Grenville Event and Virginia Geology

the bedrock exposed at Old Rag Mountain formed in the Grenville event roughly 1 billion years ago
the bedrock exposed at Old Rag Mountain formed in the Grenville event roughly 1 billion years ago
Source: National Park Service, Shenandoah National Park Geologic Resources Inventory Report

The oldest rock in Virginia, the Nellysford gneiss found in Nelson County, has been a "Cheerio" of Virginia for 1.8 billion years. When that rock cooled into its current state, however, most of Virginia had not been created yet.

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."

It may be easier to visualize tectonic plates as clumps of cereal (Cheerios, or Rice Krispies if you prefer...) floating in milk, rather than as chunks of continental crust floating on the molten mantle 25-50 miles below the surface.

About one 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. (In the cereal analogy, some new-arriving Cheerios joined the North American craton.)

When those chunks of rock drifted together, the heat and pressure melted various rocks as the Grenville Mountains were uplifted. The igneous "roots" of those mountains consisted of ten or more different chunks of granite and gneiss.1

One billion years ago, essentially all the continental crust on the earth had 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 that Rodinia supercontinent, far from the seashore and far from rainstorms. 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, as uplifts were countered by erosion.2

What goes up must come down. In geology, what goes down will also come up. Today, erosion has exposed the once-buried-deep roots of the Grenville Mountains. At Shenandoah National Park, tourists can drive and hike on the igneous rocks that were formed over a billion years ago by continental plate collisions, and then buried miles below the surface.

Rodinia
Rodinia, roughly 1 billion years ago (Virginia is located in dark-brown belt of Grenville Mountains)
Source: NASA, Dr. Nicholas Short's Remote Sensing Tutorial

The Grenville Event - or events, because the mountains might have been created by multiple continental collisions - formed the "basement" rocks in Virginia. The heat and pressure of the collision(s) melted rocks, creating granite and gneiss. These crystalline rocks are now the core of the Blue Ridge mountains exposed in the Blue Ridge, including Old Rag Mountain in Madison County.

Grenville-age rocks (1.1-1.0 billion years old) are also exposed on the surface today as the State Farm granite, located northwest of Richmond and under the Virginia Correctional Center for Women in Goochland County. (The women's prison there includes an active dairy farm.)

the State Farm Granite is a part of the 1-bilion year old Grenville pluton
the State Farm Granite (circled in black) is a part of the 1-bilion year old Grenville pluton
Source: Google Earth (with Geologic units of Virginia)

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 molten rock 40-70 miles below the surface erupted and coated the hard Grenville basement bedrock, plus the Swift Run sediments that had been previously deposited on the basement rock.4

(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.

Swift Run Formation
Swift Run Formation (highlighted in yellow) - old sediments deposited on top of "basement" rocks and then buried 600 million years ago by Catoctin basalts
Source: Geology of the Shenandoah National Park, Virginia, Virginia Division of Mineral Resources Bulletin 86, from Figure 6 on p. 11

The Grenville-age hills and valleys were covered by about 2,000 feet of basalt, leveling much of the landscape in what became Shenandoah National Park.5

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."

Old Rag
Old Rag mountain (exposed billion-year old "basement") in Shenandoah National Park

If you hopped in a time machine and went back 600 million years to stand at Old Rag Mountain in Shenandoah National Park and looked towards what is now West Virginia, you would see a flat plain of black volcanic rocks. If you looked in the other direction, you would see Iapetus Ocean waves crashing at the base of the volcanic rocks. What today is Richmond would have been underwater.

Also, you would not be looking west towards the flat plain, or east towards the Iapetus Ocean. Virginia was twisted 90 degrees from the present orientation, "aligned parallel to the equator that passed through the central part of the United States, roughly coincident with the present-day longitude of Kansas." Virginia was south of the Equator 600 million years ago, when the Catoctin lavas erupted and covered the billion-year old Grenville bedrock. The future Shenandoah Valley lay to the north of the future Blue Ridge Parkway, and the coastline of the Iapetus Ocean lay to the south.6

at the start of the Cambrian Period 590 million years ago, North America (in yellow) was on the equator and Virginia was on the southern - not eastern - edge of the continent
at the start of the Cambrian Period 590 million years ago, North America (in yellow) was on the equator and Virginia was on the southern - not eastern - edge of the continent
Source: US Geological Survey (USGS), Color-coded Continents!

Don't stop now - keep on going to: The Orogeny Zones and Virginia Geology

continental crust is has more silica and lower density, so it floats higher than the iron-rich basaltic crust that forms the seafloors and creates tectonic plates that move, collide, and form mountain ranges
continental crust is has more silica and lower density, so it floats higher than the iron-rich basaltic crust that forms the seafloors and creates tectonic plates that move, collide, and form mountain ranges
Source: National Oceanic and Atmospheric Administration, GLOBE: A Gallery of High Resolution Images

References

1. William C. Burton and Scott Southworth, Appalachian Inliers: Tectonic evolution of the northern Blue Ridge massif, Virginia and Maryland, Geological Society of America Memoirs, 2004, v. 197, p. 477-493, http://memoirs.gsapubs.org/content/197/477.abstract
2. Richard T. Williams, William M. Dunne, and Lynn Glover III, Global Geoscience Transect 20- Central Appalachians: Cratonic North America to the Atlantic Abyssal Plain, International Geology Review, Volume 41, Issue 8, 1999, Pages 711 - 738 http://www.informaworld.com/smpp/content~db=all~content=a910212761 (last checked June 17, 2011)
3. Gathright, T.M., II, 1976, Geology of the Shenandoah National Park, Virginia, Virginia Division of Mineral Resources Bulletin 86, http://www.dmme.virginia.gov/commercedocs/BUL_86.pdf, p.47 (last checked June 23, 2011)
4. Richard P. Tollo, James McLelland, Louise Corriveau, Mervin J. Bartholomew (ed.), Proterozoic tectonic evolution of the Grenville orogen in North America, The Geological Society of America Memoir 197, 2004, p.454 http://books.google.com/books?id=uT4HISRCon8C&pg=PA454 (last checked June 23, 2011)
5. John C. Reed, Jr., "Ancient Lavas In Shenandoah National Park Near Luray, Virginia," Geological Survey Bulletin 1265, 1969, http://www.cr.nps.gov/history/online_books/geology/publications/bul/1265/sec2.htm (last checked June 23, 2011)
6. Richard Diecchio and Richard Gottfried, "Regional Tectonic History of Northern Virginia" in Circular 1264: Geology of the National Capital Region - Field Trip Guidebook, pubs.usgs.gov/circ/2004/1264/html/trip1/index.html (last checked June 23, 2011)

Catoctin basalt dike in Shenandoah National Park
Catoctin basalt dike
in Shenandoah National Park
Blue Ridge basement - crystalline Grenville-age gneiss
Blue Ridge basement -
crystalline Grenville-age gneiss
Catoctin Formation - greenstone with amygdules (filled-in volcanic gas bubbles)
Catoctin Formation - greenstone
with amygdules (filled-in volcanic gas bubbles)
Catoctin basalt - metamorphosed to greenstone
Catoctin basalt -
metamorphosed to greenstone

(click on images for larger versions)


Using Cereal Bowls and Car Crashes to Understand Virginia Geology
Rocks and Ridges - The Geology of Virginia
Virginia Places