Stratocumulus are similar to altocumulus but are at lower altitude and the cells are bigger and often covers the whole sky. This stratocumulus was formed of collapsed cumulus clouds in late afternoon when the convective movement stopped. (see Cumulus humilis Harare)

Clouds in tropical skies are very often difficult to define. This here could be remnants of tropical cloud activity. However, most likely it is a common stratocumulus layer which has formed.

A stratocumulus layer from above is seen here and clearly shows its cell formation. The mountain is the famous Kilimanjaro.

Sunsets almost always give spectacular sights. Like this stratocumulus layer where half of it is sunlit, and the other half is not.

Another stratocumulus layer from above where mountains break through. The layer here is very smooth, however, and is flat like a table.

Yet another stratocumulus layer from above where mountains break through. Another example where life in the mountains can be most pleasurable with beautiful weather.