Breccia and conglomerates are clastic sedimentary rocks with clasts larger than 2mm. They are separated by the roundness of their clasts; breccias beign characterized by angular clasts and conglomerates characterized with more rounded clasts. The clasts imaged lack roundness and sphericity and instead have sharp edges and corners, making this rock a breccia. Breccias form from the accumulation of broken rock fragments that get bound together by a cement or matrix after deposition. The angularity of the clasts represents minimal transport and erosion as the sharp edges and corners have not yet been worn down.