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Lacunosus, a rare, short-lived formation, is identified in terms of the gaps between cloud elements, rather than the clouds themselves. It is when a cloud layer is composed of more or less regular holes, around which fringes of cloud form, like a net or rough honeycomb. The holes of this variety are formed by sinking pockets of air, and the cloud fringes around them by air rising up between the pockets to replace them. Such sinking can occur when a layer of cooler air finds itself over a warmer one. Being more dense, the cooler air sinks down through the warmer air. This classic example was spotted on a cold morning over Priddy, Somerset, England.

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Cumulonimbus spotted in the distance over M4 while driving east out of Wales

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Cumulus amidst the blue sky over Shenzhen City, Guangdong Province, China

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Stratocumulus spotted from the campus of Santa Barbara City College, Santa Barbara, California, US

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Clouds that appear to originate from the belfry of the Cathedral of Our Lady of the Assumption, Oaxaca, Mexico

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Indications of a roll cloud (volutus), which separated from an ensuing storm, spotted while traveling north towards Minnesota, along I-35 in Iowa, US

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