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Stack (geology)
Stack (geology)
Stack (geology)
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The Twelve Apostles stacks in Victoria, Australia

A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion.[1] Stacks are formed over time by wind and water, processes of coastal geomorphology.[2] They are formed when part of a headland is eroded by hydraulic action, which is the force of the sea or water crashing against the rock. The force of the water weakens cracks in the headland, causing them to later collapse, forming free-standing stacks[3] and even a small island. Without the constant presence of water, stacks also form when a natural arch collapses under gravity, due to sub-aerial processes like wind erosion. Erosion causes the arch to collapse, leaving the pillar of hard rock standing away from the coast—the stack. Eventually, erosion will cause the stack to collapse, leaving a stump. Stacks can provide important nesting locations for seabirds[4], and many are popular for rock climbing, primarily in Ireland[5].

Isolated steep-sided, rocky oceanic islets typically of volcanic origin, are also loosely called "stacks" or "volcanic stacks".

Formation

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Downpatrick Head Dún Briste, County Mayo, Ireland. Clear horizontal bedding is visible, exposing 350 million years of geological history.[6]

Stacks typically form in horizontally bedded sedimentary or volcanic rocks, particularly on limestone cliffs. The medium hardness of these rocks means medium resistance to abrasive and attritive erosion. A more resistant layer may form a capstone. (Cliffs with weaker rock, such as claystone or highly jointed rock, tend to slump and erode too quickly to form stacks, while harder rocks such as granite erode in different ways.)[7]

The formation process usually begins when the sea attacks lines of weakness, such as steep joints or small fault zones in a cliff face. These cracks then gradually get larger and turn into caves. If a cave wears through a headland, an arch forms. Further erosion causes the arch to collapse, leaving the pillar of hard rock standing away from the coast, the stack. Eventually, erosion will cause the stack to collapse, leaving a stump. This stump usually forms a small rock island, low enough for a high tide to submerge.

See also

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References

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Stack (geology)

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A stack, also known as a sea stack, is a coastal geological characterized by a steep, often vertical column or pillar of rock standing in the sea near a shoreline, formed through the action of ocean waves on headlands or cliffs. These structures typically consist of resistant rock types, such as or , that withstand prolonged wave impact while surrounding softer materials erode away. The formation of a sea stack begins with wave erosion carving sea caves into the base of cliffs or s, exploiting weaknesses in the rock. Over time, continued from both sides of a can connect caves to form a sea arch, a bridge-like structure spanning the erosional gap. When the roof of the arch collapses due to further wave undercutting and gravitational forces, it leaves behind an isolated pillar known as a stack, which may continue to erode at its base until it too succumbs. This process is most prominent on rocky coastlines with high wave energy, such as those influenced by prevailing winds and , and can take thousands of years to fully develop. Notable examples of sea stacks include in , a 235-foot (72-meter) rising from the , formed by ancient lava flows from along the route of the . Another iconic site is the Twelve Apostles along the in Victoria, Australia, where only seven of the original stacks remain due to ongoing , highlighting the dynamic nature of these features. In , Washington, sea stacks of the Hoh Rock Assemblage—composed of uplifted submarine basalts—record ancient shorelines and serve as habitats for marine life while demonstrating tectonic and erosional interactions. These formations not only illustrate coastal geomorphology but also contribute to by providing nesting sites for seabirds and protective zones for intertidal ecosystems.

Definition and Characteristics

Definition

A stack, or sea stack, is a geological landform consisting of a steep and often vertical column or columns of rock isolated in the near a , formed through the erosive action of waves on rocky shorelines. These formations typically range from 10 to 50 meters in height, though variations occur depending on local rock resistance and wave . Stacks primarily develop on erosional coasts, where marine processes such as wave attack and target headlands and cliffs composed of resistant rock types like or . This distinguishes them from depositional coastal features, such as spits or barriers, which form through accumulation rather than material removal. The term "stack" reflects the piled, columnar appearance of these isolated rock pillars, evoking a structure built upward from the . Stacks represent the endpoint of progressive sequences, often succeeding features like sea arches before further degradation into stumps.

Physical Characteristics

Sea stacks exhibit a distinctive pillar-like or cylindrical morphology, characterized by steep, often vertical sides that rise abruptly from the surrounding or wave-cut platforms. These structures typically feature flat or rounded tops, with heights ranging from a few meters to over 100 meters, such as the 137-meter-tall in or the 191-meter Stac an Armin in St Kilda. Diameters generally span 5 to 70 meters, with widths averaging around 46 meters in examples like the Twelve Apostles in , and they stand isolated from the mainland by 100 meters or more, surrounded by deeper water or eroded platforms. A key morphological element is the occasional presence of a capstone—a more resistant rock layer, such as coralline algal boundstone or harder sedimentary strata, that overhangs the softer underlying material and shields the top from further by wave action. This differential resistance contributes to the stack's overall form, often resulting in overhanging or bulbous upper sections. Stacks are commonly composed of layered sedimentary or volcanic rocks, where visible stratification highlights planes that influence their shape and patterns. Surface features reflect intense marine abrasion, including fluting—parallel grooves carved by wave-driven —and potholes formed by swirling pebbles trapped in depressions. Undercutting at the base is prevalent, where persistent wave attack hollows out the lower portions, creating unstable overhangs. These elements underscore the stacks' exposure to constant erosional forces originating from wave action on coastal headlands. Stability is inherently precarious due to ongoing base , which widens undercuts and promotes toppling; stacks typically persist for thousands to tens of thousands of years before collapsing into low stumps, as evidenced by submerged examples preserved over multiple eustatic cycles spanning 60,000 to 27,000 years ago. Erosion rates average 0.22 meters per year, with documented collapses accelerating this process in high-energy environments.

Formation Processes

Erosional Mechanisms

The formation of stacks in coastal geology is primarily driven by marine erosional processes that exploit weaknesses in rocky headlands, particularly through the action of waves and associated forces. These mechanisms include , where waves compress air trapped in rock cracks, causing explosive expansion that widens fissures and dislodges material; abrasion, in which sediment-laden waves scour the rock surface like sandpaper; attrition, the breakdown of rock fragments colliding in the into smaller, rounded particles; and , a chemical process where dissolves soluble minerals, notably in formations through reactions with dissolved . Wave plays a central role in accelerating these processes, with higher during stormy conditions intensifying by delivering more forceful impacts on exposed headlands. Factors such as fetch—the over which blows to generate waves—and tidal ranges determine the and intensity of wave attack, allowing to target specific zones like the intertidal area where is concentrated. Rock resistance significantly influences the rate and pattern of stack development, with lithologies of varying resistance, such as hard and weak , eroding preferentially along structural weaknesses such as joints and planes, where physical and chemical forces penetrate more easily. In stratified sequences, softer underlying layers often experience accelerated undercutting by abrasion and , leaving overlying harder caps more vulnerable to eventual collapse. On exposed coasts, these mechanisms result in erosion rates typically ranging from 0.1 to 1 meter per year, though values vary with rock type—hard rocks erode at medians of about 0.029 m/year, medium at 0.1 m/year, and weaker at 0.23 m/year. Wave heights up to 10 meters can generate impact pressures exceeding 100 kPa, further enhancing and abrasion in high-energy settings.

Developmental Stages

The development of a sea stack begins with the initial formation of coastal cliffs and headlands, primarily through weathering processes such as freeze-thaw cycles and chemical dissolution that weaken the rock structure, followed by marine undercutting where waves erode the base to create wave-cut notches. This stage establishes the foundational steep escarpments along rocky coastlines, often in areas of resistant rock like or , setting the scene for further marine erosion. In the subsequent stage, persistent wave action exploits geological weaknesses such as joints and bedding planes in the cliff face, leading to backwall that enlarges initial notches into sea caves; this unfolds over hundreds to thousands of years, depending on rock hardness and wave energy. and abrasion dominate here, gradually expanding the caves inland from the shoreline. As erosion continues, sea caves from opposing sides of a may coalesce, forming a sea arch with a thinning roof that eventually collapses under its own weight, isolating a detached pillar of rock and marking the transition to stack formation; this arch development and collapse phase occurs over thousands of years. The resulting isolated column stands as the nascent sea stack, separated from the mainland. The final maturation stage involves the continued isolation and of the stack, with waves undercutting its base and potentially causing it to topple into a low stump over time; the complete lifecycle from cliff to stump spans thousands to tens of thousands of years in many settings. Throughout all stages, factors such as post-glacial sea-level rise, which has exposed more rock to wave attack since around 14,000 to 11,000 years ago, and tectonic uplift, which can elevate landforms and reset cycles, significantly influence the pace and progression.

Variations and Examples

Types of Stacks

The most common type of stack is the sea stack, formed primarily from cliffs such as or along discordant coastlines where wave action exploits weaknesses in horizontally bedded strata. These stacks typically emerge through the erosional progression from caves to arches and eventual collapse, leaving isolated pillars that resist further breakdown due to their medium hardness. Volcanic stacks, in contrast, arise from igneous rocks like or solidified lava flows, exhibiting greater resistance to and often a more cylindrical shape compared to their sedimentary counterparts. These formations are prevalent in regions of volcanic activity, such as island arcs, where submarine platforms support emergent structures shaped by wave abrasion on hard, durable materials. Inland or river stacks represent rarer erosional remnants in non-marine environments, analogous to coastal stacks but distinct in their formation by fluvial currents, , and differential rather than marine waves. Examples include hoodoos in arid canyon settings, where softer underlying sediments are sculpted beneath protective harder caps, creating tall, irregular spires. Stacks vary significantly in size, with giant forms exceeding 50 meters in height—such as at 562 meters—proving stable over millennia due to robust composition, while dwarf stacks under 10 meters often persist only briefly before succumbing to ongoing . Capped stacks feature overhangs of resistant that shield bases from accelerated breakdown, enhancing longevity, whereas uncapped variants erode more uniformly and rapidly. Globally, stacks predominate along temperate to high-latitude coastlines characterized by strong wave regimes and rocky substrates, as seen in distributions across , , and . They are largely absent from low-energy tropical depositional shores, where coral reefs and sediment accumulation inhibit the intense erosion required for their development.

Notable Examples

The Twelve Apostles are a collection of limestone sea stacks located off the coast of Port Campbell in Victoria, , formed through the of Miocene Port Campbell Limestone cliffs by the relentless waves of the . Named the Twelve Apostles despite originally consisting of nine prominent formations, only seven stacks remain standing today due to ongoing wave undercutting and collapse, with the tallest reaching approximately 45 meters in height. These structures illustrate the rapid erosional processes that shape coastal geology, as the soft has been sculpted over the past 10 to 20 million years since the initial deposition of the sedimentary layers during the epoch. The , a dramatic stack on the island of Hoy in Scotland's archipelago, stands at 137 meters tall and exemplifies joint-controlled erosion in formations of age. This isolated pillar emerged from the erosion of a larger cliff face through and wave abrasion, with the current stack likely forming within the last few hundred years following the collapse of connecting arches, though the underlying rock dates back approximately 370 million years. Its vertical joints, a result of tectonic stresses, have facilitated preferential , highlighting how structural weaknesses accelerate stack development in resistant yet fractured lithologies; the stack gained fame after its by climbers in 1966. Dún Briste, known as the "Broken Fort," is a prominent sea stack off Downpatrick Head on Ireland's Mayo coast, rising about 20 meters above the Atlantic and composed of layered limestones that expose roughly 350 million years of geological history from the Lower period onward. The stack originated as part of a larger cliff that was isolated by marine erosion, with a connecting sea arch dramatically collapsing during a storm in 1393, leaving the remnant pillar as a testament to episodic coastal retreat in sedimentary sequences spanning to more recent deposits. Its horizontal bedding and visible stratification underscore the role of differential erosion in revealing stratigraphic records within stack formations. In contrast to sedimentary examples, the sea stacks near Kalaupapa on Moloka'i, , demonstrate volcanic origins, carved from cliffs of the Kalaupapa Basalt formation, which erupted during the approximately 300,000 to 600,000 years ago to build the peninsula's foundation. These stacks have formed relatively rapidly over the past 10,000 years through intense wave action amplified by , eroding the resistant yet jointed basaltic lava flows into isolated pillars that highlight accelerated coastal sculpting in tropical volcanic settings. The basalt's , a product of cooling lava, promotes faster isolation of stacks compared to softer lithologies elsewhere. Many notable sea stacks worldwide face heightened threats from climate-driven sea-level rise, which exacerbates wave energy at their bases and accelerates and collapse rates; for example, two stacks at the Twelve Apostles collapsed in 2005 and 2009.

Significance and Impacts

Ecological Role

Sea stacks play a crucial role in supporting coastal by providing isolated nesting habitats for seabirds, where vertical rock faces offer protection from terrestrial predators. These structures are particularly vital for species such as Atlantic puffins (Fratercula arctica), which burrow into the soft soil or crevices on stack summits and slopes, and northern gannets (Morus bassanus), which build nests on ledges, often hosting colonies of thousands of pairs. Examples include the sea stacks off Coquille Point in , which support nesting populations of pelagic cormorants (Phalacrocorax pelagicus), common murres (Uria aalge), and tufted puffins (Fratercula cirrhata), among several other species. This isolation enhances reproductive success, with stacks serving as refugia that can sustain multiple seabird species in temperate regions. At their bases, sea stacks create dynamic intertidal zones that harbor diverse marine communities, including , (Balanus spp.), and small like gobies and blennies, which thrive in the nutrient-rich, wave-sheltered pools. These areas function as natural fish aggregation points, drawing predatory such as (Sebastes spp.) and enhancing local food webs that support both marine and avian populations. The rocky substrates promote attachment for sessile organisms, fostering productivity that extends to surrounding coastal waters. The isolated configuration of sea stacks contributes to their status as biodiversity hotspots, where limited accessibility encourages among lichens, mosses, and . For instance, in California's coastal regions, stacks host unique communities, including rare adapted to saline spray, while supporting specialized like endemic snails and spiders that exploit microhabitats unavailable elsewhere. Protected areas, such as Flattery Rocks National Wildlife Refuge, amplify this role by preserving these communities from human disturbance, allowing for the development of distinct ecological niches. Sea stacks also enhance by acting as natural breakwaters, dissipating wave energy and reducing on adjacent shorelines by absorbing and refracting incoming swells. In formations, ongoing dissolution processes sequester carbon through the reaction of with and dissolved CO2, forming ions that are exported to the , contributing to long-term storage. This geochemical cycling, combined with biological productivity on stack surfaces, bolsters overall coastal carbon dynamics. However, accelerating and sea-level rise pose significant threats to stack ecosystems, potentially reducing available s through undercutting and . Projections indicate up to 50% habitat loss in some vulnerable rocky coastal areas by 2100 under high sea-level rise scenarios (0.3-1.9 m), driven by intensified wave action and inundation, which could displace colonies and intertidal communities.

Human Interactions

Sea stacks attract significant human interest through tourism and recreational activities, particularly viewing and . Iconic formations like the Twelve Apostles in Australia's draw approximately 2.6 million visitors annually, many participating in boat tours that offer close-up perspectives of the stacks against the ocean backdrop. Similarly, the in Scotland's Islands serves as a premier climbing destination, with its original route graded at HVS to E1 (equivalent to 5.9–5.10 in Yosemite Decimal System), featuring pitches that challenge climbers with strenuous cracks and exposed traverses up to 137 meters high. These activities contribute substantially to local economies; for instance, tourism along Australia's , encompassing the Twelve Apostles, generates about $1.9 billion annually, supporting thousands of jobs in hospitality and guiding services. Scientists utilize sea stacks to investigate coastal evolution and environmental changes. Techniques such as cosmogenic nuclide dating on stack surfaces help determine long-term rates and relative sea-level variations over millennial timescales, revealing limited variability in rock coast retreat despite fluctuating sea levels. , involving analysis of fossil assemblages in stack-adjacent sediments, aids in reconstructing paleoenvironments and sea-level histories during the Pleistocene. Additionally, surveys enable precise monitoring of stack dynamics, informing models of future sea-level rise impacts on rocky coastlines. Sea stacks hold cultural significance in and are often protected as heritage sites. In Ireland, Dún Briste near Head is tied to legends of battling the devil, who was cast into the , leaving the isolated stack as a remnant of the clash. The in , featuring columnar formations, is enshrined as a for its geological and cultural value, inspiring myths of the giant Finn McCool building a causeway to . Human engagement with sea stacks involves notable risks and requires management strategies. Climbing poses hazards such as unstable rock leading to falls and , compounded by slippery, wave-washed surfaces and the potential for if climbers are swept into the sea during high tides or storms. Conservation efforts include seasonal access bans to protect nesting seabirds, as seen in areas like Islands National Wildlife Refuge, where human approach to stacks is prohibited year-round to minimize disturbance during breeding periods. To counter climate-driven , artificial reefs are deployed offshore to dissipate wave energy, reducing coastal retreat rates by up to 90% in modeled scenarios and preserving stack integrity. Historical events underscore the instability of these formations. In 1990, the London Arch (formerly ) in Australia's partially collapsed without warning, stranding two tourists on the isolated outer section until their rescue by helicopter, highlighting the sudden risks to visitors near such features.

References

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