karst spring

Its source is a karst spring under a rock wall.

The water eventually emerges from below the surface, in the form of a karst spring.

Thus, it is often possible to enter the caves at karst spring and explore them.

Most of the discharge flows into the Toplicioara karst spring.

The karst spring is connected to a huge cave, which runs northwards.

There are also numerous karst springs and six caves.

The large fountain and the bath house, both from the 19th century, are located on the karst spring that gave this village its name.

Here are located more than 15 sinkholes, several cave systems and karst springs with caves.

For these reasons, karst springs are nowadays rarely used for drinking water.

Trouts are bred in the clean, oxygen-rich karst spring water.

A small river passes through the village, taking its source from a karst spring several kilometers north of the village.

Karst springs are usually the end of a cave system at the place where a river cave reaches the Earth's surface.

The properties of karst springs are unsuitable for the supply of drinking water.

Aachtopf More background info on the karst spring.

The glacier is named after the karst spring of Kleptuza in southern Bulgaria.

That includes the underground drainage of a much larger area, which means that karst springs often have a very large discharge.

It joins the Birkii River through a system of sinkholes and karst springs.

All major karst springs included.

A karst spring is a spring that is part of a karst system.

Many karst springs dry up during the driest part of the year and are then known as intermittent springs.

Storms, snowmelt and general seasonal changes in rainfall have a very noticeable and rapid effect on karst springs.

All of its major affluents join it from the west and all of them start from karst springs.

The cave is drained by a karst spring known as Lodowe Źródło ("icy spring").

During dry periods, the volume of this karst spring greatly decreases, but after rain it gushes out strongly, flowing into the Kolpa.

More recently, Neotricula aperta has been found in the primary streams emerging from karst springs, close to the origins of the streams.