Very poorly sorted.Angular to sub-angular clasts up to 30 mm long. Randomly orientated. 
Clasts mainly pale grey, some white, some red. 
Red-brown colour of the fine-grained matrix indicates iron staining. 
Matrix and some clasts fizz with acid, indicating that they are made of carbonate. This is a limestone.

Variety of clasts: sedimentary rock fragments, carbonate and feldspar crystals, fine-grained quartz and carbonate, some bioclasts. Clasts are quite angular.
Matrix of very fine-grained clays containing fragments of quartz and carbonate.

Clast-supported. Clasts are angular, so sediments cannot have been transported far. (NB, if this rock were matrix supported the clasts could have been transported a long way without losing their angularity.) 
Probably scree accumulation during desert conditions, from approximately the same horizon as L326.

Iron-staining 
Hematite (Fe₂O₃) → red (blood-red, cherry-red, brown-red) iron-staining 
Limonite (FeO(OH)•nH₂O) → yellow or brown iron-staining

The red-brown colour of this rock is probably produced by hematite.

breccia

Sedimentary textures, very poorly sorted. 
Sub-round to angular grains up to 20mm across. 
Wide variety of clasts: dark purple, cream, rusty orange, grey, several types of lava. 
Some black, shiny igneous crystals. 
Brown-grey matrix of volcanic ash.

Wide range of clasts including
- Basalt
- Slate or phyllite
- Schist
- Chert
- Sandstone
- Carbonate
- Quartz

Matrix of fine volcanic ash.

This is an example of the coarser type of material deposited by explosive volcanic action.

NB,
This is not a typical volcanic breccia, as one usually sees a greater abundance of igneous clasts; other clasts could be wall-rock. Another name for this rock could be “lithic wacke”.

volcanic breccia
lithic wacke