density differentials drive circulation