Question: What name was given to a lake due to the location of the Great Stone Face or the Profile?

full_context: Document 1: Mount Cardigan: Mount Cardigan is a prominent bare-rock summit in the towns of Orange and Alexandria in western New Hampshire. While its peak is only 3155 ft above sea level, it has extensive areas of bare granite ledges and alpine scrub, giving it the feel to hikers of a much higher mountain. Most of the summit area was denuded by devastating forest fires in 1855.
Document 2: Mount Callaghan: Mount Callaghan is a volcanic peak located east of the headwaters of the Squamish River, just northeast of the Powder Mountain Icefield and just south of the Pemberton Icefield in the Sea to Sky Country of southwestern British Columbia, Canada, about 20 km directly west of the Resort Municipality of Whistler. A crack was observed across Callaghan's summit in the spring of 1999. In 2000, a section of the summit collapsed. Callaghan Lake lies below the south face of the mountain.
Document 3: Stone Mountain: Stone Mountain is a quartz monzonite dome monadnock and the site of Stone Mountain Park in Stone Mountain, Georgia. At its summit, the elevation is 1686 ft MSL and 825 ft above the surrounding area. Stone Mountain is well-known not only for its geology, but also for the enormous rock relief on its north face, the largest bas-relief in the world. The carving depicts three Confederate figures during the Civil War: Jefferson Davis, Robert E. Lee and Stonewall Jackson.
Document 4: Avalanche Lake (New York): Avalanche Lake is a 9 acre mountain lake located in the Adirondack High Peaks in New York. Avalanche Lake sits at 2885 feet (879 m) between 4,714-foot (1,437 m) Mount Colden and-3816 foot (1163 m) Avalanche Mountain. The two mountains rise in vertical cliffs from the surface of the lake. Immediately west of Avalanche Mountain (formerly known as Caribou Mountain) lies the MacIntyre Range— 5,115-foot (1,559 m) Algonquin Peak (the second highest mountain in the state), 4829-foot (1472 m) Boundary Peak, 4,843-foot (1,476 m) Iroquois Peak and 4,380-foot (1,335 m) Mount Marshall. Mount Marcy is 2.5 (4 km) miles to the east. Avalanche Lake feeds Lake Colden to the south, in the Hudson River watershed. To the north, the trail to the lake from the Adirondak Loj surmounts Avalanche Pass, which is only slightly above lake level but separates it from the Lake Champlain (St. Lawrence River) watershed. Following the lake toward Lake Colden, the trail is choked with large boulders, and a number of wooden ladders have been built to make passage possible. There are also three places where the trail takes to wooden catwalks, first built in the 1920s, that are bolted directly into the cliff face. This section is known as the "Hitch-Up Matilda;" in 1868 when a mountain guide waded to carry one of his clients past a point with no footing on shore, her husband urged her to sit higher on his shoulders.
Document 5: Crystal Lake (Gilmanton, New Hampshire): Crystal Lake is a 455 acre water body located in Belknap County in the Lakes Region of central New Hampshire, United States, in the town of Gilmanton. Crystal Lake is at the head of the Suncook River watershed. Water flows into Crystal Lake from the Belknap Range through Manning and Sunset lakes to the north. Water from Manning Lake enters Crystal Lake via Nelson Brook. Other waterways flowing into Crystal Lake include Wasson Brook and Mill Brook. Water flows out of a dam from the southern end of Crystal Lake via the Suncook Lakes and Suncook River to the Merrimack River. Shoreline development along Crystal Lake consists primarily of summer cottages, with a few year-round residents. Belknap Mountain and Mount Major can be seen from the shoreline.
Document 6: Crawford Notch: Crawford Notch is a major pass through the White Mountains of New Hampshire, located almost entirely within the town of Hart's Location. Roughly half of that town is contained in Crawford Notch State Park. The high point of the notch, at approximately 1900 ft above sea level, is at the southern end of the town of Carroll, near the Crawford Depot train station and Saco Lake, the source of the Saco River, which flows southward through the steep-sided notch. North of the high point of the notch, Crawford Brook flows more gently northwest to the Ammonoosuc River, a tributary of the Connecticut River.
Document 7: Mount Greylock: Mount Greylock is the highest natural point in Massachusetts at 3489 ft . Its peak is located in the northwest corner of the state in the western part of the town of Adams (near its border with Williamstown) in Berkshire County. Although geologically part of the Taconic Mountains, Mount Greylock is commonly associated with the abutting Berkshire Hills to the east. The mountain is known for its expansive views encompassing five states and the only taiga-boreal forest in the state. A seasonal automobile road (open annually from late May through November 1) climbs to the summit, where stands the iconic 93 ft lighthouse-like Massachusetts Veterans War Memorial Tower. A network of hiking trails traverse the mountain, including the 2179 mi Appalachian Trail. Mount Greylock State Reservation was created in 1898 as Massachusetts' first public land for the purpose of forest preservation.
Document 8: Profile Lake: Profile Lake is a 13 acre water body located in Franconia Notch in the White Mountains of New Hampshire, at the foot of Cannon Mountain. The lake was given its name due to its location directly beneath the Old Man of the Mountain, a famous rock formation which collapsed in 2003. The lake is near the height of land in Franconia Notch; the lake's outlet is the Pemigewasset River, which flows south to the Merrimack River and ultimately the Gulf of Maine (Atlantic Ocean) at Newburyport, Massachusetts.
Document 9: Stone Mountain (North Carolina): Stone Mountain is the centerpiece of Stone Mountain State Park. It is a dome of exposed granite (specifically a quartz diorite to granodiorite) of Devonian age, which has intruded into the gneiss of the Precambrian Alligator Back Formation. It rises sharply over 600 feet (183 m) above the surrounding terrain. The mountain, which has an elevation of 2,305 feet (706 m) above sea level, is known for its barren sides and distinctive brown-gray color, and can be seen for miles. The mountain offers some of the best rock climbing in North Carolina, and the park's creeks and streams feature excellent brook trout fishing.
Document 10: Newfound Lake: Newfound Lake is located in Grafton County, New Hampshire, United States. It is situated in the Lakes Region of central New Hampshire, in the towns of Alexandria, Bridgewater, Bristol, and Hebron. Its area of 4451 acre places it behind only Lake Winnipesaukee and Squam Lake among lakes located entirely within New Hampshire, and fourth in the state overall, when Umbagog Lake on the Maine border is included. Newfound Lake is refreshed twice a year by eight underground springs and has 22 mi of shore line. The lake is about 2.5 mi wide and 6 mi long. The deepest point is 183 ft . Major tributaries include the Fowler River and the Cockermouth River. Its outlet is the Newfound River, flowing through Bristol village into the Pemigewasset River. The lake volume is 98 billion gallons of water.
Document 11: Newichawannock Canal: The Newichawannock Canal is a man-made canal which drains Great East Lake into Horn Pond at the border between Wakefield, New Hampshire, and Acton, Maine, in the northeastern United States. It is at the head of the Salmon Falls River, which the Abenaki called "Newichawannock", meaning "river with many falls". Begun in 1850 by the Great Falls Company to increase the water available for its mills in Somersworth, New Hampshire, the 0.75 mi canal is unusual as it was built for strictly industrial purposes in an area remote from the actual industrial site. The canal forms the boundary between the states of New Hampshire and Maine, and is spanned by a stone bridge built at the same time. The canal and bridge, along with related artifacts, were listed on the National Register of Historic Places in 2014.
Document 12: Old Man of the Mountain: The Old Man of the Mountain, also known as the Great Stone Face or the Profile, was a series of five granite cliff ledges on Cannon Mountain in the White Mountains of New Hampshire, United States, that appeared to be the jagged profile of a face when viewed from the north. The rock formation was 1200 ft above Profile Lake, and measured 40 ft tall and 25 ft wide. The site is located in the town of Franconia.
Document 13: List of people who died on the Presidential Range: The Presidential Range in the White Mountains of New Hampshire consist of a series of mountains whose maximum elevation reaches 6288 ft . This range represents some of the highest mountains in the United States east of the Mississippi River. Fatalities in this area are dominated by those that occur on Mount Washington, the highest summit in the range. It is notorious for its unpredictable weather, making it one of the deadliest mountains in the continental United States. Due to its unique location relative to other geographic features, it holds the world record for highest recorded surface wind speed not within a tropical cyclone. The New Hampshire Fish and Game Department conducts an average of 180 rescues a year for hikers in need of assistance.
Document 14: Old Man of Hoy: The Old Man of Hoy is a 449-foot (137m) sea stack on the island of Hoy, part of the Orkney archipelago off the north coast of Scotland. Formed from Old Red Sandstone, it is one of the tallest stacks in Britain. The Old Man is popular with climbers, and was first climbed in 1966. Created by the erosion of a cliff through hydraulic action some time after 1750, the stack is no more than a few hundred years old, and may soon collapse into the sea.
Document 15: Evans Notch: Evans Notch (elev. 1410 ft ) is a mountain pass located in the White Mountains in Maine, United States, about 1 mi east of the New Hampshire border. It is the easternmost notch through the White Mountains (the next ones to the west being Carter Notch and Pinkham Notch). To the south, the notch is drained by the Cold River, which leads via the Charles River to the Saco River, which in turn flows into the Gulf of Maine east of Saco and Biddeford. The Mad River is a small mountain stream that joins the Cold River from the west about 2 mi south of the height of land, after dropping over Mad River Falls. The notch is drained to the north by Evans Brook, a tributary of the Wild River, which flows north to the Androscoggin River. The Androscoggin leads east and south to the Kennebec River at Merrymeeting Bay north of Bath, Maine.
ground_truth: Profile Lake