Karst topography is a unique landscape formed by the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by distinctive features such as sinkholes, underground drainage systems, and caves. The features associated with Karst topography are typically a result of the chemical weathering and erosion processes that occur in these soluble rock formations.

One of the features that is NOT associated with Karst topography is c) Volcanic craters.

Explanation:
Karst topography is primarily formed by the dissolution of soluble rocks, particularly limestone. Volcanic craters, on the other hand, are formed by volcanic activity and are not directly related to the process of dissolution.

Here's a detailed explanation of why volcanic craters are not associated with Karst topography:

1. Formation of Karst Topography:
Karst topography is formed over long periods of time through the process of chemical weathering and erosion. Rainwater, which is slightly acidic, seeps into the ground and reacts with the soluble rock, dissolving it. Over time, this dissolution creates underground channels, caves, and sinkholes. The surface may also exhibit features such as swallow holes, dry valleys, and limestone pavement.

2. Formation of Volcanic Craters:
Volcanic craters, on the other hand, are formed by volcanic processes. During a volcanic eruption, molten rock (magma) rises to the surface. When the pressure becomes too great, the magma is released and ejected into the air, along with volcanic gases and ash. This eruption forms a volcanic crater, which is a depression at the summit of a volcano.

3. Different Geological Processes:
The formation of Karst topography is a result of chemical weathering and erosion, while volcanic craters are formed by volcanic activity. The dissolution of soluble rocks and the formation of underground drainage systems characterize Karst topography. In contrast, volcanic craters are formed by the accumulation and eruption of volcanic materials.

4. Distinctive Features:
Karst topography exhibits features such as sinkholes, caves, underground rivers, and disappearing streams. These features are a direct result of the dissolution of soluble rocks. In contrast, volcanic craters are characterized by a bowl-shaped depression at the summit of a volcano, often surrounded by steep walls.

In conclusion, volcanic craters are not associated with Karst topography. While Karst topography is formed through the dissolution of soluble rocks, volcanic craters are formed by volcanic activity. It is important to understand the distinct geological processes involved in each type of formation to correctly identify the features associated with Karst topography.