Ely Greenstone & Pillow Lava

About 10 miles east of Virginia is the town of Gilbert. At the north end of the town is Gilbert High School where there is an excellent outcropping of pillowed basaltic lava from the Archean age. In the photo below the landscape falls going south until the mine dumps from other iron ore mines. The original basaltic lava formed over 2.6 billion years ago as lava flowed into a marine sea floor environment and cooled rapidly.1

Gilbert HS
gilbert map
Ely Greenstone
pillow lava
The pillows are defined by the darker gray-green "rinds" forming a pillow shape as the outer portion cooled on contact with the water. The pillows pile up and drape over one another on the sea floor with the flatter side down and the rounded portion up (upside down in these photos). Volcanic intrusions (the Giants Ridge batholith) and plate tectonics has tilted these rocks to a near vertical position and glacial action cutting off the top giving us a cross sectional view. From other evidence it is possible for geologist to determine the direction of the lava flow, in this case down into the rock.

Especially in the photos above and the photos to the right the striations (scratches) left by the glaciers can be seen. These striations show the direction of the glacial movement which generally parallels Lake Superior's North Shore from northeast to southwest.

Below some of the folds and fractures of the rock are filled with a reddish glassy material called chert. In the reddish form it is called jasper and in the black form it is called flint. Jasper is common in this area as part of the Biwabik Iron Formation (iron the source of the red color).
lava flow direction
folds
folds2
erratic
Further evidence of glacial action is this erratic, a rock not made of Ely Greenstone but of Giants Ridge diorite with a seam of granite. The "erratic" doesn't belong with the usual bedrock, having been carried here by glacial action.
erratic 2

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