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Wizard Island
Wizard Island
Wizard Island
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Wizard Island is a volcanic cinder cone which forms an island at the west end of Crater Lake in Crater Lake National Park, Oregon. The top of the island reaches 6,933 feet (2,113 m) above sea level, about 755 feet (230 m) above the average surface of the lake.

Key Information

The cone is capped by a volcanic crater about 500 feet (150 m) wide and 100 feet (30 m) deep. The crater was named the "Witches Cauldron" by William Gladstone Steel in 1885, who also gave Wizard Island its name at the same time.[5] The land area of the island is 315.85 acres (127.82 ha).

Formation

[edit]

Wizard Island was created after Mount Mazama, a large complex volcano, erupted violently approximately 7,700 years ago, forming its caldera which now contains Crater Lake. Following the cataclysmic caldera-forming eruption, which left a hole about 4,000 feet (1,200 m) deep where the mountain had once stood, a series of smaller eruptions over the next several hundred years formed several cinder cones on the caldera floor. The highest of these cones, the only one to rise above the current lake level, is Wizard Island, which rises over 2,700 feet (820 m) above the lowest point on the caldera floor and the deepest point in the lake.[6]

Another large cinder cone, Merriam Cone, is in the northeast part of the lake. Although Merriam Cone rises about 1,400 feet (430 m) above the caldera floor, its summit is still 505 feet (154 m) below the average lake level. Its surface features and lack of a crater indicate that Merriam Cone formed under water.

Access

[edit]

Current public access to Wizard Island is available only during the summer months when boat tours on Crater Lake are in operation. The tours depart from Cleetwood Cove at the north end of the lake, and circle the lake in the counterclockwise direction, stopping at a dock at Governors Bay on the south side of Wizard Island.[7]

Passengers on boat trips early in the day may choose to disembark on the island, but must be prepared to spend the entire day on the island if subsequent boats are too full to take on additional passengers. Those on late afternoon boat trips are not permitted to disembark. A final boat is dispatched at the end of each day to pick up any stragglers since overnight camping is not permitted on the island.[citation needed]

Two hiking trails are available on Wizard Island, one of which switchbacks up the flanks of the cone and circles the crater on top while the other trail meanders from the dock towards the western end of the island.[7]

  • Looking up out of the crater of Wizard Island from the bottom
    Looking up out of the crater of Wizard Island from the bottom
  • Crater Lake and Wizard Island in 1997
    Crater Lake and Wizard Island in 1997
  • Crater Lake bathymetry survey showing Wizard Island and Merriam Cone
    Crater Lake bathymetry survey showing Wizard Island and Merriam Cone
  • Geologic map of Wizard Island and the lake floor
    Geologic map of Wizard Island and the lake floor
Panoramic view of the volcanic crater of Wizard Island, seen from the rim

Notes

[edit]

References

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Wizard Island

View on Grokipedia
from Grokipedia
Wizard Island is a cinder cone volcano located within the caldera of Crater Lake in Crater Lake National Park, Oregon, United States. It formed as part of post-caldera volcanic activity following the cataclysmic eruption and collapse of Mount Mazama approximately 7,700 years ago, emerging while the lake filled with precipitation. Rising about 760 feet (232 meters) above the lake surface, it represents only 2% of its total volume, with the majority submerged and three other underwater post-caldera cones nearby. The island's summit features a tree-covered crater roughly 500 feet (152 meters) in diameter and 100 feet (30 meters) deep, known historically as the "Witches Cauldron." Named in 1885 by William Gladstone Steel for its resemblance to a wizard's , Wizard Island's last eruption occurred around 4,800 years ago, producing a small rhyodacite on its eastern flank. Composed primarily of andesitic lava and , the cone sits on the floor near the western structural margin and supports an with trees up to 800 years old. Access to Wizard Island is limited to seasonal boat tours departing from Cleetwood Cove trailhead, the park's only legal shore access point, allowing visitors to hike trails like the 1.9-mile Summit Trail to the crater rim. These tours, operated by concessioners, provide opportunities for exploration until the cove trail closes for rehabilitation from 2026 to 2028. As a significant geological feature, Wizard Island highlights the ongoing volcanic history of the .

Geography

Location and Setting

Wizard Island is situated at the western end of within , , . Its approximate geographic coordinates are 42°56′19″N 122°08′48″W. As part of the , the island emerges from , a high-elevation lake resulting from volcanic activity and the collapse of . The lake's surface sits at an elevation of 1,883 m (6,178 ft), providing a stark backdrop for the island's prominence. Wizard Island serves as a key visual and ecological feature in the lake, which measures approximately 32 km (20 mi) in shoreline circumference. The surrounding steep walls, rising up to 600 m (2,000 ft) above the water, contribute to the island's profound isolation, establishing it as a distinct insular within the .

Physical Characteristics

Wizard Island occupies a land area of approximately 1.28 km² (316 acres). The island's attains a maximum of 2,115 m (6,940 ft) above , rising 232 m (760 ft) above the surface of . It exhibits a symmetrical shape, evoking the profile of a wizard's , encircled at its base by rugged lava flows. A , known as the Witches Cauldron, measures roughly 90 m (300 ft) in diameter and 27 m (90 ft) deep. The island's steep slopes consist of talus fields interspersed with forested sections, dropping directly into the lake without beaches or shallow coastal margins.

Geology

Formation and Age

Wizard Island formed as part of the post- volcanic activity following the cataclysmic eruption and collapse of approximately 7,700 years ago, which created the . The island itself emerged roughly 400 years later, around 7,300 years ago, during the early stages of the caldera's filling with rainwater and snowmelt. This timeline places Wizard Island's initial development within a broader context of renewed volcanism in the , where smaller vents reactivated after the main event. The cone's formation resulted primarily from phreatomagmatic eruptions, in which ascending interacted explosively with the rising lake waters, generating steam explosions that deposited layers of cinder, ash, and . These eruptions built the symmetrical structure, with subaerial growth extending about 250 meters above the current lake surface and additional subaqueous extensions reaching 70 meters below it. Effusive phases also contributed lava flows from vents on the island's flanks, further shaping its profile as the lake level rose. Wizard Island represents one of several smaller post- vents within the , including the central platform and Merriam Cone, which collectively reactivated the magmatic system over centuries following the collapse. , particularly radiocarbon analysis of organic sediments and layers interlayered with Mazama ashfall deposits, confirms this sequence and relative age, showing Wizard Island's materials overlying the climactic eruption products. These methods establish the island's buildup as occurring progressively during the 250- to 750-year period of initial lake filling. Since its primary construction phase, Wizard Island has experienced no major eruptive activity, with only a minor rhyodacite dome forming on its east flank around 4,800 to 5,000 years ago, classifying the as dormant. Sediment accumulation of up to 30 meters on the lake floor since then indicates prolonged quiescence.

Geological Features

Wizard Island is primarily composed of andesitic cinders, , and ejected during explosive volcanic eruptions that built its structure. The cone's materials include black scoriaceous lapilli and blocks, with red and brown cinders concentrated near the summit, while fine is scarce and fragments are generally larger than 1 inch in . Bombs up to 2 feet across occur near the base, and blocks exceeding 6 feet are found along the rim, reflecting the explosive nature of the eruptions. At the island's base, dark, rugged aa-type lava flows encircle the lighter , forming a stark contrast in color and texture. These flows, composed of blocky with fragments up to 30 feet long and smooth glassy surfaces, extend westward for about 0.5 miles above the lake surface and cover a larger submerged area to the east. The aa flows feature prominent ridges up to 60 feet high in channels like Skell Channel, where troughs contain jade-green pools floored by . The summit , known as the Witches Cauldron, is a bowl-shaped depression approximately 470 feet (143 meters) across and 90 feet (27 meters) deep, filled with loose volcanic debris including black scoriaceous lava fragments and foreign inclusions. This loose material makes the crater floor unstable and slippery, particularly after . Rocks near the rim show evidence of hydrothermal alteration, linked to the volcanic activity that formed the , including alteration in andesitic stockwork and associated thermal features. Wizard Island integrates with Crater Lake's rim as a post- feature within the 7,700-year-old collapse structure of , positioned along the western caldera floor amid ring fault lines from the cataclysmic event. Its deposits date to post-Mazama activity around 7,200 years ago.

Ecology

Flora

The flora of Wizard Island is characteristic of a subalpine ecosystem, shaped by the island's volcanic origins, high elevation (reaching 6,933 feet or 2,113 meters at the summit), and short growing season of approximately 100 days. The island's plant life is adapted to nutrient-poor, porous pumice and ash soils derived from post-caldera eruptions, with vegetation zones transitioning from dense forests on the lower slopes to open meadows near the crater rim. The slopes are dominated by coniferous forests, primarily lodgepole pine (Pinus contorta var. latifolia) and whitebark pine (Pinus albicaulis), which form dense stands that stabilize the steep terrain and provide habitat structure. Lodgepole pine, identifiable by its bundles of two needles and prickly cones, grows up to 100 feet (30 meters) tall and thrives in the acidic, well-drained volcanic substrates. Whitebark pine, found at the highest elevations, features five-needle bundles and can live over 500 years, often in form near the treeline. However, whitebark pine populations on the island are threatened by white pine blister rust, a non-native fungal , as well as mountain pine beetle infestations and fire suppression, contributing to ongoing decline in this . The beneath these includes shrubs and trees such as ( spp.), which produce edible berries and support local by birds, mountain hemlock (), and subalpine fir ( var. lasiocarpa). Mountain hemlock, with its drooping branches and small cones, is prevalent from about 5,000 feet (1,524 meters) upward, while subalpine fir occupies higher drainages and rim areas, rarely exceeding 100 feet (30 meters) in height. These species contribute to a layered community that enhances soil retention on the island's slopes. Wizard Island supports over 100 vascular plant species, as documented in early surveys, though the broader park encompasses more than 700 native vascular plants; the island's isolation limits its total diversity while preserving unique subalpine assemblages. Near the summit, alpine meadows feature vibrant wildflowers, including lupine (Lupinus spp.) with its pea-like blooms and Indian paintbrush (Castilleja spp.) displaying vivid red or yellow inflorescences, which bloom briefly during summer in the open, rocky areas above the treeline. These herbaceous communities add seasonal color and support pollinators in the harsh high-elevation environment. Plants on Wizard Island exhibit key adaptations to the nutrient-deficient volcanic soils, including mycorrhizal associations that enhance phosphorus and nitrogen uptake from the low-fertility pumice. Many conifers and understory species form symbiotic relationships with ectomycorrhizal fungi, which extend root systems and improve nutrient acquisition in the porous, low-organic-matter substrates. Nitrogen-fixing plants, such as certain legumes in the meadows, further aid soil enrichment by converting atmospheric nitrogen, facilitating pioneer colonization on barren cinder deposits. Due to the island's remote location in the deep waters of , no introduced have established, preserving the native and preventing disruption to the endemic communities. This isolation, combined with active management, maintains the ecological integrity of the subalpine flora.

Fauna

Wizard Island, a small volcanic rising 760 feet above 's surface, supports a limited community of mammals adapted to its rocky, forested terrain and subalpine conditions. The island's mammalian primarily consists of smaller . Golden-mantled ground squirrels (Callospermophilus lateralis) are common, often observed foraging in open areas and rocky slopes where they cache food for winter. Pikas (Ochotona princeps) inhabit the island's talus slopes and rocky outcrops, emitting their characteristic high-pitched calls while gathering vegetation for haypiles in crevices. These thrive in the island's harsh environment, relying on the sparse cover for sustenance and shelter. The absence of large predators underscores the island's ecological constraints; black bears (Ursus americanus) and cougars (Puma concolor) are not resident, as the limited habitat and isolation prevent sustained populations, though rare transient sightings of bears have occurred via swimming from the mainland, including a documented instance in September 2024. Amphibians are similarly restricted, with newts such as the endemic Mazama newt (Taricha granulosa subsp. mazamae) found along the shores and in small water bodies on the island. Birds represent a more dynamic component of the island's fauna, with both resident and migratory utilizing its cliffs, forests, and proximity to the lake. Clark's nutcrackers (Nucifraga columbiana) are prominent, serving as key seed dispersers for whitebark pine by caching uneaten seeds that germinate into new trees, thus shaping the island's coniferous vegetation. Peregrine falcons (Falco peregrinus) nest on the island's steep cliffs, preying on smaller birds and in the surrounding airspace. Waterfowl, including common mergansers and various ducks, frequent the lake's shores near Wizard Island during breeding and migration seasons, foraging in the clear waters. Seasonal migrations bring additional , such as warblers and hummingbirds, to the island in spring and fall, temporarily boosting avian diversity before they depart for wintering grounds. Invertebrates on Wizard Island include and beetles well-adapted to the volcanic soils and variable microhabitats, with like checkerspot butterflies (Euphydryas spp.) and ground beetles (Carabidae) exploiting the island's herbaceous patches and rock crevices for nectar, pollen, and prey. Overall, the island's is lower than that of the mainland due to its geographic isolation, small land area of about 315 acres, and lack of connectivity, which restricts colonization by larger or less mobile . This isolation fosters a unique, resilient subset of the park's , dependent on the island's limited for food and habitat.

History

Discovery and Naming

The Klamath Tribe's oral histories recount the dramatic eruption of over 7,000 years ago, which formed the containing and profoundly impacted the landscape, though these traditions do not assign a specific name to Wizard Island. Klamath and Modoc traditions also describe Wizard Island's formation as the head of the underworld spirit Lao, thrown into the lake after defeat in a battle with the sky spirit , linking it to the cataclysmic events. The first authenticated non-native sighting of and Wizard Island occurred on June 12, 1853, when a party of prospectors led by John W. Hillman, including Isaac Skeeters and others, encountered the body of water while searching for gold in the Rogue River Valley. Initially mistaking it for the more distant Klamath Lake from afar, the group descended to its rim and named it Deep Blue Lake for its striking color. Earlier claims of discovery by explorer during his 1845 expedition are considered unsubstantiated, as his party only viewed the surrounding mountains without reaching the lake. Wizard Island was named in 1885 by William Gladstone Steel during his first visit to on August 15 of that year, when he observed the island's prominent rising sharply from the water. Steel, inspired by the cone's distinctive pointed shape resembling a wizard's hat, christened it Wizard Island two days later, and he also dubbed the lake's main the "Witches Cauldron" in his early promotional writings to evoke its mystical allure. A dedicated conservationist, Steel launched a 17-year campaign to protect the site, founding organizations like the Oregon Alpine Club and lobbying , which culminated in the official recognition of Wizard Island as part of , established by President on May 22, 1902.

Exploration and Human Impact

Following the establishment of on May 22, 1902, which encompassed Wizard Island and provided federal protection against development, early scientific exploration of the island began in earnest. In 1902, USGS geologists Joseph S. Diller and Horace B. Patton conducted detailed surveys of the region, including Wizard Island, as part of their comprehensive study that mapped and described the area's volcanic landscape. These efforts continued through the 1900s, with Diller's subsequent reports in 1912 further documenting the island's post-caldera features based on field observations from boat landings and climbs. Human presence on Wizard Island has remained minimal since the park's creation, with no permanent settlements allowed to preserve its natural state. Occasional temporary research camps have supported studies in and , such as water quality monitoring and sediment core sampling conducted by scientists from the island's shores. In the 1930s, the constructed the main trail on the island from the boat landing to the summit in 1934, with three switchbacks, to support ranger-led tours and visitor access. The contributed to other trail maintenance and construction in the park during this period. Modern human impacts on Wizard Island primarily stem from seasonal visitor foot traffic, which has led to localized trail erosion and , particularly along steeper slopes. These effects are mitigated through park regulations, including trail use limits, mandatory stay-on-trail policies, and seasonal closures enforced by the superintendent's to prevent further degradation. The island's cultural significance has been amplified through its depiction in art and literature, such as paintings by Grace Russell Fountain and Mabel Russell Lowther in the early , which highlighted its dramatic beauty and bolstered conservation advocacy leading to the park's protection.

Recreation and Access

Visitor Access

Wizard Island is accessible solely by boat tours departing from the dock at Cleetwood Cove on the northern rim of . These tours are operated by Xanterra Parks and Resorts under the name Explor Crater Lake, using U.S. Coast Guard-certified vessels designed to carry up to 49 passengers each. To reach the departure point, visitors must hike the 1.1-mile (one-way) Cleetwood Cove Trail, which descends 700 feet in elevation and typically takes 30-45 minutes; the return ascent is more strenuous and can take up to an hour. Private boats are prohibited to preserve the lake's exceptional , with access limited to these authorized tours. The trail and tours operate seasonally in summer, generally from early July to mid-September, though exact dates vary annually based on weather and park conditions; in 2025, tours operated from early July to mid-September, but they will be unavailable from 2026 through 2028 due to rehabilitation of the Cleetwood Cove Trail and marina facilities. Options for reaching Wizard Island include the full Wizard Island Tour, which combines a 2-hour narrated lake cruise with a stop for several hours on the island followed by a return shuttle (totaling 6-7 hours), or the direct Wizard Island Shuttle, a 15-20 minute ride departing at set times like 9:00 a.m. and 11:30 a.m. to allow disembarkation for extended exploration before an afternoon return. Each has limited capacity of 40-49 passengers, and reservations are required well in advance via the operator's website or by calling 866-292-6720, particularly for early departures enabling island access; same-day tickets may be available but are not guaranteed. Tours are weather-dependent, with frequent cancellations due to high winds, low visibility, or smoke, and should prepare for variable conditions including cold temperatures on the water. entry requires a of $30 per vehicle (valid for seven days), and shuttles from centers to the are available via Crater Lake Trolley during peak season.

Activities and Trails

The primary recreational activity on Wizard Island is the Wizard Island , a strenuous 2.2-mile (3.5 km) round-trip path that gains 760 feet (232 m) in elevation from the boat dock at 6,175 feet (1,882 m) to the at 6,933 feet (2,113 m). The trail begins with switchbacks winding through dense forest of western hemlock and whitebark pine before emerging onto open cinder fields and a rocky ascent to the rim of the island's 90-foot-deep (27 m) , where a short 0.3-mile (0.5 km) loop allows hikers to circle the 's edge for panoramic views of . Interpretive signs along the route highlight key aspects of the island's geology, such as its formation, and , including native plant species and volcanic influences on local habitats. A secondary option, the Fumarole Bay Trail, provides a more moderate 1.7-mile (2.7 km) round-trip hike with 150 feet (46 m) of elevation gain, leading from the dock to a shallow, rocky cove ideal for brief exploration. Swimming is allowed in Crater Lake waters adjacent to Wizard Island, including near the Fumarole Bay cove, but the cold temperatures—ranging from 38°F to 62°F (3°C to 17°C) at the surface, depending on season and weather—make it a brisk experience limited to within 100 yards (91 m) of the island; snorkeling and SCUBA diving are prohibited to protect the lake's ecosystem, and swimmers must remain at least 50 yards (46 m) from any boat, dock, or buoy. The island offers no dedicated swimming facilities, and the rocky shoreline requires caution. Picnicking and photography are common pursuits, with visitors capturing the island's dramatic volcanic landscapes and lake vistas during their allotted time ashore, typically 3 to 5 hours before returning via scheduled boat pickup. The island has minimal infrastructure, including only composting toilets near the dock and no additional restrooms, concessions, or permanent docks beyond the tour landing. To preserve the fragile environment, park regulations mandate staying on designated trails to prevent , strictly prohibit collecting rocks, plants, or any natural materials, and encourage participation in optional ranger-led interpretive programs available during peak summer season.

References

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