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The Great American Eclipse

PBS Space Time·
5 min read

Based on PBS Space Time's video on YouTube. If you like this content, support the original creators by watching, liking and subscribing to their content.

TL;DR

Solar eclipses require a new moon, but most new moons miss Earth because the Moon’s orbit is tilted about 5 degrees relative to the ecliptic plane.

Briefing

A total solar eclipse across the continental United States on August 21 arrives after a long drought—America’s first total solar eclipse in 40 years—because the Moon’s shadow must line up precisely with Earth. Solar eclipses happen only at new moons, but most new moons miss Earth because the Moon’s orbit is tilted about 5 degrees relative to the ecliptic plane. When the Moon crosses that plane during a new moon, the shadow can land on Earth; that alignment typically occurs about twice a year, producing one solar eclipse and one lunar eclipse (sometimes three). This year’s solar event is preceded by a partial lunar eclipse on August 7, visible to anyone who can see the Moon, but totality on August 21 depends on being inside a narrow path of the Moon’s umbra.

The eclipse begins at 9:04 AM Pacific time as the penumbra reaches the West Coast, with first totality landfall at Depot Bay, Oregon. Early on, the change can be subtle—light looks sharper and the usual circular “dapples” through leaves become bitten-out shapes. Those leaf gaps act like pinhole cameras, projecting the Sun’s image onto the ground; watching those projections can be a safe, indirect way to observe the partial phases. Direct viewing is dangerous without proper protection: sunglasses won’t cut it. Eclipse glasses made from aluminized mylar or approved welder’s glass (like number 14) are required.

As the Moon covers more of the Sun, the two disks appear to match in size by coincidence: the Moon’s angular diameter this August is about 0.538 degrees, slightly larger than the Sun’s 0.527 degrees, allowing a total eclipse. If the Moon were a bit farther away and smaller, the result would be an annular eclipse—leaving a bright ring around the Moon. Totality is the rare payoff: the sky darkens, blue deepens, temperatures drop, and thin, shifting “shadow bands” ripple across surfaces. Scientists have long puzzled over shadow bands, with leading ideas pointing to atmospheric turbulence.

At the peak, the “diamond ring” marks the last sliver of sunlight before it vanishes. Then the chromosphere appears as a red glow from hydrogen in the Sun’s upper atmosphere, followed by Baily’s beads—sunlight squeezing through lunar valleys—before the corona emerges as a ghostly halo. The sky also briefly reveals bright celestial neighbors: Regulus near Leo, plus planets including Venus, Mars, Jupiter, and Mercury (which is usually hard to spot near the Sun). Totality at Depot Bay runs just under two minutes, with the umbra about 110 kilometers (70 miles) wide and moving eastward around 2,000 miles per hour.

To catch it, viewers need clear skies and a spot inside the narrow track stretching from Oregon to South Carolina, where the eclipse slips into the Atlantic at Cape Romain at 2:49 PM Eastern time. Booking early matters because eclipse tourism is intense, and weather can ruin plans—so backups and forecasts several days ahead are essential. The practical message is straightforward: plan for the path, protect your eyes, and be ready for a brief but dramatic transformation of daylight into a brief, safe-to-stare-at spectacle.

Cornell Notes

A total solar eclipse on August 21 will cross the continental United States, with totality possible only inside a narrow umbral path. Solar eclipses occur at new moons, but most new moons miss Earth because the Moon’s orbit is tilted about 5 degrees relative to the ecliptic plane; alignment happens only when the Moon crosses that plane. This year’s geometry also depends on the Moon’s angular size: in August it spans about 0.538 degrees, slightly larger than the Sun’s 0.527 degrees, enabling totality rather than an annular eclipse. During totality, the chromosphere, Baily’s beads, and the corona become visible, along with bright stars and several planets. The event’s rarity—America’s first total eclipse in 40 years—comes from both orbital alignment and the Moon’s shadow size matching Earth.

Why do solar eclipses require a new moon, and why don’t they happen every month?

Solar eclipses occur when the Moon’s shadow falls on Earth, which requires the Moon to be between the Sun and Earth—this alignment happens during new moons. But the Moon’s orbit is tilted about 5 degrees relative to the ecliptic plane. Because of that tilt, the Moon’s shadow usually misses Earth. Only when the Moon crosses the ecliptic plane during a new moon can the shadow land on Earth, which typically happens about twice a year.

What determines whether an eclipse is total or annular?

Totality depends on the Moon’s apparent angular diameter being large enough to completely cover the Sun. In August, the Moon spans about 0.538 degrees, while the Sun is about 0.527 degrees, allowing the Moon to fully obscure the Sun. If the Moon is farther from Earth and appears smaller, it won’t cover the Sun completely, producing an annular eclipse that leaves a bright ring around the Moon.

How does the eclipse change what people see before totality?

As the eclipse progresses, light looks clearer and shadows sharpen, and leaf “dapples” through trees shift from circular to crescent-like shapes as the Sun’s image gets partially blocked. The gaps between leaves can project the Sun’s image onto the ground like pinhole cameras. Near totality, the sky darkens, blue deepens, temperature drops, and thin, moving “shadow bands” ripple across surfaces.

What are the key visual features during totality?

Totality reveals multiple layers of the Sun that are normally hidden by glare: the chromosphere appears as a red glow from hydrogen electron transitions, Baily’s beads sparkle around the Moon’s rim as sunlight leaks through lunar valleys, and the corona emerges as a faint, ghostly halo. The “diamond ring” effect marks the final sliver of sunlight before it disappears, and then the Sun’s disk is fully covered.

Where and when does totality occur, and how fast does the umbra move?

Totality first makes landfall at Depot Bay, Oregon, around 10:16 AM Pacific time and lasts just under two minutes. The umbra is about 110 kilometers (70 miles) wide and races eastward at roughly 2,000 miles per hour. After crossing many states, it exits into the Atlantic at Cape Romain, South Carolina, at 2:49 PM Eastern time.

What practical steps are emphasized for safely viewing the eclipse?

Viewers are urged to find a location inside the narrow path of totality (Oregon to South Carolina) and to check forecasts days in advance, with a backup plan for clouds. Eye safety is critical: eclipse glasses made from aluminized mylar or approved welder’s glass (like number 14) are required; regular sunglasses are not sufficient. Hotels should be booked early because demand is high.

Review Questions

  1. What orbital geometry prevents most new moons from producing solar eclipses visible from Earth?
  2. How do angular size and distance differences between the Moon and Earth explain total versus annular eclipses?
  3. During totality, which solar features become visible, and what role do Baily’s beads and the corona play?

Key Points

  1. 1

    Solar eclipses require a new moon, but most new moons miss Earth because the Moon’s orbit is tilted about 5 degrees relative to the ecliptic plane.

  2. 2

    Eclipses occur only when the Moon crosses the ecliptic plane during a new (or full) moon, typically producing about two eclipse opportunities per year.

  3. 3

    This August’s total eclipse depends on angular size: the Moon’s apparent diameter (~0.538 degrees) slightly exceeds the Sun’s (~0.527 degrees).

  4. 4

    Annular eclipses happen when the Moon appears smaller and leaves a bright ring of sunlight around the Moon’s disk.

  5. 5

    Safe viewing requires approved eclipse glasses (aluminized mylar or number 14 welder’s glass); sunglasses are not adequate.

  6. 6

    Totality at Depot Bay, Oregon begins around 10:16 AM Pacific time and lasts just under two minutes, with the umbra moving east at about 2,000 miles per hour.

  7. 7

    Successful viewing hinges on being inside the narrow path of totality and planning for weather and crowds with backups and early lodging.

Highlights

The 40-year wait is explained by two constraints: orbital alignment (the Moon crossing the ecliptic plane) and the Moon’s shadow size matching Earth.
Leaf “dapples” through trees can act like pinhole cameras, projecting the Sun’s image and revealing the eclipse’s early bite.
Totality brings out the chromosphere (red hydrogen glow), Baily’s beads (sunlight through lunar valleys), and the corona (a faint halo).
The umbra is about 110 kilometers wide and sweeps across the country at roughly 2,000 miles per hour, making timing and location crucial.

Topics

  • Total Solar Eclipse
  • Eclipse Geometry
  • Eye Safety
  • Shadow Bands
  • Celestial Observations