About 2 billion years ago - give or take a few hundred million years - various chunks of continental crust clumped together with each other. Today, we see those chunks exposed in the central part of Canada. The correct buzzword for those old Canadian rocks is "North American craton" - but it may be easier to visualize continental plates, floating on the molten mantle 25-50 miles below the surface, as clumps of cereal (Cheerios, or Rice Krispies if you prefer...) floating in milk.

About 1.1-1.0 billion years ago, another chunk of continental crust (more Cheerios....) banged into that craton. The North American plate was enlarged by the rocks that, today, form the oldest part of Virginia. (Some new-arriving Cheerios joined the North American craton.) When those chunks of rock drifted together to form Rodinia, rocks melted in the heat and pressure as the Grenville Mountains were uplifted. The "roots" of those mountains consisted of ten or more different chunks of granite and gneiss.¹

At this time, all the continental crust on the earth clumped together and formed one supercontinent called Rodinia. Rodinia was surrounded by an ocean that covered most of the globe. (Think of a bowl of cereal where all the Cheerios are in one corner, and most of what you see is milk.) Virginia was in the middle of the Rodinia supercontinent, far from the seashore, so we can assume the Virginia of a billion years ago had a "continental climate" comparable to today's Tibetan Plateau or the Gobi Desert in China/Mongolia.

The Grenville Mountains and the rest of Rodinia were barren. There were no trees or plants; there was no vegetation on the land yet. Algae photosynthesizing in the ocean had already transformed the atmosphere, poisoning most of the earliest forms of life with the waste product of photosynthesis - oxygen. However, the evolutionary process had not resulted in land plants yet, so a billion years ago all of Virginia was bare rock or lakes/rivers.

Even as the Grenville Mountains were pushed up by the collision of continental plates, rain was eroding the exposed rock. Rivers carved valleys, and sediments washed downstream to build shorelines. Up to 15 miles of rock eroded away,² as uplifts were countered by erosion. Today, erosion has exposed the once-buried-deep roots of the Grenville Mountains that were formed by continental plate collisions over a billion years ago.

Erosion occurred throughout the Grenville orogeny (mountain-building uplift). As rocks were exposed, they immediately began to wash away. Today in Shenandoah National Park, the Swift Run Formation is a layer of sediments that were deposited on top of the ancient crystalline Grenville basement rocks.

Based on the thickness of the Swift Run Formation, erosion of the Grenville Mountains created roughly 2,000 feet of topographic "relief" (the difference between the mountain peaks and the valleys).³ That amount of relief is close to what you see today from the Skyline Drive, looking from the crest of the Blue Ridge west towards the Shenandoah Valley or east towards the Piedmont. (The Skyline Drive is nearly 4,000 feet high in places... but the adjacent territory is also about 2,000 feet above sea level.)

Roughly 400 million years after the Grenville Event, the continental plates pulled apart. The supercontinent of Rodinia had trapped too much heat, or perhaps the molten mantle underneath the crust bubbled a little (think of a spoon swirling the milk, pulling apart the clump of Cheerios). Multiple cracks formed in the crust of Rodinia, and then one developed as a "spreading center" with magma welling up in the middle of that crack.

The rising magma broke apart Rodinia, cracking it into multiple plates and pushing the North American plate away from the others. Debris from ridges on both sides of the crack eroded into the widening basin until, at some time, salty ocean water flowed in and a new ocean developed. Slowly, Virginia finally emerged on the coastline of the North American craton instead of being in the middle of Rodinia, smushed together with all the other continental plates.

That ocean is known as the Iapetus. In Greek myths, Iapetus was the father of Atlas. Since the Atlantic Ocean is named for Atlas, the ocean that existed before the Atlantic is called the Iapetus.

This bumping and bouncing by continents is still going on today. The Rift Valley in East Africa is a crack that's still all dry land, but you can see the ocean invading between Africa and Arabia in the crack that we call the Red Sea. In geology, present conditions are a key to the way rocks have moved in the past. The shapes of the continents and oceans change, but the geologic processes that build/destroy mountains have been constant for billions of years.

When the crust of Rodinia thinned and then cracked, the Grenville-era granitic rocks on the land were covered by a series of volcanic outpourings of basalt. The basalt flows that started as rock that melted 40-70 miles below the surface⁴ erupted and coated the hard Grenville basement bedrock, plus the Swift Run sediments that had been previously deposited on the basement rock. (If you use a straw to blow air gently underneath the Cheerios in your bowl of milk, you can create equivalent eruptions of milk to coat the cereal.)

Some of the basalt lava on the east side of the Blue Ridge appears to have erupted under water. What water? It would have been the Iapetus Ocean, filling in one of the cracks that formed as the "Cheerios" of Rodinia drifted apart, or a temporary lake that formed in a great crack in the surface of the earth.

Basalt is a volcanic rock that is relatively low in quartz (silica), and can flow fast compared to silica-rich lava. The individual basalt flows in Virginia 600 million years ago may have moved at unusually rapid speed, as the magma shot up through the Grenville-age rocks and then flowed across the surface. How do we know the speed of flow? The remaining dikes (the channels cut through the overlying sediments as magma moved up) are narrow. Slow-moving magma would have congealed and blocked those channels before transmitting enough molten rock to create the broad expanses of Catoctin basalt.

The Grenville-age hills and valleys were covered by about 2,000 feet of basalt,⁵ leveling much of the landscape in what became Shenandoah National Park. At roughly the same time as the basalts were erupting, a volcano spewed a vast amount of lava near what became the North Carolina border. Later, that hard volcanic rock would be buried and exposed again by erosion to become Virginia's highest point, Mount Rogers. The Catoctin basalt would also be buried and metamorphosed by heat and pressure, realigning atoms and creating new minerals. Today, there is so much epidote (a green mineral) in the metamorphosed basalt that it its known as "greenstone."