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Cape Evans
Cape Evans
Cape Evans
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Cape Evans (77°38′S 166°24′E / 77.633°S 166.400°E / -77.633; 166.400 (Cape Evans)) is a rocky cape on the west side of Ross Island, Antarctica, forming the north side of the entrance to Erebus Bay.[1]

Key Information

History

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The cape was discovered by the British National Antarctic Expedition, 1901–04, under Robert Falcon Scott, who named it the "Skuary" after the birds. Scott's second expedition, the British Antarctic Expedition, 1910–13, built its headquarters here, renaming the cape for Lieutenant Edward Evans, Royal Navy, second in command of the expedition.[1] Scott's headquarters building still exists and is known as Scott's Hut.[2]

Historic sites and monuments

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Scott's Hut has been designated a Historic Site or Monument (HSM 16), following a proposal by New Zealand and the United Kingdom to the Antarctic Treaty Consultative Meeting.[3]

A cross on Windvane Hill, Cape Evans, was erected by the Ross Sea Party, led by Captain Aeneas Mackintosh, of Sir Ernest Shackleton's Imperial Trans-Antarctic Expedition of 1914–1917, in memory of three members of the party who died in the vicinity in 1916: Arnold Spencer-Smith, Aeneas Mackintosh and Victor Hayward. The cross has been designated a Historic Site or Monument (HSM 17), following a proposal by New Zealand and the United Kingdom to the Antarctic Treaty Consultative Meeting.[3]

The whole site is protected as Antarctic Specially Protected Area (ASPA) No.155 largely because of its historic significance as one of the principal sites of early human activity in Antarctica.[4]

Lakes

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Cape Evans in southwest

Skua Lake

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77°38′S 166°25′E / 77.633°S 166.417°E / -77.633; 166.417. A small lake close northwest of Island Lake at Cape Evans. Named by the British Antarctic Expedition (1910–13) because of the nearby skua rookery.[5]

Algal Lake

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77°38′S 166°25′E / 77.633°S 166.417°E / -77.633; 166.417. A small, roughly circular meltwater lake about midway between Skua Lake and Island Lake. Named by USARP biologists David T. Mason, Charles R. Goldman and Brian J.B. Wood, Jr., who studied the lake in the 1961–62 and 1962-63 seasons. The name derives from the striking mat of blue-green algal remains around the leeward edge of the lake.[6]

Island Lake

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77°38′S 166°26′E / 77.633°S 166.433°E / -77.633; 166.433. A lake lying southeast of Skua Lake at Cape Evans. It appears that the descriptive name was given by members of the British Antarctic Expedition (1910–13), who built their winter quarters hut at Cape Evans.[7]

Other features

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Features around Cape Evans include North Bay, South Bay, Cape Evans Hut, Tryggve Point, Turks Head Bay, Turks Head, Inaccessible Island, Tent Island, Dellbridge Island, Little Razorback Island and Big Razorback Island.[8]

North Bay

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77°38′S 166°23′E / 77.633°S 166.383°E / -77.633; 166.383. A small bay on the north side of Cape Evans. Named by members of the British Antarctic Expedition, 1910-13.[9]

Windvane Hill

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Memorial cross at Cape Evans

77°38′S 166°24′E / 77.633°S 166.400°E / -77.633; 166.400. Small hill just northeast of the extremity of Cape Evans. So named by the British Antarctic Expedition (1910–13) because an anemometer station was established on this site.[10]

South Bay

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77°38′S 166°25′E / 77.633°S 166.417°E / -77.633; 166.417. A small bay on the south side of Cape Evans. Named by members of the British Antarctic Expedition, 1910-13.[11]

The Ramp

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77°37′55″S 166°25′47″E / 77.63202°S 166.429595°E / -77.63202; 166.429595. A steep rocky slope 0.5 nautical miles (0.93 km; 0.58 mi) inland from Cape Evans. The slope is 0.5 nautical miles (0.93 km; 0.58 mi) long and rises to 50 metres (160 ft). Descriptively named by the British Antarctic Expedition (BrAE), 1910-13.[12]

Pakaru Icefalls

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77°37′49″S 166°44′31″E / 77.630333°S 166.741909°E / -77.630333; 166.741909. Icefalls between Cape Evans and Turks Head on the southwest shore of Ross Island. The feature comprises a very irregular and broken glacial area to the north of Turks Head Ridge with ice descending to Erebus Bay. Descriptively named, Pakaru being a Maori word meaning "broken."[13]

Tryggve Point

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77°39′S 166°42′E / 77.650°S 166.700°E / -77.650; 166.700. A point 1 nautical mile (1.9 km; 1.2 mi) northwest of Turks Head. First charted by the British Antarctic Expedition, 1910–13, under Scott, who named it for Tryggve Gran, Norwegian ski expert with the expedition.[14]

Turks Head

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77°40′S 166°46′E / 77.667°S 166.767°E / -77.667; 166.767. A precipitous black headland over 200 metres (660 ft) high, 5 nautical miles (9.3 km; 5.8 mi) east-southeast of Cape Evans. Discovered by the British National Antarctic Expedition (1901–04) and so named because of its resemblance to a head swathed in a turban.[15]

References

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Sources

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Public Domain This article incorporates public domain material from websites or documents of the United States Geological Survey.

Revisions and contributorsEdit on WikipediaRead on Wikipedia

Cape Evans

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from Grokipedia
Cape Evans is a rocky headland on the southwestern shore of in , , situated at 77°38′S, 166°24′E and forming the northern entrance to Erebus Bay. Originally referred to as "Skuary" by Scott's earlier (1901–1904) due to the abundance of skuas in the area, it was renamed in 1911 by Captain to honor his second-in-command, Lieutenant Edward Ratcliffe Garth Russell Evans, during the British (Terra Nova) Expedition (1910–1913). The cape served as the expedition's primary winter quarters and scientific base, where a prefabricated —measuring 15.2 by 7.6 meters (50 by 25 feet) with an attached stable for 19 ponies—was constructed in 1911 to accommodate up to 25 personnel conducting geological, biological, and meteorological research amid the harsh conditions. The site's historical prominence extends to Ernest Shackleton's (1914–1917), when the Ross Sea Party, led by , overwintered there twice and used the existing hut as their base while laying supply depots across the to support the party's transcontinental crossing. Tragically, three party members—Reverend Arnold Spencer-Smith, Mackintosh, and Victor Hayward—died during the expedition due to , exposure, and a blizzard, prompting the erection of a wooden cross on nearby Wind Vane Hill on January 16, 1917, as a ; this cross, now weathered but structurally sound, stands as a poignant symbol of the era's perils. Designated as Historic Sites and Monuments (HSM) 16 for and HSM 17 for the memorial cross under the , Cape Evans was redesignated in 2002 as (ASPA) No. 155 to safeguard its archaeological and historical integrity, including preserved artifacts like canned food, clothing, and scientific instruments left from both expeditions. Conservation efforts, led by the Antarctic Heritage Trust in collaboration with the , have included restorations in 1961 and ongoing maintenance to combat deterioration from freeze-thaw cycles and salt contamination, including the 2024-25 season's archaeological work, ensuring the site's role as a testament to the remains accessible for educational and scientific purposes while minimizing human impact.

Geography

Location and Terrain

Cape Evans is situated at coordinates 77°38′S 166°24′E on the west side of in , forming the north side of the entrance to Erebus Bay. This position places it along the southwestern coast of , approximately 10 km south of , in close proximity to . The cape is a small, triangular, low-lying ice-free area of volcanic origin, characterized by gently sloping rocky terrain with outcrops. To the west, it borders the , while overlooks it from the east, dominating the skyline. The climate at Cape Evans exemplifies extreme Antarctic conditions, with a mean annual air temperature of approximately -20°C at sea level. Winters feature average temperatures below -20°C and extremes as low as -57°C, accompanied by strong katabatic winds descending from the interior plateau. Summers bring brief periods of milder weather, with mean January temperatures around -4.8°C, enabling limited surface melt on exposed rocks and snowdrifts during sunny intervals.

Geology

Cape Evans forms part of the Ross Island volcanic field in , situated on the western flank of , the region's dominant . The cape consists primarily of alkaline volcanic rocks extruded from , with the exposed bedrock dominated by two kenyte flows—a type of or tephriphonolite characterized by large phenocrysts. These flows represent effusive eruptions that built the ice-free rocky , with the youngest flow reaching thicknesses of up to 15 meters in places and locally swelling to 50 feet. The formation of Cape Evans dates to the Pleistocene epoch, with indicating that at least one kenyte flow at the cape's tip is approximately 55 ± 10 ka old, placing it in the . This ancient volcanic activity contributed to the cape's physical stability as a low-lying, triangular protruding from the surrounding ice, where the resistant lava flows resist glacial erosion and maintain an ice-free status amid the broader . Overlying the kenyte are thin deposits of outwash consisting of sand and gravel-sized fragments derived from kenyte, , , and , along with scattered large blocks of lithic , , and within an ice-cored moraine from the Barne Glacier. A younger, thin flow of partially covers the kenyte to the northeast, adding to the cape's basaltic components. Geological investigations of Cape Evans began in the early 20th century but were systematically mapped during the 1960–1961 austral summer, with a detailed survey documenting the kenyte flows and their stratigraphic relationships. This work, published in 1963, described the two kenyte flows and emphasized their role in the cape's morphology, noting how the outwash and morainal deposits mantle the underlying volcanics and limit exposures to the north of the Barne Glacier's end moraine. Subsequent studies, including paleomagnetic and 40Ar/39Ar dating in the early 2000s, have refined the eruptive chronology, confirming the Pleistocene origins and integrating Cape Evans into broader models of Mount Erebus's long-lived activity spanning over 1 million years. These findings underscore the cape's significance as a window into the Erebus Volcanic Province's petrology and eruptive history.

History

Discovery and Naming

Cape Evans was first sighted during the British National Antarctic Expedition (1901–1904), led by , as part of the exploratory efforts in the region. The expedition, aboard the ship Discovery, focused on scientific observations and mapping in , with the team establishing their primary base at Hut Point on and conducting coastal surveys to document the island's features. During these surveys around , the cape was identified as a prominent rocky promontory on the west side, forming the north entrance to Bay. Scott named the feature "the Skuary" in recognition of the abundant birds observed flocking in the area, highlighting the region's avian during the austral summer. Early expedition records noted the cape's potential as a sheltered location along the coastline, though it was not selected for the main base due to the challenges of ice conditions and the suitability of Hut Point for the Discovery's overwintering. These initial observations contributed to broader understandings of Ross Island's geography but did not lead to immediate occupation. The name was changed to Cape Evans during Scott's subsequent British Expedition (1910–1913), honoring Lieutenant Edward Ratcliffe Garth Russell Evans, the .

Terra Nova Expedition

The British Expedition (1910–1913), commonly known as the and led by , selected Cape Evans on as its primary base after arriving in on 4 January 1911. Scott renamed the cape, previously known as "the Skuary," in honor of his , Lieutenant Edward Ratcliffe Garth Russell Evans, recognizing its suitability as a sheltered site free from heavy pack ice during the brief summer. Scott's Hut, a prefabricated structure measuring 50 by 25 feet (15 by 7.6 meters), was erected as winter quarters between 5 and 18 January 1911, accommodating up to 25 men and including attached stables for 19 ponies. Construction proceeded rapidly despite logistical hurdles, including the loss of one motor sledge through thin on 8 January and subsequent blizzards that delayed unloading of supplies from the Terra Nova. The hut was insulated with local seaweed, fitted with a cooking range and stove, and divided into living quarters, a mess room, and storage areas to support overwintering. At Cape Evans, the expedition conducted essential preparations for the attempt, including motor sledging trials with two remaining Arrol-Johnston vehicles to test supply hauling over the Barrier ice; these proved promising in initial runs but broke down early during the main journey. Ponies, sourced from and , underwent acclimatization in the hut's stables, though many struggled with the cold and soft snow surfaces, requiring improvised snowshoes; one such pony, "Bones," led by Tom Crean, was shot on 9 December 1911 near the end of a depot-laying march starting from the base. Scientific observations formed a core activity, with teams recording meteorological data, geological samples, and biological specimens, while the site functioned as the main depot for caching , , and for outward parties. The base remained operational until early 1912, supporting multiple depot-laying trips from January to March 1911 and serving as a staging point for the polar party's departure on 1 November 1911. The last support party turned back in early January 1912, and when the Terra Nova departed in February 1912, the polar party had not yet returned, so Cape Evans was stocked with emergency supplies and artifacts, leaving the hut as a potential station.

Historic Sites and Monuments

Scott's Hut

Scott's Hut was constructed in January 1911 by the British Antarctic (Terra Nova) Expedition team at Cape Evans, serving as their primary overwintering base. The single-story wooden structure, prefabricated in England and assembled on-site in just nine days between January 4 and 17, measured approximately 15 meters long by 7.6 meters wide, making it the largest hut built during the Heroic Age of Antarctic exploration. It incorporated imported materials such as Douglas fir and Scots pine for framing and paneling, supplemented by local volcanic rock for foundations and some on-site adaptations for the attached stables. The design included an open verandah on three sides for protection against the harsh weather, with the stables built as a lean-to along the north side using recycled ship timbers, fodder bales, and rubberoid roofing. The interior layout was pragmatically divided to support both daily living and scientific work, reflecting the expedition's dual focus on and . The main living quarters occupied the eastern end, featuring tiered bunk beds for up to 25 men, a central for cooking and heating fueled by seal blubber, and communal tables cluttered with utensils and personal effects. Adjacent to this was a dedicated equipped for meteorological, geological, and biological studies, complete with workbenches, chemical storage, and observation tools. Storage areas, including partitioned sections along the walls and under bunks, held provisions like canned meats, boxes, and dried , as well as sledging gear and spare parts; the attached stables provided shelter for the 19 ponies, divided into seven bays with a corridor for access. Original furnishings, such as wooden bunks labeled with names like those of and Simpson, remain in place, evoking the cramped yet organized environment. Preserved within the hut are over 8,000 artifacts that capture the material culture of the expedition, ranging from everyday items to specialized equipment. Key examples include scientific instruments like thermometers and barometers in the laboratory, woolen clothing and boots hung on hooks, expedition diaries and photographic plates stored on shelves, and unique oddities such as pony snowshoes, a disassembled bicycle for man-hauling, and stacks of seal blubber for fuel. Provisions like unopened cans of jam, penguin eggs, and butter remain edible in appearance due to the freezing conditions, while the stables hold pony tack, brushes, and fodder bags. Outside the structure, skeletal remains of the expedition's ponies lie near the stables, a somber reminder of the animals' role and hardships. These items, largely untouched since 1912, provide invaluable insights into the logistics and daily routines of polar exploration. As a cornerstone of the Terra Nova Expedition's operations, symbolizes the ambition and adversity of the Heroic Age, encapsulating the era's blend of scientific inquiry and national endeavor. Last occupied in before the polar party's departure, the hut was stocked with supplies for potential return and sealed, its frozen-in-time state preserved through international conservation efforts.

Monuments and Protection

Cape Evans hosts two key Historic Sites and Monuments (HSMs) recognized under the . HSM 16 designates , constructed in January 1911 by the British Antarctic Expedition led by as the base for the . HSM 17 marks a commemorative cross on Windvane Hill, erected on January 16, 1917, by the Ross Sea Party of Ernest Shackleton's to honor three members—Aeneas , Victor Hayward, and Arnold Spencer-Smith—who died in 1916: Spencer-Smith from and and Hayward lost in a blizzard while crossing sea ice. The entire site, encompassing these monuments and surrounding features, was designated as (ASPA) No. 155 in 2004 through Antarctic Treaty Consultative Meeting (ATCM) Measure 2, with subsequent revisions to its management plan adopted in 2005, 2008, 2010, 2015, and 2021. This status, administered under the , aims to preserve the area's outstanding historical value—linked to early 20th-century —and its scientific significance for understanding past human activity in , while minimizing environmental disturbance. Entry to ASPA 155 requires a permit issued by competent national authorities, limiting access to essential scientific, conservation, or management purposes; tourism visits are guided and capped at 40 people within the area and eight inside the hut at any time, with an annual maximum of 2,000 visitors. Conservation efforts are led by the New Zealand-based Antarctic Heritage Trust (AHT), which has maintained the site since the 1980s under agreements with New Zealand's government and international partners. The AHT's work includes stabilizing artifacts within , such as freezing and conserving perishable items like food tins and clothing to prevent deterioration, and structural repairs to the hut's framework against weathering. Broader measures address through strict protocols to control , including inspections of visitors and equipment to prevent introduction of non-native organisms that could alter the pristine environment around the monuments. These ongoing initiatives ensure the site's integrity as a of history. Challenges to preservation include climate change effects, such as warming-induced melting of beneath the structures, which causes ground instability and potential flooding from increased precipitation and variability around . This has prompted adaptive strategies in the ASPA management plan, like elevated foundations and monitoring of glacial retreat near the site. Human-related pressures, including unauthorized access and potential observed at other historic sites, have reinforced the need for enhanced permit systems and international cooperation to enforce protections.

Lakes

The lakes at Cape Evans, including Skua Lake, Algal Lake, and Island Lake, are situated within (ASPA) No. 155, which safeguards the site's historical, archaeological, and ecological values, with access restrictions to minimize human impact.

Skua Lake

Skua Lake is the largest and most prominent freshwater meltwater pond at Cape Evans on , , situated a short distance inland southeast of near a breeding colony of south polar skuas (Stercorarius maccormicki). It forms through the accumulation of in a shallow depression within the ice-free volcanic terrain, influenced by local , wind-blown salts, and avian inputs from nearby bird activity. Named by members of the (1910–1913) due to its proximity to the , the lake exemplifies early exploratory naming practices tied to observable wildlife features. The pond typically experiences seasonal ice cover that persists through winter and breaks up in summer, exposing clear water enriched with dissolved organic matter and supporting dense benthic algal communities dominated by filamentous such as Phormidium frigidum. In summer, water temperatures can reach up to 9°C at the surface, with benthic layers warming further due to solar penetration, and depths varying from shallow margins to up to several meters in central areas. Ecologically, Skua Lake plays a key role in the local microbial ecosystem, harboring layered microbial mats of and diatoms that drive through beneath the thinning ice. These mats, along with sparse including planktonic rotifers and the Daphniopsis studeri, form a low-diversity sustained by nutrient inputs from skua and inflows. The lake serves as a vital resource for the adjacent skua population, providing freshwater for drinking and bathing during the breeding season, which enhances its productivity to levels comparable to eutrophic temperate systems.

Algal Lake

Algal Lake is a small, roughly circular lake situated inland from the coast at Cape Evans on , , positioned approximately midway between Skua Lake and Island Lake. The lake spans about 50 m in diameter and lies at coordinates 77°38′S, 166°25′E, forming part of the ephemeral freshwater systems fed by seasonal in the region. Its clear waters remain relatively transparent throughout the austral summer, contrasting with the more turbid conditions in nearby lakes influenced by bird activity. The lake derives its name from the prominent mats of algal remains, particularly , observed along its leeward shore, a feature highlighted during early scientific observations in the region. These mats, remnants of dense benthic growth, were noted in studies conducted under U.S. Operation Deep Freeze between 1961 and 1963, when researchers accessed the site for initial limnological assessments supported by naval logistics. Biologically, Algal Lake supports a sparse planktonic but hosts a robust benthic layer dominated by filamentous , including and diatoms, which form thick mats on the lake bottom. The benefits from nutrient enrichment derived from surrounding volcanic kenyte soils and wind-blown salts from the nearby , fostering higher benthic compared to planktonic forms. The lake's neutral and stable summer conditions enable these microbial assemblages to thrive as a key component of freshwater . Research on Algal Lake has focused on its role as a model for , with early surveys in the 1960s measuring rates and light inhibition effects on . Studies by Goldman et al. documented benthic exceeding planktonic output by more than 20-fold, underscoring the lake's importance in understanding nutrient dynamics and microbial resilience in extreme environments. Subsequent comparative analyses in the further quantified oxygen levels and seasonal variations, establishing Algal Lake as a benchmark for studies in the area.

Island Lake

Island Lake is a small, isolated pond situated southeast of Skua Lake on the rocky volcanic terrain of Cape Evans, , , at coordinates 77°38′S 166°26′E. Measuring approximately 150 meters along its longest axis with a surface area of about 500 m², it exemplifies the ephemeral freshwater bodies typical of the ice-free areas in the region on . Named descriptively by members of the British Antarctic Expedition (, 1910–1913) for the small central islet that characterizes its form, the lake served as a minor landmark near the expedition's winter quarters. Its hydrological regime is driven by seasonal , with liquid water present only during the brief austral summer from late to late , after which it freezes solid, reaching temperatures as low as -13°C and conductivities up to 189 mS cm⁻¹ by mid-winter. The maximum depth is shallow at 1.6 meters, promoting rapid freezing and limiting persistence. Ecologically, Island Lake supports sparse microbial communities, including and benthic mats dominated by , reflecting minimal productivity compared to more biologically active neighboring lakes like Algal Lake. This relative simplicity has positioned it as a less intensively studied site, occasionally referenced in comparative limnological research on Ross Island's pond ecosystems as a baseline for understanding isolation effects on microbial in extreme Antarctic environments.

Other Features

North Bay

North Bay is a sheltered coastal inlet located on the northwest side of Cape Evans, an ice-free volcanic area on in , . It features sandy gravel beaches along approximately a 1 km stretch of coastline, backed by rocky cliffs and adjacent to the prominent ice cliffs of the Barne Glacier, which rise perpendicularly up to 200 feet high. The bay's waters are typically frozen in winter, forming a substantial foot that extends from the shore, while its depths accommodate small vessels and expedition ships during the brief summer season. This configuration provides natural protection from the prevailing southerly winds, though it remains exposed to northerly swells. During the British Antarctic (Terra Nova) Expedition of 1910–1913, led by Captain , North Bay served as the primary landing and mooring site for the expedition's ship, Terra Nova, which anchored about 200 yards offshore in January 1911 to unload stores, ponies, and equipment for establishing the base camp. The vessel was secured to the fast ice for winter overwintering, leveraging the bay's relative shelter to mitigate the harsh conditions of , though occasional ice breakouts necessitated relocating gear higher up the beach. This logistical hub facilitated the construction of just 30 meters inland on Home Beach and supported ongoing operations, including sledge journeys and scientific observations, until the ship's departure in 1912. Later, the Ross Sea Party of Ernest Shackleton's 1914–1917 also attempted landings in North Bay due to its status as one of the few ice-free spots in the region. Today, North Bay forms part of (ASPA) No. 155, designated to preserve its historical and scientific values, with access restricted to permitted visitors to minimize disturbance. The area is monitored for environmental impacts, including exacerbated by wind, foot traffic, and legacy human activities, as well as potential contamination from hydrocarbons and in sediments. Ongoing conservation efforts by organizations like the Antarctic Heritage Trust focus on protecting artifacts and stabilizing the shoreline to counteract these threats in the fragile polar ecosystem.

Windvane Hill

Windvane Hill is a low hill rising to approximately 20 meters above , situated about 150 meters southeast of at Cape Evans on . Composed of exposed basaltic rock, its summit provides panoramic views of Erebus Bay to the north and the active volcano approximately 22 kilometers northeast. The hill's elevated and open position makes it particularly susceptible to the region's strong katabatic winds, which accelerate downslope from the . During the British Antarctic (Terra Nova) Expedition of 1910–1913, led by , Windvane Hill was selected for meteorological observations due to its exposure. An and wind vane were installed on the summit, connected by electric wires to recording instruments inside , allowing continuous monitoring of wind speeds and directions essential for expedition planning and safety. The site's name derives directly from this instrumental setup, as charted by the expedition. The hill also holds a memorial significance from a subsequent expedition. In 1916, survivors of Shackleton's Ross Sea Party, who had taken refuge at Cape Evans, erected a wooden on the rocky summit to honor three members who perished that year: Reverend Arnold Spencer-Smith, , and Victor Hayward. This , a simple structure of local wood, stands as a poignant reminder of the hardships faced by early polar explorers in the region. It is designated as and Monument No. 17 under the for preservation.

South Bay

South Bay is an open coastal indentation located immediately south of Cape Evans on the western shore of , , forming part of the northern entrance to Erebus Bay and adjacent to the vast expanse of the . This bay is characterized by its exposure to the prevailing southerly winds and currents from , resulting in dynamic ice conditions that include extensive fast ice during winter months and frequent disruptions from tide cracks along the shoreline. The bay's fast ice typically forms by early March, creating a relatively stable surface for overland travel, though it is punctuated by pressure ridges, slushy patches, and open water pools that develop due to tidal influences and . The shoreline of South Bay consists of gravelly beaches composed of weathered volcanic materials, including coarse derived from olivine kenyte and agglomerates, interspersed with scattered boulders from nearby glacial moraines. These shores extend southward toward the snout of the Barne Glacier, providing a rugged, ice-free margin that contrasts with the surrounding frozen seascape. The bay's openness, approximately spanning the distance from to features like Little Razorback Islet, makes it wider and more exposed than the neighboring North Bay to its north, contributing to heavier swells from the northeast and northerly directions that render it less suitable for ship compared to more sheltered areas. Historically, during the British (Terra Nova) Expedition of 1910–1913, the bay served as a key route for transporting supplies and equipment, including motor sledges and ponies, across its hard bay to access the via the Southern Road; however, its exposure limited prolonged anchoring, with the expedition ship Terra Nova preferring positions nearer to protected beaches. Seals, particularly Weddell seals, were observed hauling out along the tide cracks and fast edges, occasionally falling prey to loose expedition dogs, which underscores the bay's role in opportunistic seal procurement for food and fuel. Environmentally, South Bay exhibits pronounced interactions with the adjacent , where seasonal polynyas—areas of open water amid the fast —form due to wind-driven divergence and , attracting marine wildlife such as seals and potentially supporting algal blooms beneath the . These polynyas and the bay's proximity to calving events from the Barne lead to periodic influxes of icebergs and brash , heightening the risk of sudden breakouts; for instance, during the unusually warm summer of , the fast in South Bay began fracturing shortly after North Bay, prompting urgent sledging departures to avoid isolation from southern routes. Such dynamics make the bay a challenging yet vital corridor for , with its fast enabling vehicle and sledge access when consolidated, but prone to hazardous cracks and thaws that could sever connections to the interior. Thermometers were deployed here by the to monitor thickening, recording growth from 4 inches in early May pools to over 14 inches by mid-month, reflecting the bay's variable freezing regime influenced by shelf currents.

The Ramp

The Ramp is a prominent geological feature at Cape Evans, consisting of a steep, rubbly slope rising inland from the cape with a 30° incline, approximately 100-150 feet (30-45 meters) high and up to 3,000 feet (900 meters) wide at its base. Partly covered with snow and , it leads to a boulder-strewn area featuring conical mounds formed by the of kenyte lava rocks. This moraine-like structure is supported on the decaying end of a , with significant underlying exposed due to the glacier's rapid retreat, and includes curious cones 8-20 feet high that result from a combination of action and rock . During the British Antarctic Expedition (1910-1913), The Ramp served as a key access route and vantage point when was unsafe for travel, enabling regular evening walks for exercise and meteorological observations, such as reading the thermometer screen known as "Bertram." Expedition members, including Edward Wilson and Henry Bowers, used it for these routine activities despite challenging blowing and drifting conditions, and it provided panoramic views over Cape Evans and . While not explicitly documented for heavy sledge transport, it formed part of the broader terrain for man-hauling and motor sledge movements between sites like Hut Point and Cape Evans once formed in late to early April 1911. In modern times, researchers access Cape Evans via helicopter or tracked vehicles to the adjacent coastal area, utilizing nearby terrain features like The Ramp for safe entry to the while adhering to guidelines. The Ramp's formation involves ongoing glacial decay and seasonal snow accumulation compacted by katabatic winds, renewing its icy surface each winter, though the core structure remains tied to and morainic debris. Hazards include slippery blue patches and loose boulders, making traversal treacherous particularly in low visibility or darkness, with the exposed contributing to potential instability. Although specific crevasses are not noted on The Ramp itself, the surrounding slopes are heavily crevassed, and summer melting exacerbates surface instability across the feature.

Pakaru Icefalls

The Pakaru Icefalls are a series of irregular and fractured glacial ice cascades located on the southwestern shore of , , between Cape Evans and Turks Head, at coordinates 77°38′S 166°39′E. These icefalls form part of the eastern slopes above Cape Evans, where glaciers originating from the flanks of descend toward Erebus Bay, creating a dramatic inland feature amid the volcanic terrain. The name "Pakaru" derives from the Māori language, where it means "broken," aptly describing the tumbled, shattered appearance of the ice masses as they spill over steep gradients. This broken morphology arises from the glaciers' flow over abrupt topographic drops, causing differential movement that generates extensive crevassing—deep fissures formed by tensile stresses as the ice extends and accelerates. , the process of ice loss through and sublimation, intensifies during warmer austral summer periods, further fracturing the structure and enhancing the icefalls' dynamic, chaotic profile. These icefalls serve as a striking scenic backdrop to the Cape Evans region, contributing to the area's rugged volcanic-glacial landscape that has long drawn scientific and exploratory interest. However, their fractured and unstable nature presents potential hazards, including ice avalanches triggered by gravitational instability or seasonal warming, which can pose risks to nearby traverses or research activities in this remote setting.

Tryggve Point

Tryggve Point is a small promontory situated on the southwestern coast of , , projecting into Erebus Bay approximately 1.2 km southeast of Cape Evans and 1.2 km northwest of Turks Head. The feature lies at coordinates 77°39′S 166°42′E and rises to an elevation of about 7 meters above . It forms part of the ice-free volcanic terrain characteristic of the region, first explored during the British National Antarctic Expedition (1901–04) under , though the specific point was charted during the subsequent British Antarctic Expedition (1910–13). The promontory is named after Tryggve Gran (1888–1980), a Norwegian skiing expert recruited for the British Antarctic Expedition of 1910–13, known as the . Gran served as the expedition's primary skiing instructor and participated in the Western Geological Party led by Griffith Taylor, which conducted coastal surveys west of Cape Evans. He later joined the search party that discovered the bodies of Scott and his polar companions in November 1912. Geologically, Tryggve Point exposes a cross-section of ancient volcanic deposits, including over 150 meters of pillow lavas and hyaloclastites overlain by cone materials, indicative of eruptive activity from the Volcanic Province. These rocky outcrops, with minimal vegetation typical of coastal sites, make it a distinct for along the Erebus Bay shoreline, aiding in coastal charting and safe passage for expedition vessels and modern research operations.

Turks Head

Turks Head is a prominent on the southwestern coast of , , situated approximately 5 miles east-southeast of Cape Evans. This feature marks the boundary between the Cape Evans area and South Bay, serving as a key coastal landmark exposed to the open swells of the . Discovered during the National Antarctic Expedition (1901–1904), it was descriptively named for its distinctive profile, which resembles a head swathed in a turban. The headland rises as a precipitous formation to a of 158 meters, characterized by steep cliffs eroded by persistent wind and marine action along the volcanic coastline. Composed primarily of as part of the Erebus Volcanic Province, its rugged morphology exemplifies the erosional processes shaping Ross Island's shoreline. Situated at approximately 77°40'S 166°46'E, Turks Head stands about 5 nautical miles east-southeast of the main Cape Evans promontory, contributing to the irregular topography of the region that includes icefalls and glacial features to its north. Its composition reflects the broader geological history of alkaline in the area, with lavas dating back to the Pleistocene.

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