the ice sheet stopped in Pennsylvania 18,000 years ago at the peak of the Wisconsin glaciation
Source: ESRI, ArcGIS Online
The Laurentide Ice Sheet stopped north of the Ohio River and the Pennsylvania Turnpike. During the furthest extent of the ice in the Wisconsin stage that ended 18,000 years ago, Virginia was exposed to cold weather but not buried underneath a thick layer of ice.
Perhaps there was a small mountaintop glacier on Mount Rodgers, the highest peak in Virginia at 5,729 feet, but no evidence of glaciation remains. Peaks in Virginia may have been covered with snow during the winter, but wind and sun removed the snow before it was compressed to form glaciers. Mount Mitchell in North Carolina is 6,684 feet in elevation, and in the 1970's there was a claim of glacial scratches on the bedrock of that peak. However, later investigation revealed that cables used in logging operations had carved the grooves.1
John B. McKeon, John T. Hack, Wayne L. Newell, James O. Berkland and Loren A. Raymond, "North Carolina Glacier: Evidence Disputed," Science, New Series, Volume 184, Number 4132 (April 5, 1974), p.89, http://www.jstor.org/stable/1737466 (last checked April 19, 2017)
Virginia still experienced significant impacts from the cold climate in the Ice Age. The Laurentide Ice Sheet altered the location of the Atlantic Ocean shoreline, and the winds, rains, and temperature of the paleoclimate was shaped by the presence of the Laurentide Ice Sheet.
The weight on the ice sheet pressed down on the bedrock, depressing the land into southern Pennsylvania. The land further south flexed in response to the pressure and bent upwards. As a result, at the peak of the Ice Age the land along Virginia's coastline was raised up. Sea level was already as much as 400 meters lower because so much water was trapped in the glaciers, and the eastern coastline of Virginia was as much as 40 miles east of the current location. The flexing earth raised the Virginia coastline even higher and extended the Coastal Plain even further to the east.
Today, the ice sheet has retreated far north and the depressed bedrock in Pennsylvania is rebounding upwards. The area along the current Atlantic Ocean shoreline, the crust that was uplifted in response to the nearby ice, now is sinking back down. That adjustment, combined with global warming, is causing faster-than-average sea level rise along Virginia's Atlantic Ocean shoreline and in the Chesapeake Bay.2
"Glacial Rebound: The Not So Solid Earth," National Aeronautics and Space Administration, August. 26, 2015, https://www.nasa.gov/feature/goddard/glacial-rebound-the-not-so-solid-earth; "Sinking Atlantic Coastline Meets Rapidly Rising Seas," Scientific American, April 14, 2016, https://www.scientificamerican.com/article/sinking-atlantic-coastline-meets-rapidly-rising-seas/ (last checked April 19, 2017)
In the Valley and Ridge province, blocks of stone cracked loose from the bedrock on the sandstone ridges, slid downhill, and created piles of boulders in a talus slope below the quartzite bedrock. When the climate warmed, the hillsides stabilized and the forests returned. Trees grew below the talus pile and above their eroding bedrock source, but not on the barren boulders themselves.
The freezing and thawing cycle was less intense, however, and few new rocks were added to the talus in the last 10,000 or so years. The pile of talus rock slid downhill under the force of gravity, but new talus was no longer added regularly on the uphill edge of the talus pile. Over centuries, a gap developed between the source bedrock and the talus pile, and trees grew in that gap. The isolated block fields - below the trees and now separated from the layer of sandstone that eroded to form the original talus pile - stand out against the forested mountainsides today, remnants of an ancient climate.3
"Glimpses of the Ice Age from I-81," US Geological Survey, 1998, http://pubs.usgs.gov/gip/i81/i81.pdf (last checked February 19, 2015)
"Block fields" are still visible on the western slope of Massanutten Mountain. During the last glacial period, cold winds blew across the mountains and little vegetation could grow there. Cracks in the sandstone bedrock widened as the moisture in them froze. The ice froze and melted repeatedly, creating The Channels on Clinch Mountain at the border of Russell and Tazewell counties.
The Channels was created when joints and fractures in the sandstone at the top of Clinch Mountain were widened by the freezing and thawing of ice during the Plestocene
Glaciers did not carve the landscape in southwestern Virginia, but the Ice Age climate (as well as earthquakes) may have been a factor in creating the largest known landslides in eastern North America. For 20 miles, land has slumped along the eastern slope of Sinking Creek Mountain west of modern-day Blacksburg.
When the climate was colder, vegetation was less and erosion was evidently higher. Soil washed away at the base of rock layers on the mountain, and earthquakes may have triggered a series of massive landslides until 10,000 year ago.3 There are marks of glaciers on the highest mountain in North Carolina, but none remain in Virginia.
glacial advance... to Pittsburgh, but not into modern-day Virginia
Source: US Geological Survey, National Atlas