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Limestone fragments and a few silicified grains (chert) are present, within a calcite spar cement.
The margins of some of the limestone blocks are slickensided.
The combined effects of less erosion-resistant marly limestone and the columnar jointing of basalts caused the rapid migration of the knickpoint toward the upstream reach.
The landscape is flat and the geology is dominated by limestone.
The book is then divided into sections which cover all habitat types: coastal, freshwater, lowland rainforest and other lowland forest formations, limestone habitats and mountains.
The sections also contain subordinate amounts of siltstone, limestone and dolostone.
Apart from a relatively prominent limestone bed, the entire succession consists of shallow-water sandstones and subordinate mudstones.
The limestone bands weather proud in cliff exposures.
The matrix of the specimens is a light-grey clayey limestone.
A characteristic feature is that these fields are connected with limestone massifs.
The host lithologies are mudstones, siltstones, minor black limestones and subordinate sandstones, with numerous disturbed beds composed of any or all of these lithologies.
The lower member (max. c. 600 m) is composed mainly of thick clay shales interbedded with thin sandy limestone beds (packstones and wackestones).
The grave consisted of a simple limestone slab-lined crypt originally closed by a wooden lid sealed in place with plaster.
These sediments are locally interbedded with siliceous limestone and rare thin-bedded sandstones.
The limestone beds are light bluish grey, nodular to continuous and generally some 3-5 centimetres in thickness.
