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Tidal wave

A tidal wave is generally a large wave or series of waves in the caused by the gravitational interactions between the , , and Sun, manifesting as the rise and fall of sea levels known as . The term is often misused to describe tsunamis or storm surges, which are unrelated to tidal forces. "Tidal wave" can also refer to various phenomena in entertainment, music, and other contexts, as detailed in later sections of this article.

Oceanography

Definition and characteristics

A tidal wave is a long-period shallow-water wave generated by the gravitational interactions between the , , and Sun, resulting in the periodic rise and fall of water levels commonly referred to as . Unlike other ocean waves driven by wind or seismic activity, tidal waves are predictable and global in scale, driven primarily by the Moon's gravitational pull, which is about twice as strong as the Sun's due to its proximity. These waves propagate as undulations across the ocean basins, with the influencing their patterns through the Coriolis effect. Key characteristics of tidal waves include exceptionally long wavelengths, often spanning thousands of kilometers, and periods ranging from approximately 12 to 24 hours, corresponding to the semidiurnal and diurnal tidal cycles. In the open , their amplitudes are typically low, rarely exceeding 1 meter, but they can amplify significantly in coastal regions due to funneling effects and in enclosed basins. Tidal waves are classified as Kelvin waves in certain contexts, where they propagate along coastlines with minimal transverse motion, or as part of amphidromic systems, where rotating wave patterns circulate around nodes of zero in the ocean. These systems create co-oscillating patterns that explain varying tidal behaviors around the world's coastlines. The physical properties of tidal waves are governed by shallow-water wave dynamics, with propagation speed given by the equation c = \sqrt{gh}, where g is the (approximately 9.8 m/s²) and h is the undisturbed depth. This speed increases with depth, allowing tidal waves to travel across deep at rates up to several hundred kilometers per hour before slowing in shallower coastal zones. in these waves dissipates primarily through bottom in shallow waters and tidal mixing, which influences ocean circulation and nutrient distribution. Representative examples of tidal ranges highlight their variability; in the , , extreme funneling amplifies tides to up to 16 meters between high and low water, driven by with the basin's geometry. Such amplifications underscore the predictable yet locally intense nature of tidal waves, contrasting with their subdued open-ocean expression.

Formation and causes

Tidal waves, more accurately termed tides, arise primarily from the differential gravitational forces exerted by on 's oceans, which deform the ocean surface into two bulges: one on the side facing the celestial body and another on the opposite side due to the arising from the orbital motion of the Earth-Moon and Earth-Sun systems. 's gravitational influence dominates, generating a approximately 2.2 times stronger than 's, despite the Sun's much greater mass, because the Moon is far closer to (about 390 times nearer than the Sun). 's rotation modulates this effect by sweeping locations beneath the bulges twice daily, while the Coriolis effect, resulting from this rotation, deflects tidal currents and contributes to the overall pattern of tidal circulation. The equilibrium tide theory offers a foundational, idealized of these processes, assuming a frictionless, ocean that adjusts instantaneously to the tide-generating without interference from landmasses or rotational dynamics. In this model, the theoretical h at a point on Earth's surface is derived from the perturbing potential and approximated by h \approx \frac{G M r^2}{g d^3} \cdot \frac{3 \cos^2 \theta - 1}{2}, where G is the , M is the mass of the (or Sun for solar tides), d is the distance to the body, r is Earth's , g is , and \theta is the from the point directly beneath the body (the sub-lunar or sub-solar point). This formulation captures the latitudinal variation in tidal forcing, predicting maximum bulges at the and zero at about 54.7° when the body is overhead, though actual heights in the model are small (around 0.5 meters for lunar tides). A more comprehensive framework is provided by the dynamic tide theory, which incorporates the complexities of , irregular geometries, frictional dissipation, and resonant responses to explain observed patterns. Unlike the uniform response in equilibrium theory, dynamic treat oceans as shallow-water systems where energy propagates as forced oscillations, amplified or damped by shapes and boundaries; key features include amphidromic points—central nodes of no vertical motion around which the tidal crest rotates, with cotidal lines emanating outward like spokes on a wheel. This theory accounts for the semidiurnal or diurnal dominance in different regions, driven by the interplay of gravitational forcing and rotational deflection via the Coriolis effect. The relative positions of the Moon and Sun further modulate tidal amplitudes through constructive and destructive interference of their forces. Spring tides occur when the Sun, Moon, and Earth align during new or full moons, aligning the bulges to produce maximum ranges (up to 20% greater than average). Conversely, neap tides arise at first and third quarter moons, when the solar bulge is perpendicular to the lunar one, partially canceling the effect and yielding minimum ranges. These cycles repeat approximately every two weeks, superimposed on the basic gravitational framework.

Global distribution and effects

Tidal patterns exhibit significant global variation, primarily semidiurnal in most ocean basins, characterized by two high and two low tides each lunar day, as observed along the U.S. East Coast and in the Atlantic and Indian Oceans. Diurnal tides, featuring one high and one low tide per day, dominate in the Pacific Ocean margins and the Gulf of Mexico, while mixed semidiurnal-diurnal regimes prevail in transitional zones like the U.S. West Coast. These distributions arise from the interplay of gravitational tidal forces with continental shelves, which amplify ranges in shallow coastal areas, and ocean basin geometries that propagate waves as standing oscillations. Notable extreme tidal ranges occur in specific locations, such as the Bristol Channel in the United Kingdom, where spring tides can exceed 14 meters due to funneling by the narrowing estuary. The Gulf of Mexico maintains predominantly diurnal tides with ranges typically under 1 meter, contrasting with the mixed patterns in the amphidromic systems of the North Sea, where cotidal lines radiate from a central nodal point of near-zero range, leading to progressive increases toward surrounding coasts. Global tidal range maps, derived from satellite altimetry data of the TOPEX/Poseidon mission via models like TPXO, reveal these patterns with high resolution, assimilating altimeter observations to estimate elevations and currents across the world's oceans. Environmentally, facilitate by resuspending and redistributing particles along continental shelves and into deeper waters, shaping morphology. Through vertical mixing, they drive from deeper layers to the surface, enhancing primary productivity and sustaining fisheries in coastal ecosystems, as can boost regional production by up to 15% in some open-ocean areas. However, intense tidal action also accelerates by abrading shorelines and undermining sediments, contributing to habitat loss in vulnerable areas. Human activities are profoundly influenced by these dynamics, with tidal currents reaching speeds of over 5 knots in constricted channels, complicating and requiring precise timing for safe shipping passages. To mitigate such challenges while harnessing tidal energy, infrastructure like the in generates 254 megawatts, the world's largest capacity, by exploiting barrage systems during ebb and flood cycles.

Tidal bores

A is a tidally generated solitary that manifests as a high-velocity front propagating upstream against the river flow, typically forming when the incoming encounters narrowing channels or estuaries with large tidal ranges exceeding 4 meters. This phenomenon acts as an amplified form of coastal tidal , where the tidal surge compresses into a distinct front. The formation mechanics involve the compression of tidal energy within funnel-shaped estuaries, resulting in a that abruptly elevates the water level. Bores develop under conditions of rapid tidal rise and low river outflow, often during spring , and can be undular or breaking depending on the depth ratio across the jump. Wave heights reach up to 10 meters in extreme cases, with propagation speeds of 10-30 km/h, influenced by channel geometry and freshwater . Notable examples include the in the , which attains heights up to 2 meters and travels approximately 50 km upstream along the River Severn at speeds around 16 km/h, drawing spectators during high . The Qiantang River Bore in represents the world's largest, surging up to 9 meters high at speeds exceeding 40 km/h and serving as an annual spectacle that attracts thousands of viewers. In , the along the produces waves up to 4 meters high that propagate as far as 800 km inland, establishing it as a premier destination for extreme surfers seeking prolonged rides. Tidal bores exert ecological influences by generating intense turbulence and , which disrupt fish habitats and patterns in estuarine environments. For instance, the sudden surge can hinder upstream movements of migratory , altering access to spawning grounds despite enhancing overall mixing that benefits . Recreationally, these bores support events, such as those on Alaska's Bore Tide, where waves up to 3 meters high travel at 16-24 km/h, enabling extended rides but posing risks from the powerful front. Historically, 19th-century records document the destructive potential of the in , known as the mascaret, which reached heights of 7.3 meters and caused the loss of over 200 ships between 1789 and 1850 through and collisions.

Internal tides

Internal are oscillations occurring within the ocean's stratified layers, particularly at the interface between water masses of differing densities, in contrast to surface tidal waves. These baroclinic waves have typical wavelengths of 50 to 200 km for low modes and periods that align with tidal cycles, such as the semi-diurnal period of about 12.4 hours for the dominant M2 . They arise from the same barotropic forcing responsible for surface but are enabled by vertical density stratification in the . Internal form when barotropic currents flow over seafloor , including seamounts, mid-ocean ridges, and slopes, thereby converting from the surface into internal modes. This generation process accounts for approximately 1 terawatt of global internal wave energy. Key characteristics include vertical displacements reaching up to 100 meters—far exceeding those of —and propagation primarily as low-mode that can develop into solitary or internal bores over distance. These drive vertical mixing that upwells nutrients from deep waters to the sunlit surface layer, sustaining blooms and thereby influencing the global through enhanced biological productivity and carbon export. Their intense associated currents and shear also present navigational hazards to and structural risks to offshore . Detection of internal tides relies on instruments such as autonomous underwater gliders for profiling density and velocity, and moored acoustic Doppler current profilers for time-series measurements of currents. A prominent generation and study site is the Hawaiian Ridge, where internal tides radiate energy fluxes of around 15 gigawatts and dissipate coherently over distances exceeding 1,000 kilometers.

Distinction from tsunamis

Nature of tsunamis

A is a series of generated by a large and sudden displacement of water in the sea or large lakes, most commonly triggered by underwater earthquakes. These typically feature wavelengths ranging from 100 to 1,000 kilometers in the open and initial propagation speeds exceeding 700 kilometers per hour. Tsunamis are primarily generated by seismic activity in subduction zones, where tectonic plates converge and one is forced beneath another, accounting for approximately 80% of all events. The energy is released through sudden fault slip along the plate boundary, resulting in vertical or horizontal movement of the seafloor that displaces overlying water and initiates wave formation. Other mechanisms include submarine landslides and volcanic eruptions, which contribute to a smaller fraction of tsunamis, around 6% for volcanic sources and less for landslides. In the open ocean, tsunami waves propagate with low amplitudes of 30 to 60 centimeters due to their immense relative to water depth, allowing them to travel efficiently across entire ocean basins. As they approach coastal areas, shoaling effects cause the waves to slow, compress in , and amplify dramatically, often reaching heights exceeding 30 meters through run-up and inundation of shorelines. For instance, the 2011 Tōhoku in , triggered by a magnitude 9.1 subduction zone , produced maximum run-up heights of nearly 40 meters and resulted in over 18,000 deaths. Detection relies on global seismic networks to identify sources and the Deep-ocean Assessment and Reporting of Tsunamis (DART) buoy system, which measures sea-level changes in real time to confirm wave propagation and enable early warnings. In deep , tsunami speed approximates the shallow- wave equation c = \sqrt{gh}, where g is and h is depth, yielding velocities around 700-800 km/h in typical depths of 4 km. Approximately 80% of tsunamis originate along the , a seismically active encircling the basin, with an average of about 10 major events occurring per century. Media often mislabels these seismically driven waves as "tidal waves," despite their unrelated generation.

Historical and cultural misconceptions

The term "" emerged in 19th-century English as a mistranslation of the word "," which literally means "harbor wave," reflecting the dramatic inland flooding that resembled an extreme tide. This linguistic choice arose from early Western observations of tsunami impacts in , where the waves' gradual rise and retreat mimicked tidal movements, leading to widespread adoption of the erroneous label despite tsunamis being unrelated to astronomical . Historical records illustrate this misconception through specific events, such as the 1883 Krakatoa eruption, where the resulting waves—killing over 36,000 people in Java and Sumatra—were commonly described as "tidal waves" in contemporary accounts, obscuring their volcanic seismic origins. Similarly, the 1946 Aleutian Islands earthquake generated a tsunami that devastated Hilo, Hawaii, claiming 165 lives; initial reports and warnings mislabeled it as a "tidal wave," contributing to delayed evacuations and heightened confusion about the threat. These examples highlight how the term perpetuated a false association with predictable tides, hindering effective response. The misconception persisted culturally into the late 20th and early 21st centuries, evident in media coverage of the 2004 tsunami, where many reports interchangeably used "tidal wave" despite the event's trigger, reinforcing public underestimation of its speed and destructiveness. Prior to this disaster, analyses of newspaper and newswire articles from the preceding four years showed predominant use of "tidal wave" over "tsunami," with the 2004 event prompting a gradual lexical shift in toward the accurate term. This ongoing confusion has implications for disaster preparedness, as associating tsunamis with tides can lead individuals to dismiss warnings, assuming the waves align with predictable coastal cycles rather than sudden seismic events. Scientific efforts to rectify this began in the mid-20th century, with agencies like the (NOAA) and the (USGS) actively promoting "" since the 1970s to emphasize its distinct geophysical causes, such as undersea earthquakes. By the 2000s, major dictionaries had updated entries to prioritize "" as the standard term, noting "tidal wave" as a deprecated , which helped standardize scientific communication and public materials. These initiatives underscore the importance of precise terminology in enhancing global awareness and mitigating risks from these unpredictable waves.

Entertainment

Films

Films featuring tidal waves, often within the disaster genre, typically portray massive waves as catastrophic forces overwhelming coastal areas, blending elements of , , and human drama. These productions frequently draw on real-world events for inspiration but dramatize them under the "tidal wave" moniker, emphasizing spectacle over scientific precision. A prominent example is the 2009 South Korean film Haeundae (internationally titled Tidal Wave), directed by , which depicts a fictional striking the area of . The story follows multiple characters, including a and his family, as they navigate personal conflicts amid the impending disaster triggered by undersea earthquakes. Produced with a budget of approximately $10 million, the film utilized extensive (CGI) to simulate the destructive waves and collapsing structures, marking it as 's first major disaster movie. It achieved significant commercial success, selling over 11.4 million tickets in alone, ranking among the country's top-grossing films at the time. Earlier cinematic depictions include the 1933 American film Deluge, directed by Felix E. Feist, which presents a post-apocalyptic scenario where earthquakes along the U.S. coasts culminate in a massive tidal wave submerging New York City. The plot shifts from the initial destruction to the survivors' struggles in a lawless aftermath, with innovative miniature effects used to depict the flooding of Manhattan's skyline. Long considered a lost film, it was rediscovered in the 1980s and is noted for pioneering the disaster genre's focus on urban annihilation. In Japanese cinema, the 1973 tokusatsu disaster film (known internationally as or Tidal Wave), directed by Shirō Moritani and based on Sakyo Komatsu's novel, illustrates tectonic shifts causing tsunamis and volcanic eruptions that threaten to sink the nation. While not strictly a (giant monster) production, it incorporates elements of monstrous natural forces overwhelming and other cities, influencing later genre works. The film grossed approximately ¥4.47 billion in and heightened public discourse on seismic vulnerabilities. Another notable entry is the 1997 American made-for-television movie Tidal Wave: No Escape, directed by , where a series of destructive waves ravage coastal communities, prompting a retired (played by ) to uncover a behind the events. The plot revolves around artificially induced surges rather than natural tides, blending thriller elements with disaster visuals achieved through practical effects and models. Aired on , it exemplifies mid-1990s telemovie trends in sensationalizing environmental threats. These films often conflate —seismic sea waves—with true tidal waves driven by gravitational forces, exaggerating wave heights and behaviors for dramatic effect, such as towering crests that defy real hydrodynamics. For instance, Haeundae amplifies wave scales to immerse audiences in chaos, prioritizing emotional stakes over geophysical accuracy. This misrepresentation persists across the genre, where tidal terminology evokes tidal bores or surges but visually mimics tsunami inundation. Beyond titled works, films inspired by the 2004 Indian Ocean tsunami, such as the 2012 Spanish production The Impossible directed by , have indirectly bolstered tidal wave-themed narratives by humanizing disaster survival. Based on the real experiences of survivor and her family vacationing in , it portrays the waves' raw power through a mix of practical sets and , earning critical acclaim for its intensity and grossing $198 million worldwide. Such stories have contributed to greater tsunami awareness in , prompting discussions on preparedness in regions like and .

Amusement rides

Tidal Wave at in , , , is a prominent example of a water-based amusement ride themed around tidal surges, operating as a Shoot-the-Chutes attraction since its opening on April 7, 2000. Riders board one of three large boats, each accommodating 20 passengers, and ascend a 85-foot (26-meter) chain-lift hill before plummeting down a near-vertical drop into a lagoon, generating a massive splash that soaks participants and onlookers alike. The ride's design simulates the forceful impact of a tidal wave crashing into a themed American fishing village in the Amity Cove area, enhancing the immersive experience with surrounding wreckage and water effects. Sponsored by from 2019 until at least 2024, it remains one of Europe's tallest , drawing crowds especially during summer months when Thorpe Park sees over 1.6 million annual visitors as of 2023. In the United States, similar Tidal Wave rides have featured in various theme parks, emphasizing high-splash drops to evoke ocean wave dynamics. At in , the Tidal Wave Shoot-the-Chutes operated from 1991 to 2018, lifting boats to a height before releasing them into a splash pool that created a dramatic tidal-like surge, with riders experiencing speeds up to 5 mph. This attraction, manufactured by , used gravity-based mechanics rather than powered launches, focusing on the exhilarating freefall and subsequent wave impact for family thrills. Though removed in 2019 to make way for new developments, it exemplified the ride type's popularity in Midwestern parks during its nearly three-decade run. These rides typically employ chain lifts for ascent and rely on for the descent, with boat capacities allowing for throughput of several hundred riders per hour depending on cycle times of 2-3 minutes; for instance, Thorpe Park's setup supports efficient operation during peak seasons. Post-2000s industry-wide incidents on water attractions, such as restraint failures and maintenance lapses reported across global parks, prompted enhanced protocols including automated sensors, reinforced barriers, and regular inspections to prevent ejections or collisions—measures now standard on Shoot-the-Chutes like Tidal Wave to ensure rider security. The conceptual tie to natural tidal phenomena underscores their appeal, blending entertainment with a nod to oceanic forces without replicating hazardous real-world events.

Music

Albums

Several albums titled Tidal Wave or bearing similar names have been released across various genres, often evoking themes of overwhelming emotion or natural force through their musical style and artwork. These releases span from rock to contemporary and , with artists drawing on the metaphor to convey intensity in their soundscapes. The self-titled album Tidal Wave by n rock The Tidal Wave, released in August 1970, captured the group's energetic pop-rock sound during their peak popularity. Featuring tracks like "Spider Spider," "Green Mamba," and the hit "Mango Mango," the LP was produced amid the band's rising fame in , blending garage influences with accessible melodies that resonated locally. The album's raw production reflected the era's vibrant music scene, contributing to the band's , though it remained regionally focused with limited international distribution. In the reggae genre, Jamaican singer Frankie Paul's Tidal Wave, released in 1985 on , showcased his early roots with upbeat rhythms and socially infused lyrics. Key tracks included the title song "Tidal Wave," "Music Is The Staff Of Life," and "Your Love Is Amazing," highlighting Paul's smooth vocals over classic instrumentation. The marked a transitional phase in his career, bridging and emerging , and achieved modest sales primarily in the U.S. and markets. The Nolans' Tidal Wave, a 1991 pop by the Irish-New Zealand vocal group, leaned into and adult contemporary styles, released on 21 September . Produced during a later chapter of the group's career, it featured polished harmonies and radio-friendly hooks, reflecting their evolution from variety show fame to more mature pop outings. The LP received attention in and but did not chart highly, solidifying their niche appeal among fans of nostalgic pop. American rock band Taking Back Sunday's Tidal Wave, their seventh studio released on 16 2016 via , revitalized their roots with diverse tracks blending , , and experimental elements. Recorded during tours following their 2014 release Happiness Is, the 's production emphasized surging guitars and introspective lyrics, peaking at number 36 on the 200. Critics praised its reinvigorated energy and willingness to evolve, calling it one of the band's most varied efforts. More recently, Swedish stoner rock band Tidal Wave's The Lord Knows, released on 20 2023 through Ripple Music, delivered fuzz-heavy riffs and psychedelic grooves across tracks like "" and "Marijuana Trench." Building on their 2019 debut Blueberry Muffin, the album's raw, high-impact production drew influences from classic heavy rock, earning acclaim for its memorable anthems and immersive sound. It underscored the band's growing presence in the underground rock scene, with positive reviews highlighting its riff-driven intensity. American band Our Last Night's Tidal Wave, released on February 28, 2025, is a covers album featuring reinterpreted tracks in their signature style.

Songs

Songs titled "Tidal Wave" span multiple genres, often leveraging the phrase as a for intense emotional or personal upheavals, such as in relationships or inner turmoil. One of the earliest notable examples is the "Tidal Wave" by & His Del-Tones, released in 1964 on the album Summer Surf. This track exemplifies the surf rock subgenre with its fast-paced, reverb-laden guitar riffs that mimic crashing waves, contributing to the genre's cultural association with beach culture. In , All Time Low's "Tidal Waves" (featuring ), from their 2015 album , blends upbeat melodies with lyrics depicting emotional "waves" of regret and reconciliation, running approximately 4:09. The band released "Tidal Wave" in 2016 as the title track of their album Tidal Wave, featuring a Ramones-inspired punk energy with themes of irreversible change and loss. In , almost monday's "tidal wave," issued as a single in 2024, captures summer vibes with light, synth-driven production and lyrics evoking romantic infatuation as an unstoppable force. These tracks highlight the title's versatility, from instrumental evocations of nature to lyrical explorations of human emotion, without delving into album production details beyond basic context.

Other uses

Military operations

was a major low-level aerial bombing operation launched by the (USAAF) on August 1, 1943, targeting the oil refineries around , , to sever a critical component of the ' fuel supply. The mission involved 178 B-24 Liberator heavy bombers departing from bases in , flown at altitudes as low as 50 feet to evade detection and improve bombing accuracy against the sprawling refinery complex, which accounted for about 60% of Nazi Germany's petroleum production. Conceived by Colonel Jacob E. Smart as part of the broader Allied oil campaign, the codename "Tidal Wave" evoked the intended overwhelming, wave-like mass assault on the heavily defended targets. The encountered severe challenges, including navigational errors that led to disorganized attacks and intense anti-aircraft fire from and defenses, resulting in the loss of 54 —approximately 30% of the force—and 310 killed, with over 100 captured as prisoners of . Despite these heavy , the achieved partial success by damaging or destroying key facilities, temporarily reducing Romania's oil output by around 40%, which strained logistics in the short term. In recognition of the mission's valor, all 1,726 participating airmen were awarded the Distinguished Flying Cross, marking one of the largest single distributions of the decoration in USAAF history, while five Medals of Honor were posthumously or directly bestowed for extraordinary heroism. Strategically, Operation Tidal Wave formed a pivotal element of the Allied effort to target Germany's synthetic and natural oil infrastructure, contributing to the cumulative pressure that would later culminate in the near-total collapse of fuel production. Follow-up high-altitude raids on recommenced in April 1944 from newly captured Italian airfields by the US , escalating the campaign and inflicting more sustained damage. Although the refineries were largely rebuilt by late 1943, restoring full capacity, the operation's disruption and the ensuing attacks accelerated the Allies' path to air superiority over by diverting German resources and exposing vulnerabilities in their . The mission's legacy endures as a symbol of bold but costly innovation in aerial warfare, often remembered as "Bloody Sunday" for its disproportionate losses relative to tactical gains. It has been documented in several films, including the 1944 USAAF production Air Siege, which chronicled Fifteenth Air Force operations against Ploiești. These portrayals, alongside veteran accounts, underscore how the operation, while not decisive on its own, informed subsequent precision bombing strategies that proved instrumental in the war's outcome.

Sports and games

In sports, the name "Tidal Wave" is associated with amateur swimming teams in the United States. The Kennesaw Tidal Wave Swim Club, founded in the fall of 1998 at Kennesaw State University with an initial roster of 60 swimmers, competes in regional meets as part of USA Swimming's competitive framework. In video games, "Tidal Wave" refers to a notoriously difficult Extreme Demon level in Geometry Dash, created by OniLink and verified by player Zoink on September 9, 2023, after 49,534 attempts. This 2.1/2.2 update level is renowned for its intense gameplay, including precise wave segment obstacles that demand exceptional timing and control to navigate successfully. The level's verification marked it as one of the hardest challenges in the game's demon community, briefly topping difficulty lists before subsequent ratings. Board and card games occasionally incorporate "Tidal Wave" as a thematic element, such as in expansions for of the Seas, where a (tidal wave) tile introduces dynamic hazards that intensify over rounds, affecting all players and creatures on the board in a 2-8 player survival-style navigation game.

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