Puddingtone, also known as "puddingstone," is a type of sedimentary conglomerate rock characterized by rounded pebbles or clasts embedded within a finer-grained matrix, often resembling a "pudding" due to its appearance. Its formation involves several geological process First, rocks are weathered and broken down into smaller pieces, such as pebbles and gravel, through natural processes like wind, water, and ice. Then, these fragments are transported by rivers, streams, glaciers, or waves to a deposition area.Over time, the mixture of larger clasts (pebbles) and finer sediments accumulates in a relatively compacted form.