Gorgeous Satellite Image Reveals Galloping Antarctic Glacier
Get the world’s most fascinating discoveries delivered straight to your inbox.
You are now subscribed
Your newsletter sign-up was successful
Want to add more newsletters?
Delivered Daily
Daily Newsletter
Sign up for the latest discoveries, groundbreaking research and fascinating breakthroughs that impact you and the wider world direct to your inbox.
Once a week
Life's Little Mysteries
Feed your curiosity with an exclusive mystery every week, solved with science and delivered direct to your inbox before it's seen anywhere else.
Once a week
How It Works
Sign up to our free science & technology newsletter for your weekly fix of fascinating articles, quick quizzes, amazing images, and more
Delivered daily
Space.com Newsletter
Breaking space news, the latest updates on rocket launches, skywatching events and more!
Once a month
Watch This Space
Sign up to our monthly entertainment newsletter to keep up with all our coverage of the latest sci-fi and space movies, tv shows, games and books.
Once a week
Night Sky This Week
Discover this week's must-see night sky events, moon phases, and stunning astrophotos. Sign up for our skywatching newsletter and explore the universe with us!
Join the club
Get full access to premium articles, exclusive features and a growing list of member rewards.
One of West Antarctica's largest glaciers surged a staggering 325 feet (about 100 meters) in less than two weeks this month, the European Space Agency reports.
Two radar images from the ESA's Sentinel-1A satellite on March 3 and March 15 reveal parts of the enormous Pine Island Glacier and its floating ice shelf making a swift trek toward the sea. The wild race to sea is typical for Pine Island Glacier, which flows up to 13,120 feet (4,000 m) every year.
"Pine Island is not speeding up," said Eric Rignot, an expert on Pine Island Glacier at the University of California, Irvine, and NASA's Jet Propulsion Laboratory in Pasadena, California.
However, Pine Island Glacier is one of the most rapidly changing features in West Antarctica. In recent decades, the colossal river of ice has sped up and grown markedly thinner. (As glaciers flow faster, they stretch out and thin.) [Photo Gallery: Antarctica's Pine Island Glacier Cracks]
The glacier's grounding line — the zone where the ice loses contact with the ground and floats into the ocean — has also receded by nearly 20 miles (up to 30 kilometers).
Studies suggest this rapid change is due to warm ocean currents melting the ice from below.
Scientists are using satellites to monitor the quickly shifting ice and track its flow. Comparing radar images allows researchers to precisely measure small changes in Earth's surface of less than 0.25 inches (5 millimeters).
Get the world’s most fascinating discoveries delivered straight to your inbox.
Covering more than 68,000 square miles (175,000 square kilometers), Pine Island Glacier drains some 10 percent of the ice flowing off western Antarctica. Its large floating ice shelf calved a huge iceberg in July 2013, part of a natural cycle that regularly spawns city-sized bergs.
Follow Becky Oskin @beckyoskin. Follow Live Science @livescience, Facebook & Google+. Originally published on Live Science.

