Millihertz to Kilohertz

After a magnitude-9 earthquake the entire planet vibrates like a struck gong, with its deepest mode at about 0.3 mHz — one oscillation every 54 minutes. The surface rises and falls by fractions of a millimeter. You cannot hear it (human hearing starts at 20 Hz), but gravimeters and seismometers worldwide pick it up. The 2004 Sumatra quake kept Earth ringing measurably for weeks.

Ocean swells, tidal constituents, and seiches (standing waves in harbours or lakes) all oscillate in the millihertz band. A 10-second ocean swell is 100 mHz; a harbour seiche with a 10-minute period is about 1.7 mHz. Monitoring these frequencies helps coastal engineers predict resonance in ports and design breakwaters that don't amplify destructive wave energy.

Not directly — our senses are far too fast. But some physiological rhythms operate here: the Mayer wave, a ~0.1 Hz oscillation in blood pressure, sits at the high end of the millihertz scale, and slower vasomotion (tiny blood vessel contractions) can dip below 10 mHz. You don't feel them as vibrations, but they show up clearly on a continuous blood-pressure monitor.

Infrasound is sound below the ~20 Hz threshold of human hearing. The lowest infrasound blends into the millihertz range — the International Monitoring System for nuclear-test detection listens down to about 20 mHz. Sources include volcanic eruptions, meteor airbursts, severe storms, and ocean microbaroms (standing pressure waves between ocean swells and the atmosphere).

Instruments record a time series (pressure, acceleration, displacement) over hours or days, then apply a Fourier transform to extract frequency content. Superconducting gravimeters can resolve Earth's free oscillations below 1 mHz by measuring gravity changes of 10⁻¹² g. The trick is not a fast sensor but a patient, ultra-stable one and enough data to separate signal from drift.

The Nyquist theorem requires a sample rate at least twice the highest frequency you want to capture. Human hearing tops out near 20 kHz, so you need at least 40 kHz. The extra 4.1 kHz provides headroom for the anti-aliasing filter to roll off. The specific number 44,100 was chosen because it factored neatly into the video frame rates of the PAL and NTSC systems used to store digital audio on videotape during early CD mastering.

Kilohertz (kHz) measures oscillation frequency — cycles per second. Kilobits per second (kbps) measures data throughput — bits transferred per second. A 44.1 kHz audio sample rate means 44,100 snapshots per second, but each snapshot may be 16 bits, yielding 705.6 kbps for one channel. The two units describe fundamentally different things: how fast something vibrates vs. how fast data flows.

AM radio was developed first and was allocated the medium-frequency band (535–1,705 kHz) because those wavelengths travel long distances by bouncing off the ionosphere at night. FM came later and was assigned the VHF band (87.5–108 MHz) — higher frequency means shorter range but much better audio fidelity and resistance to static. The allocation reflects both physics and regulatory history.

Yes. A typical dog whistle emits ultrasound between about 23 and 54 kHz — well above the human ceiling of ~20 kHz but within a dog's hearing range, which extends to roughly 65 kHz. Some "silent" whistles do leak a faint hiss that keen human ears pick up, but the dominant output is ultrasonic. Cats hear even higher, up to about 85 kHz.

Traditional landline phone calls sample voice at 8 kHz, which by Nyquist captures frequencies up to 4 kHz. Human speech intelligibility lives mostly between 300 Hz and 3,400 Hz, so 8 kHz is just enough. It is why phone calls sound muffled compared to in-person conversation — you lose all the higher harmonics that make a voice sound natural. HD Voice (VoLTE) bumps the rate to 16 kHz, doubling the bandwidth and noticeably improving clarity.