Agricultural worlds consume minerals—phosphorus, potassium, calcium, magnesium, sulphur, iron and trace elements—and at planetary scale those materials become strategic bulk commodities.
A productive world may possess ideal climate, abundant water and mature agricultural infrastructure while lacking the geological reserves required to sustain industrial biomass production indefinitely.
Elsewhere, entire planets contain those reserves and possess no meaningful agricultural value.
The Lithovore™ exists to correct that allocation, joining the mineral wealth of one world to the biological potential of another.
Developed by IFA Science & Technology, The Lithovore is a planetary-scale orbital mining station designed to convert the geological mass of non-productive worlds into mineral feedstock for interplanetary agriculture.
The station establishes orbit around a selected planetary body and begins a continuous extraction cycle. Its primary excavation array removes geological material directly from the surface. Orbital capture systems intercept the liberated mass and transfer it into the station’s processing complex, where useful mineral fractions are separated, concentrated and prepared for bulk transport.
It mines the planet from orbit.
THE RIGHT MATERIAL ON THE WRONG WORLD
Planetary formation places useful material independently of agricultural demand.
It nevertheless produces precisely the right material in places incapable of turning it into agricultural value.
A viable agricultural world may contain insufficient accessible phosphorus.
A barren moon may contain enormous phosphate-bearing formations.
A productive world may require potassium while an uninhabitable planet contains potassium-bearing minerals across entire geological provinces.
One possesses the productive environment but an incomplete mineral inventory.
The other possesses the missing inventory but no meaningful agricultural future.
The Lithovore connects them.
IFA Science & Technology therefore stopped treating each agricultural planet as a closed geological system.
Mineral availability became an interplanetary problem.
The relevant resource base is no longer the geology beneath the field.
It is the geology of every economically accessible world around it.
THE STATION
The Lithovore is mobile orbital infrastructure built around continuous planetary extraction.
The station is built around several integrated systems:
- Primary excavation array
- Orbital mass-capture systems
- Bulk-material handling infrastructure
- Mineral fractionation and refining complexes
- High-volume storage
- Power generation and thermal management
- Geological and orbital observation systems
- Interplanetary export infrastructure
These systems operate concurrently.
While one region of the target is being excavated, previously captured material is already being processed. Refined mineral streams enter storage while earlier production is transferred into bulk transport.
The Lithovore is therefore designed around continuous mass flow rather than individual mining operations.
Rock enters the system and agricultural feedstock leaves it; everything between those states occurs in orbit.
TARGET ACQUISITION
Before The Lithovore arrives, IFA survey teams determine whether a planetary body justifies deployment.
Orbital spectroscopy, gravimetric analysis, geological modelling and exploratory surveys establish the composition and distribution of useful material.
IFA purchases deep-survey archives and depleted-claim data from Shubin Interstellar, whose long history of turning terraforming assets into mining infrastructure offers a catalogue of worlds already judged by commercial geology. Argo Astronautics supplies the orbital mass-handling architecture, while the fracture-control assemblies license rugged mining interfaces from Greycat Industrial. IFA retains control of target selection, extraction policy and every tonne that leaves the gravity well.
The initial assessment concentrates on resources required by large-scale biological production:
- Phosphorus-bearing material
- Potassium-bearing minerals
- Calcium
- Magnesium
- Sulphur
- Iron
- Trace elements
- Water-bearing minerals and volatiles, where present
- Industrial materials useful to the wider agricultural supply chain
Individual deposits are only the beginning of the calculation. The target itself is evaluated as an inventory: the crust and accessible deeper geology each have a composition, and every layer of mass carries a different processing cost.
The decisive question is how much of the world is worth processing.
THE MINING ARRAY
The defining component of The Lithovore is its primary excavation array.
Its operating principle begins with technology already familiar throughout the mining industry: analyse the target, establish its composition and structural response, then apply controlled laser energy until the material fractures.
The Lithovore scales that principle from an individual deposit to a continuously surveyed planetary extraction front.
High-energy analytical probes map useful material beneath the surface and return composition, depth, resistance and instability data to the station. The excavation array uses that model to select its beam geometry, point of incidence and energy profile.
Multiple emitter groups act as a coordinated mining head. Their output is concentrated on a defined working zone rather than dispersed across the landscape.
Energy delivery is increased until the target material enters a controlled fracture state. The objective is the same as conventional mining: exceed the resistance of the material without surrendering the operation to uncontrolled overcharge.
At Lithovore scale, that working window is maintained by continuous geological sensing, beam modulation and repositioning of the active array.
As geological data changes, the active zone moves with it. High-value formations are opened first, after which overburden is removed and adjacent strata become accessible. Extraction advances without constructing a conventional mine across the surface or forcing a planetary fleet to lift every load through the gravity well. The mine remains in orbit; only its working front touches the world.
FRACTURE AND EXTRACTION
In established Star Citizen mining practice, documented in CIG's Mining Basics and Design Notes: Mining, fracture and extraction are separate operating modes.
The fracture beam transfers energy into a surveyed target. Material resistance determines the power required to begin the process; instability determines how carefully that energy must be controlled. A productive fracture holds the target inside its operating window until structural failure is complete.
The Lithovore performs the same calculation across an extraction front measured in geological formations.
Once fractured material separates from the surface, the station changes from fracture control to mass recovery. Extraction arrays establish controlled ascent corridors through the debris plume and draw selected material towards orbital capture infrastructure.
Composition data remains attached to the operation. Recoverable fragments are routed according to mineral content, mass and trajectory; low-value material is rejected before it consumes primary processing capacity.
Large fragments are reduced again where required. Fine material is consolidated into stable transfer streams. Every recovered fraction then enters the station’s bulk-material network for characterisation and separation.
The same mining principle is carried to planetary scale: where a conventional mining ship fractures a rock and extracts its valuable contents, the Lithovore works across entire formations and recovers the fractions agriculture can use.
THE EXTRACTION FRONT
Early Lithovore operations resemble extremely selective mining.
The richest and most accessible geological regions are processed first.
As the station becomes established, the economics of the target change.
By then the power, capture and processing infrastructure is already in orbit, and bulk export has begun.
Material that would not independently justify construction of a mining operation may become economically viable simply because The Lithovore is already there.
The extraction front therefore expands from high-grade deposits into lower-grade formations and eventually into bulk crust. Mountain systems are reduced, basins excavated and surface strata removed across areas visible from orbit.
Eventually the distinction between a deposit and its surrounding geology becomes economically unimportant.
The mine expands until the target itself becomes the mine.
ORBITAL FRACTIONATION
Planetary crust enters the station as mixed geological mass.
Captured material contains both agriculturally useful minerals and bulk material with no immediate agricultural application. The Lithovore separates it. Incoming mass is characterised, reduced where necessary and directed through processing systems appropriate to its composition. Useful mineral fractions are progressively concentrated. Phosphorus-bearing material enters one processing stream. Potassium-bearing material another. Calcium, magnesium, sulphur, iron and useful trace elements are separated according to downstream requirements. Industrial metals and other valuable materials can be diverted into secondary production streams. Volatiles can be recovered where useful. Material with insufficient value is removed from the primary agricultural chain. The world enters The Lithovore as geology. It leaves as inventory.
MINERAL CONCENTRATES
The Lithovore converts captured geology into separated mineral inventory.
Primary processing divides the incoming mass into useful mineral fractions and concentrates them for storage.
Phosphorus-bearing material, potassium-bearing minerals, calcium, magnesium, sulphur, iron and trace-element streams move into dedicated orbital inventories.
Bulk transports carry those concentrates from the extraction world to agricultural worlds across the production network.
Bulk transports carry those concentrates outward, allowing a single extraction world to become the geological reserve of several agricultural planets at once.
CONTINUOUS MASS FLOW
The Lithovore is designed around throughput.
Excavation, processing, storage and export operate concurrently. Captured material moves through the station while new mass rises from below, and orbital inventories feed outbound transports without waiting for the extraction front to stop.
The complete chain operates simultaneously:
PLANETARY MASS → ORBITAL EXCAVATION → CAPTURE → FRACTIONATION → STORAGE → BULK EXPORT
The scale of the installation makes interruption undesirable.
Once a viable extraction campaign has begun, The Lithovore is intended to maintain industrial flow for as long as the target remains economically productive.
The continuous movement of planetary mass through the station defines the machine.
INTERPLANETARY MINERAL SUPPLY
The Lithovore separates agricultural production from the geology of the world that supports it.
A farming world can draw upon mineral reserves located elsewhere in its production network.
Mineral concentrates arriving from Lithovore operations enter local agricultural supply inventories.
IFA can therefore select agricultural worlds primarily for the characteristics that matter to cultivation: climate, water availability, surface conditions, location, established infrastructure and suitability for Agriform™.
The geology required to sustain production can therefore come from somewhere else. A planet with mediocre native fertility may still become an extraordinary agricultural producer when the mineral inventory it lacks is imported.
GOLIATH
GOLIATH™ makes that separation increasingly necessary.
Extreme biomass production requires extreme material throughput.
Every harvested crop physically removes elements from the cultivation environment.
At sufficiently high yields, accessible planetary reserves eventually become a constraint regardless of the world’s original fertility.
The Lithovore moves that constraint elsewhere.
A GOLIATH production world draws upon an interplanetary mineral supply chain capable of replacing what production removes.
The crop consumes at the rate for which it was engineered; the Lithovore determines which world supplies the difference.
ASHFIELD
ASHFIELD™ operates at the opposite end of the material chain.
After agricultural production, ASHFIELD recovers resources whose remaining value justifies another cycle.
The Lithovore supplies the replacement material required beyond local recovery.
The systems are complementary. Transporting planetary mass across interplanetary distances only to discard an economically recoverable fraction after one harvest would be inefficient, so IFA recovers locally where recovery is cheaper and calls upon the Lithovore where replacement offers the better return.
The objective is uninterrupted production at the lowest useful material cost.
THE PLANET BECOMES THE DEPOSIT
Traditional mining identifies deposits within a planetary body.
The Lithovore can eventually make that distinction obsolete.
As high-grade reserves decline, extraction expands into progressively lower-grade material.
Infrastructure already in orbit reduces the marginal cost of continued processing.
Geological formations once classified as overburden become feedstock, followed by the material surrounding exhausted deposits and, eventually, entire regions of crust.
At sufficient operational maturity, the target is no longer treated as a collection of mines.
It is treated as a bulk geological inventory.
Its remaining mass is continuously compared against energy cost, processing capacity, transportation requirements and demand elsewhere.
The relevant question is no longer where the ore lies, but how much of the world is still worth taking.
PLANETARY CONSUMPTION
This is the operating regime for which The Lithovore was ultimately designed.
Selective extraction becomes systematic extraction. The excavation front expands across the target. Surface geography disappears. Mountain ranges cease to be geographical features and become material volumes. Crustal structure is evaluated according to processing value rather than landscape. The Lithovore consumes it industrially. Slowly enough to control the mass. Precisely enough to recover useful material. Continuously enough to justify the station. For major planetary bodies, this process can continue for extremely long operational periods. For smaller bodies, terminal extraction can approach complete industrial disassembly. The endpoint is not predetermined. It is calculated.
TERMINAL EXTRACTION AND DIVESTMENT
Most target bodies will eventually reach a point where continued processing no longer justifies the required energy and time.
Some worlds are left behind at that point; others remain valuable long enough to pass into terminal extraction.
A sufficiently favourable body within an established agricultural supply network can pass into terminal extraction.
At this stage, preservation of planetary geography has no operational relevance.
Extraction geometry is determined by recoverable composition, structural behaviour, orbital dynamics and remaining mass.
The Lithovore continues until the remaining material is worth less to agricultural production than the energy and time required to recover it.
The remaining body may retain substantial conventional mining value.
After the agriculturally useful crust and mantle fractions have been removed, a target may retain a dense metallic body with substantial conventional mining value. Final assay determines whether that remnant should be processed further, retained as strategic inventory or transferred to a specialist extraction company.
Where a commercial market exists, IFA sells the residual body together with its geological model, orbital survey record and established approach infrastructure.
The purchaser receives a concentrated mining asset together with the knowledge required to exploit it, while IFA converts the world's remaining non-agricultural value into capital for the next deployment.
MASS IS GRAVITY
The Lithovore may disregard geography.
It cannot disregard physics. Removing planetary mass changes the body from which it is removed. Sufficient extraction can alter mass distribution, rotational behaviour and local gravitational conditions. Material transferred into orbital processing must itself be controlled. Large-scale excavation can alter moments of inertia. Terminal processing of smaller bodies can progressively change their orbital and rotational characteristics. The Lithovore therefore maintains continuous dynamic models alongside its geological models. Extraction geometry and rate are adjusted according to the changing physical state of the target. Capture trajectories are coordinated with orbital infrastructure. Mass storage aboard and around the station is managed accordingly. At planetary consumption scale, geology and orbital mechanics become the same industrial problem.
POWER
The Lithovore requires extraordinary energy.
There is no useful way around that requirement.
Planetary excavation, mass capture and industrial mineral processing cannot be supported by conventional agricultural power infrastructure.
The station therefore carries or operates alongside dedicated large-scale generation systems designed for continuous industrial output.
Energy requirement is one reason The Lithovore favours enormous extraction campaigns.
Deploying infrastructure of this scale for limited mineral recovery would be irrational.
The station becomes viable when projected demand justifies sustained conversion of planetary geology into exportable material.
The capital requirement is immense.
The corresponding resource base is measured in worlds.
AGRIFORM
Agriform™ and The Lithovore solve opposite planetary problems.
Agriform™ asks whether a world can be made productive. The Lithovore asks what that world can contribute to production. Sometimes both questions describe the same planet, but often they divide two worlds into complementary roles.
A world with excellent agricultural potential but poor mineral reserves can become a major IFA production centre.
A barren planet with unsuitable atmosphere, temperature, gravity or surface conditions may still contain enormous agricultural value.
One becomes the field; the other becomes material for the field. Each receives the role its conditions can support.
AGRICULTURAL GEOLOGY WITHOUT PLANETARY BORDERS
The Lithovore fundamentally changes how IFA evaluates planetary geology.
A geological survey of an agricultural world is no longer sufficient. IFA evaluates planetary systems according to the movement of useful matter between worlds. A moon can represent centuries of phosphorus supply. A sterile terrestrial planet can become a strategic potassium reserve. Asteroids can supplement specific mineral streams. Rejected Agriform™ candidates can be reassessed as resource bodies. Geological value becomes independent of habitability. Agriculture no longer ends where the soil ends. Its resource base can extend millions of kilometres from the field.
MOBILITY
The Lithovore is a station.
It is relocatable infrastructure. That mobility defines its strategic value. When a target approaches the end of economically useful extraction, the station prepares to disengage. Processing winds down. Remaining inventories are exported. Capture infrastructure is recovered where practical. The station disengages from the target. Then The Lithovore moves. Its next destination may already have been surveyed decades earlier. Another barren planet. Another moon. Another geological inventory waiting in the wrong place. The station establishes a new orbit. The extraction cycle begins again. It brings the mining industry with it.
THE CONSUMPTION ECONOMY
The Lithovore changes the meaning of an uninhabitable world.
A barren planet is not empty, a sterile moon is not useless, and a failed agricultural candidate is not necessarily a failed asset.
Every solid planetary body contains an inventory assembled by geological processes over billions of years.
IFA determines whether that inventory possesses greater value where it currently exists or redistributed through biological production elsewhere.
If redistribution offers the greater value, the Lithovore enters orbit. The world need not support life of its own to sustain the worlds that do.
SCIENCE & TECHNOLOGY
The Lithovore began with a limitation familiar to every agricultural system.
Crops remove minerals. IFA answered first with better nutrient management, then with recovery and larger terrestrial mines.
Eventually planetary agriculture exceeded the usefulness of treating geology as a local resource.
The limitation was not the absence of minerals, but their location.
IFA Science & Technology combined high-energy orbital excavation, geological modelling, mass capture, mineral fractionation, orbital processing and interplanetary bulk logistics into a single mobile industrial platform.
The result makes planetary geology transferable. An agricultural world can consume resources it never possessed, supplied by a barren world that will never produce a harvest of its own. The Lithovore establishes the industrial connection between them.
THE LITHOVORE™
It arrives around a world that will never grow a crop.
The extraction array activates. Rock leaves the surface. The station catches it. Geology enters processing. Mineral concentrates leave aboard bulk transports. Millions of kilometres away, those minerals enter agricultural substrate. Roots absorb them. GOLIATH converts them into biomass. The Terra-Combine removes that biomass. Another production cycle begins. The target world becomes smaller. The agricultural world produces again. There is no contradiction. One planet had matter. The other had value for it. THE LITHOVORE™