The Schumann Resonance is the electromagnetic "heartbeat" of Earth, oscillating at approximately 7.83 Hz. This tool treats daily variations in the Schumann field as "scanlines" in a slow-scan transmission.
By arranging 365 days of data as horizontal lines (like an old fax machine), patterns emerge that may represent structured information encoded in Earth's electromagnetic field.
This isn't just visualization—it's pattern detection. The tool uses autocorrelation, Fourier analysis, symmetry detection, and entropy analysis to determine if the patterns are random or structured.
Autocorrelation: Measures if patterns repeat over time
Edge Coherence: Detects organized boundaries vs. noise
Symmetry Analysis: Looks for geometric organization
Entropy Analysis: Measures information density
Fourier Transform: Identifies dominant spatial frequencies
To analyze actual Schumann Resonance data, download measurements from: