In the early morning hours of August 14, 2026, residents across Washington and surrounding areas witnessed an extraordinary sight: a brilliant fireball streaking through the night sky.
The event was much more than an ordinary shooting star.
NASA estimates that the space rock was approximately 16 inches (40 centimeters) in diameter, weighed around 170 pounds (77 kilograms) and was traveling at approximately 33,000 miles per hour when it entered the atmosphere.
The object ultimately broke apart high above Douglas County, Washington, releasing an estimated amount of energy equivalent to approximately 10 tons of TNT.
Even more exciting for meteorite hunters, radar observations indicate that some pieces may have survived the journey through the atmosphere and reached the ground.
NASA reports that the fireball was first visible approximately 48 miles above the Soap Lake area of Washington.
It was traveling almost directly north.
The meteor remained visible for approximately 36 miles as it raced through the upper atmosphere.
Its trajectory began near:
47.412° N, 119.412° W
and the end of NASA's observed luminous trajectory was near:
47.850° N, 119.408° W
The object therefore traveled almost directly north rather than moving significantly east or west.
The major fragmentation occurred approximately 28 miles above Sim's Corner in Douglas County.
At this point, tremendous atmospheric forces caused the object to break apart.
NASA estimates that the energy released during the event was equivalent to approximately:
10 tons of TNT.
That does not mean there were ten tons of meteorites.
The original object itself was estimated to weigh only around 170 pounds.
The TNT figure describes the tremendous amount of kinetic energy released as the extremely fast-moving object interacted with Earth's atmosphere.
The fragmentation also generated a pressure wave that reached the ground.
This may be the most exciting part of the event.
NASA reports that Doppler weather radar indicates that small meteorites may be on the ground in the area.
Weather radar can sometimes detect meteorites after a fireball breaks apart.
Once meteorites slow sufficiently, they stop glowing and enter a phase known as dark flight.
During dark flight, the pieces fall toward Earth at much slower speeds.
Radar can sometimes detect these falling fragments.
NASA scientists have successfully used NEXRAD Doppler weather radar to locate meteorite falls elsewhere in the United States.
Meteorite fragments can produce distinctive radar signatures as they descend through the atmosphere.
Scientists look for objects that:
appear shortly after the fireball
begin at higher altitude
move progressively toward lower altitude
appear in approximately the correct location
have radar characteristics consistent with falling material
NASA explains that meteorite radar signatures can sometimes remain visible for several minutes after a fireball disappears.
This technique has helped researchers calculate meteorite strewn fields and has contributed to successful meteorite recoveries.
This question is more complicated than simply looking underneath the point where the meteor exploded.
The major fragmentation occurred high above the Sim's Corner/Waterville Plateau region of Douglas County.
However, fragments retained forward momentum after the explosion.
They were also affected by atmospheric winds while falling.
Therefore, meteorites would not necessarily have fallen directly underneath the explosion.
Instead, they could be scattered across an elongated region called a:
A strewn field is the area across which fragments from a meteor become scattered.
Large pieces behave differently from small pieces.
A heavier meteorite retains momentum longer and is generally less affected by winds.
A tiny meteorite slows more quickly and can be carried considerable distances by upper-atmospheric winds.
Consequently, meteorite fragments can become separated by miles.
As of August 16, 2026, NASA has confirmed the fireball's trajectory and reported radar evidence suggesting meteorites may have reached the ground.
However, NASA's public Meteorite Falls database has not yet published a dedicated Douglas County strewn-field map.
That distinction is important.
The coordinates near 47.850° N, 119.408° W represent approximately the end of the observed glowing trajectory high in the atmosphere.
They should not be interpreted as the meteorite landing coordinates.
A proper landing calculation requires information about:
fragmentation altitude
fragment velocity
fragment mass
atmospheric density
wind speed
wind direction at different altitudes
Doppler radar returns
NASA uses this type of information to model other meteorite falls.
Meteorite researchers use computer models known as dark-flight models.
These simulations can estimate where fragments of different sizes might have landed.
For example, scientists might calculate separate trajectories for hypothetical fragments weighing:
1 gram
10 grams
100 grams
1 kilogram
5 kilograms
Smaller meteorites are generally carried farther by winds.
Larger meteorites usually land closer to their ballistic trajectory.
NASA has used this technique for recent meteorite falls. In some cases, calculated landing zones have been accurate enough to guide meteorite hunters toward successful recoveries.
A freshly fallen meteorite may be surprisingly difficult to recognize.
Many are dark gray or black and can resemble ordinary terrestrial rocks.
One of the best clues is a thin outer coating called a:
Fusion crust
The outer surface of a meteorite becomes extremely hot during atmospheric entry.
A very thin layer melts and then rapidly cools, creating a dark crust.
Fresh meteorites can therefore have a black or dark brown exterior while the inside may be considerably lighter.
Other possible characteristics include:
unusually heavy weight for their size
rounded or softened edges
shallow thumbprint-like depressions
tiny metallic grains
attraction to a magnet
a dark fusion crust
However, none of these characteristics alone proves that a rock is a meteorite.
Washington State contains enormous quantities of volcanic basalt.
Some basalt can look remarkably similar to meteorites.
Certain terrestrial rocks can even react to magnets because they contain iron-bearing minerals.
For that reason, finding a black magnetic rock in Douglas County does not automatically mean you've found part of the August 14 meteor.
Scientific examination is needed for confirmation.
If you discover an unusual dark rock in the suspected fall area, do not immediately wash or scrub it.
A freshly fallen meteorite can contain scientifically valuable material on its surface.
Instead:
Photograph the rock exactly where you discovered it.
Photograph the surrounding ground.
Record the exact GPS coordinates.
Record the date and time.
Avoid excessive handling.
Pick it up using clean gloves, aluminum foil or another clean material when practical.
Place it in a clean container or bag.
Keep the specimen dry.
Have the specimen examined by a qualified meteorite researcher or laboratory.
Accurate location information can be nearly as scientifically valuable as the meteorite itself because researchers can compare the recovery location with their predicted trajectory.
If pieces are eventually recovered, scientists will determine their composition and classification.
Most meteorites originate from asteroids formed during the earliest history of our solar system.
Many contain material approximately:
4.5 billion years old.
That means someone walking across a field in Douglas County could potentially discover a rock that formed before Earth looked anything like the planet we know today.
Interestingly, no.
The event happened during the annual Perseid meteor shower, which made the timing particularly confusing.
NASA determined that the object's trajectory was inconsistent with the Perseids.
Instead, it was a sporadic meteor, most likely a small asteroid fragment that happened to encounter Earth during the Perseid season.
This remains unknown.
The original object was estimated at approximately 170 pounds, but atmospheric entry destroys a tremendous amount of material.
Some material vaporizes.
Some becomes extremely small particles.
Other portions can survive as meteorites.
NASA currently describes the potential surviving material from the Douglas County event as small meteorites.
Until fragments are recovered or a detailed radar-based mass analysis is published, claims about specific surviving sizes should be considered estimates rather than established facts.
Finding an ordinary meteorite is exciting.
Finding a meteorite from a documented fall is even more scientifically valuable.
Scientists know exactly when the Douglas County object entered Earth's atmosphere:
August 14, 2026 at approximately 12:48 a.m. PDT.
They also know its direction, approximate speed, estimated size and fragmentation altitude.
If a meteorite is recovered and its exact location documented, researchers can connect the physical rock with the recorded atmospheric event.
Scientists could then analyze its minerals and chemical composition to determine what type of asteroid produced the fireball.
This part of Washington is particularly interesting because Douglas County already has an association with meteorites.
The famous Waterville Meteorite, weighing more than 73 pounds, was discovered in the Waterville area in 1917.
More than a century later, Douglas County may have received another delivery from space.
This time, however, modern cameras, satellites, atmospheric sensors and Doppler radar recorded the event.
The August 14, 2026 Washington fireball has provided scientists with an unusually interesting opportunity.
We currently know that an approximately 16-inch space rock weighing around 170 pounds entered Earth's atmosphere at roughly 33,000 mph.
We know that it traveled north over Central Washington.
We know that its major fragmentation occurred approximately 28 miles above Douglas County.
And most importantly for meteorite hunters:
NASA says Doppler radar indicates that small meteorites may have reached the ground.
What we don't yet have is equally important:
No officially published Douglas County strewn-field map has yet identified a precise search zone.
If NASA or meteorite researchers publish detailed radar analysis and dark-flight calculations, scientists may eventually be able to narrow the search from a large portion of Douglas County to a much smaller area.
And somewhere within that area could be pieces of a 4.5-billion-year-old visitor from space, waiting to be discovered.
Douglas County (specifically in Washington State) has historic orchard lands with lead and arsenic contamination in the soil. Between 1900 and 1950, farmers used lead arsenate pesticides on fruit trees, leaving persistent chemical residues in the topsoil that do not break down over time. I would be very careful in this area and probably stay away from this area if possible.
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Respiratory Virus Flu Alert for Wa State
Recent earthquakes from Wa state may disturb the dirt. The dirt may be flying in the air and in the wind.
Magnitude 3.4 February 22, 2025 Maple Valley, WA
Magnitude 2.3 February 21, 2025 Centralia, WA
Magnitude 2.2 February 22, 2025 Mt St Helens, WA
Magnitude 1.6 February 20, 2025 Mt Baker, WA
Magnitude 1.5 February 20, 2025 Aberdeen, WA
Magnitude 1.3 February 20, 2025 Bremerton, WA
There are diseases that appear when the dirt is disturbed.
Influenza, commonly known as the flu, is a contagious respiratory illness caused by influenza viruses, but
Because Valley fever has the same symptoms as pneumonia caused by bacteria or viruses, it is often misdiagnosed or undiagnosed. This can lead to ineffective treatments or delays in appropriate antifungal treatment for people who need it.
Valley fever is a fungal infection caused by Coccidioides organisms. Like seeds from plants, a fungus grows and spreads from tiny spores that are too small to see. When soil or dirt are stirred up by strong winds or while digging, dust containing these fungal spores can get into the air. It can cause signs and symptoms such as a fever, cough and tiredness.
Valley fever is a lung infection caused by breathing in fungal spores from the soil. Valley Fever lives in dust and soil in lives in Arizona, California, Nevada, New Mexico, Texas, Utah, and in south-central Washington. The fungi's spores can be stirred into the air by anything that disrupts the soil, such as earthquakes, farming, construction and wind
People can then breathe the fungi into their lungs. Mild cases of valley fever usually resolve on their own. In more-severe cases, doctors treat the infection with antifungal medications.
The initial, or acute, form of valley fever is often mild, with few or no symptoms. Signs and symptoms occur one to three weeks after exposure. They tend to be similar to flu symptoms. Symptoms can range from minor to severe, including:
If you don't become ill or have symptoms from valley fever, you may only find out you've been infected later. You may find out when you have a positive skin or blood test or when small areas of residual infection in the lungs (nodules) show up on a routine chest X-ray. The nodules typically don't cause problems, but they can look like cancer on X-rays.
If you develop symptoms, especially severe ones, the course of the disease is highly variable. It can take months to fully recover. Fatigue and joint aches can last even longer. The disease's severity depends on several factors, including your overall health and the number of fungus spores you inhale.
If the initial Valley Fever infection doesn't completely resolve, it may progress to a chronic form of pneumonia. This complication is most common in people with weakened immune systems.
People who live in these areas can try to avoid spending time in dusty places, close windows and doors to prevent dust accumulation, and use air filtration in homes and vehicles. People who are at risk for severe disease should avoid areas with lots of dust, such as construction or excavation sites, or wear an N95 respirator if dust cannot be avoided.
Arsenic in the soil can cause a variety of health problems, including cancer, heart disease, and diabetes. Exposure can occur by swallowing or inhaling contaminated soil.
Short-term effects
nausea, vomiting, diarrhea, weakness, loss of appetite, shaking, cough, and headache.
Long-term effects
What is arsenic and why is it in the environment?
Arsenic is a naturally occurring element that is normally present throughout our environment in water, soil, dust, air, and food. Levels of arsenic can vary from place to place due to farming and industrial activity as well as natural geological processes such as earthquakes.
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