Research Infrastructure

Built Like the Earth

GeoVerse is organized like the Earth itself. Deep inside sits the core runtime that everything depends on; at the outermost layer, a planetary system where each researcher joins with an orbit of their own.

Planetary system GeoPlanet

The layer that extends beyond the lab. Researchers’ workstations and collaborators each connect as a node.

Sedimentary basin GeoStrata

The record layer where agents’ work accumulates strata by strata, and, after review, hardens into knowledge.

Crust GeoWeb

The surface researchers meet first. What happens in the systems below shows up on screen here.

Mantle GeoADK

The convective layer that turns plans into execution. Research pipelines run as nodes and edges, with human approval at key steps.

Outer core GeoAuth

The layer that wraps everything unseen. Every request passes authentication and permission checks before reaching the core.

Inner core GeoCore

The common runtime at the deepest point, holding the state of nodes, GPUs, services and accounts in one place.

Outward expansion → operational records → human interface → pipelines → access control → core runtime

At the innermost layer, the physical base GeoCore stands on is the cluster below.

The physical foundation that runs our research — an introduction to our workstation and compute cluster scale.