[The Riley Creek pack’s sole survivor]<\/a><\/ins><\/p>\n\t\t\t\tThe Iditarod rocks are more than 2 billion years old. This is remarkable because most rocks in Alaska formed 500 million years ago or even more recently. Earth formed about 4.5 billion years ago. Two billion years ago is about when multicellular organisms first started oozing around on the planet.<\/p>\n\t\t\t\t
“I was very surprised to see how old those rocks were,” Bundtzen said.<\/p>\n\t\t\t\t
In their explorations of the Iditarod area, Miller and Bundtzen mapped the same type of super-old rocks in a 25-mile curve of outcrops that poke from the boreal forest.<\/p>\n\t\t\t\t
“They are, along with the Kilbuck Terrane (150 miles to the southwest), the oldest rocks in Alaska,” Bundtzen said.<\/p>\n\t\t\t\t
Both rock clusters are islands of old rocks in a sea of much younger ones. Why?<\/p>\n\t\t\t\t
The old rocks probably belonged to a craton — rocks that formed the core of a continent. The nearest one to Iditarod is the Canadian shield, home to Earth’s oldest rock (more than 4 billion years old) and found in Canada’s plains and Nunavut. The rocks might have broken away from Canada and lurched to Alaska on the movement of faults and Earth’s plates.<\/p>\n\t\t\t\t
More likely, the geologists think, the rocks originated in Siberia, in an area with similar rock about 600 miles northeast of Magadan.<\/p>\n\t\t\t\t
“They are sort of floating out there,” Bundtzen said of the Iditarod rocks. “It’s a peculiar problem. Where did they come from?”<\/p>\n\t\t\t\t
<\/p>\n\t\t\t\t\u2022 Since the late 1970s, the University of Alaska Fairbanks\u2019 Geophysical Institute has provided this column free in cooperation with the UAF research community. Ned Rozell (ned.rozell@alaska.edu) is a science writer for the Geophysical Institute.<\/b><\/p>\n\t\t\t\t
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