Acadia National Park

Acadia National Park is an American national park located along the mid-section of the Maine coast, southwest of Bar Harbor. The park preserves about half of Mount Desert Island, part of the Isle au Haut, the tip of the Schoodic Peninsula, and portions of 16 smaller outlying islands. It protects the natural beauty of the rocky headlands, including the highest mountains along the Atlantic coast. Acadia boasts a glaciated coastal and island landscape, an abundance of habitats, a high level of biodiversity, clean air and water, and a rich cultural heritage.

The park contains the tallest mountain on the Atlantic Coast of the United States ( Cadillac Mountain), exposed granite domes, glacial erratics, U-shaped valleys, and cobble beaches. Its mountains, lakes, streams, wetlands, forests, meadows, and coastlines contribute to a diversity of plants and animals. Weaved into this landscape is a historic carriage road system financed by John D. Rockefeller Jr. In total, it encompasses .

Acadia has a rich human history, dating back more than 10,000 years ago with the Wabanaki people. The 17th century brought fur traders and other European explorers, while the 19th century saw an influx of summer visitors, then wealthy families. Many conservation-minded citizens, among them George B. Dorr (the "Father of Acadia National Park"), worked to establish this first U.S. national park east of the Mississippi River and the only one in the Northeastern United States. Acadia was initially designated Sieur de Monts National Monument by proclamation of President Woodrow Wilson in 1916, then renamed and redesignated Lafayette National Park in 1919. The park was renamed Acadia National Park in 1929.

Recreational activities from spring through autumn include car and bus touring along the park's paved loop road; hiking, bicycling, and horseback riding on carriage roads (motor vehicles are prohibited); fishing; rock climbing; kayaking and canoeing on lakes and ponds; swimming at Sand Beach and Echo Lake; sea kayaking and guided boat tours on the ocean; and various ranger-led programs. Winter activities include cross-country skiing, snowshoeing, snowmobiling, and ice fishing. Two campgrounds are located on Mount Desert Island, another campground is on the Schoodic Peninsula, and five lean-to sites are on Isle au Haut. The main visitor center is at Hulls Cove, northwest of Bar Harbor. Park visitation has been steadily increasing in Acadia over the past decade, with 2021 seeing a record count of 4.07 million visitors.

Geography

The park includes mountains, an ocean coastline, woodlands, lakes, and ponds. In addition to nearly half of Mount Desert Island, the park designation also preserves a portion of the Schoodic Peninsula on the mainland, as well as the majority of Isle au Haut and Baker Island, all of Bar Island, three of the four Porcupine Islands (Sheep, Bald and Long), the Thrumcap (an islet), part of Bear Island, and Thompson Island in Mount Desert Narrows, as well as several other islands and islets."Acadia National Park Maps"
. ''nps.gov''. National Park Service. March 2, 2018. Retrieved November 29, 2018. Bar Island, which can be visited on foot over a sandbar around low tide, and the Porcupine Islands are in Frenchman Bay by Bar Harbor. About of carriage roads were designed and financed by John D. Rockefeller Jr. on Mount Desert Island, of which continue to be maintained inside the park.

Acadia National Park encompasses a total of . At least on Mount Desert Island are included in the park, along with on Isle au Haut, about on smaller islands, and on the Schoodic Peninsula. , the permanent park boundary, as established by act of Congress in 1986, included of privately owned land under conservation easements managed by the National Park Service, which plans to acquire the land at some point.

Features

The mountains of Acadia National Park offer hikers expansive views of the ocean, island lakes, and pine forests. Twenty six significant mountains rise in the park, ranging from at Flying Mountain's summit to at Cadillac Mountain's summit. Cadillac Mountain, named after the French explorer Antoine de la Mothe Cadillac, is on the eastern side of the island. Cadillac is the tallest mountain along the eastern coastline of the United States."Places To Go: Scenic Areas"
. ''nps.gov''. National Park Service. February 8, 2018. Retrieved November 29, 2018. The summit of Cadillac is the first place in the United States where one may watch the sunrise from October 7 through March 6, due to its eastern location and height.

The Park Loop Road leads to many scenic viewpoints along the coast, through forests and to the top of Cadillac Mountain. The road traverses the eastern side of Mount Desert Island in a one-way, clockwise direction from Bar Harbor to Seal Harbor, passing features such as the Tarn (a pond), Champlain Mountain (location of a popular, exposed cliffside trail named Precipice), the Beehive (another, smaller mountain), Sand Beach (a saltwater swimming area), Gorham Mountain, Thunder Hole (a crevasse into which waves crash loudly), Otter Cliff, Otter Cove, Seal Harbor, Jordan Pond, Pemetic Mountain, the Bubbles, Bubble Rock, Bubble Pond, Eagle Lake, and the side road to the summit of Cadillac Mountain. Some of the island's west side features include Echo Lake and beach (a designated freshwater swimming area), Acadia Mountain, Beech Mountain, Long Pond, and Seal Cove Pond. Bass Harbor Head Light is situated atop a cliff on the southernmost tip of the west side of the island. Baker Island Light and Bear Island Light are the other two lighthouses managed by Acadia.

Somes Sound is a long fjard formed during a glacial period that nearly divides the island in half. The sound is deep at its deepest point, and is bordered by Norumbega Mountain to the east, and Acadia Mountain and Saint Sauveur Mountain to the west. The towns of Southwest Harbor and Northeast Harbor face one another across the inlet to Somes Sound.

History

Native people

Native Americans have inhabited the area called Acadia for at least 12,000 years, including the coastal areas of Maine, Canada, and adjacent islands. The Wabanaki Confederacy ("People of the Dawnland") consists of five related Algonquian nations—the Maliseet, Mi'kmaq, Passamaquoddy, Abenaki and Penobscot. Some of the nations call Mount Desert Island ''Pemetic'' ("range of mountains"), which has remained at the center of the Wabanaki traditional ancestral homeland and territory of traditional stewardship responsibility to the present day. The etymology of the park's name begins with the Mi'kmaq term ''akadie'' ("piece of land") which was rendered as ''l'Acadie'' by French explorers, and translated into English as Acadia.

The Wabanaki traveled to the island in birch bark canoes to hunt, fish, gather berries, harvest clams and basket-making resources like sweetgrass, and to trade with other Wabanakis. They camped near places like Somes Sound.

In the early 17th century, Asticou was the chieftain of the greater Mount Desert Island area, one district of an intertribal confederacy known as Mawooshen led by the grandchief Bashaba. Castine (''Pentagoet'' in the native language) was the grandchief's favored rendezvous site for the Wabanaki tribes. The site is located just west of Mount Desert Island at the mouth of the Bagaduce River in eastern Penobscot Bay. From 1615, Castine developed into a major fur trading post where French, English, and Dutch traders all fought for control. Sealskins, moose hides, and furs were traded by the Wabanakis for European commodities. By the early 1620s, warfare and introduced diseases, including smallpox, cholera and influenza, had decimated the tribes from Mount Desert Island southward to Cape Cod, leaving about 10 percent of the original population.Prins, Harald E. L.; McBride, Bunny (December 2007)
"Asticou's Island Domain: Wabanaki Peoples at Mount Desert Island 1500–2000, Acadia National Park, Ethnographic Overview and Assessment, Volume 1"archive
. pp. 5-6, 19, 29. Northeast Region Ethnography Program of the National Park Service. Boston, Massachusetts. Retrieved November 20, 2018.

The border established between the United States and Canada after the American Revolution split the Wabanaki homelands. The confederacy was dissolved around 1870 due to pressure from the American and Canadian governments, though the tribal nations continued to interact in their traditional ways. In the nineteenth century, Wabanakis sold handmade ash and birch bark baskets to travelers. The Wabanaki performed dances for summer tourists and residents at Sieur de Monts and the town of Bar Harbor. Wabanaki guides led canoe trips around Frenchman Bay and the Cranberry Islands.

For two years, 1970–71, the nations operated a Wabanaki educational center called T.R.I.B.E. (Teaching and Research in Bicultural Education) on the west side of Eagle Lake. American Indian land claims in Maine were legally settled in 1980 and 1991. The annual Bar Harbor Native American Festival began in 1989, jointly sponsored by the tribes and the Abbe Museum. The Maine Indian Basketmakers Alliance was formed in 1993, assisting in the coordination of the annual festival with the museum.

Currently, each tribe has a reservation and government headquarters located within their territories throughout Maine. Some Wabanakis live on Mount Desert Island, while others visit for board meetings at the Abbe Museum, to advise on and perform in exhibitions, for craft demonstrations, and to gather sweetgrass and sell handmade baskets at the annual festival.

Exploration

The Italian explorer Giovanni da Verrazzano sailed along the coast of Mount Desert Island during an expedition for the French Crown in 1524. He was followed by Estêvão Gomes, a Portuguese explorer for the Spanish Crown in 1525. French explorer Jean Alfonse arrived in 1542. Alfonse entered Penobscot Bay and recorded details about the fur trade. Portuguese navigator Simon Ferdinando guided an English expedition in 1580.

A few hundred people were living on Mount Desert Island when Samuel de Champlain arrived in 1604. Two Wabanakis led Champlain to Mount Desert Island, which he named Isle des Monts Deserts (Island of Barren Mountains) due to its barren peaks; he named Isle au Haut (High Island) due to its height.

While he was sailing down the coast on 5 September 1604, Champlain wrote:

Settlement

The first French missionary colony in America was established on Mount Desert Island in 1613. The colony was destroyed a short time later by an armed vessel from the Colony of Virginia as the first act of overt warfare in the long struggle leading to the French and Indian Wars. The island was granted to Antoine de la Mothe Cadillac by Louis XIV of France in 1688, but ceded to England in 1713. Massachusetts governor Sir Francis Bernard, 1st Baronet assumed control of the island in 1760. In 1790, Massachusetts granted the eastern half of the island to Cadillac's granddaughter, Mme. de Gregoire, while Bernard's son John retained ownership of the western half. The first record of summer visitors vacationing on the island was in 1855, and steamboat service from Boston was inaugurated in 1868. The Green Mountain Cog Railway was built from the shore of Eagle Lake to the summit of Cadillac Mountain in 1888. In 1901, the Maine Legislature granted Hancock County a charter to acquire and hold land on the island in the public interest. The first land was donated by Mrs. Eliza Homans of Boston in 1908, and had been acquired by 1914.

Rusticators

Artists and journalists had revealed and popularized the island in the mid-1800s. Painters came from the Hudson River School, including Thomas Cole and Frederic Church, inspiring patrons and friends to visit. The term ''rusticator'' was used to describe these early visitors who stayed in the homes of local fishermen and farmers for modest fees. The accommodations soon became insufficient for the increasing amount of summer visitors, and by 1880, thirty hotels were operating on the island. Tourism was becoming the major industry.

Cottagers

For a select few Americans, the 1880s and the Gay Nineties meant affluence on a scale without precedent. Mount Desert Island, being remote from the cities of the east, became a summer retreat for families such as the Rockefellers, Morgans, Fords, Vanderbilts, Carnegies, and Astors. These families, with the help of developers such as Charles T. How, constructed elegant estates, which they called cottages. Luxury, refinement, and large gatherings replaced the buckboard rides, picnics, and day-long hikes of the rusticators. For more than forty years, the wealthy dominated summer activity on Mount Desert Island, but the Great Depression and World War II brought an end to the extravagance.

Park origins

The landscape architect Charles Eliot is credited with the idea for the park. George B. Dorr, called the "Father of Acadia National Park," along with Eliot's father Charles W. Eliot (president of Harvard from 1869 to 1909), supported the idea both through donations of land and through advocacy at the state and federal levels. Dorr later served as the park's first superintendent. President Woodrow Wilson first established its federal status as Sieur de Monts National Monument on July 8, 1916, administered by the National Park Service. It was the first national park created from private lands gifted to the public.

Congress redesignated the national monument as Lafayette National Park on February 26, 1919, the first American national park east of the Mississippi River and the only one in the Northeastern United States. The park was named after the Marquis de Lafayette, an influential French participant in the American Revolution. Jordan Pond Road was started in 1922 and completed as a scenic motor highway in 1927. The Cadillac Mountain Summit Road, begun in 1925, was completed in 1931.

The name of the park was changed to Acadia National Park on January 19, 1929, in honor of the former French colony of Acadia which once included Maine. In 1929 Schoodic Peninsula was donated to Acadia by John Godfrey Moore's second wife Louise and daughters Ruth and Faith. Keeping up with the taxes on the Schoodic land became a drain on the family finances and they thought this world be a fitting way to honor John Godfrey Moore. There was an unspoken stipulation in the discussions — the heirs were anglophiles that did not want to have their land as part of Lafayette National Park. Conservationist George Dorr, who is referred to as the “Father of Acadia National Park,” suggested the name Acadia and the deal went through after the name changed, ensuring the expansion.

From 1915 to 1940, the wealthy philanthropist John D. Rockefeller Jr. financed, designed, and directed the construction of a network of carriage roads throughout the park."Acadia's Historic Carriage Roads"
. ''nps.gov''. National Park Service. December 14, 2015. Retrieved November 23, 2018. He sponsored the landscape architect Beatrix Farrand, whose family owned a summer home in Bar Harbor named Reef Point Estate, to design the planting plans for the carriage roads (c. 1930). The network originally encompassed about of crushed stone carriage roads with 17 stone-faced, steel-reinforced concrete bridges (16 financed by Rockefeller), and two gate lodges—one at Jordan Pond and the other near Northeast Harbor."The Carriage Roads of Acadia National Park"archive
. ''nps.gov''. May 2007. National Park Service. Retrieved December 9, 2018. About of carriage roads are maintained and accessible within park boundaries. Granite coping stones along carriage road edges act as guard rails; they are nicknamed "Rockefeller's Teeth." The carriage roads are open from the end of the spring mud season, generally in late April, through the summer, autumn, and winter months, until the following spring thaw causes another closure in March to prevent damage to the gravel surface.

Acadia National Park's first naturalist, Arthur Stupka, also had the distinction of being the first NPS naturalist to serve in any of the NPS's eastern United States districts. He joined the park staff in 1932, and in the capacity of park naturalist he wrote, edited and published a four-volume serial entitled ''Nature Notes from Acadia'' (1932–1935).

Administrative history

Superintendents

Fire of 1947

Beginning on October 17, 1947, more than of Acadia National Park burned in a fire that also destroyed an additional of Mount Desert Island outside the park. The fire began along Crooked Road west of Hulls Cove (northwest of Bar Harbor). The forest fire was one of a series of fires that consumed much of Maine's forest in a dry year. The fire burned until November 14, and was fought by the Coast Guard, Army Air Corps, Navy, local residents, and National Park Service employees from around the country. Sixty-seven of the historic summer cottages along Millionaires’ Row, along with 170 other homes, and five hotels were destroyed. Restoration of the park was substantially supported by the Rockefeller family. Regrowth has occurred naturally with new deciduous forests consisting of birch and aspen enhancing the colors of autumn foliage, adding diversity to tree populations, and providing for the eventual regeneration of spruce and fir forests.

Climate

The region is characterized by a large seasonal variation in temperature with warm to hot summers that are often humid, and cold to severely cold winters. According to the Köppen climate classification system, Mount Desert Island has a warm-summer humid continental climate (''Dfb''). The average annual temperature in the park is 47.3 °F (8.5 °C). July is the warmest month with an average of 69.7 °F (20.9 °C), while January is the coldest month with an average of 23.8 °F (-4.6 °C). The record high and low temperatures are 96 °F (36 °C) and -21 °F (-29 °C), respectively. The plant hardiness zone is 5b with an average annual extreme minimum air temperature of -11.4 °F (-24.1 °C).

Average annual precipitation in Bar Harbor is 55.54" (1411 mm). November is the wettest month with 5.89" (150 mm) of precipitation on average, while July is the driest month with 3.27" (83 mm). Precipitation days are spread evenly throughout the year with December averaging the most days with about 14, while August averages the least with about 9. The annual average days with precipitation is 139. Snow has been recorded from October to May, although the majority falls from December to March. The snowiest month is January with 18.3" (46 cm), and the annual average is 66.1" (167 cm).

Geology

The Cadillac Mountain Intrusive Complex is part of the Coastal Maine Magmatic Province, consisting of over a hundred mafic and felsic plutons associated with the Acadian Orogeny. Mount Desert Island bedrock consists mainly of Cadillac Mountain granite. Perthite gives the granite its pinkish color. The Silurian age granite ranges from 424 to 419 million years ago (Mya). Diabase dikes trend north–south through the complex. Almost 300 million years of erosion followed before the deposition of glacial features during the Pleistocene. Glacial polish, glacial striations, and chatter marks are evident in granitic surfaces. Other glacier-shaped features include The Bubbles (two rôche moutonnées) and the U-shaped valleys of Sargent Mountain Pond, Jordan Pond, Seal Cove Pond, Long Pond, Echo Lake, and Eagle Lake. Somes Sound is a fjard and terminal moraines form the southern end of Long Pond, Echo Lake, and Jordan Pond. Bubble Rock is an example of a glacial erratic.

Bedrock formation

More than 500 Mya, layers of mud, sand and volcanic ash were buried beneath the ocean where high pressure, heat and tectonic activity created a metamorphic rock formation called the Ellsworth Schist. White and gray quartz, feldspar, and green chlorite comprise the schist, which is the oldest rock in the Mount Desert Island region. Erosion and shifting of tectonic plates eventually brought the schist to the surface.

About 450 Mya, an ancient continental fragment, or micro-terrane, called Avalonia collided with North America. The collision buried the schist along with accumulations of sand and silt, creating the Bar Harbor Formation which consists of brown and gray sandstone and siltstone layers. Material from volcanic flows and ash were also deposited on the formation, creating the volcanic rock found on the Cranberry Islands. Further volcanic activity introduced igneous rocks into the Bar Harbor Formation. As the igneous intrusions cooled, crystallized minerals formed including a gabbro composed of dark, iron-rich minerals.

Mount Desert Island granite was created about 420 Mya, with one of the oldest granite bodies being Cadillac Mountain, the largest on the island. The granite body rose slowly through bedrock, fracturing it into large pieces, some of which melted under intense heat. As the granite cooled, the bedrock fragments were left surrounded by crystallized granite in a shatter zone that is visible on the eastern side of the mountain. A fine-grained, black igneous rock called diabase intruded into the granite during later volcanic activity. Diabase bodies, or dikes, are visible along the Cadillac Mountain road and on the Schoodic Peninsula.

During the next several hundred million years, the rock layers that still covered the large granite bodies, along with softer rock surrounding the granite, were worn away by erosion.

Glaciation

During the last two to three million years, a series of ice sheets flowed and receded across northern North America, eroding mountains and creating U-shaped valleys.
The glacier that covered Mount Desert Range, part of which is now called Mount Desert Island, was thick and moved at the rate of a few yards (meters) per year. The mountain range was heavily eroded by the glacier which rounded off mountaintops, carved saddles, deepened valleys, and created the fjard known as Somes Sound, nearly dividing the current island in half."The Story of Glaciers"archive
. ''nps.gov''. National Park Service. Retrieved December 7, 2018. Evidence of the last glacial period, the Wisconsin glaciation from about 75,000 to 11,000 years ago, is visible as long scratches, or striations, and crescent-shaped gouges created by material carried along at the base of the ice. As the climate warmed, the glaciers melted and receded, leaving boulders that had been carried or further south from their original locations. These boulders, or glacial erratics, lie in valleys and on mountaintops, including Bubble Rock on the South Bubble.

The coastal areas of Maine sank slightly under the extreme weight of the ice sheets, allowing seawater to cover lowlands thus forming the present-day islands. Evidence of sea caves and past beaches can be found about above current sea level. As the ice receded and the land stabilized, lakes and ponds formed in valleys dammed by glacial debris. Rivers and streams flowed again through the watershed, continuing the gradual erosion of the drainage paths.

Erosion and weathering

Acadia has a coastline composed of rocky headlands, and more heavily eroded stony or sandy beaches. Coastal areas directly facing the wind-driven waves of the Atlantic Ocean are solely composed of large boulders as all other material has been washed out to sea. Areas partially protected by rocky headlands contain the remains of more eroded rocks, consisting of pebbles, cobbles and smaller boulders. Sheltered coves, such as at Sand Beach, contain fine-grained particles that are primarily the remains of shells and other hard parts of marine life, including mussels and sea urchins.

Granitic ridges are subjected to frost weathering. Joints, or fractures, are slowly enlarged as trapped water repeatedly freezes and melts, eventually splitting off a block. Bright pink scars with granitic rubble below are evidence of such weathering; one example can be seen above the Tarn, a pond just south of Bar Harbor.

At least twelve sea caves are located in several coastal areas of the park. Sea caves are formed when waves cause erosion of coastal rock formations. If a sea cave is enlarged enough, it may break through a headland to form a sea arch.

Mass wasting and slope failure

Frequent thawing in winter prevents large accumulations of snow, and keeps the ground well saturated. Ice storms are common in winter and early spring, while rain occurs throughout the year. Saturated soils, thawing, and heavy precipitation lead to rockfalls every spring along Mount Desert Island's loop road, as well as slumping along coastal bluffs.

Mass wasting (slope movement) of marine clay, deposited when the sea level was much higher, occurs along Hunters Brook on Mount Desert Island. Slumping of the greenish-gray clay destabilized the bank, changing the course of the stream. The eastern end of Otter Cove's beach contains eroded gullies of marine clay. Mass wasting and slope failure may occur wherever marine clay is exposed.

Seismic activity

Earthquakes with epicenters near the park have caused landslides, damaging roads and trails. Earthquakes in Maine occur at a low but steady rate, with magnitudes usually less than 4.8 on the Richter scale.

Paleontology

The Presumpscot Formation has yielded a diverse collection of mostly marine fossils. The formation is composed of silt and clay deposited between 15 and 11,000 years ago when isostatic loading raised sea level as land was submerged to about above the current level. Post-glacial rebound lowered sea level, exposing the seabed to a depth of about below the current level. A global rise in sea-level flooded the shelf to the current level.

Plant fossils include pollen, spores, logs, and other plant macrofossils. Invertebrate fossils include foraminifera (protists that form test shells), sponge spicules, bryozoans, bivalves, gastropods, '' Spirorbis'', beetles, ants, barnacles, decapod crustaceans (crabs, shrimp, lobsters, etc.), ostracodes (seed shrimp), and ophiuroids ( brittle stars). Vertebrate fossils include fish and a few rare large mammals, such as walruses, whales, and a mammoth. Walrus remains have been reported on Andrews Island, west of Isle au Haut; Addison Point, northeast of the Schoodic Peninsula; and Gardiner, west-northwest of Isle au Haut. The mammoth bones were found at Scarborough, southwest of Isle au Haut.

Ecology

The ecological zones at Acadia National Park, from highest to lowest elevation, include: nearly barren mountain summits; northern boreal and eastern deciduous forests on the mountainsides; freshwater lakes and ponds, as well as wetlands like marshes and swamps in the valleys between mountains; and the Atlantic shoreline with rocky and sandy beaches, intertidal and subtidal zones.

Tiny subalpine plants grow in the granite joints on mountaintops and on the downwind side of rocks. Stunted, gnarled trees also survive near the summits. Spruce- fir boreal forests cover much of the park. Stands of oak, maple, beech, and other hardwoods more typical of New England represent the eastern deciduous forest. Pitch pines and scrub oaks inhabit isolated forests at their northeastern range limit, while jack pines reach the southern limit of their range in Acadia.

Fourteen great ponds and ten smaller ponds provide habitat for many fish and waterfowl species. More than 20% of the park is classified as wetland. Marshes and swamps form the transition between terrestrial and aquatic environments, maintaining biodiversity by providing a habitat for a wide range of species. Native wildlife frequent wetlands alongside species that are nesting, overwintering or migrating, such as birds along the Atlantic Flyway. Wetlands are composed of 37.5% marine (sea water), 31.6% palustrine (stagnant water), 20% estuarine (coastal, brackish water), 10.7% lacustrine (freshwater lakes and ponds), and 0.2% riverine (flowing streams). Approximately of perennial streams and of intermittent streams flow through the park, while about of shoreline surround 110 lakes and ponds encompassing .

Intertidal flora and fauna inhabit more than of rocky coastline. The nutrient-rich marine waters cover the intertidal plants and animals twice a day. Pools of calm water form among the rocks around low tides, inhabited by starfish, dog whelks, blue mussels, sea cucumbers, and rockweed.

Flora

Flora common to both deciduous and coniferous woodlands include lowbush blueberry, Canadian bunchberry, hobblebush, bluebead lily, Canada mayflower, wild sarsaparilla, shadbush, starflower, rosy twisted stalk, wintergreen, and white pine trees."Common Native Plants"
. ''nps.gov''. National Park Service. July 15, 2016. Retrieved December 3, 2018.

Coniferous forest trees include the balsam fir, eastern hemlock, red pine, red spruce, and white spruce. The park has a potential natural vegetation of northeastern spruce/ fir within temperate coniferous forests, according to the original A. W. Kuchler types. Spruce-fir forests cover more than sixty percent of the naturally vegetated habitats in the park. Other coniferous forest plants include dewdrop, mountain holly, pinesap, one-flowered pyrola, shinleaf, trailing arbutus, northern woodsorrel, and drooping woodreed.

An invasive insect known as the red pine scale was confirmed on dying red pines on the south side of Norumbega Mountain near Lower Hadlock Pond in 2014.

Deciduous forest trees include the white ash, big-toothed and trembling aspen, American beech, paper and yellow birch, red oak, American mountain ash, as well as mountain, red, striped, and sugar maples. Other deciduous forest plants include large-leaved aster, chokecherry, red-berried elder, Christmas fern, threeleaf goldthread, early saxifrage, false Solomon's seal, small Solomon's seal, and twinflower.

Trees commonly found in the mountains and dry, rocky places of the national park include gray birch, common juniper, jack pine, and pitch pine, while smaller trees, or shrub, species include green alder and pin cherry. Other common shrubs and flowering plants found in the mountains and rocky areas include alpine aster, bearberry, velvetleaf blueberry, bush-honeysuckle, black chokeberry, three-toothed cinquefoil, mountain cranberry, bracken fern, Rand's goldenrod, harebell, golden heather, mountain holly, black huckleberry, creeping juniper, sheep laurel, red raspberry, Virginia rose, mountain sandwort, bristly sarsaparilla, sweetfern, and wild raisin. Poverty oatgrass