Space & Beyond • Strange Sky Events • Impact Science
Meteorites, impacts and craters are the physical evidence left behind when objects from space collide with planets. Most incoming meteoroids burn up harmlessly in Earth’s atmosphere, but some survive atmospheric entry, strike the ground, and leave scars that can remain visible for millions or even billions of years.
This Strange Sounds master pillar explains how meteorites form, how impact craters are created, why some explosions occur in the atmosphere while others excavate massive basins, and how scientists study the geological fingerprints of ancient collisions.
This page also explores impact winters, planetary bombardment, extinction-level events, Earth’s hidden crater record, and why the Moon preserves ancient scars far better than our constantly recycled planet.

TL;DR
- Meteorites are fragments of cosmic objects that survive atmospheric entry.
- Impact craters form when high-speed objects strike planetary surfaces.
- Most incoming objects explode or burn up before impact.
- Airbursts release energy in the atmosphere without creating classic craters.
- The Moon preserves ancient craters because it lacks erosion and plate tectonics.
- Earth constantly erases impact evidence through weathering and geological recycling.
- Large impacts can trigger global climate effects and mass extinctions.
- Impact craters provide crucial evidence about Solar System history.
The impact chain explained (space → atmosphere → crater)
Most impact stories begin in space.
An asteroid fragment, comet fragment or meteoroid encounters Earth’s atmosphere and rapidly transforms through several stages.
| Stage | Description |
|---|---|
| Meteoroid | Rocky or metallic object traveling through space. |
| Meteor | Visible atmospheric streak. |
| Fireball / Bolide | Exceptionally bright atmospheric entry event. |
| Meteorite | Fragment surviving to reach the ground. |
| Impact crater | Geological scar produced by collision. |

Atmospheric-entry events are explored in: Fireballs, Bolides, Meteors & Atmospheric Explosions Explained.
Meteorites explained
A meteorite is any fragment of a meteoroid that survives atmospheric entry and reaches the ground.
Meteorites provide direct physical samples from space.
Scientists classify meteorites into three major groups:
| Meteorite Type | Main Composition |
|---|---|
| Stony meteorites | Silicate rock |
| Iron meteorites | Nickel-iron metal |
| Stony-iron meteorites | Mixed rock and metal |
Some meteorites are older than Earth itself and preserve material from the early Solar System.
How impact craters form
Impact craters form when objects strike planetary surfaces at extremely high speeds.
The collision releases enormous kinetic energy almost instantly.
Typical crater formation stages include:
- Atmospheric entry
- Shockwave generation
- Surface excavation
- Ejecta dispersal
- Crater collapse and modification
Even relatively small asteroids can release energy equivalent to nuclear explosions.
Types of impact craters
| Crater Type | Description |
|---|---|
| Simple crater | Small bowl-shaped crater. |
| Complex crater | Larger crater with central uplift structures. |
| Multi-ring basin | Massive impact basin with multiple rings. |
| Buried crater | Impact structure hidden beneath sediments. |
Earth contains many hidden or heavily eroded craters that were only discovered through satellite imaging and geophysical surveys.
Airburst vs ground impact
Not all incoming objects create craters.
Many large objects explode in the atmosphere before reaching the ground.
| Event Type | Main Result |
|---|---|
| Airburst | Atmospheric explosion with shockwave. |
| Ground impact | Crater formation and ejecta. |
| Fragmentation event | Meteorite strewn field. |
The Tunguska event likely represents a powerful airburst, while Barringer Crater in Arizona represents a direct impact.
Why Earth hides craters but the Moon preserves them
Earth constantly recycles its surface.
Processes that erase impact scars include:
- Erosion
- Plate tectonics
- Volcanism
- Glaciation
- Ocean sedimentation
The Moon lacks most of these processes, allowing craters to remain visible for billions of years.
Major impact events in history
| Impact Event | Importance |
|---|---|
| Chicxulub impact | Associated with dinosaur extinction. |
| Barringer Crater | Classic preserved impact crater. |
| Tunguska | Massive atmospheric explosion without crater. |
| Chelyabinsk | Modern atmospheric-entry event recorded globally. |
| Sudbury Basin | One of Earth’s largest known impact structures. |
Impact winters and extinction events
Large asteroid impacts can alter global climate.
Possible consequences include:
- Atmospheric dust clouds
- Sunlight reduction
- Wildfires
- Tsunamis
- Acid rain
- Food-chain collapse
The Chicxulub impact is widely associated with the extinction of non-avian dinosaurs approximately 66 million years ago.
Planetary bombardment across the Solar System
Impact craters appear throughout the Solar System.
Heavily cratered worlds include:
- The Moon
- Mercury
- Mars
- Callisto
- Ceres
- Many asteroids
Scientists believe the early Solar System experienced periods of intense bombardment known as the Late Heavy Bombardment.
Event Embed Zone (301 sink for fireball and meteorite posts)
This pillar is designed to absorb thin meteorite finds, articles about meteorite impacting homes, cars and infrastructures on Earth and news about new impact crater discovery on Earth or other solar system planets through 301 redirects.
Famous & Visitable Impact Craters — Earth’s Greatest Collision Sites
Barringer Meteor Crater — Arizona, USA — ~50,000 Years Old
- Site: Nearly 1 mile (1.2 km) wide and ~560 feet (170 m) deep
- Trigger: Iron-nickel bolide impact
- Pattern: Exceptionally preserved impact crater in desert terrain
- Amazing Find: The famous 1,406 lb Holsinger Meteorite fragment recovered from the site
- Importance: Widely considered the best-preserved impact crater on Earth
Nördlinger Ries — Bavaria, Germany — ~15 Million Years Old
- Site: Massive 24 km-wide crater basin
- Trigger: High-energy asteroid impact
- Pattern: Medieval town built directly inside crater basin
- Amazing Find: Impact created over 70,000 tons of microscopic diamonds
- Importance: Buildings in Nördlingen contain diamond-bearing impact rock
Hapcheon Crater — South Korea — ~42,000 Years Old
- Site: ~7 km-wide confirmed impact structure
- Trigger: Powerful ~1,500-megaton asteroid collision
- Pattern: Buried crater discovered beneath agricultural landscape
- Amazing Find: Shocked quartz and shatter cones recovered through 2020s drilling
- Importance: One of East Asia’s most important confirmed impact discoveries
Wabar Craters — Saudi Arabia — Modern Era Discovery
- Site: Multiple craters located in the Rub’ al Khali desert
- Trigger: Fragmenting iron meteorite impact
- Pattern: Young desert craters preserving impact glass
- Amazing Find: Crater rims surrounded by melted silica glass from impact heat
- Importance: One of the clearest preserved recent desert impact fields
Hidden & Prehistoric Impact Discoveries — Buried Catastrophes and Ancient Planetary Scars
Chicxulub Crater — Yucatán, Mexico — ~66 Million Years Old
- Site: ~180 km-wide buried impact structure
- Trigger: Giant asteroid impact at end of Cretaceous period
- Pattern: Planetary-scale extinction event
- Amazing Find: Gravity-anomaly mapping revealed buried crater structure beneath sediments
- Impact: Associated with extinction of ~75% of all life including non-avian dinosaurs
Vredefort Dome — South Africa — >2 Billion Years Old
- Site: ~300 km-wide impact structure
- Trigger: Massive ancient asteroid collision
- Pattern: Largest confirmed impact structure on Earth
- Amazing Find: Preserved central uplift and shock-deformed geology
- Importance: Key evidence for early Solar System bombardment history
Amazing Meteorite Finds — Rare Space Rocks Recovered on Earth
Hoba Meteorite — Namibia — Discovered 1920
- Type: Massive iron-nickel meteorite
- Pattern: Flat shape slowed atmospheric descent
- Amazing Find: Largest known intact meteorite on Earth (>60 tons)
- Importance: Did not form a classic crater due to atmospheric deceleration
Canyon Diablo Meteorites — Arizona, USA
- Type: Iron-nickel meteorite fragments
- Pattern: Thousands of fragments scattered around Barringer Crater
- Amazing Find: Helped confirm impact origin of Meteor Crater
- Importance: One of the most famous meteorite strewn fields in history
Peekskill Meteorite — New York, USA — 1992
- Type: Stony meteorite fall
- Pattern: Bright fireball recorded on multiple cameras
- Amazing Find: Meteorite crashed directly into a parked car trunk
- Importance: One of the most famous filmed meteorite falls ever recorded
2000–2026 — Modern Meteorite Recoveries and Scientific Discoveries
Ohio Meteorite Recovery — USA — 2026
- Trigger: ~7-ton meteor producing major sonic-boom airburst
- Pattern: Meteorite recovery following atmospheric explosion
- Amazing Find: First authenticated fragments classified as eucrites from asteroid 4 Vesta
- Importance: One of the largest modern US meteorite recovery operations
Houston Meteorite Fall — Texas, USA — 2026
- Trigger: Daylight fireball exploding with ~26 tons TNT equivalent
- Pattern: Urban meteorite fall associated with sonic-boom-producing airburst
- Amazing Find: Confirmed fragment crashed through residential roof
- Importance: Rare direct-hit modern meteorite incident
Edmonton Meteorite Fall — Canada — 2022/2023
- Trigger: Loud atmospheric-entry event over residential region
- Pattern: Multi-fragment meteorite recovery
- Amazing Find: Fragment penetrated roof and landed on resident’s bed
- Importance: One of the most widely publicized modern Canadian falls
Tarda Meteorite — Morocco — 2020
- Type: Rare ungrouped carbonaceous chondrite
- Pattern: Daylight meteorite fall producing pristine fragments
- Amazing Find: Highly sought-after samples by research institutions worldwide
- Importance: Extremely rare primitive Solar System material
Santa Filomena Meteorite Fall — Brazil — 2020
- Type: H5-6 ordinary chondrite
- Pattern: Massive meteorite shower over populated area
- Amazing Find: Hundreds of stones recovered shortly after fall
- Importance: Large fresh-fall sample set for planetary science
Muonionalusta Meteorite Finds — Sweden — 2000s–2026
- Type: Ancient iron-nickel meteorite
- Pattern: Continued discoveries from prehistoric strewn field
- Amazing Find: Stunning Widmanstätten crystal patterns highly prized by collectors
- Importance: Some polished specimens sold for hundreds of thousands of dollars
Global Meteorite Hunting and Scientific Recovery Networks
Sahara and Atacama Desert Finds — 2000–2026
- Pattern: Tens of thousands of meteorites recovered from stable desert environments
- Importance: Expanded planetary-science collections dramatically
- Common Finds: Chondrites, iron meteorites, lunar meteorites and Martian fragments
Antarctic Meteorite Recovery Programs — Global Scientific Collaboration
- Pattern: Dark meteorites concentrated on bright ice fields
- Importance: Antarctica became one of the world’s most important meteorite recovery regions
- Scientific Value: Exceptional preservation in cold stable environments
Meteoritical Bulletin Database — Official Global Registry
- Function: Peer-reviewed authentication and classification of meteorites
- Pattern: Tens of thousands of specimens cataloged between 2000 and 2026
- Importance: Primary scientific registry for confirmed meteorite finds and falls
American Meteor Society Fireball Logs — Live Witness Tracking
- Function: Global fireball and witness-report database
- Pattern: Real-time documentation of atmospheric-entry events
- Importance: Helps scientists reconstruct trajectories and locate meteorite falls
How meteorites are found and classified
Meteorite hunters often search deserts, ice fields and dry lake beds because meteorites are easier to spot in stable environments.
Scientists analyze:
- Mineral composition
- Nickel content
- Isotopic signatures
- Fusion crusts
- Shock features
Frequently Asked Questions
What is the difference between a meteor and a meteorite?
A meteor is the visible atmospheric streak. A meteorite survives to reach the ground.
Why does Earth have fewer visible craters than the Moon?
Earth constantly erases craters through erosion, tectonics and geological recycling.
What causes impact craters?
Impact craters form when high-speed objects collide with planetary surfaces.
What is an airburst?
An airburst is an atmospheric explosion caused by fragmentation before ground impact.
Can impacts cause extinctions?
Yes. Extremely large impacts can trigger global climate disruption and mass extinctions.
Are meteorites valuable?
Some rare meteorites are scientifically important and highly valuable to collectors.
Stay Curious
Subscribe to the Strange Sounds newsletterfor daily cosmic weirdness, meteor impacts, fireball sightings and strange sky events.
