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[* Not included on published map. Ma = million years ago. D = diameter.] |
No. |
Crater (location) |
Date |
Importance |
Lat |
Long |
1* |
Suavjärvi (Russia) |
~2400 Ma |
Apparently the oldest known crater, it is still recognizable despite obscuring by post-impact geological processes. |
63.1 N |
33.4 E |
2 |
Vredefort (South Africa) |
2023 ± 4 Ma |
Largest known structure (D=300 km); unique textural features indicate high-pressure shock impact. |
27.5 S |
27.5 E |
3 |
Sudbury (Ontario, Canada) |
1850 ± 3 Ma |
This large crater (D=200 km) is the only one with shock-melted body that hosts rich nickel-copper ore deposits. |
46.6 N |
81.2 W |
4* |
Shoemaker (Australia ) |
1630 ± 5 Ma |
Fourth oldest of ~170 known craters; named for the late Eugene Shoemaker, "Father of planetary geology." |
25.9 S |
120.9 E |
5 |
Acraman (Australia) |
~590 Ma |
Discovered by identifying and mapping distant impact breccia layer in surrounding late pre-Cambrian rocks. |
32.0 S |
135.5 E |
6* |
Lockne (Sweden) |
>455 Ma |
Impacting bolide entered shallow water; key features of resulting crater now preserved on uplifted land. |
63.0 N |
14.8 E |
7* |
Brent (Ontario, Canada) |
396 ± 20 Ma |
Pioneering Canadian studies in 1950s and 1960s of this buried structure advanced understanding of impact processes. |
46.1 N |
78.5 W |
8 |
Clearwater (Quebec, Canada) |
290 ± 20 Ma |
Rare paired craters (D= 26 and 36 km) formed by two close but separated bolides. |
56.2 N |
74.5 W |
9* |
Araguinha (Brazil) |
244.4 ± 3.25 Ma |
Largest crater in South America; tree cover makes craters hard to find in the tropics, and few are known. |
16.8 S |
53.0 W |
10* |
Manicouagan (Quebec) |
214 ± 1 Ma |
Deep erosion has revealed Earth's only complex, multi-ring structure-common on the moon. |
51.4 N |
68.7 W |
11* |
Puchezh-Katunki (Russia) |
167 ± 3 Ma |
Among the eight largest craters known, this is the smallest (D=80 km) shown at true scale on main map. |
57.0 N |
43.7 E |
12* |
Chukcha (Russia) |
<70 Ma |
Northernmost crater known (see Arctic map). Ice hides (and erodes) many craters at high latitudes. |
75.7 N |
97.8 E |
13 |
Chicxulub (Mexico) |
64.98 ± 0.05 Ma |
Produced K/T (dinosaur) extinction event and global ejecta (with "fingerprint" iridium layer); see Inset VI. |
21.3 N |
89.5 W |
14 |
Montagnais (Nova-Scotia) |
50.50 ± 0.76 Ma |
First crater recognized at sea (buried on continental shelf); nearly all other known craters are on land. |
42.9 N |
64.2 W |
15 |
Wanapitei (Ontario) |
37.2 ± 1.2 Ma |
Younger, smaller crater inside Sudbury (no.3); only known example of a second impact in the same place. |
46.8 N |
80.8 W |
16 |
Popigai (Russia) |
35.7 ± 0.2 Ma |
Detailed studies of this large (D=100 km) crater discovered diamonds produced by high-pressure shock waves. |
71.6 N |
111.2 E |
17 |
Chesapeake Bay (Virginia, USA) |
35.5 ± 0.3 Ma |
Largest crater in USA (D=85 km), buried by younger sediments, was discovered in 1980s by geophysical surveys. |
37.3 N |
76.0 W |
18* |
Ries (Germany) |
15.1 ± 0.1 Ma |
New rock type, suevite, a mix of broken bedrock fragments and impact-melt glass, discovered in well-studied crater. |
48.9 N |
10.6 E |
19* |
Bosumtwi (Ghana) |
1.07 Ma |
Source of tektites — small, glassy blobs of impact melt strewn far to the west — forming Ivory Coast tektite field. |
6.5 N |
1.4 W |
20* |
Monturaqui (Chile) |
<1 Ma |
Shock-melted impactite, containing Ni-Fe spherules from the impacting meteorite, is found here. |
23.9 S |
68.3 W |
21* |
Río Cuarto (Argentina) |
<0.1 Ma |
Southernmost crater, and elliptical; only known crater formed by stony, rather than far less common iron, meteorite. |
32.9 S |
64.2 W |
22* |
Lonar (India) |
0.052 ± 0.006 Ma |
Well-preserved crater formed in basalt lava surface; affords unique comparisons with craters in similar lunar lavas. |
20.0 N |
76.5 E |
23 |
Barringer (Meteor)(Arizona, USA) |
0.049 ± 0.003 Ma |
"Textbook" crater (see Inset VI) — the first recognized as caused by meteorite impact — was used in astronaut training. |
35.0 N |
111.0 W |
24* |
Haviland (Kansas, USA) |
<0.001 Ma |
Unusual meteorites found near a 15 m-wide buffalo wallow, shown to be an impact crater by excavations in 1929. |
37.6 N |
99.2 W |
25 |
Sikhote Alin (Russia) |
0.000055 Ma |
Large meteorite shower, seen by many in 1947, left >100 small craters and >8000 meteorites over ~ 50 km2 area. |
46.1 N |
134.7 E |
No. |
Volcano (location) |
Date |
Importance |
Lat |
Long |
1 |
Yellowstone (Wyoming, USA) |
2 Ma |
Huge eruption (2500 km3 of magma) blanketed western U.S. with ash (>2 cm in California, 1500 km away; see inset V). |
44.4 N |
110.7 W |
2 |
Santorini (Greece) |
1640 B.C. |
Bronze Age caldera-forming eruption influenced decline of Minoan civilization; tsunami may have inspired biblical flood legends. |
36.4 N |
25.4 E |
3 |
Etna (Italy) |
1500 B.C. |
First historically documented eruption; Europe's largest volcano, Etna has been frequently active since. |
37.7 N |
15.0 E |
4 |
Vesuvius (Italy) |
A.D. 79 |
Pompeii and Herculaneum buried; earliest known written account for any eruption, by Pliny the Younger. |
40.8 N |
14.4 E |
5 |
Taupo (New Zealand) |
~180 |
16,000 km2 (15% of North Island) devastated; only a deceptively tranquil caldera lake now marks the eruption site. |
38.8 S |
176.0 E |
6 |
Rabaul (Papua New Guinea) |
540±90 |
Caldera- (and harbor-) forming eruption; regional volcano observatory established after 1937 eruption. |
4.3 S |
152.2 E |
7 |
Ojos del Salado (Chile) |
~700 |
World's highest active volcano, at 6,887 m; no known historical eruptions, but strong fumarolic activity. |
27.1 S |
68.5 W |
8 |
Lakí-Grimsvötn (Iceland) |
1783 |
Enormous lava flows; livestock poisoned by volcanic fluorine and 10,000 Icelanders starve; cooled Europe's climate. |
64.4 N |
17.3 W |
9 |
Unzen (Japan) |
1792 |
Japan's deadliest eruption; collapse of dome produced debris avalanche and tsunami, killing 14,500. |
32.8 N |
130.3 E |
10 |
Tambora (Indonesia) |
1815 |
Largest historical explosive eruption, resulting in ~60,000 deaths and 1816's "year without summer" (June snow in New England!). |
8.3 S |
118.0 E |
11 |
Krakatau (Indonesia) |
1883 |
Caldera collapse; 40-m-high tsunamis kill >34,000; explosions heard >4500 km away; vivid sunsets. |
6.1 S |
105.4 E |
12 |
Mont. Pelée (West Indies) |
1902 |
High-speed, incandescent pyroclastic flows kill 28,000 in minutes; response launched modern volcanology. |
14.8 N |
61.1 W |
13 |
Santa María (Guatemala) |
1902 |
5,000 killed when volcano erupts after long repose; growth of lava dome began 20 years later and continues to date. |
14.8 N |
91.6 W |
14 |
Novarupta-Katmai (Alaska, USA) |
1912 |
Largest 20th century eruption (including "Valley of Ten Thousand Smokes"); sound heard 1200 km away; climate affected globally. |
58.3 N |
155.2 W |
15 |
Parícutin (Mexico) |
1943 |
Volcano birth in cornfield witnessed by farmers; cinder cone grows to 336-m height in first year, to 424 m by 1952. |
19.5 N |
102.3 W |
16 |
Surtsey (Iceland) |
1963 |
New island formed by 4-year eruption, providing field laboratory for biologists to study arrival of flora and fauna to new land. |
63.4 N |
20.3 W |
17 |
Tolbachik (Kamchatka) |
1975 |
Eruption time and place accurately predicted (TV crews were on hand), in world's most volcanically active region. |
55.8 N |
160.3 E |
18 |
Nyiragongo (Congo) |
1977 |
Highly fluid flows from summit lava lake reached speeds of 60 km/hr; slower flows in 2002 engulfed center of Goma city. |
1.5 S |
29.3 E |
19 |
Mount St. Helens (Washington, USA) |
1980 |
Well-studied landslide, later found to be common worldwide, showed that flank collapse can trigger explosive eruptions. |
46.2 N |
122.2 W |
20 |
Kilauea (Hawaii, USA) |
1983 |
Start of ongoing rift eruption, longest-running in Hawaii since A.D. 1400; has already created ~2.2 km2 of new land. |
19.4 N |
155.3 W |
21 |
Ruiz (Colombia) |
1985 |
Small eruption melted icecap of 5,389-m-high volcano; resulting mudflows killed >22,000, in towns >40 km from crater. |
4.9 N |
75.3 W |
22 |
Oshima (Japan) |
1986 |
Highest historical lava fountains (>1,500 m); this island south of Tokyo has erupted more than 80 times since A.D. 605. |
34.7 N |
139.4 E |
23 |
Redoubt (Alaska, USA) |
1989 |
Jumbo jet's engines all fail in ash cloud, but two were restarted 1500 m above mountains; $80 million damage to plane. |
60.5 N |
152.8 W |
24 |
Pinatubo (Philippines) |
1991 |
Evacuations save up to 20,000 lives; mudflow damage, some recurring long after eruption ended, leaves >200,000 homeless. |
15.1 N |
120.4 E |
25 |
Juan de Fuca Ridge (off NW USA) |
1993 |
First well—documented deep ocean eruption-world's most common type, but never witnessed—along divergent boundary (see inset I). |
46.5 N |
129.6 W |
| [M = magnitude. Magnitudes listed here are selected from technical articles on these events and may differ from published catalog values] |
No. |
Earthquake (location) |
Date |
Importance |
Lat |
Long |
1 |
Shanxi (eastern China) |
1556 |
Deadliest earthquake on record with 830,000 reported killed. Near Xian, China's ancient capital. |
35.5 N |
109.7 E |
2 |
Cascadia (Pacific NW, USA) |
1700 |
M ~9 shock; subsidence drowned local coastal forests and triggered tsunamis that damaged distant Japan. |
47.6 N |
125.1 W |
3 |
Lisbon (Portugal) |
1755 |
Offshore event that caused strong shaking, 6- to 15-m-high tsunami waves, and a fire in Lisbon that killed ~60,000. |
36.5 N |
11.3 W |
4 |
New Madrid (Missouri, USA) |
1811-12 |
Three very large shocks over a 2-month period rang church bells near Philadelphia and cracked ice in Chesapeake Bay. |
36.0 N |
90.0 W |
5 |
Charleston (South Carolina, USA) |
1886 |
Shaking felt from Bermuda to Minnesota; moderate to severe damage to masonry buildings in Charleston. |
32.9 N |
80.1 W |
6 |
Nobi (Japan) |
1891 |
Ground ruptures showed that movements along faults caused this M 8 earthquake. First modern aftershock study. |
35.4 N |
136.8 E |
7 |
Assam (northeastern India) |
1897 |
M >8 earthquake in Himalaya collision belt; Earth's liquid iron core deduced from its seismograms. |
26.0 N |
91.0 E |
8 |
North Shikoku Basin (Japan) |
1906 |
Earliest well-documented deep earthquake (340 km), showing that earthquakes can occur in Earth's deep mantle. |
34.0 N |
138.0 E |
9 |
San Francisco (California, USA) |
1906 |
M 7.8 shock on San Andreas fault; fire destroyed much of city (see inset VII). Stimulated earthquake science and elastic-rebound theory. |
37.8 N |
122.5 W |
10 |
Messina (Italy) |
1908 |
~85,000 dead from widespread effects of ground shaking, slope failures, fire, and a tsunami in the Strait of Messina. |
38.0 N |
15.5 E |
11 |
Zagreb (Croatia) |
1909 |
Mohorovicic discovered a jump in seismic-wave speeds, generally marking the crust-mantle boundary (the "Moho"). |
45.5 N |
16.1 E |
12 |
Gansu Province (China) |
1920 |
M 8.3-8.6 earthquake in the broad India-Eurasia collision belt. Widespread damage and ~200,000 deaths. |
36.6 N |
105.3 E |
13 |
Kanto (south of Tokyo, Japan) |
1923 |
M 7.9 subduction shock killed 146,000 (99,000 in Tokyo), including losses from a tsunami and giant firestorm. |
35.4 N |
139.1 E |
14 |
West Nelson (New Zealand) |
1929 |
Earth's solid inner core, inside the liquid outer core. revealed in its seismic records (by Inge Lehmann in 1936). |
41.8 S |
172.2 E |
15 |
Chillán (southern Chile) |
1939 |
Occurred at 80-km depth within the subducting Nazca slab, causing 28,000 deaths; led to improved building codes in Chile. |
36.2 S |
72.2 W |
16 |
Unimak Island (Alaska, USA) |
1946 |
M 8.5 shock triggered submarine landslide, generating tsunami with run-up to 31 m on nearby Unimak Island and 18 m in Hawaii. |
53.3 N |
163.0 W |
17 |
Offshore Kamchatka (Russia) |
1952 |
Seismograms of this well-recorded M 9 earthquake showed early evidence of slow, whole-earth vibrations. |
52.8 N |
159.5 E |
18 |
Adreanof Islands (Alaska, USA) |
1957 |
A M 9.1, second of only five earthquakes in the magnitude 9 range, all in a 12-year period, since global recording began around 1895. |
51.3 N |
175.8 W |
19 |
Valdivia (southern Chile) |
1960 |
Largest earthquake (M 9.5) yet recorded, confirming whole-earth vibrations; triggered a giant Pacific-wide tsunami. |
38.2 S |
72.6 W |
20 |
Southern Alaska (USA) |
1964 |
Second largest recorded earthquake (M 9.2) caused extensive soil failure in Anchorage area and widespread tsunami damage. |
61.1 N |
147.6 W |
21 |
Offshore northern Peru |
1970 |
Within Nazca slab at 73-km depth, killing ~54,000, including 25,000 at Yungay, a town buried by an associated rock avalanche. |
9.2 S |
78.8 W |
22 |
Tangshan (China) |
1976 |
Devastated the city, causing the most fatalities for a 20th century earthquake-estimates range from 255,000 (official) to 655,000. |
39.5 N |
117.9 E |
23 |
Northridge (California, USA) |
1994 |
Rocked the Los Angeles basin; economic loss estimated to exceed $20 billion, a record for U.S. earthquakes. |
34.2 N |
118.5 W |
24 |
Northwestern Bolivia |
1994 |
Deepest large-magnitude earthquake (M 8.3 at 636 km); shaking felt to Canada; whole-earth vibrations further refined Earth's structure. |
13.8 S |
67.6 W |
25 |
Kobe (Japan) |
1995 |
Major port city devastated: 5500 dead, 310,000 homeless, and world record $150 billion in earthquake and fire losses. |
34.6 N |
135.0 E |
26 |
Sumatra-Andaman (Indonesia) |
2004 |
M 9.0+ earthquake ruptures >1000 km of subduction boundary; tsunamis kill a record >230,000, some deaths as distant as Africa. |
3.31 N |
96.0 E |
| [Table not included on published map] |
This 400-yr history represents just 0.001 mm measured (0.000004 inch) at the same scale as the 550-million-year geological timeline at the bottom of the back of the map. |
|||
No. |
Scientist(s) |
Date |
Importance |
1 |
Abraham Ortelius (Holland) |
1596 |
Recognized the close geometrical fit of E & W Atlantic shorelines, suggesting separation of continents over time. |
2 |
James Hutton (Scotland) |
1785 |
Key idea in geology: "The present is the key to the past"; later championed by Lyell in Principles of Geology. |
3 |
Matthew Maury (USA) |
1855 |
Mid-Atlantic ridge discovered by wire depth soundings; data used for telegraph cable routing. |
4 |
Edward Suess (Austria) |
1890 |
Similarities in land fossils of southern continents suggest they were once joined as a supercontinent (Gondwanaland). |
5 |
Bernard Brunhes (France) |
1906 |
Earth's magnetism, recorded in rock minerals, shows rapid switching of north and south poles in geologic past. |
6 |
Alfred Wegener (Germany) |
1915-29 |
Advanced bold but controversial continental drift theory in four editions of Origin of Continents and Oceans. |
7 |
Arthur Holmes (UK) |
1928 |
Proposed mantle convection drives continental drift and mountain building; elaborated in 1930s by David Griggs. |
8 |
Kiyoo Wadati (Japan) |
1935 |
Inclined seismic zones are first mapped, under Japan; discussion of their origin anticipates the subduction concept. |
9 |
Maurice Ewing and Bruce Heezen (USA) |
1947-54 |
Seafloor sediments thicken with distance from Mid-Atlantic Ridge, suggesting bedrock ages increase similarly. |
10 |
Bill Menard and Bob Dietz (USA) |
1952 |
Fracture zones first mapped on seafloor; now known to be inactive transform faults (20) that record past plate motions. |
11 |
Marie Tharp, Bruce Heezen, and Maurice Ewing (USA) |
1953-61 |
A median rift (tensional) valley, a central magnetic anomaly, and earthquakes characterize the Mid-Atlantic Ridge. |
12 |
Ted Irving (Australia), Keith Runcorn (UK) |
1956 |
Earth's former magnetic pole positions, recorded in rocks, differ among continents, but are reconciled by continental drift. |
13 |
Ron Mason, Arthur Raff, and Victor Vacquier (USA) |
1958-62 |
Seafloor magnetic anomalies off western US show a striped pattern and some are offset at fracture zones. |
14 |
Harry Hess, Bob Dietz (USA) |
1960-62 |
Ocean basins open along ridges by seafloor spreading, carrying continents along (conveyor belt analogy). |
15 |
Bob Coats, Jack Oliver, and Bryan Isacks (USA) |
1961-67 |
Subduction process is conceived, explaining the occurrence of arc volcanoes and earthquakes along narrow zones. |
16 |
Many scientists (mostly USA) |
1961-69 |
New global seismic network improves accuracy of earthquake locations, helping resolve and define plate boundaries. |
17 |
Tuzo Wilson (Canada) |
1963a |
Hotspot concept explains trends of intraplate volcanic island chains; helps track past plate motions. |
18 |
Allan Cox, Richard Doell, Brent Dalrymple (USA) |
1963b |
Time scale of magnetic polarity reversals (5) is derived from radiometric ages of magnetized rocks. |
19 |
Fred Vine & Drum Matthews (UK), Larry Morley (Canada) |
1963c |
Magnetic stripes (13) record magnetic polarity reversals (18) during spreading (conveyor belt is also a tape recorder). |
20 |
Tuzo Wilson (Canada) |
1964-65 |
Transform faulting conceived; later confirmed from fault motions for earthquakes by Lynn Sykes. |
21 |
Lynn Sykes, Wm Stauder, Bryan Isacks, Peter Molnar (USA) |
1966-72 |
Earthquake activity and fault motions, deduced from seismic records, reflect and help define plate motions. |
22 |
Jason Morgan (USA), Dan McKenzie & Bob Parker (UK) |
1967 |
Plate motions quantitatively modeled; later refined by Le Pichon, Chase, Minster & Jordan, and others. |
23 |
International drilling programs (DSDP/ODP) |
1968-on |
Drilling of seafloor and dating of those rocks confirm seafloor ages predicted by the spreading model. |
24 |
US Navy/NASA, Bill Haxby, Sandwell & Smith (USA) |
1978-on |
Marine gravity and seafloor relief mapped by satellite radar echoes from small-but-measurable effect on sea level. |
25 |
NASA, Dept of Defense, and many others (USA) |
1985-on |
Astronomical and satellite survey methods (such as GPS) accurately measure present-day plate motions. |
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