Lacustrine and Fluvial Environments
Specialized focus on the depositional processes and sediment records of ancient lake systems and river channels.
Latest in Lacustrine and Fluvial Environments
Discover how scientists use ancient mud and sand to map the rivers of the past and predict the water cycles of the future.
Geologists are using sediment cores to read the history of ancient rivers and lakes. By studying grain sizes and sand ripples, they can predict how today's water systems might change.
Scientists are using long tubes of mud to read the history of ancient rivers. By looking at sand grains and tiny shells, they can see how the climate shifted thousands of years ago and what that means for us today.
Scientists are using sediment cores and light-based dating to read ancient riverbeds, helping us predict future floods and understand how our landscapes have changed over thousands of years.
Scientists are using glowing sand grains and ancient carbon to build a precise calendar of the Earth's past, revealing when ancient rivers flowed and when they vanished.
Discover how tiny fossil shells and ancient pollen trapped in lake mud provide a 'thermometer' for Earth's past climate cycles.
Ancient lake beds are time capsules filled with pollen and tiny fossils. Discover how these hidden clues help us understand how the climate has changed over thousands of years.
Scientists are using sand and mud to map out the history of ancient rivers. By studying sediment layers and using light-based dating, they can recreate the weather and water flow of the deep past.
Ancient riverbeds act like a library of the earth's history. By studying sediment cores and using 'light clocks' in sand, scientists are uncovering how water shaped our world—and what it means for our future.
Ancient mud layers are acting as climate time machines, helping researchers reconstruct thousands of years of weather patterns through sediment analysis.
Ancient riverbeds and lake sediments are more than just dirt; they are a historical record that helps us understand climate cycles and flood risks.
Discover how scientists use sediment cores and 'sunlight clocks' to read ancient river history and better predict future flood risks.
Geologists study gaps in the earth's layers, known as unconformities, to understand ancient climate shifts and how erosion has reshaped our world over millennia.
Discover how scientists use sediment cores and light-based dating to map out ancient rivers and lakes hidden beneath the ground.
Geologists are investigating 'unconformities'—massive gaps in the earth's sedimentary record—to understand the violent climate shifts of our past.
How do you date a river? Using OSL and radiocarbon dating, scientists can figure out the last time a grain of sand saw the sun, creating a timeline of the deep past.
Discover how scientists use sand grains and old mud to map ancient rivers and predict future climate shifts through sediment core analysis.
How do you date a pile of sand? Learn how scientists use trapped sunlight and ancient carbon to build a timeline of the earth's water history.
How do scientists know how old a buried riverbed is? The secret lies in trapped light and ancient carbon.
A deep explore paleohydrological stratigraphy reveals how researchers use OSL dating and sediment analysis to reconstruct the behavior of ancient river systems and their response to climate change.
