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Trail in the Huron National Forest, Michigan. The Huron National Forest is prone to frequent seasonal forest fires, due to ecological and geological factors including the domination of the jack pine in sections the forests, the needles of which are extremely flammable, [2] sandy soil composition as a result of glacial outwash plain geology of sections of the Huron National Forest, [3] and jack ...
The Manistee National Forest is a national forest located in the Lower Peninsula of Michigan. It has a total area of 540,187 acres (2,190 km 2 ). It was established in 1938, and combined with the Huron National Forest in 1945 for administrative purposes, creating the Huron-Manistee National Forests .
The Huron–Manistee National Forests are two separate national forests, the Huron National Forest and the Manistee National Forest, combined in 1945 for administration purposes and which comprise 978,906 acres (3,960 km 2) [2] of public lands, including 5,786 acres (23 km 2) of wetlands, extending across the northern lower peninsula of ...
Kirtland's warbler (Setophaga kirtlandii), also known in Michigan by the common name jack pine bird, [3] [4] or the jack pine warbler, is a small songbird of the New World warbler family . Nearly extinct just years ago, populations have recovered due to the conservation efforts of Phil Huber and the U.S. Forest Service .
The Nordhouse Dunes Wilderness is a 3,450-acre (14.0 km 2) listed wilderness area within the Manistee National Forest. It is located north of Ludington, Michigan , and is best known for its 4 miles (6.4 km) of undeveloped Lake Michigan shoreline.
A large portion of the area is the Grayling outwash plain, a broad outwash plain including sandy ice-disintegration ridges; jack pine barrens, some white pine-red pine forest, and northern hardwood forest. Large lakes were created by glacial action. [10] Headwaters of the Au Sable, Black, Manistee, Pigeon, and Sturgeon Rivers are in Otsego County.
Glaciers shaped the area, creating a unique regional ecosystem. A large portion of the area is the so-called Grayling outwash plain, which consists of broad outwash plain including sandy ice-disintegration ridges; jack pine barrens, some white pine-red pine forest, and northern hardwood forest. Large lakes were created by glacial action. [7]
Glaciers shaped the area, creating a unique regional ecosystem. A large portion of the area is the Grayling outwash plain, a broad outwash plain including sandy ice-disintegration ridges, jack pine barrens, some white pine-red pine forest, and northern hardwood forest. Large lakes were created by glacial action. [11]