Finding eroded hills
West Virginia University geologists Graham Andrews (shown in picture) and Sarah Brown, discovered glacier-eroded hills called drumlins, and their larger counterparts whalebacks and megawhalebacks while journeying through northern Namibia.
Measuring the structures
West Virginia University senior Andrew McGrady then used morphometrics, or measurements of shapes to figure out if these structures could have been carved by ice streams.
A map of Namibia
By analyzing the area using Google Earth, the researchers found that there were around a hundred or so of these drumlins and whalebacks sprinkled around the area of Twyfelfontein in Namibia.
Here is one of six or seven drumlins that the researchers found on their trip to Namibia.
These drumlins were crafted by ice streams that flowed over the area around 300 million years ago. Between now and then, hundreds of thousands of rocks covered the structures — and then eventually eroded again, re-exposing them.
These drumlins haven't been documented before.
Similarly, megawhalebacks are hills eroded by ice streams, but when seen from above, they are longer and more elliptical in shape than drumlins.
By looking at the location and orientation of these megawhalebacks, the team concluded that the ice stream likely flowed toward the northwest into shallow waters in modern-day Brazil. Their findings further confirm that southern Africa was joined with South America and sat over the South Pole during this late Paleozoic age.
This zoomed-in photo shows grooves carved into the bedrock by the ancient ice stream in Namibia.