Rongorongo: Why Deciphering Easter Island’s Script Keeps Failing

On a small island in the far Pacific, a handful of wooden boards still refuses to give up its words. The script is called rongorongo, and for a century and a half people have tried to read it. Some claimed victory, others promised a breakthrough, a few announced full decipherments that later collapsed. Today, the tablets are as eloquent as ever, yet the message remains out of reach. This is not for lack of effort. It is because the conditions needed to crack a script—context, quantity, and comparison—were largely stripped away before scholars arrived.

What follows is the story of how those attempts faltered, and why the tablets keep their silence. Along the way we will look closely at the objects themselves, the reading order, the famous “calendar” passage, the hopeful claims, and the sober reasons they did not hold. It is, in short, a case study in why some scripts yield and others do not.

What rongorongo is (and what it might not be)

Rongorongo survives on a small corpus of wooden objects—mostly tablets, plus a staff, a reimiro chest ornament, and a few other pieces—inscribed with rows of tiny human, animal, plant, and abstract signs. The number of authentic inscriptions is commonly given as about twenty-six, scattered today in museums from Rome to Santiago and Berlin. That is a library so thin that every line matters. The script’s status is debated: some hold it to be true writing for Old Rapanui; others call it a mnemonic device for chants. Either way, it is a sophisticated system with strict order and excellent craftwork.

The carving is precise. Scribes incised the signs with great control and very few mistakes. They wrote in a distinctive pattern called reverse boustrophedon: the first line runs leftward; the next runs rightward with the glyphs turned 180 degrees; then left again, and so on. If you rotate the tablet at the end of each line, the text always reads left-to-right. That pattern is one of the few things everyone agrees on.

Close view of alternating lines on the Santiago staff showing reverse boustrophedon
Detail of the Santiago staff with alternating line orientation, a hallmark of rongorongo layout. Source: Wikimedia Commons

Discovery and loss, almost at the same time

The first outsider to note the inscribed tablets was the missionary Eugène Eyraud in 1864. Within just a few years, Bishop Tepāno Jaussen of Tahiti began collecting the boards as scientific curiosities, spurred by reports that such writing existed on Rapa Nui. During that same decade, the island suffered catastrophic raids by Peruvian slavers and the ravages of introduced disease. Communities were emptied, elders were lost, and with them, knowledge that had passed by memory. By the time the tablets reached museums, context was fractured and the reading tradition—if one still lived—had no safe ground on which to stand.

That is the first failure condition. Decipherment thrives on living memory, bilingual labels, or robust local explanations. Rapa Nui was denied those supports at the critical moment. What remained were remarkable objects, thin documentation, and stories that did not always agree.

The tablets themselves: what they show clearly

Each board is unique, yet several features repeat. Surfaces are planed and sometimes fluted. The signs, often a few millimetres high, sit in regular rows. On tablets such as the Mamari board and the two “Santiago” tablets, the carving is tight and consistent across long passages. Elsewhere, a staff carries lines that wind around the shaft, forcing the carver to adjust spacing and stroke. The visual discipline is striking. It suggests trained hands and standard habits down to the sequence of strokes within a single glyph.

These physical clues prove a system, not a casual scratch. But a system can encode many things: full language, numbers, names and titles, ritual prompts. The challenge is deciding which.

Recto of rongorongo Tablet B with long horizontal lines of glyphs
Recto of Tablet B (Aruku-Kurenga), a key text for sign counts and distribution studies. Source: Wikimedia Commons

How people tried to read them

Jaussen hoped to recover the key by asking an islander in Tahiti, Metoro Tau‘a Ure, to “read” the boards aloud. He dutifully recorded what Metoro chanted. The results—highly variable, often Tahitian rather than Rapanui, and mainly descriptions of what a glyph might depict—have long been judged unreliable for phonetic reading. They look less like text and more like free association or ritual gloss. As a guide to language values, they do not hold. As a glimpse of how someone might talk around the boards in the late nineteenth century, they are fascinating but inconclusive.

Later, scholars turned to comparison. The most influential framework came in 1958 from Thomas Barthel, who catalogued hundreds of sign types and assigned each a code. His sign list remains the reference. Statistical work since then suggests that many of those hundreds are variants and ligatures; counts in the range of a hundred-plus core signs are often cited. That is a plausible inventory for a logo-syllabic system, or for a compact set of mnemonic cues. Unfortunately, counts do not choose between those options on their own.

The famous “calendar”—and its limits

One passage is widely accepted as calendrical: a series on the Mamari tablet that maps a cycle of nights consistent with a lunar month. The sequence aligns with astronomical expectation and with Polynesian calendrical practice. It is the best-grounded match between a rongorongo text and a specific referent. Yet even here, we do not read the words; we identify the structure. The rest of the corpus has not yielded equivalently secure anchors, and without anchors, letters and sounds have nowhere to settle.

Highlighted sequence on the Mamari tablet interpreted as a lunar calendar
The well-known calendrical passage marked on the Mamari tablet, often cited as the strongest structural identification in the corpus. Source: Wikimedia Commons

High hopes and bold claims

Across the twentieth century and into the twenty-first, several researchers announced partial or full solutions. Some saw genealogies and ritual pairings in repetitive strings. Others proposed number words, phonetic complements, even entire reading algorithms. A few monographs attracted press, then met sustained criticism. The pattern is familiar from other undeciphered scripts: enthusiastic pattern-finding followed by sober counter-examples, with no consensus at the end.

What usually goes wrong? Proposals succeed on a few short lines and fail elsewhere. A value that fits here breaks the distribution there. A sign supposed to function as a phonetic element refuses to behave consistently in new contexts. Or the reading requires so much latitude—homophones on demand, wild polysemy, free alternations—that falsification becomes impossible. When a theory can always rescue itself, it has left the terrain of decipherment.

Why attempts keep failing: the nuts and bolts

1) The corpus is too small and too damaged. The surviving texts number only in the twenties. Several are fragmentary or badly worn. For a full phonetic decipherment, that is simply not enough material. Even Linear B needed hundreds of tablets and a lucky structural hunch to give way.

2) There is no bilingual, no long plain-text context. Rosetta-style helps are absent. We do not have a tablet beside a translation, nor a list of month-names beside festival scenes. Without such anchors, values drift.

3) Provenance is patchy. Many boards were collected after the reading tradition was broken, often with scant excavation records. We cannot place most tablets in precise ritual, social, or geographic contexts. Decipherment loves context; rongorongo lost it.

4) The sign inventory is tricky. Barthel’s list tallied ~600 signs, but many are variants. Narrower counts around a hundred-plus core types are plausible. That range could fit a syllabary, or a constrained set of logograms, or a mnemonic system. Statistics alone cannot decide, and mixed systems blur categories further.

5) The subject matter may be specialised. If the boards cue ritual recitations, lists of offerings, or initiatory names, their vocabulary will be narrow and repetitive. That is the worst case for decipherment: few topics, heavy formulae, and many proper names. You can fit multiple readings to such data without contradiction.

6) Late copies confuse the timeline. Radiocarbon dates on some pieces fall in the nineteenth century; at least one tablet has yielded a fifteenth-century date, suggesting deeper roots. A mixed horizon means scribal traditions may have changed—materials, conventions, even purposes—making the small corpus internally uneven.

Reading order and layout: one clear win

Although sound values remain elusive, layout is secure. The reverse boustrophedon format is not guesswork; it is obvious from the carving. So is line order: many tablets begin at a corner with neat margins, and the surface wear supports a standard sequence of handling. Scribal quality is high, with remarkably few corrections. This tells us that scribes followed well-learned patterns and copied with confidence. Unfortunately, perfect penmanship does not equal an alphabet key.

What modern imaging and new dates add

Recent documentation campaigns have produced photogrammetric models and high-resolution images of crucial tablets, improving readings of faint strokes and expanding sign counts on specific pieces. A tranche of radiocarbon tests has also complicated, and possibly enriched, the timeline. Some tablets cluster in the 1800s; at least one piece strongly indicates pre-European centuries. If authenticated across more objects, that suggests a tradition older than missionary contact, even if its late use was already rare or restricted. It supports neither easy “post-contact invention” dismissals nor any quick phonetic mapping. It does, however, justify continued, careful work.

The “why it mattered” question

Even without a reading, the script matters for cultural history. Rapa Nui produced a formal, island-wide system of incised signs used on valuable objects, with disciplined layout and trained scribes. That alone is extraordinary for a small, remote community. Whether the system mapped language line-by-line or cued specialised recitations, it encoded and protected knowledge. It also bound identity to material culture in a way that survived catastrophe. The tablets reached us because people valued them even when their words were fading.

Could a breakthrough still come?

It is not impossible, but any success will almost certainly be partial and incremental. Three paths look promising: first, exhaustive, transparent documentation of every stroke on every authentic object; second, careful statistical modelling that respects scribal variation and tests hypotheses across the whole corpus; third, deepening ethnographic and linguistic work with Rapanui oral traditions and Old Rapanui language, to tighten plausible semantic domains. A dramatic “aha” moment is unlikely. A slow drift from mystery to constrained understanding is not.

How to look at a tablet and see more

Stand before a good photograph and trace the rows with your finger. Watch the line flip and your brain flip with it. Notice how certain signs repeat in clusters, and how others serve as separators. Look for small corrections—rare but telling—that show a scribe catching an error. Then step back and imagine the board in a house or at a ceremony, handled carefully, perhaps chanted in company. That, at least, is something we can say with confidence: these boards were made to be seen and used, not simply hoarded.

Lessons from a failed decipherment

Rongorongo is not a failure; decipherment attempts are. The boards remind us that writing systems are not puzzles made for us. They are tools embedded in particular lives. When violence, disease, and removal smash the surrounding world, the tool may survive but the instructions do not. Scholars inherit beautiful fragments and do the best they can. Sometimes “the best” is an honest admission: here is structure, here are numbers, here is a likely calendar, and beyond that, we will not pretend to more than we know.

Why the tablets still move people

Because they do what portraits do: they place us near another mind. Not with a face this time, but with the evidence of deliberate marks laid in sequence by trained hands. Every line says, this mattered. In a museum case or an online image, you can feel that urgency. Even if the words never come back, the care is legible.

Recto of the Great Santiago tablet with broad, evenly spaced lines
One of the largest tablets, frequently reproduced in nineteenth-century facsimiles and modern studies. Source: Wikimedia Commons

In short

The decipherment of rongorongo has not failed from lack of imagination. It has failed because the tablets reached us almost naked of context, few in number, and cut off from a reading tradition already collapsing under outside pressures. We have a likely lunar passage, clear layout rules, improving documentation, and mixed but intriguing dates. We do not have the bilinguals, the bulk, or the continuity that give other scripts a fighting chance. That is a hard truth, but a useful one. It tells us where to spend our energy: on patient documentation, respectful collaboration with Rapanui knowledge holders, and careful, falsifiable proposals that touch the whole corpus rather than a single tempting line.

Malta’s Cart Ruts: Prehistoric Parallel Grooves That Puzzle Archaeologists

Across Malta and Gozo, pairs of parallel grooves slice the rock as if the islands were scored with a giant’s comb. Locals call them cart ruts. Archaeologists prefer a cooler label, yet the effect is the same. Everywhere the limestone lies bare, you find twin tracks that swoop, split, cross, and sometimes seem to vanish over a cliff. The puzzle is familiar and still unsolved. What made them, when were they cut, and why do so many run together in dense clusters?

The fascination comes from scale as much as mystery. Thousands of metres of ruts survive. Some pairs keep a steady gauge. Others widen or taper. A few dig so deep that you can stand in them up to your knees. One field in the south of Malta is so busy with crossings that a British archaeologist nicknamed it Clapham Junction. He was thinking of a railway yard, packed with tracks, points, and switchbacks. That image stuck because it fits the scene.

What the ruts are, in practical terms

Each rut is a channel cut into the bedrock. The two in a pair run broadly parallel, with spacing that hovers around the width you would expect from a two-wheeled vehicle or a sledge with twin runners. Depth varies from a shallow groove to cuts more than half a metre deep. Profiles differ too. Some ruts have a neat U shape. Others carry a sharper V, especially where the limestone is hard. At junctions the grooves braid and diverge. In places they climb slopes so steep you wonder what load could ever have been hauled there without slipping.

The rock matters. Malta is built from limestones of different character. The soft Globigerina beds weather quickly when wet, while the Coralline units resist wear. That variation helps explain why ruts deepen in one place and barely mark another. It also feeds the debate about formation. If wheels or runners bit into a wet surface, the softer layers would yield first. Over time, repeated journeys might turn a faint track into a channel deep enough to steer the next traveller without effort.

Where to see them

To grasp the pattern, start at Misraħ Għar il-Kbir on the edge of the Dingli cliffs. The field there holds hundreds of intersecting grooves. Some run straight for a surprising distance. Others veer and pivot, as if the route was adjusted mid-journey. The scale makes the point. This was not a casual scratch or a one-off procession. It was a working landscape put to use again and again.

Next, cut across to San Ġwann and the Mensija ruts. Here the grooves weave through a now-urban setting. Seeing them in a neighbourhood makes their persistence real. Builders stepped around them. Paths curved to accommodate them. They are heritage patterns that stubbornly outlasted changing plans.

On Gozo, the Ta’ Ċenċ plateau carries fine examples above sheer cliffs. The openness of that landscape lets you watch the ruts ride the contours and then vanish towards the edge. North-east on Malta, the Xemxija Heritage Trail preserves a Punico-Roman road segment with clear channels underfoot. These are later in date than some prehistoric candidates, but they demonstrate how rock tracks behave when used over time. They also show how later travellers adopted old habits whenever bedrock dictated the route.

How old are they

Dating is the hardest part. Most ruts lack secure archaeological contexts. Many were exposed long after their creation, when soil eroded away. Researchers use indirect clues instead. At a few sites, ruts appear to pass beneath tombs or walls of known date, which sets a latest possible period for their formation. At others, tool marks and finds from nearby features hint at a broad window from the Temple Period through the Bronze Age and beyond.

That wide range may be the real answer. The islands saw long use of the same outcrops. One generation might mark a route lightly. Another, centuries later, could deepen the grooves while repeating the same path. In wet winters the rock softens and tyre-like loads bite more readily. In drier spells the surface hardens and wear slows. The result is a palimpsest, carved and re-carved by people who cared more about moving goods than leaving a tidy pattern for us to decipher.

What made them: the main ideas on the table

Several hypotheses compete, and each has strong points. One camp argues for wheeled carts with a standard axle width. Under heavy loads, and especially when the bedrock was damp, wooden wheels could cut a little deeper each season. Another view prefers sledges on twin runners. Runners loaded with stone would slide better than thick wheels when clay and limestone turned slick. A third suggestion pushes away from transport altogether. On that reading some grooves are deliberate furrows laid out to manage water or to extend thin arable soils across stubborn rock. Others point to quarrying. Chiselled channels could guide blocks from a cut face down towards a waiting track or jetty.

Evidence overlaps. Where wear is smooth and symmetrical, rolling contact remains plausible. Where the contact zone shows sharper tool marks, a sledge or pre-cut guide trough makes more sense. The islands were busy. There is no rule that says a single method must explain every track in every place. What unites the ideas is friction, weight, and repetition. However the movement happened, it happened often enough to bite the stone.

Close view of deep parallel grooves with steady gauge at Misraħ Għar il-Kbir
Cart ruts at Misraħ Għar il-Kbir showing depth and spacing that suggest repeated use. Source: Wikimedia Commons

What the measurements tell us

Systematic surveys have compared widths, depths, and profiles across dozens of sites. The pattern is tighter than first impressions suggest. Many ruts cluster around similar gauges. Depths vary, but the relationship between depth and shape tracks rock type. Where the limestone softens easily, U-shaped channels predominate. Where it resists, sharper V profiles hold. This coherence hints at regular practice. People were not improvising every time they moved a load. They followed established routes and reused widths that matched their equipment.

Calculations based on ground clearance make an elegant point. Imagine a cart with a modest axle and large wooden wheels. On a slippery slope, once the grooves deepened to the height of the axle, the cart would bottom out. The driver would be forced to shift to a new line beside the old one. That behaviour neatly explains the clusters at sites like Clapham Junction. Grooves come in sets because old channels eventually became too deep to use. The result looks like a rail yard because the landscape is full of retirements and replacements.

Why the ruts cross and wander

Crossings seem chaotic until you picture traffic management without engineered roads. In fields and quarry zones people would have wanted options. If one line turned slick, they could switch to a neighbouring path. If a block cracked and needed to be dumped, they would pull to one side. Slight changes in destination compound the effect. Even when routes head broadly the same way, a few degrees of difference at the start produce crossings further on.

The shape of the land matters again. Ridges funnel movement. Shallow basins collect water and become traps. The ruts circumambulate those hazards. Where the ground tilts, tracks climb diagonally to soften the gradient, then swing back. A map of the field becomes a tuition in invisible constraints, written in stone.

Do any run into the sea

Some coastal sites show grooves on the foreshore that now dip into shallow water. Local reports and older notes describe ruts that once ran further across the rock before modern building or erosion took them. It is tempting to link these to lower sea levels in the past or to gradual tilting of the islands. Both ideas have logic. So does a simpler thought. Shorelines move even on human timescales. A few centuries of storm damage and rockfall can alter the edge enough to interrupt tracks that originally stayed dry. Whatever the mechanism, the sight of twin channels disappearing below the waves has fed the popular imagination. It shows how close daily work once ran to water.

What site names reveal

The most famous field sits by a complex of caves known as Għar il-Kbir, “the big cave.” The nickname Clapham Junction is shorthand among guides, but the Maltese name keeps the landscape anchored in its real setting. Elsewhere the toponyms speak about agriculture and quarries. San Ġwann’s Mensija ruts run through a zone of fields and garden walls. The Xemxija road carries pilgrim crosses carved on the rock, reminders that later travellers repurposed earlier infrastructure. On Gozo, Ta’ Ċenċ sits high above the sea, with long views that explain why routes collected there. Names underline habits. People used the same places again and again because the ground told them to.

Cart ruts running through a suburban setting at Mensija
Mensija cart ruts at San Ġwann, with modern streets and walls respecting ancient grooves. Source: Wikimedia Commons

Science at work on an old question

Recent studies have brought geomorphology to bear on the problem. Researchers test how quickly limestone weakens when wet, how loads distribute across narrow wheels or runners, and how slope and surface texture accelerate wear. They model the forces needed to produce observed depths within realistic timeframes. They also compare rut shapes across the islands to see whether the same types recur in different settings. Together these methods move the debate away from arm-waving towards numbers that can be checked.

Alongside this, archaeologists revisit old field notes and photographs. Some early excavations captured ruts partly buried under soil. Those records give a sense of how much erosion has changed the sites since. They also help tie particular grooves to nearby tombs, walls, and tool marks, which nudges the dating a little closer.

Transport, fields, or a bit of both

It may be fruitful to stop asking for a single answer. In a small island landscape, tasks crowd together. Quarrying, hauling, farming, and ritual passages could all mark the same outcrop at different times. A shallow groove used to channel run-off might have made a perfect guide for a sledge once the season turned. A block path cut to move stone might have doubled as a route for the heavy jars and amphorae that supplied a nearby site. When communities reuse the same ground for centuries, boundaries between functions blur.

The best approach is to read each field on its own merits. Does the rut emerge from a quarry face or aim towards one. Do grooves step neatly down a slope with consistent spacing, which suits controlled descent. Are there signs of chisel work within the channels. Do nearby features match a farmed landscape, such as small field systems and water management. Answers will differ site by site, and that is not a weakness. It is how living landscapes behave.

Twin grooves on the Ta’ Ċenċ plateau near the cliff edge
Cart ruts riding the contours on the Ta’ Ċenċ plateau, with a dramatic drop nearby. Source: Wikimedia Commons

Visiting well and reading the ground

The sites are open, windswept, and deceptively delicate. Bedrock shows wear from every modern footstep. Try to keep to obvious paths and avoid walking inside the deeper channels. After rain the rock turns slick and fragile. This is also when the ruts look their clearest, as water pools in the grooves and makes their pattern show. Early light helps. Shadows draw sharp lines that reveal intersections you might miss at midday.

Bring a simple checklist. Watch for a steady gauge between the grooves. Note where one pair widens or narrows. Look at the profile: U or V. Trace the route up and down the slope. Where does it choose to cross a ridge. Where does it dodge a shallow hollow that would hold winter water. In a few minutes you will find yourself reading a path from the point of view of the person who last hauled a load along it. That shift is the gift these sites offer.

Why the ruts matter now

They are not only a curiosity for guidebooks. They are part of a long story of work, habit, and adaptation. The tracks remind us that infrastructure does not always look like a paved road. Sometimes it is a pair of grooves that quietly steer a community’s labour across a rocky slope. They also act as a shared archive. Farmers, quarrymen, carters, and pilgrims left their mark in the same stone. The result is a common text written over centuries in a script that takes patience to learn.

For Malta and Gozo, the ruts form a thread that ties prehistoric settlement to later urban life. They cross parish boundaries and municipal zones without caring about them. They show how the islands’ geology shaped movement, how weather narrowed choices, and how people found efficient routes that we can still trace today. You do not need to agree on a single origin story to feel their importance. Standing in one of the deeper pairs and looking along its line is enough.

Rock-cut grooves on the Punico-Roman road at Xemxija
A Roman-period road segment on the Xemxija Heritage Trail preserves clear grooves from prolonged traffic. Source: Wikimedia Commons

Questions worth taking forward

Several lines of enquiry look promising. First, more fine-grained measurement. Cheap 3D scanning can capture rut profiles and depths at thousands of points, letting researchers compare sites precisely. Second, targeted excavation at the edges of fields where shallow soil still covers the rock. Finds trapped in that layer could fix dates for first use or latest reuse. Third, experimental archaeology that matches local limestone, reconstructed carts or sledges, and controlled loads. Trials on short test beds would show how quickly grooves form under realistic conditions.

There is also room for landscape history. Many tracks now end abruptly at modern walls or roads. Old aerial photographs and nineteenth-century plans can reveal how lines continued before development. In a few cases, geophysical methods might trace ruts where thin colluvium hides them. A joined-up map would help explain why routes favour one pass over another and how sets relate across hillsides.

A measured closing thought

These grooves do not need a single dramatic explanation to be worth our attention. Their power lies in accumulation. Step after step, wheel after wheel, runner after runner, they turned stubborn ground into a guide. The pattern looks chaotic from a distance. Up close it reads like sense, pressed into stone by people who knew exactly what they were doing. That is the part that lingers when you walk away. The island keeps its lines, and the lines keep their stories.