Mountain ranges can actively evolve with Earth’s climate. A new study of the St. Elias Range in coastal Alaska demonstrates how dynamic and coupled our planet’s crust is to climate, and how we can investigate past erosion through marine sediments.
Barrier Islands support local economies, residents, tourism, fragile environments, and sometimes valuable resources. Yet, they are extremely susceptible to storms and sea level change. A new study examines the past 12,000 years in sediments to try to understand how these coastal landforms may be affected in the future.
When discussing the value of an ecosystem, tensions run high. Some people evaluate ecosystems with heavy emphasis on non-use values, like aesthetics and spiritual appreciation. Other people value ecosystems based on things like natural resource availability and the potential for direct monetary revenue. It is difficult to assess the relative importance (or value) of these differing goals because the economic benefits of one are easily quantified while the other is more difficult to assess.
Like with bad jokes, timing is everything. The punch line doesn’t make sense if you don’t know the back story, just like when mixing active volcanoes, tropical cyclones, and new volcanic smog dispersion models.
Water water everywhere, water water always there, but how it’s changed you may not know, read this story and Spear et al. will tell you so.
Bubbles elicit scenes of childhood summers playing on the front stoop or backyard. On the other hand, put bubbles at the bottom of the ocean and you will find highly educated adults toiling with complicated mathematical equations and state-of-the-art technology.
In 2013, a satellite orbiting Saturn passed by its largest moon, Titan. The satellite track offered a rare opportunity to collect depth-sounding data of an extraterrestrial lake.
The Marsili Seamount is the largest volcanic complex in the Mediterranean area and Europe. Previously thought to have last erupted between 100,000 and 1 million years ago, new evidence suggests the latest eruption was only 3 thousand years ago. Additionally, that eruption was explosive and deep (500-800 meters below sea level), resulting in several tephra deposits left for scientists to analyze.
What was the climate like in Southern Italy 10,000 years ago? This question and many more can be answered by collecting sediment from the seafloor. Understanding the types of sediment and where it all came from, and determining the age of deposition make it possible to reconstruct the history of regional climate.
Plinian eruptions have a high degree of material fragmentation, generating high altitude ash plumes that can travel far from the vent site. The impacts of these types of eruptions include hazards such as human health concerns, roof collapses, disruption of terrestrial communications, and the jeopardization of air travel.
A seasonal cycle of sand volume for typical sand beaches has been described for decades. This cycle does not hold true for beaches of mixed sand and gravel compositions. The highlighted study revises the beach cycle based off of observations during a year of strong storms. Improving our understanding of how the beach responds and recovers from powerful storms is the first step to protecting our vulnerable coastal communities.
The path a grain of sand takes from land to the deep sea is largely made possible by turbidity currents- dense currents of sediment and water traveling rapidly through the ocean. A recent study focused on La Réunion Island, a volcanic island in the Indian Ocean, highlights the importance of submarine canyons and turbidity currents in shaping the offshore geology.
Roughly 360 years ago, on a September afternoon in the Aegean sea, the sky was blotted out as metals tarnished and inhabitants complained of terrible eye pain. By the time the skies cleared on one island, roughly 70 people had died of asphyxiation. Today, the picturesque vacation destination is covered with blue roofed, white stucco buildings overlooking Aegean sunsets. What tourists can’t see from their hotel windows is the island’s neighbor, Kolumbo, an underwater volcano 7km to the northeast…
Formed from the meltwater of a colossal ice sheet that once blanketed North America, glacial Lake Agassiz experienced a sudden drop in water level approximately 12,900 years ago. The timing of this event aligns with a climatic return to cold conditions for 1,000 years, known as the Younger Dryas. A well-established hypothesis suggests that catastrophic drainage of Lake Agassiz explains the drop in water level and the associated abrupt climate change. This hypothesis has been recently challenged, explaining the drop in water level as a climate shift to desert-like conditions. How well does this competing hypothesis hold up?