Hourwiz Explains · video notes

A hole through the Earth: our full simulation

From the Hourwiz video “Jump into this hole.” · Checked Oct 15, 2026

Watch on YouTube (opens in a new tab)

In the video we built the planet in code and dropped you in. Here's the full simulation: how the model works, every number it gave, where you'd come out, and the files, so you can check our work.

The thought experiment

A magic tunnel straight through the center: no air, no heat, and we ignore Earth's spin. You step in at rest and fall. Physicist Alexander Klotz (2015) puts the spin's effect at “about four seconds over a forty minute trip”, and Earth's slightly squashed shape at about ten seconds.

Our method

Our model. Two Node scripts we wrote, no outside libraries, run on Oct 15, 2026 with Node v24.21.0. Every input is a published value listed in the sources below.

How we checked the model

The results: two Earths

Our model. Times are from the moment you jump. Speeds in mph, from our run; the crust here is PREM's global average, 24.4 km.

Our model: the fall, textbook Earth vs real Earth
On the wayTextbook Earth (even density)Real Earth (PREM, layered)
Deepest hole ever dug (Kola, 12.262 km)50.0 s · 1,097 mph50.0 s · 1,098 mph
Through the crust (24.4 km)1 min 10.5 s · 1,547 mph1 min 10.5 s · 1,550 mph
Mantle boundary (670 km)6 min 12.7 s · 7,898 mph6 min 08.4 s · 8,165 mph
Top of the core (2,891 km)13 min 19.8 s · 14,821 mph12 min 43.5 s · 17,051 mph
Inner core starts (5,149.5 km)18 min 29.8 s · 17,365 mph17 min 01.0 s · 21,568 mph
The center (top speed)21 min 05.2 s · 17,694 mph (7.91 km/s)19 min 05.3 s · 22,188 mph (9.92 km/s)
The far side42 min 10.4 s38 min 10.7 s
Back home, if nobody grabs you84 min 20.8 s76 min 21.3 s

Our model: the real Earth gets you through 3 min 59.8 s faster (9.5%), with a top speed of about 22,200 mph instead of 17,700.

Bonus: New York to Los Angeles, no engine

A straight tunnel between the two cities (3,873 km long, 302 km down at its deepest) takes 42 min 10.4 s on the textbook Earth and 41 min 50.6 s on the real one, topping out near 5,400–5,500 mph (our model). Klotz: “42 minutes for short trips and 38 minutes for long trips”.

Heat and pressure on the way down

Our model (pressure). Our tunnel ignores heat; these are the conditions the tunnel walls would face.

Our model: pressure by depth (PREM)
DepthPressureIn atmospheres
Base of the crust (24.4 km)0.6 GPaabout 6,000
Mantle boundary (670 km)23.8 GPaabout 0.24 million
Top of the core (2,891 km)135.8 GPaabout 1.3 million
Inner core starts (5,149.5 km)329.1 GPaabout 3.2 million
The center (6,371 km)364.1 GPaabout 3.6 million

The deepest hole ever dug, to scale

Our math. Kola's 12.262 km divided by Earth's 6,371 km radius (NASA) is 0.19%.

Kola is about 0.2% of the way to the center (0.1% of the way through). The full trip is about 7,918 miles (USGS).

Our model, to scale: if Earth's radius were a football field (surface on one goal line, the center on the other, 100 yards)
WhatReal depthOn the field
The deepest minenearly 4 km (about 2.4 mi)about 2 in
The ocean's deepest point (Challenger Deep)10,935 m (35,876 ft)about 6 in
Kola, the deepest hole12,262 m (7.6 mi)about 7 in
Average continental crustabout 30 km (about 5 km under the oceans)about 17 in
Top of the core2,891 kmthe 45-yard line
Top of the inner core5,149.5 kmthe 81-yard line

Where you'd come out

Our calculation · Natural Earth data. The point straight through the center, the antipode, is at the same latitude in the other hemisphere and 180° of longitude away (USGS). We tested each point against Natural Earth's 1:10m country outlines (public domain). “Nearest land” is the nearest outline point, so it slightly over-estimates the distance. City coordinates are approximate city centers.

Our calculation: where you'd come out
StartYou come out atLand or ocean?Nearest land
New York, NY40.71°S, 105.99°EOceanAustralia, 664 mi (1,069 km)
Los Angeles, CA34.05°S, 61.76°EOceana remote French island, 917 mi (1,476 km)
Chicago, IL41.88°S, 92.37°EOceana remote French island, 809 mi (1,303 km)
Houston, TX29.76°S, 84.63°EOceana remote French island, 689 mi (1,109 km)
Phoenix, AZ33.45°S, 67.93°EOceana remote French island, 616 mi (992 km)
Miami, FL25.76°S, 99.81°EOceanAustralia, 816 mi (1,313 km)
Seattle, WA47.61°S, 57.67°EOceana remote French island, 285 mi (459 km)
Denver, CO39.74°S, 75.01°EOceana remote French island, 151 mi (243 km), the closest call
Atlanta, GA33.75°S, 95.61°EOceana remote French island, 1,048 mi (1,686 km)
Washington, DC38.91°S, 102.96°EOceanAustralia, 741 mi (1,193 km)
Anchorage, AK61.22°S, 30.10°EOceanAntarctica, 523 mi (841 km)
Honolulu, HI21.31°S, 22.14°ELand: Botswanaon land; Namibia is 75 mi (120 km) away
Beijing, China39.90°S, 63.59°WLand: Argentinaon land; 64 mi (103 km) from the nearest coast or border
Chengdu, China30.57°S, 75.93°WOcean (Pacific)Chile, 251 mi (404 km)

Left out on purpose. Our script flags any landing point within about 50 km of a coast or border. We only list points we're sure of; the rest stay off this page until we've checked them on a map.

Download our model's output

Plain-text files from the runs above. Open the CSVs in any spreadsheet.

Edited for the web. In the run log we removed our internal source-row tags and one place name; the numbers are unchanged. The antipode file has only the rows on this page.

Images in the video

Everything else, including the tunnel, the drill rig and the to-scale graphics, is drawn in code by Hourwiz.

Sources

Every fact on this page comes from these pages, opened on Oct 15, 2026. Things change: check the live page before you rely on it.

  1. A. R. Klotz, “The Gravity Tunnel in a Non-Uniform Earth”, Am. J. Phys. 83, 231 (2015) Fall times, 1.09 g, orbit match, spin effect. Full text: ar5iv
  2. NASA NSSDC, Earth fact sheet Radius 6,371 km, GM, mass, mean density.
  3. NASA NSSDC, Sun fact sheet Effective temperature 5,772 K.
  4. IRIS EMC, PREM (Dziewonski & Anderson, 1981) The layered Earth model.
  5. PREM_1s table (CDS mirror of the IRIS file) Layer depths and densities; our 21-point check.
  6. NIST CODATA 2022, Newtonian constant of gravitation
  7. NIST, standard atmosphere 1 atm = 101,325 Pa.
  8. NIST, unit conversions Exact foot and mile.
  9. NASA, what is microgravity? (grades 5–8) Free fall; the station's 17,500 mph.
  10. ESRF, “The Earth's centre is 1000 degrees hotter than previously thought” (2013) 330 GPa and about 5,500 K at the inner-core boundary.
  11. USGS, This Dynamic Earth: inside the Earth Crust about 5 km under oceans, about 30 km under continents.
  12. EarthDate, Kola Superdeep 40,230 ft (7.62 mi), May 1970, 9 inches wide, 180 °C vs 100 °C expected.
  13. BBC Future, “The deepest hole we have ever dug” (May 6, 2019) Stopped in 1992; the heat; no money after the Soviet collapse.
  14. Guinness World Records, deepest penetration into the Earth's crust
  15. Wikipedia, Kola Superdeep Borehole Longer curved wells; still the deepest below the surface.
  16. Skeptoid #307, Brian Dunning (Apr 24, 2012) The recording is a hoax.
  17. Guinness World Records, deepest mine Nearly 4 km down.
  18. NOAA Ocean Service, ocean depth Challenger Deep about 10,935 m (35,876 ft).
  19. NFL rulebook (2024) 100 yards goal line to goal line.
  20. USGS Yellowstone Volcano Observatory, volcanism on the other side of the world (Mar 30, 2026) Antipodes; 12,742 km (7,918 mi); US in the Indian Ocean; Hawaii to Botswana.
  21. Big Think, Frank Jacobs, Strange Maps on antipodes (Jul 23, 2010) Almost no overlap in North America; China and South America.
  22. Atlas Obscura, Frank Jacobs, on tunnels through the Earth (Apr 19, 2024)
  23. NOAA Ocean Service, sea surface temperature facts The ocean covers 71% of Earth's surface.
  24. Natural Earth, terms of use Public domain. Data: natural-earth-vector

Our model is a thought experiment: a frictionless tunnel with no air, no heat and no spin, rounded as shown. NASA, USGS, NOAA, ESRF and the authors cited didn't make, review or endorse this page or the video.

No sponsor and no affiliate links on this page. Vendors are named so you can check them yourself, not as recommendations.

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