Site |
Location |
N Lat º |
W Long º |
Description |
Runup Height (cm)* |
Coseismic Uplift (cm)* |
Site Characteristic |
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Costa Rica |
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1 |
Boca del Rio Matina |
10.12º |
83.19 º |
The water retreated 400 m followed by large waves that flooded 180 m inland. Two drownings occurred in the canal near Matina. Widespread liquefaction. Dead fish were observed following the tsunami. |
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Beach/ River Mouth |
2 |
Boca del Pantano |
10.07º |
83.16º |
The water first receded ~100 m and then returned within 3 min without flooding. |
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Beach |
3 |
12 Millas de Moin |
10.07º |
83.16º |
Two minutes after the earthquake, a 2 m wave flooded 30 to 70 m inland. Sand movement. |
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Beach |
4 |
6 Millas de Moin |
10.00º |
83.10º |
The water slowly retreated about 20 m |
135 |
|
Beach |
5 |
Moin |
10.00º |
83.08º |
The water retreated about 200 m. A sea wave overtopped 3 m high dikes in the Moin River. |
|
125-140 |
Harbor/ River Mouth |
6 |
Westfalia |
9.94º |
83.00º |
The water retreated about 200 m and returned to the shoreline without appreciable runup or flooding. Sand movement. |
130 |
74 |
Beach |
7 |
Cahuita |
9.74º |
82.84º |
The sea receded 75 m then returned slowly to a level lower than previous. Dead fish were observed. |
|
38 |
Reefs |
8 |
Puerto Viejo |
9.66º |
82.76º |
The sea receded 100 m followed by a large wave, receded again and was followed by a large wave with 30 -70 m runup. Sand movement and dead fish were also noted. |
155 |
38-45 |
Reefs |
9 |
Final de Cocles |
9.64º |
82.72º |
The sea receded 20 m then returned slowly over a 5 - 6 min period with no runup. |
|
29-54 |
Beach and Cliffs |
10 |
Punta Uva |
9.64º |
82.69º |
Water retreats 400-600 m |
200 |
40-45 |
Beach |
11 |
Manzanillo |
9.63º |
82.66º |
The sea receded 180 m and returned in 5 min to flood 30 to 70 m inland. Sand movement and 1.5 m sand mounds were deposited. |
83-130 |
30-40 |
Beach |
12 |
Gandoca |
9.60º |
82.60º |
The sea receded 300 m in 5 min and returned to flood about 70 m inland. Sand Movement. |
125 |
30-40 |
Beach |
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Panama |
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13 |
San-San Natural Refuge |
9.54º |
82.53º |
Tsunami waves deposited a great deal of sand on the beach near the mouth of the San-San River, a wildlife refuge near the Costa Rica border, creating dunes which covered numerous turtle nests with approximately 1 m of sand and caused a decrease in the number of newborn turtles (see Fig. 6). |
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Beach |
14 |
|
9.51º |
82.49º |
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15 |
Playa de Julio Abrego |
9.43º |
82.41º |
A farmer reports that the before the quake occurred, the sea was very quiet. Minutes after the event the sea receded between three and six times. The last wave was the largest and the water penetrated 100 m inland. The NE-SW trend of fallen palm trees and other types of vegetation surrounded by sand and onshore flooding is seen in Fig. 4. |
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|
Beach |
16 |
Changuinola River/ Tiribibi Pt. |
9.42º |
82.38º |
Figure 5 shows the onshore flooding in this area and a zone of brown grass and vegetation parallel to the coastline. Sand deposition and fast currents |
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Beach |
17 |
Lime Point (Boca del Drago) |
9.41º |
82.33º |
Every person interviewed at this location reports that the sea was very quiet before the earthquake; but one-half to one hour before the event the sea was unusually warm. The sea receded approximately six times out to the coral reefs (approximately 100 m from shore) which looked like a stone wall. All six times the sea returned with a great roar and noise. The last wave was estimated to be 2 m high and flooded parts of the coastal road. This estimate was verified in the field by one of the authors (E. Camacho). The following day, the Boca del Drago passage had many dead fish floating in the water. Sea recedes 6 times and exposed reefs. Flooded coastal roads |
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Reef |
18 |
West Knapp Hole |
9.41º |
82.33º |
This site is located in the coast facing Almirante Bay. Before the earthquake, the sea was calm. Minutes after the quake, there was a great turbulence in the sea, similar to rapids of the strong current of a river. The strong current flooded from 5 to 10 m of the beach. Great turbulence with strong currents observed after earthquake. 5-10 m runup |
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Beach on Almirante Bay |
19 |
Ground Creek |
9.40º |
82.31º |
The sea was quiet before the quake. Water receded several times and returned as a strong river current approximately 0.6 m high, which deposited many fish along the banks of the creek which were flooded in some parts up to 10 m inland. Water receded, returns as strong current 0.6 m high. 10 m runup |
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Beach on Almirante Bay |
20 |
Punta Cauro |
9.43º |
82.32º |
This site faces the Caribbean Sea. The sea was quiet before the earthquake. The sea receded five times and returned making great noise. One witness left some clothes drying on a rock some 2 m or more above the surface of the water near a cliff. After the high waves ceased, she returned to get her clothes, and discovered they had been taken by the waves. She thinks the last wave was the one that took her clothes. A few days later, she recovered her clothes, which may have been brought back by the strong sea currents which run parallel to the coast in this area. Water receded 5 times and the last wave was ~ 2 m high. |
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Beach with Cliffs |
21 |
Boket Bay |
9.43º |
82.30º |
This site faces the Caribbean Sea. Ten to fifteen minutes after the earthquake, a 2.5 to 3 m high wave was observed from a house standing on top of a hill.2.5-3.5 m wave 10-15 min after earthquake. |
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Cove |
22 |
Bocas del Toro |
9.34º |
82.25º |
The sea was quiet before the earthquake. Ten minutes after the event, the sea receded approximately 400 m from the cove facing the town. The sand bar, Las Delicias (Grassy Bank) which is usually covered by 0.6 to 0.7 m of water, emerged and remained subareal from 5-7 minutes. After this period, several 0.6 to 0.7 m high waves started to enter the cove with great force. The water was full of sediment and flooded 100 to 150 m inland, mainly on the north part of town, which is located in an extremely flat area. Water receded 10 min after earthquake and exposed an offshore sandbar usually 0.6 m deep. Wave runup 10-15 m. |
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Reef |
23 |
Nancy Key |
9.33º |
82.22º |
As observed from Hospital Point, 10 to 15 minutes after the earthquake, the sea receded several times and returned as a strong river current from Bocas del Toro passage. Water receded several times and returned as a strong current. |
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Point |
24 |
Isla San Cristobal |
9.29º |
82.27º |
In the northwest portion of the island, in the mouth of Paloma Creek, the sea receded several meters for approximately 45 minutes. Many fish got trapped in the dry terrain. The water returned as a slow wave recovering the areas that had emerged minutes before. .Sea recedes several meters for 45 min, water returns as a slow wave. |
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Creek |
25 |
Isla Carenero |
9.34º |
82.23º |
Approximately 15 to 20 minutes after the earthquake, the sea receded, and the usually submerged sand bank Las Delicias could be seen for about 15 minutes. The sea returned with just one very gentle wave and penetrated 100 to 150 m inland crossing the southern tip of the island, which is an extremely flat area. The inhabitants that remained on the island report that the water reached to their knees. The southern portion of the island remained flooded for approximately 20 minutes before the sea receded with great strength back to its original stage. Sea receded 15-20 min after earthquake, remained out for ~ 15 min and returns as gentle wave with 100-150 m run up |
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Beach |
26 |
Isla Bastimentos |
9.35º |
82.21º |
In the northwest portion of the island, known as Old Bank, the sea receded several meters 10 to 15 minutes after the earthquake. Some submarine vegetation could be seen during this period of time before the sea gently returned 15 minutes later. The sea receded 10-15 min after earthquake and returned gently. |
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Reef |
* Runup heights and coseismic uplifts from Plafker and Ward (1992). Site specific information is provided in Appendix 2 of the Electronic Supplement. |
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