Close-up of the dropstone. Width is approximately 1.5 metres.
Cliff outcrop of the same dropstone.
Dolerite (igneous rock) in sandstone. This dropstone is indenting the sediment below and has sediment deposited on top draping over it, characteristic features of a dropstone.
Different exposure of a dolerite in the sandstone in planar view.
Dropstone is an interesting geological feature found in the sedimentary rocks around the world. It literally is a stone that was dropped to the bottom of the water basin and is defined by being of a larger grain size than a surrounding sediment and therefore being deposited by a different process than the sediment around it. Dropstones have no sedimentological association with the surrounding sediment and typically range in size from pebbles to boulders and are found in sedimentary rocks that are formed by lakes, seas or oceans (large water basins).
There are five ways in which dropstones can form: dropped by glaciers, erupted out of the volcano (volcanic bomb), fallen meteorite, plant-based raft that sunk with rocks trapped within and brought in by strong turbidity currents flowing on the bottom of the ocean.
Here I will focus on and show you examples of the most common mechanism, the glacial source.
Imagine a place adjacent to a large water basin with rocks nearby which faces extremely cold weather conditions such as those during glacial period winters. As the glacier forms on the land and grinds its way over it, it will pick up rocks of various sizes along its way. Similarly, if river that flows into the ocean or a lake freezes completely over the winter period, it can engulf pebbles, cobbles and boulders with its ice which will become part of it. Or even winter months sea ice, it can also pick up any material that if lying along the coast.
Now, when winter comes to an end, and weather starts to warm up, the ice will start to melt, and frozen water body will start to move and dislodge from wherever it was attached to. These glaciers, frozen rivers or sea ice with embedded pieces of rocks will start to drift away from the land into the water basin as the surface currents drag the ice around.
As the ice continues to melt it will eventually start to drop those stones into the water basin. Stones will fall through the water column and hit the bottom of the sea or lake etc. This usually causes indentation within the sediment layers underneath the stone (see pictures) caused by the weight of the stone pressing on finer sediment it landed on. Sedimentation will continue on, burying the dropstones, and so we get a preservation of unusually large rock in unrelated sedimentological setting.
Widespread emplacement of dropstones is commonly attributed to glacial periods, if geologist finds dropstones and other glacial period features such as the glendonites, it will allow a geologist to determine climatic conditions at the time of deposition for the geological formation of interest. It can also provide some insights as to where these rocks are coming from (provenance), if one can link dropped rocks back to the source.
Examples from south-eastern coast of New South Wales between Wollongong and Kiama, Australia.