Millihertz to Gigahertz

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.

No. Clock speed is only one factor. A modern 3 GHz core can do far more work per cycle than a 2005-era 3 GHz Pentium 4 thanks to wider pipelines, better branch prediction, and larger caches. And a 2.5 GHz chip with 16 cores can outperform a single 5 GHz core on multi-threaded workloads. GHz tells you how fast the clock ticks, not how much work each tick accomplishes.

The 2.45 GHz frequency sits in the ISM band, so it doesn't need a broadcast license. Contrary to popular belief, it is not the resonant frequency of water — water absorbs microwave energy across a broad range. 2.45 GHz was chosen because it penetrates food a few centimeters deep before being absorbed, cooking the interior rather than just scorching the surface. At much higher frequencies, energy would be absorbed in the outer millimeter.

The 2.4 GHz band has longer wavelengths that penetrate walls better and travel farther, but it only has three non-overlapping channels and is congested by Bluetooth, microwaves, and neighbors. The 5 GHz band offers 23+ non-overlapping channels and higher throughput, but signals attenuate faster through walls. Wi-Fi 6E adds the 6 GHz band — even more channels, even shorter range.

Overclocking raises the clock multiplier or base clock in the BIOS, increasing operating frequency beyond the manufacturer's spec. A chip rated at 3.6 GHz might hit 5.2 GHz with extra voltage and aggressive cooling. The risks are heat (silicon degrades faster at high temperatures), instability (random crashes if voltage is insufficient), and reduced lifespan. Extreme overclockers use liquid nitrogen to keep the chip at -196°C for record-breaking single benchmarks.

Millimeter-wave (mmWave) 5G operates between roughly 24 and 47 GHz — frequencies with very short wavelengths (hence "millimeter"). These bands offer enormous bandwidth (up to 800 MHz per channel vs. 100 MHz on sub-6 GHz), enabling multi-gigabit speeds. The trade-off is brutal: mmWave signals are blocked by walls, foliage, even rain. Carriers deploy it in dense urban areas and stadiums where short-range, high-capacity service makes economic sense.