Pyros Island covers approximately 34 square kilometres and rises 3,847 metres above sea level. Its geology is almost entirely volcanic: basalt substrate beneath a skin of obsidian glass that covers roughly 80 percent of the island's visible surface. The remaining 20 percent — the low shoreline groves and the caldera interior — is the only part where soil has established any foothold.
The ascent route has been walked by Tohu guides for untold generations before the first commercial expeditions began eleven years ago. It runs approximately 14 kilometres one-way and climbs through six distinct terrain zones, each with its own character, its own dangers, and its own toll on the blood.
Ascent Route — Annotated Map
PYROS ISLAND — STANDARD ASCENT ROUTE (14 km one-way)
═══════════════════════════════════════════════════════
╔═══════════════════╗
║ THE CRATER ║ ← MALOA'S BLOOD (the tree)
║ (caldera floor) ║ Descent into crater: ~300 m
╚══════╦════════════╝ Phlogiston-V at maximum density
║
┌──────┴──────────┐
│ THE RIM │ ← Elevation: 3,847 m
│ (Day 5 camp) │ Last water cache here
└──────┬──────────┘ Inês do Carmo waited here
│
╔═════════════════╧═════════════════╗
║ THE SIEVE ║ ← ~1.2 km traverse
║ (valley of fire — full immersion ║ Air boils visually
║ in Phlogiston-V atmosphere) ║ No thin places
╚═════════════════╤═════════════════╝ Day 5 morning
│
┌──────┴──────────┐
│ VENT ZONE │ ← Fumaroles, acid vapor
│ (4th-day peril) │ Random. Unjudging.
└──────┬──────────┘ No warning. No smell.
│
╔═════════════════╧═════════════════╗
║ THE CRUST ║ ← Hollow lava-tube field
║ (thin glass over void — lava ║ The Long Span: 40 steps
║ tubes beneath, no floor) ║ Weight is everything here
╚═════════════════╤═════════════════╝ Day 4 (afternoon)
│
╔═════════════════╧═════════════════╗
║ THE DEEP GLASS ║ ← Nearly vertical
║ (shoulder-high obsidian scythes ║ Navigate sideways
║ — wall with handholds) ║ Day 3 terrain
╚═════════════════╤═════════════════╝
│
╔═════════════════╧═════════════════╗
║ FIRST GLASS FIELD ║ ← First Phlogiston-V layer
║ (waist-high scythes, broken ║ Here the mountain wakes
║ mirrors throwing doubled sun) ║ Day 2 territory
╚═════════════════╤═════════════════╝
│
┌──────┴──────────┐
│ THE LODGE │ ← Last soft place on Pyros
│ (shore base) │ Briefing room, cold drinks
└──────┬──────────┘ Night 1 accommodations
│
┌──────┴──────────┐
│ BLACK ROCK │ ← Sea level, boat landing
│ (the landing) │ Where the Tohu counts the boats
└─────────────────┘ 14 km / 3,847 m to the rim
KEY: Phlogiston-V active zone begins above FIRST GLASS FIELD
Blood oxygen readings drop ~5–6 points per 24 hours above the lodge
Grey lichen grows in glass cracks throughout ALL glass zones
Drone/sensor failure: within 2 hours above the First Glass Field
Formation & Geology
Pyros is a shield volcano of unusual character. The caldera floor sits approximately 300 metres below the rim — a downward crater rather than the more common upward cone — and the caldera walls are near-vertical, smooth obsidian, offering little in the way of natural handholds. The interior of the crater is warm year-round, heated by residual magmatic activity far below.
The island's obsidian surface formed over a series of rapid lava events: flows that hit sea air and cooled almost instantaneously, producing glass rather than stone. When these flows later drained through internal channels, they left hollow tubes beneath the glass ceiling — the structural reality that makes the Crust so dangerous. In the Deep Glass zone, the obsidian fractured on cooling into the standing parallel formations the hunters call scythes, all leaning in the same direction from the prevailing wind at the time of formation.
Below the glass zones, in a band roughly 200 metres wide at the island's base, enough soil and organic matter has accumulated to support plant life. The velu grove grows here — small trees bearing yellow fruit that smells of lemon at first and of something much darker after three days' heat. The Tohu have grown up with velu. The hunters from the company boat often do not recognize it and have been known to bite it, assuming it is one of the lemons in the company's fruit bowl. It is not a lemon. The difference is important on Pyros, where the smell of aged velu is exactly the smell the Phlogiston-V gas is waiting for.
Zone-by-Zone Terrain Guide
The Black Rock — Sea Level Landing
The boat touches Pyros at a shelf of black basalt that juts above the waterline on the island's western face. There is no beach here, no gentle approach — only the rock, the sea, and the Tohu standing above it, already counting. The rock is slick at the waterline, rough higher up, and honeycombed at its base with caves the sea has carved.
This is where the Tohu performs the second count: not how many came, but how many will finish. In thirty years of standing on this rock, no Tohu has needed both hands for that number.
Above the rock, the black sand beach extends north and south for perhaps 400 metres before the glass begins. The sand is fine, dark as coal, and warm underfoot even at first light. The velu grove starts here at the southern end. The Lodge is a 20-minute walk from the landing, on the edge where the sand gives out.
The Lodge & The Green Belt
The Lodge is the last soft place on Pyros. The company maintains it well: cold drinks, woven chairs, a long open room with the sea in every window. The briefing takes place here — the lume assignment, the five-day window, the company man's careful language for the things that are going to try to kill you, and the Tohu's heavier, more honest version of the same.
Above the Lodge, the black sand runs out. Above that, the glass begins. A line of demarcation exists around 180 metres elevation where the Phlogiston-V gas begins to concentrate. You cannot see it. You cannot smell it. The light just begins to behave strangely — a shimmering that is not quite heat shimmer, because it sits still rather than rising.
One tip from the Tohu, worth more than any gear the company sells: learn the smell of velu before you leave the Lodge. There is a bowl of fruit on the company's table. Take the yellow one, bite it, and hold that sourness in memory. Then, on the third day, ask yourself if you can smell something similar but richer, sweeter, turned. If you can, and if you notice it arriving around your own face, stop walking immediately.
The First Glass Field
Elevation: 180 m — 900 m | Day 2 territory
The black sand gives out and the glass begins. The First Glass Field is where the mountain makes its first serious point: the obsidian scythes stand waist-high initially, then shoulder-high in the upper reaches, leaning uniformly in the direction of the original prevailing wind — which is to say, toward you. Each blade is curved, sharp on every edge, and reflective: on a clear morning the field throws the sun back doubled. Climbers emerge from the glass fields with blood from cuts they did not feel while they were bleeding.
The Phlogiston-V gas layer sits above the transition point between Zones 2 and 3 — approximately 220 metres elevation. Once you cross that line, the mountain can taste you. The rule from the Tohu: small breath, through the nose, slow. The mouth is a door. Keep the door small.
Drones fail in Zone 3 within two to three hours. The acid the mountain breathes corrodes filters, sensors, and electronic housings progressively from the moment you enter the gas layer. By the end of the first day on the glass, most electronic equipment is degraded or dead. The exception is the lume — the blood-oxygen reader the company issues — which is sealed in ceramic and built specifically to survive. The mountain eats your eyes. It leaves you your clock.
The Deep Glass
Elevation: 900 m — 2,200 m | Day 3 territory
The slope tilts until it is less a slope than a wall. In the Deep Glass, climbing becomes a sideways affair: the scythes are taller than a person, the gaps between them narrow, and movement through them requires turning the body sidewise and threading it through the blades. The face of every scythe is a mirror. The face of every mirror holds a fragment of your reflection, stretched and slid along beside you. The hunters who have climbed the Deep Glass uniformly report that they stopped looking sideways after the first hour. The mirrors show you something you do not want to see when you are frightened.
The Deep Glass is where the packs come open. A pack that felt manageable at the Lodge is an anchor in Zone 4 — because the blood has been thinning since Zone 3, and thinned blood cannot carry weight the way healthy blood can. Gear gets jettisoned here: spare boots, stoves, folding tools, second coats. The slope behind a climbing party fills slowly with their shed and shining skin.
The scythes in Zone 4 cannot be gripped with gloves. The obsidian edges cut through standard climbing gloves within hours. The Tohu climb barefoot, and the soles of their feet have developed, over generations, a reading capacity that no boot replicates. You will bleed. The question is only how much, and whether your wounds encounter grey lichen before they close.
The Crust
Elevation: 2,200 m — 2,900 m | Day 4 territory
After the vertical effort of the Deep Glass, the Crust arrives like a kindness: a long, gently domed plain of pale obsidian, almost flat, smooth, quiet under the sun. The hunters see it and their shoulders come down. This is a mistake.
The Crust is a roof. Under it, the old lava tubes — where flows once ran and then drained — create hollow channels of unknown depth. The glass over them cooled to a skin: in some places an arm's breadth thick, in others no more than a dinner plate. A single person, light and careful, stepping precisely where the Tohu's feet have said yes — can cross it. A person carrying excess weight, or moving quickly, or stepping wide of the marked print — cannot.
The Crust does not crack when it fails. It turns from floor into air: a section the size of a small room will simply cease to be there, without warning, without sound until the sound of it is already behind you and below you. The Long Span — a 40-step bridge of crust over the widest tube — is the most dangerous single passage on the standard route.
The Crust demands free arms. A climber needs both arms extended, free, and responsive — to throw weight from a failing foot to a good one in the fraction of a second the glass allows. Any object carried in the hands, any pack that restricts arm movement, reduces survival probability on the Long Span to near zero. The Tohu are direct about this. They are not always listened to.
The Vent Zone
Elevation: 2,900 m — 3,400 m | Day 4 afternoon
The Vent Zone is the only part of Pyros that does not judge you. Every other hazard on the mountain is personal: the gas responds to your history, the crust responds to your weight, the glass responds to how carefully you have learned to listen. The vents respond to nothing. They breathe because the furnace below is breathing, on its own schedule, without reference to anything happening on the surface.
Fumaroles and seams open and close across the upper slope. When a vent exhales, the vapor comes down the rock the way water comes down a window — fast, spreading, carrying the concentrated acid breath of the mountain's interior. It smells, before it hits you, almost pleasant: a sharp mineral sweetness. That is the last thing you smell clearly. After that, the eyes close, the chest forgets the rule about slow breathing, and everything is yellow.
The Tohu's protocol for a vent encounter: down immediately, every person's hand on the next person's shoulder, eyes shut, mouth shut, breathe through the shirt fabric, move as a chain toward clean air. Do not let the chain break. If it breaks, the person lost will try to save themselves by moving faster, and moving faster means deeper into the yellow.
The Sieve — Valley of Fire
Elevation: 3,400 m — 3,700 m | Day 5 morning
The Sieve is a long, shallow bowl of obsidian lying just beneath the crater rim — the last ground between the ascent and the prize. It is filled, brim to brim, with Phlogiston-V at its highest and oldest concentration. There are no thin places in the Sieve. The whole valley is awake and tasting.
The air above the Sieve does not shimmer the way hot air shimmers. It boils — slow, silent, visible as a distortion through which the far rim seems to swim like a stone seen through water. A body carrying any metabolic trace of vice walks into this valley and provides the gas with everything it needs. A body that carries none — the clean body, the empty body, the body pointed entirely at something beyond itself — provides the gas with nothing, and the gas parts around it.
There is one documented instance of a climber with a lume reading of 58 — nearly 12 points below the company's safety threshold — crossing the Sieve clean. The Tohu's explanation, offered years later, was not about metabolic chemistry. It was about direction.
The Rim & The Crater
Elevation: 3,847 m (rim) | Day 5 midday
The rim is the end of the ascent and the beginning of the descent into the prize. It is a narrow ring of solid rock around the caldera's edge, with a straight fall on the inner side of approximately 300 metres to the caldera floor. At the rim, for the first time in five days, a climber can look down at Maloa's Blood.
The tree grows on the caldera floor in a tangle of its own black stilt-roots, braced against the black walls on three sides. Its fruit — a dozen or so on a mature tree, each a sphere the size of a sleeping child, armoured in obsidian-glazed plates — hang heavy in the root tangle. In the red light of the crater they throw the light back like struck jewels. The red light of the crater is real: the residual magmatic heat gives the caldera air a warmth and a colour. The effect, for a person arriving at the rim after five days of black and silver, is very difficult to describe without borrowing the word holy.
The descent into the crater takes roughly two hours. The ascent from the crater to the rim, after drinking, takes somewhat less — the fruit goes to work quickly. Camp on the rim, keep water. The descent off the mountain, after the crater visit, runs roughly six to eight hours depending on conditions. Expect the mountain to have changed during your absence. It usually has.
Climate & Storms
Pyros sits in a weather corridor that generates intense storms with limited warning. The company monitors mainland weather stations for storm prediction but has an acknowledged accuracy rate of roughly 60 percent at the island's elevation, where local atmospheric conditions often override regional forecasts.
Rain on Pyros is acid rain — the island's atmospheric chemistry descends with the precipitation, and water that lands on an open wound, a rubbed eye, or a cut palm is not benign. In a full storm, the rain finds every cut the glass has opened over five days and lights them all at once. It is advisable to cover any wound before any weather change.
Lightning on a glass mountain is not like lightning anywhere else. It strikes, and the strike runs — leaps, glass face to glass face — until a whole slope is a single shattering web of white. The thunder is not behind it. It is inside it. Find the deepest overhang available, tie yourself to the rock, and wait. The storms usually resolve in four to six hours. The mountain does not become safer during a storm, but it becomes consistent: it is trying to kill everything, and that is, at least, honest.
The Tohu have lived in the shadow of this caldera for generations longer than written record can reach. Their blood carries approximately 15 percent Denisovan ancestry — a genetic heritage also found in populations throughout Melanesia and associated with adaptation to low-oxygen environments. The company's geneticists have confirmed what the Tohu have always known: they are the island's first children, and the mountain does not drink its own. This is the reason a Tohu guide can climb Pyros barefoot in five days without losing any meaningful blood oxygen, while a sea-level-adapted body loses five to six points per day under the same conditions.