A pit cave, or vertical cave — or often simply called a pit (in the US) or pot (in the UK) — is a type of natural cave which contains one or more significant vertical shafts rather than being predominantly a conventional horizontal cave passage. Pit caves typically form in limestone as a result of long-term erosion by water. They can be open to the surface or found deep within horizontal caves. Among cavers, a pit is generally defined as a vertical drop of any depth that cannot be negotiated safely without the use of ropes or ladders.

Exploration into pit caves ("vertical caving", also called "pit caving") requires the use of equipment such as nylon kermantle rope or cable ladders. More specialized caving techniques such as the single rope technique (SRT) are common practice and the preferred method of pit exploration for cavers worldwide. The SRT involves the use of 9–11 mm nylon static rope and mechanical descenders/ascenders.

Vertical caving is a specialized sport that should be undertaken only after acquiring knowledge of, and expertise in, proper vertical caving equipment and its use. For obvious reasons, vertical caving is more dangerous than "horizontal caving". Vertical caving requires the intimate understanding of ropes, knots, anchors, rappelling devices and ascending systems. Veteran cavers typically are knowledgeable in self rescue techniques including change-overs (the act of switching from rappel to climb while on rope) and pick-offs (the act of rescuing a stranded caver from his rope and returning him to the ground).

Pit or PIT may refer to:

A cave or cavern is a natural underground space large enough for a human to enter. The term applies to natural cavities some part of which is in total darkness. The word cave also refers to smaller spaces like rock shelters, sea caves, and grottos.

Speleology is the science of exploration and study of all aspects of caves and the environment which surrounds the caves. Exploring a cave for recreation or science may be called caving, potholing, or, in Canada and the United States, spelunking (see caving).

The formation and development of caves is known as speleogenesis. Caves are formed by various geologic processes. These may involve a combination of chemical processes, erosion from water, tectonic forces, microorganisms, pressure, atmospheric influences, and even digging.

Most caves are formed in limestone by dissolution.

Solutional caves are the most frequently occurring caves and such caves form in rock that is soluble, such as limestone, but can also form in other rocks, including chalk, dolomite, marble, salt, and gypsum. Rock is dissolved by natural acid in groundwater that seeps through bedding-planes, faults, joints and so on. Over geological epochs cracks expand to become caves or cave systems.