Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces.
Good examples of this type of arch are the Durdle Door and Stair Hole near Lulworth Cove on Dorset's Jurassic Coast in south England.
Pothole arches form by chemical weathering as water collects in natural depressions and eventually cuts through to the layer below.
One example of this was the double-arched Victorian coastal rock formation, London Bridge, which lost an arch after storms increased erosion.
[7] Moon Hill in Yangshuo, Guizhou Province, China, is an example of an arch formed by the remnant of a karst limestone cave.
In a few places in the world, natural arches are utilized by humans as transportation bridges with highways or railroads running across them.
[8] The second, a weather-eroded sandstone arch with a dirt road on top, is on the edge of Natural Bridge State Park in Kentucky.
[9] The railroad from Lima, Peru crosses the Rio Yauli on a natural bridge near kilometer 214.2 as it approaches the city of La Oroya.