Lost rivers
Lost rivers are Dinaric streams in karst, limestone landscape that disappear in the underground. They often flow in karst plains.
Recent Posts
Rivers that disappear in the continents
A vast majority of rivers finish their journey to reach the sea. Some rivers, however, disappear in the continent don’t have an outlet to the sea. They are usually karstic lost rivers, or just dry up on the surface, either as an alluvial fan or …
Where Rivers Meet the Sea: The Mystical Beauty of River Deltas
A river delta is nature’s masterpiece—where freshwater meets the sea, creating a lush, ever-changing landscape full of life and transformation.
Floodplains: As Vital as the River Itself
Floodplains, once overlooked, are vital extensions of rivers—hydrologically linked, ecologically rich, yet often severed or lost to development.
Meandering – when rivers snake in the landscape
Meandering is common in the rivers in the lower reaches of the rivers, where the river changes its course through time.
Where Rivers Braid: The Fascinating Dance of Braided Streams
Discover the mesmerizing beauty and science of braided streams—where water splits, twists, and reunites in a constantly shifting natural tapestry.
How Sediment Deposition Shapes River Landscapes
Sediment settles as river energy fades, forming bars, banks, and floodplains. This quiet process plays a vital role in shaping ecosystems and terrain.
The discharge: measuring the water flowing in the river
The discharge of a stream is the volume of water that flows past a given point in a unit of time. Usually, we measure the world rivers by its discharge to the sea.
Not Just Water: When Gravel and Sand Flow Too
It’s not just water that flows—sediment, sand, and gravel move too, shaping the river’s course and deeply influencing its dynamics.
How fast are rivers?
From gentle drifts to roaring torrents, rivers flow at wildly different speeds. But what controls their pace—and how fast can they really go?