Natural history
[edit]
Tobin Harbor Trail in the Laurentian Mixed Forest ProvinceA number of habitats exist on the island, the primary being boreal forest, similar to neighboring Ontario and Minnesota. Upland areas along some of the ridges are effectively "balds" with exposed bedrock and a few scrubby trees, blueberry bushes, and hardy grasses. Occasional marshes exist, which are typically the by-product of beaver activities. There are also several lakes, often with wooded or marshy shores. The climate, especially in lowland areas, is heavily influenced by the cold waters of Lake Superior.
Flora[edit]
According to the A. W. Kuchler U.S. Potential natural vegetation Types, Isle Royale National Park has a Great Lakes Spruce/Fir (93) potential vegetation type and a Northern Conifer Forest (22) potential vegetation form.
The predominant floral habitats of Isle Royale are within the Laurentian Mixed Forest Province. The area is a temperate broadleaf and mixed forests biome transition zone between the true boreal forest to the north and Big Woods to the south, with characteristics of each. It has areas of both broadleaf and conifer forest cover, and bodies of water ranging from conifer bogs to swamps.
Conifers include jack pines (Pinus banksiana), black and white spruces (Picea mariana and Picea glauca), balsam firs (Abies balsamea), and eastern redcedars (Juniperus virginiana).
Deciduous trees include quaking aspens (Populus tremuloides), red oaks (Quercus rubra), paper birches (Betula papyrifera), American mountain ash (Sorbus americana), red maples (Acer rubrum), sugar maples (Acer saccharum), and mountain maples (Acer spicatum). There are over 600 species of flowering plants found in Isle Royale National Park such as wild sarsaparilla, marsh-marigold, wood lily and prickly wild rose.
Fauna[edit]
See also: Wolves and moose on Isle Royale and List of fish of Isle Royale National Park
Moose swimming at Isle Royale.
Isle Royale National Park is known for its timber wolf and moose populations, which are studied by scientists investigating predator-prey relationships in a closed environment. There is a cyclical relationship between the two animals: as the moose increase in population, so do the wolves. Eventually, the wolves kill too many moose and begin to starve and lower their reproductive rates. This is made easier because Isle Royale has been colonized by roughly just one third of the mainland mammal species, because it is so remote. In addition, the environment is unique in that it is the only known place where wolves and moose coexist without the presence of bears.
Other common mammals are red foxes, beavers, and red squirrels. Some foxes are accustomed to human contact and can be seen prowling the campgrounds at dawn, looking for stray scraps left by unwary campers. For its part, the wolf is an elusive species which avoids human interaction. Few documented cases of direct wolf/human contact existed for most of the island's history. In the 2024 season dozens of wolf sightings were reported around the Rock Harbor area. Ermine have been periodically sighted around docks. Other mammals that can be seen include mink along the various lake shores and muskrats (occasionally) at beaver ponds. Several species of bat also exist on the island. Reptiles include the eastern garter snake, painted turtle, and northern redbelly snake. Six species of frogs and three species of salamander also live on the island.
Historically neither moose nor wolves inhabited Isle Royale. Just prior to becoming a national park the large mammals on Isle Royale were Canada lynx and the boreal woodland caribou. Archeological evidence indicates both of these species were present on Isle Royale for 3,500 years prior to being removed by direct human actions (hunting, trapping, mining, logging, fires, competition for resources from exotic species and possibly disease due to the introduction of invasive species). The last caribou documented on Isle Royale was in 1925. Though lynx were removed by the 1930s, some have periodically crossed the ice bridge from neighboring Ontario, Canada, the most recent being an individual sighting in 1980. Although lynx are no longer present on
the island, their primary prey, snowshoe hares, remain. Before the appearance of wolves, coyotes were also predators on the island. Coyotes appeared around 1905 and disappeared shortly after wolves arrived in the 1950s. Four wolves were brought from Minnesota in 2018 after some debate as to whether or not the introduction was an unnatural intervention.
Rocky shoreline
Moose are believed to have colonized Isle Royale sometime between 1905 and 1912. It was initially believed that a small herd of moose (moose typically do not travel in herds) colonized the islands by crossing the ice from the adjacent mainland; later this theory was modified to a herd of moose swimming 20 miles across Lake Superior from the nearest mainland. The improbability of these theories received little scrutiny until recent years. Although no thorough scientific investigation to determine how moose arrived on Isle Royale has been carried out to date, both cultural and genetic evidence indicates they were likely introduced by humans to create a private hunting preserve in the early 1900s. The cultural evidence that moose were trapped in northwestern Minnesota and transported to Isle Royale seemed unlikely until decades later when genetic evidence revealed the moose on Isle Royale were more closely related to moose in the far northwestern Minnesota/Manitoba border area than the mainland adjacent to Isle Royale in far northeastern Minnesota bordering Ontario. Further evidence has also shown that the Washington Harbor Club, a group of well-to-do businessmen, owned various buildings on Isle Royale in addition to railroads that ran from Baudette to Duluth and Two Harbors and so had the means to transport moose from northwestern Minnesota to Two Harbors.
There are usually around 25 wolves and 1000 moose on the island, but the numbers change greatly year to year. In the 2006–2007 winter, a survey found 385 moose and 21 wolves in 3 packs. In spring 2008, 23 wolves and approximately 650 moose were counted. However, recent reductions in winter pack ice had ended replenishment of the wolf population from the mainland. Due to genetic inbreeding, the wolf population had declined to two individuals in 2016, causing researchers to expect that the island's wolf population would eventually become extinct. At the same time, the island's moose population had exploded to an estimated 1600. By November 2017, the wolf population was down to one, a female.
In December 2016, the National Park Service put forward an initial plan to bring additional wolves to the island in order to prevent the pack from disappearing completely. The decision to relocate 20–30 wolves to the island was approved and from September 2018 to September 2019, 19 wolves were relocated to Isle Royale from various locations in Minnesota, Michigan, and Ontario. As of April 14, 2020, there were an estimated 14 wolves remaining on the island.
Geology[edit]
Isle Royale geological map
Cross-section of the Lake Superior basin showing the tilted strata of volcanic rock that form Isle Royale
The island is composed largely of ridges, running roughly southwest-to-northeast. The main ridge, Greenstone Ridge, is over 1,000 ft (300 m) in many places. Greenstone belts are exposed, with rounded stones of chlorastrolite, also known as greenstone, near and in the lake.
The two main rock assemblages found on the island include the Portage Lake Volcanics and the Copper Harbor Conglomerate, both Precambrian in age. The volcanics are mainly ophitic flood basalts, some 100 individual flows over an accumulated thickness of at least 10,000 feet. The conglomerate outcrops on the southwestern portion of the island and consists of sedimentary rock derived from volcanic rocks in present-day Minnesota. Glacial erosion accentuated the ridge and valley topography from pre-glacial stream erosion. Glacial striations indicate a generally westward movement of the glaciers as do the recessional moraines west of Lake Desor. Drumlins are found west of Siskiwit Lake.: 8, 14–15, 21, 25, 42, 45 
Recent analyses by the USGS of both unmineralized basalt and copper-mineralized rock show that a small amount of naturally occurring mercury is associated with mineralization.
Native copper and chlorastrolite, the official state gem of Michigan, are secondary minerals filling pore spaces formed by vesicles and fractures within the volcanic rocks. Prehnite and agate amygdules are also plentiful island gemstones.: 55, 58–61