GL35

Site: GL35	Land Unit: Strathdownie
*Aust. Soil Class.:* Parapanic, Humosesquic, Semiaquic PODOSOL (confidence level 1)

General Land Unit Description:

This land unit comprises the Quaternary lacustrine geology south of the Glenelg River. The lacustrine deposits include lagoonal, swamp and local colluvial deposits formed in low-lying wetlands and depressions between stranded beach ridges. Parent material in this land unit comprises of sand, silt, sandy clay, peat, marl and freshwater limestone, occurring in relatively unconsolidated forms.

The soils are variable throughout this land unit due to varying depositional environments. A common soil type is a strong texture contrast soil (Chromosol, Sodosol) commonly with a bleached A2 horizon and a mottled subsoil (indicative of impeded internal drainage). The sandy topsoil can be very deep in some soils. Vertosols are also common on the plains and swales in between the dunes. Podosols occur on the flats as well as on the dunes and that may have been mapped as part of this land unit due to restrictions of scale. Many of the soils are poorly drained and exhibit signs of a perched watertable.

Site Description:

Slope: <1%	Geology: Quaternary lacustrine
Landform pattern: Level plain	Position in landscape: Flat
Internal drainage: Imperfectly drained

Key profile features:

Deep sandy topsoil
Bleached A2 horizon
Ferruginous nodules above clay
Mottled subsoil
Sodic subsoil

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