As the primary ecosystem in Bering Land Bridge National Preserve, tundra covers hundreds of thousands of acres within its boundaries. The word "tundra" refers to a treeless landscape found in cold climates. At high altitudes, it is known as "alpine tundra," and at low altitudes but higher latitudes (closer to the Arctic Circle), it is known as "arctic tundra."
Although vast and sometimes desolate, the tundra is anything but an infertile environment. During its short summer season, the tundra will be covered in a lush ground cover of grasses, Alaskan cotton, wildflowers, lichens, and mosses. It provides a home for small mammals like voles, shrews, and ground squirrels, as well as their larger predators such as raptors, foxes, wolves, wolverines, and bears. The vegetation feeds the tundra's roving herbivores, such as muskox, caribou, and reindeer, and serves as a habitat for small songbirds and their insect prey.
NPS Photo - Andrea Willingham
The word "pingo" comes from an Inupiaq name for a cone-shaped hill or mound of soil with a core of ice. It can be anywhere from a few feet high to over 200 feet high and 2,000 feet in diameter.
There are two types of pingos: closed system and open system.
Closed-system pingos are the most common type, and form in relatively level areas where unfrozen groundwater is trapped by permafrost. The water is forced inward where it then freezes and expands, heaving the overlying ground upward and creating the
Open-system pingos are usually smaller and forms when groundwater flows downhill and gets trapped beneath the permafrost. The liquid water pushes itself up through cracks in the permafrost, where it then freezes and expands, pushing the overlying soil into little cone-shaped mounds.
Pingos can grow by as much as 5 feet per year and then continue growing slowly (about 1 foot per year) for millennia.
These formations are created in areas with permafrost and seasonal frost as a result of contraction cracks from wedges of ice. The pressure created by an ice wedge forces the soil upward around the crack to form 2 small ridges. This creates a concave, low-center polygon.
Another type that can form is a high-center polygon, created in poorly-drained areas where water fills the center of the polygon and the ice wedge troughs. The collected water conducts heat from the sun, melting the underlying permafrost, deepening the ice wedge troughs. Eventually these can grow large enough to form a lake.