Mars’s Alien Obelisk: A Pyramid of the Ancients Unearthed

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While it might be tempting to surmise that the Martian landscape is devoid of significant activity, this ruddy, arid planet teems with intriguing phenomena.

These occurrences are predominantly linked to its geology. Mars is characterized by an abundance of rock formations. Indeed, the sheer volume of rocks that have undergone extensive weathering over millennia on Mars occasionally results in features that, with a degree of imaginative perception, bear a resemblance to man-made or biological constructs.

This phenomenon is akin to the notion of monkeys with typewriters; while the ultimate creation of literary masterpieces like Shakespeare is improbable, we may occasionally encounter geological specimens that so closely mimic organisms that they could momentarily deceive an entomologist.

The geological context in which the feature appears. You can see it at the far right. (NASA/JPL-Caltech/UArizona)

The most recent instance of these captivating Martian visual illusions to capture public attention involved a striking formation, initially identified in 2002, that bears a strong resemblance to a three-sided pyramid situated within a wind-eroded valley known as Candor Chasma.

This discovery rapidly gained traction, with abridged images of the geological anomaly circulating across social media platforms and tabloid publications.

The photographic evidence itself originates from genuine NASA data, acquired by orbital spacecraft that first documented the area in 2001.

The earliest recorded recognition of this pyramidal structure can be traced back to 2002, when independent researcher Wilmer Faust drew attention to an unusual feature he observed in a Mars Global Surveyor (MGS) image, specifically cataloged as E06-00269.

The Mars Global Surveyor image obtained in 2001. (M. C. Malin, K. S. Edgett, S. D. Davis, M. A. Caplinger, E. Jensen, K. D. Supulver, J. Sandoval, L. Posiolova, and R. Zimdar, E06-00269, Malin Space Science Systems Mars Orbiter Camera Image Gallery, 2002)

Subsequent assertions regarding an earlier discovery appear to be temporally inconsistent; however, one aspect that remained consistent was the fascination surrounding the so-called Candor Tetrahedron.

Since its initial observation, other orbital missions have also captured imagery of the locale, most notably the HiRISE camera aboard NASA’s Mars Reconnaissance Orbiter.

The high-resolution imagery provided by HiRISE is remarkable, yet when the wider landscape surrounding the tetrahedron is examined, the formation begins to appear less anomalous and more consistent with its true nature: a moderately irregular mountain sculpted by the same erosional forces that shaped the surrounding canyons.

Candor Chasma ranks among the most expansive canyons on Mars, having been shaped by a confluence of hydrological processes, mass wasting events, aeolian activity, and potentially even tectonic movements over billions of years.

Another view of the geological context, showing nearby features of similar height. This image was taken by the Mars Reconnaissance Orbiter’s HiRISE camera, which acquires colour infrared information along a central strip. (NASA/JPL-Caltech/UArizona)

This canyon system is also dotted with geological formations that scientists have termed “positive relief knobs.” These are essentially subterranean rock structures that have proven more resistant to erosion than the bedrock that once enveloped them; as the surrounding material has been worn away by erosional processes, these resistant knobs have emerged as elevated features.

These knobs are not insubstantial; they can reach diameters of up to a kilometer (3,280 feet) and heights of tens of meters. The Candor Tetrahedron, with a diameter of approximately 290 meters and a height of 145 meters – slightly exceeding the typical knob height – still fits within this broader geological context of layered rock being sculpted into isolated hills.

This Martian formation exhibits parallels with natural pyramidal mountains found on Earth. For instance, Cerro Tusa in Colombia rises 457 meters above its surroundings, with a base spanning 1.8 kilometers. Furthermore, China’s Guizhou province is renowned for its mountainous topography that assumes pyramidal shapes.

A close examination of the image revealing the pyramid indicates that it rests upon a substratum of aeolian ripples – rippled ridges formed by the persistent winds on Mars, suggesting ongoing erosional activity.

It is also observable that the ridges on this mountain are not perfectly geometric, as one might anticipate from an artificial construction, but rather possess an irregular and uneven texture. Moreover, the three discernible sides are not uniform in their dimensions.

The human capacity for pattern recognition is a profound cognitive mechanism; we possess an inherent tendency to seek significance within data that may be inherently devoid of it. We are particularly predisposed to identify features that resemble other humans or facial structures, but geometric configurations and formations can equally capture our attention.

However, Mars does not require the embellishment of pareidolia to be a subject of fascination. Its geological processes and atmospheric dynamics have sculpted landscapes that are both strikingly familiar and profoundly alien to anything observable on Earth.

Moreover, through the advancements in technology such as the Mars Reconnaissance Orbiter, it is possible to meticulously explore these Martian vistas. This enables us to envision ourselves standing amidst the towering cliffs and rugged terrains of Mars, where for eons, only the wind has dared to sound.

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