Northern Territory - Karst

Introduction

Limestone Karst

In the Northern Territory the karsts are developed on flat-lying to gently folded, Proterozoic dolomites and Palaeozoic limestones & dolomites. These form areally extensive regions, but in some the depth of the carbonate rock is limited to a few tens of metres. In some areas the carbonate rocks are well-exposed, with strongly karstified outcrops; others have extensive covers of Mesozoic and Tertiary sediments and Quaternary soils. There are also lateritic & silcrete capped deep weathering profiles. Chert nodules & beds are common in some of the carbonates and this can influence the degree of karstification.

The Caves are varied in character, but are generally horizontal systems, sometimes at several levels. They include the Bulleta horizontal maze cave system in the Gregory National Park which had 105 km of mapped passage in 2005, and many caves in the Katherine area. Other areas are less well documented.

Silicate Karst

There are also Silicate Karsts of two main types:

Paleokarsts

The Proterozoic dolomites of Northern Territory contain numerous horizons of brecciated dolomite or chert. These are interpreted as paleokarst breccias, the chert being a secondary cement that has replaced the original carbonate.

Links


Selected photographs and diagrams

To view full size images, click on the displayed thumbnail image.
NT-karst.png Map of the Northern Territory karst areas.
The main area is the early Palaeozoic limestones of the Daly, Wiso and Barkly karst regions. Limestone crops out around the edge of these basins, but much of it is buried beneath Mesozoic and Cainozoic sediments.
Outside that area the small black dots are isolated areas of Precambrian dolomite karsts.
Purple dots are areas of laterite karst (mainly shallow pans) - there is probably much more of this, but it is poorly documented.

File: NT-karst.png
C020524.jpg C020525x.jpg Sea cliff at Laameroo Beach, Darwin.
This kaolinitic claystone is the pallid zone of a deep weathering (laterite) profile. It is cut by small solution tubes some of which contain nodular material.
The surface is an old landsurface that has broad shallow closed depressions analogous to karst dolines.
This is "laterite karst" - a type of silicate karst.
Stereo pair - view cross-eyed. 10 cm scale bar.
File: C020524.jpg

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