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Gaet'ale Pond
Gaet'ale Pond
Gaet'ale Pond
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Hot spring in the pond

Key Information

Gaet'ale Pond is a small hypersaline lake located near the Dallol crater in the Danakil Depression (Afar Region, Ethiopia). It is located over a hot spring of tectonic origin and has no apparent inlet or outlet streams. The water of Gaet'ale Pond has a salinity of 43%, making it the saltiest water body on Earth.[1]

Location and origin

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Gaet'ale Pond is the largest of a series of small ponds located approximately 4 kilometres (2.5 mi) southeast of Dallol springs. It is crescent-shaped with a diameter of about 60 metres (200 ft).

According to residents of the nearby village of Ahmed'ela, an earthquake in January 2005 reactivated a thermal spring and the pond was created.[2] For this reason, its temperature of 50–55 °C (122–131 °F) is hotter than the environment.[3]

Composition of the water

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The salts in the water of Gaet'ale Pond are mainly composed by calcium chloride at 2.72 mol/kg and magnesium chloride at 1.43 mol/kg. It also contains small amounts of Na+, K+ and NO−
2 ions. The total amount of dissolved solids content is 433 g/kg, or 43.3%. It also contains traces of iron(III) that form a complex with chloride, giving the water a characteristic yellow color.[1]

Bubbles of odourless gas are emitted from the lake surface. It is likely volcanically-produced carbon dioxide. Bird and insect corpses have been found around the pond, and it has been proposed that the gas may be harmful for small animals or humans.[3]

References

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Gaet'ale Pond

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Gaet'ale Pond is a small, hypersaline pond situated in the of northern , recognized as the saltiest on with a (TDS) concentration of 433 g kg⁻¹, primarily composed of (CaCl₂) and (MgCl₂). This crescent-shaped feature, approximately 60 meters in diameter, features yellowish, oily waters due to iron(III) complexes and exhibits bubbling activity from underlying geothermal sources, with surface temperatures ranging from 50 to 55 °C and an extremely acidic of 1.7. Located at coordinates 14°12'47.1" N, 40°19'17.3" E in the , about 4 km southeast of the Dallol hydrothermal area, the pond lies within one of the hottest and driest places on the , at an elevation around 120 meters below in a tectonically active formed by the divergence of three tectonic plates. The Danakil Depression's , characterized by salt flats, volcanic activity, and temperatures often exceeding 50 °C, contributes to the pond's isolation and harsh conditions, where lethal emissions from the site have been observed to kill birds and pose hazards to visitors. The pond emerged as a reactivated thermal spring following a major seismo-volcanic crisis and in 2005, initially manifesting as a that erupted up to 3 meters high for several years before stabilizing into its current form, surrounded by a ledge of (rock salt) and featuring small fountains of bright yellow water amid its reddish-orange hues from iron salts. Its unique chemical profile, including a calcium-to-magnesium ratio of 3.1 and trace elements like , sodium, and nitrates, has drawn scientific interest as a potential analog for habitats and studies, though recent analyses indicate an absence of detectable microbial life; additionally, its oil-like properties have potential applications in , while its status as a growing highlights both its geological significance and the risks associated with the volatile terrain.

Geography and Formation

Location

Gaet'ale Pond is situated at coordinates 14°12′47.1″N 40°19′17.3″E in the of , approximately 4 km southeast of the Dallol crater. The pond lies within the , a vast lowland expanse that ranks among the lowest and hottest inhabited places on , with much of its terrain dropping to around 120 meters below . This region experiences extreme aridity, receiving 100-200 mm of annual , and is marked by persistent volcanic activity due to its position in the northernmost segment of the system. Gaet'ale Pond is adjacent to expansive salt flats, such as the Asale salt flats, and surrounding hydrothermal fields, underscoring its placement in a highly active tectonic where the African, Arabian, and Somali plates diverge. It is located roughly 80 km northwest of the volcano, an active known for its persistent . Access to the pond is challenging owing to its remote desert setting; it can be reached via rugged, unpaved tracks from the town of Berahile, approximately 50 km to the southwest, typically requiring specialized 4x4 vehicles and guided tours due to the harsh environmental conditions and security considerations in the area.

Geological Origin

Gaet'ale Pond is situated within the , part of the Afar Triple Junction, where the Nubian (African), Arabian, and Somali plates diverge, resulting in , rifting, and associated hydrothermal activity. This tectonic regime, initiated around 24 million years ago during the with the separation of Arabia from , forms the northernmost segment of the System and drives ongoing volcanic and seismic processes in the region. The pond originated as a dormant , potentially linked to earlier explosions such as one recorded in near the adjacent Dallol area, but it remained inactive until reactivation during the major seismo-volcanic crisis of 2004–2005. This event involved a magnitude 5.5 earthquake and a 60 km-long magmatic dyke intrusion in the Dabbahu rift segment, approximately 200–250 km south of the site, which propagated stress and fluids northward, triggering hydrothermal resurgence at Gaet'ale. Following reactivation, the feature initially manifested as a approximately 3 meters high, fed by geothermal fluids through fractures in the underlying layers. Over the subsequent 5–10 years, continuous hydrothermal discharge and localized dissolution led to its evolution into a stable hypersaline pond, roughly 70 meters in diameter by the early 2010s, aligned along a northwest-southeast trending fault lineament. This development is underlain by basaltic volcanism from the Afar Traps and Stratoid Series, overlain by a 2 km-thick sequence of evaporites—including , , and —deposited during ancient marine incursions from an isolated arm of the .

Physical Characteristics

Dimensions and Morphology

Gaet'ale Pond measures approximately 70 meters in diameter and forms a small, roughly circular hypersaline pool situated within the . Its water level lies about 1.5 meters below the surrounding salt flat, contributing to its compact scale amid the expansive landscape. The pond's morphology is characterized by terraced edges resulting from salt precipitation, which create step-like ledges and a scalloped perimeter around the water body. These terraces, often covered in a thin layer of up to 10 centimeters thick, give the pond a distinctive, amphitheater-like structure with white-to-yellow crusts encircling the yellowish-orange water surface. The surrounding terrain features a steep descent to the pond's edge, requiring cautious navigation along the slopes. Bubbling occurs on the surface due to subsurface volcanic gases, and the pond has exhibited occasional small activity, including jets up to 3 meters high in the years following its 2005 reactivation. The pond's dimensions have remained relatively stable since its reactivation. High thermal activity in the area promotes patterns that reinforce the terraced morphology.

Thermal and Hydrological Features

Gaet'ale Pond's water temperature is consistently maintained between 50°C and 55°C, primarily due to from underlying hot springs associated with the region's volcanic activity. This thermal regime results from the pond's position over a reactivated hydrothermal system, where subsurface fluids rise under pressure through layers. The pond's hydrology is characterized by exclusive reliance on subsurface hydrothermal inputs, with no observable surface inflows or outflows. Continuous of these mineral-rich fluids sustains the pond's volume against losses from in the hyperarid , where annual rainfall is less than 200 mm and air temperatures frequently exceed 40°C. This balance leads to a stable water level approximately 1.5 m below the surrounding salt flats, occasionally exhibiting minor variations. Bubbling activity, driven by dissolved gases including CO₂ and H₂S, is episodic, as no gas emissions were observed during sampling in January 2018. Evaporation rates are exceptionally high, driven by the low and elevated ambient temperatures of the region, fostering supersaturated conditions in the pond. This process contributes to the formation of terraces that reinforce the pond's edges. Visible bubbling throughout the surface arises from dissolved gases, including CO₂ and H₂S, emanating from the hydrothermal source and causing intermittent jets or fountains that influence local water dynamics. These emissions, often episodic, can lead to slight fluctuations in water levels and pose hazards due to their .

Chemical Composition

Salinity and Acidity

Gaet'ale Pond is hypersaline, with (TDS) measured at 433 g kg⁻¹ (43.3% ) in 2017, establishing it at that time as the saltiest natural water body on Earth, surpassing in (maximum 40.2% ). This was approximately 10 to 12 times the of average (about 3.5%). A more recent 2018 analysis reported higher TDS of 682 g L⁻¹, with inferred from extreme conductivity (> maximum measurable mS cm⁻¹) and dominant content, confirming its continued hypersalinity. The 2017 salinity was confirmed through ion chromatography and inductively coupled plasma optical emission spectrometry (ICP-OES) on water samples. Earlier analyses from around 2011 reported much lower TDS values of 96.4 to 110.4 ppm, indicating significant increases over time, likely due to and hydrothermal inputs. The 2018 study noted challenges in precise quantification due to the brine's and . In terms of acidity, a 2017 measurement reported a pH of 1.7 using a calibrated on fresh samples, but pH measurements in such hypersaline brines are challenging due to effects on electrodes. A 2018 measurement yielded pH 6.2, with lab analysis of diluted samples (1:50) giving pH 3.4, suggesting temporal or methodological variations. Prior 2011 measurements indicated a pH range of 3.5 to 3.95. The pond's elevated temperatures, ranging from 50 to 60 °C, contribute to hypersaline conditions by accelerating evaporation.

Mineral and Elemental Content

The 2017 analysis showed the water dominated by chloride ions (Cl⁻) at 281 g kg⁻¹, with minor nitrate (NO₃⁻) at 3.9 g kg⁻¹ and no detectable sulfate (SO₄²⁻). Major cations were calcium (Ca²⁺) at 109 g kg⁻¹ and magnesium (Mg²⁺) at 34.9 g kg⁻¹, with a Ca:Mg weight ratio of 3.1, highlighting calcium chloride (CaCl₂) and magnesium chloride (MgCl₂). Sodium (Na⁺) and potassium (K⁺) were trace at 1.3 g kg⁻¹ and 2.4 g kg⁻¹, respectively.
IonConcentration (g kg⁻¹, 2017)
Cl⁻281
Ca²⁺109
Mg²⁺34.9
Na⁺1.3
K⁺2.4
NO₃⁻3.9
SO₄²⁻nd
Iron (Fe) was present as Fe(III) complexes, giving a yellow hue, though not quantified. Aluminum (Al) and silica (SiO₂) were not detected. A 2018 study reported higher concentrations in mM: Cl⁻ 12,168; Ca²⁺ 4,048; Mg²⁺ 1,925; Na⁺ 58; ⁺ 40; Br⁻ 95; HCO₃⁻ 4; with SO₄²⁻ not mentioned but consistent with prior absence. The Ca:Mg ratio remained similar (~2.1 molar, ~3.5 weight). No significant trace elements like (As) or lead (Pb) were reported. Precipitation around the margins and upon evaporation forms crusts of calcium and magnesium chlorides, such as sinjarite (CaCl₂·2H₂O) and bischofite (MgCl₂·6H₂O), with possible (KMgCl₃·6H₂O). Needle-shaped bischofite crystals formed during 2017 sample handling, indicating . Chemical analyses used ion chromatography for anions and ICP-OES for cations in 2017, confirming the chloride-rich profile from hydrothermal sources. The 2018 study employed similar methods, noting the brine's extreme properties.

Biological and Ecological Aspects

Absence of Life Forms

Gaet'ale Pond is entirely barren of life, exhibiting no detectable macroscopic organisms such as plants or animals, nor any microscopic life forms including bacteria or archaea. Comprehensive surveys using techniques like 16S rRNA gene metabarcoding, fluorescence-activated cell sorting, and scanning electron microscopy have confirmed this absence, with any detected DNA sequences attributed to airborne contamination rather than active communities. Volcanological assessments in 2016 and subsequent microbiological studies in 2019 and 2023 further validate the pond's sterility across its hypersaline, acidic waters. Measurements indicate variability, with pH ranging from ≈1.7 (2017) to negative values (2023). The lack of biodiversity stems from the pond's polyextreme conditions, where hypersalinity (433 g kg⁻¹ , primarily CaCl₂- and MgCl₂-dominated), hyperacidity ( ≈1.7), and elevated temperatures (50-60°C) combine to exceed the survival thresholds of even the most tolerant extremophiles. These factors create physicochemical barriers, including low (below 0.611) and high chaotropicity (over 87.3 kJ/kg), that disrupt cellular stability and metabolic processes essential for life. Cultivation attempts and ATP measurements have yielded no evidence of viable microbes, underscoring that no known organisms can simultaneously endure this multifaceted stress. The pond is embedded within the hyperarid Asale salt flats of the , a barren expanse of deposits devoid of and supporting minimal faunal activity. While sparse halophytic plants may occur in slightly less extreme peripheral zones of the broader depression, the immediate vicinity around Gaet'ale remains inhospitably sterile, with only occasional dead and birds observed, often due to toxic gas emissions. In contrast to geothermal sites like Yellowstone National Park's acidic hot springs, which harbor diverse acidophilic communities adapted to low and heat, Gaet'ale's additional hypersalinity imposes an insurmountable barrier, preventing microbial colonization despite the presence of single-extreme-tolerant species elsewhere in the Dallol area. This multi-extreme positions Gaet'ale as a rare terrestrial analog for lifeless environments on other .

Toxicity and Environmental Effects

Gaet'ale Pond releases toxic gases primarily consisting of carbon dioxide (CO₂) of volcanic origin, with occasional traces of hydrogen sulfide (H₂S) impurities in the emanating vapors. These emissions, derived from a near-surface magma chamber, accumulate in low-lying areas due to CO₂'s density, creating hazardous pockets that pose risks to nearby wildlife. The lethality of these gases is evidenced by documented deaths of small animals, including birds such as the and insects like locusts, found preserved around the pond due to its hypersaline . At least ten bird carcasses have been observed in the vicinity, attributed directly to CO₂ inhalation, which displaces oxygen and causes asphyxiation. This reinforces the pond's complete sterility, as no life forms can survive the combined gaseous and chemical extremes. Acidic vapors from the pond, linked to its low of approximately 1.7 and (HCl) content in volcanic emissions, contribute to the of surrounding salt flats and rocks, forming terraced structures through chemical . These vapors also generate sulfurous aerosols that disperse locally within the , potentially altering air quality in the immediate area, though the hyper-arid climate restricts broader atmospheric spread. No significant sulfurous odor indicative of dominant H₂S has been reported at the site. Long-term environmental effects remain understudied, but the episodic nature of gas eruptions suggests potential for localized ; however, the region's extreme limits propagation to systems, with no reported contamination of regional aquifers. The pond's reactivation in coincided with a major seismo-volcanic in the Danakil, including over 15 earthquakes exceeding magnitude 5 and a 60-km dyke intrusion, highlighting correlations between seismic activity and increased emissions. Ongoing volcanological monitoring, initiated following the 2005 events, involves periodic assessments of gas emissions and seismic correlations to track potential escalations in activity, with recommendations for simple flame tests to detect CO₂ concentrations in air pockets. These observations underscore the pond's role as a dynamic hydrothermal feature within the rift zone.

Human Significance

History and Discovery

Prior to its reactivation, Gaet'ale Pond was a minor, dormant thermal feature in the Danakil Depression, visible in Landsat satellite imagery from February 6, 2003, but lacking any prior scientific mapping or documentation. Known locally to the Afar people, it was named "Gaet'ale," reflecting its yellowish appearance. The pond emerged prominently in January 2005 following a major seismo-volcanic crisis in the region, triggered by a series of earthquakes reaching magnitudes up to 5.5, alongside dyke intrusions and heightened activity at nearby volcano. This reactivation transformed the dormant spring into an active initially reaching 3 meters in height, which persisted for about three years before subsiding into the current hypersaline pond formation, tied to ongoing . The first scientific documentation occurred during a visit on , 2013, by an international team of geoscientists attending the 24th Colloquium of African Geology, marking the onset of formal studies on its thermal and geological features. Subsequent milestone included a 2016 study detailing the volcanic reactivation and its hazards, providing the initial comprehensive geological timeline. In 2017, a chemical analysis confirmed Gaet'ale as holding the record for the highest natural , advancing understanding of its extreme hydrogeochemistry.

Tourism and Safety Concerns

Gaet'ale Pond has emerged as a notable attraction within the , drawing adventure travelers since its reactivation in 2005, which enhanced its visibility as part of broader volcanic in the region. Its vibrant, otherworldly appearance—characterized by acidic, multicolored waters amid stark salt flats—appeals to those seeking extreme natural phenomena, often included in multi-day tours exploring nearby Dallol crater and hydrothermal features. These expeditions typically originate from in or, less commonly due to border dynamics, from in , emphasizing the pond's integration into rugged, off-the-beaten-path itineraries. Annual visitor numbers to the Danakil area, encompassing Gaet'ale Pond, grew to the thousands pre-2020, fueled by improved access via a new road from to Dallol completed around 2015, though exact figures for the pond itself remain estimates due to its remote location and bundled tour formats. Tourism to the region resumed and expanded after disruptions from the and the Tigray conflict (2020-2022), with Ethiopia's overall revenue increasing 27% to $1.16 billion in 2023; as of 2025, guided tours continue to operate safely in the Danakil. Visiting Gaet'ale Pond presents significant hazards, primarily from toxic emissions that accumulate in low-lying areas around the , leading to asphyxiation risks evidenced by frequent dead birds and insects observed at its shores. The pond's scalding waters, reaching temperatures up to 50°C from its thermal spring origin, pose burn dangers, while the surrounding unstable salt flats and extreme ambient heat—often exceeding 50°C in the —exacerbate dehydration and terrain collapse risks. Reported incidents include respiratory distress from gas exposure among visitors, underscoring the site's hostility despite no widespread fatalities directly attributed to the pond. Safety measures are enforced through mandatory guided tours organized by licensed operators, who provide security escorts and adhere to protocols established under Ethiopia's Ministry of Tourism since the formation of the Ethiopian Tourism Organization in 2013. Recommendations include avoiding the pond's edges to minimize gas accumulation, carrying sufficient and protective gear against , and monitoring for seismic activity that could prompt temporary access restrictions in this volcanically active zone; while gas masks are not universally required, operators advise heightened caution during visits to mitigate inhalation hazards.
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