Hyland Hills Ski Area, Minnesota
Hyland Hills Ski Area, Chalet Road, Bloomington, Minnesota, USA
The Mississippi Headwaters Webcam looks across the exact spot where the Mississippi River leaves Lake Itasca and starts running south. A line of stepping stones crosses the outlet, and on a summer afternoon there are usually people balancing over them or wading in water that barely reaches the knee. Behind them the lake opens past a wide band of reeds toward a pine shoreline. The river is roughly 5.5 meters (18 feet) wide here and shallow enough to walk across. From this outlet it runs 4,107 kilometers (2,552 miles) to the Gulf of Mexico, a trip a single drop of water takes about 90 days to finish.
The outlet sits at the north end of Lake Itasca, about 450 meters (1,475 feet) above sea level. That is the entire vertical budget for the river: everything below this point is a slow drop to the sea over 4,107 kilometers (2,552 miles). Lake Itasca itself is a glacial lake of roughly 4.7 square kilometers (1,200 acres), fed by smaller lakes and streams to the south, and the reed bed across the frame marks where its shallow north arm ends. Henry Schoolcraft reached the lake in 1832 and identified it as the river’s true source, settling a question that several earlier expeditions had answered wrongly.
Minnesota protected the surrounding land as a state park in 1891, the first in the state and the second in the country after Niagara Falls State Park. It now covers about 132 square kilometers (32,690 acres) and holds 157 lakes. Much of it is old growth red and white pine, with individual trees more than 200 years old, which is why the shoreline behind the outlet reads as mature forest rather than second growth. The park’s high ground reaches 475 meters (1,558 feet).
The Mary Gibbs Mississippi Headwaters Center stands a short walk from the water and holds the exhibits, gift shop and cafe, which is why foot traffic feeds onto this beach steadily through the day. Mary Gibbs was the nation’s first female park commissioner, and the building carries her name. On camera, the stone marker post to the left of the stepping stones is where most people stop for a photograph before crossing.
Winter is the defining season this far north. The park’s average winter minimum runs near -20 C (-4 F), and roughly 139 centimeters (54.6 inches) of snow falls in a normal year. Lake Itasca freezes, the outlet ices over, and the beach that carries the summer crowd typically becomes an unbroken white surface with ski and snowshoe tracks across it. Daylight is short, so the usable window on the camera narrows toward the middle of the day.
Summer runs the other way. July highs average about 25.8 C (78.4 F), warm enough that wading the outlet is the main reason most people come, and the camera picks up a steady stream of them from late morning onward. Annual rainfall is around 686 millimeters (27 inches), most of it in the warm months, so a clear afternoon can turn to a thunderstorm and back inside an hour. Spring arrives late here, with ice out and the first green in the reeds coming well after the calendar says it should. Autumn cools quickly, the birch and maple mixed into the pine turn, and the beach empties weeks before the snow sets in.
Wilderness Drive loops through the park’s old growth stands and is the usual way to see the big pines without a long walk. Aiton Heights Fire Tower is the other main stop, where a 30 meter (100 foot) climb opens up a view over the lake country that no ground level trail gives. Preacher’s Grove is a stand of red pine near the East Arm of the lake, and the Itasca Indian Cemetery and burial mounds sit on the same shore.
The park keeps 53 kilometers (33 miles) of hiking trails, including a 15 kilometer (9.6 mile) section of the North Country National Scenic Trail, and 48 kilometers (30 miles) of cross country ski trails once the snow sets in. Douglas Lodge, built in 1905, still takes overnight guests and serves meals at the south end of the park. Wildlife is a real part of the draw: more than 200 bird species have been recorded here, along with over 60 mammals including beaver, porcupine, black bear and wolves. Park Rapids, 34 kilometers (21 miles) south, is the nearest town of any size and the usual base for anyone staying outside the park.
More cameras on the same river and in the same corner of Minnesota:
At the north end of Lake Itasca, inside Itasca State Park in Clearwater County, northern Minnesota. Park Rapids is the nearest town, about 34 kilometers (21 miles) south, and the site sits roughly 450 meters (1,475 feet) above sea level.
The outlet where the river leaves the lake: the line of stepping stones, the beach people gather on, the reed bed along the lake’s north arm and the pine shoreline behind it. In summer there are usually people wading or crossing the stones.
Yes. The river is roughly 5.5 meters (18 feet) wide and knee deep or less at the outlet, with stepping stones set across it. Crossing on foot is the main thing people come here to do, and it happens in front of the camera all day in summer.
About 5.5 meters (18 feet) where it leaves Lake Itasca. It stays that size only briefly before the channel narrows into the forest and turns north, then east, then south.
Around 90 days for a single drop of water, over the 4,107 kilometers (2,552 miles) between Lake Itasca and the Gulf.
Cold in winter and mild in summer. The park’s average winter minimum is near -20 C (-4 F) with about 139 centimeters (54.6 inches) of snow a year, while July highs average about 25.8 C (78.4 F). Annual rainfall is around 686 millimeters (27 inches).
Henry Schoolcraft, in 1832. Earlier expeditions had pointed at other lakes, and his conclusion is the one that held up.
Late morning through afternoon in summer gives the most activity, since that is when people are crossing the stones. Winter typically shows an iced over outlet and a snow covered beach, with a short daylight window around midday.