While the northern and southern boundary of the Caribbean Plate are complex and diffuse, with zones of seismicity stretching several hundred kilometers across, the eastern boundary is that of the Lesser Antilles subduction zone. This long subduction zone lacks a uniform curve and has an average dip of 50–60°. The largest known earthquake on the plate interface was a M7.5–8.0 event in 1843, but it did not generate a large tsunami. In opposition, the three largest events between 1950 and 1978 were intraplate normal faulting events.
Earthquake
The mainshock and the primary aftershock occurred on the previously mapped Roseau Fault, a, northeast-dipping normal fault that forms the western portion of the northwest-trending Les Saintes channel graben within the overriding North American Plate. Late 1990s bathymetric studies showed that it had vertical fault scarps approaching. The type of slip was primarily extensional, but included a small amount of left-lateral slip, and may have contributed to hydrological/volcanic effects that were observed on the island of Dominica, where a flooded fumarole drained twice.
Damage
A maximum intensity of VIII was recorded at Terre-de-Haut, where some serious damage occurred to a school, a church, and to some homes near the sugar loaf. The same intensity was observed at Terre-de-Bas, where damage was moderate and non-structural in nature. At Petite-Anse, a small area contained some damaged walls, but no complete collapses occurred. At Grand-Bourg on the island of Marie-Galantethe town hall, a church, and a college were red-tagged. The same intensity was assigned to the nearby commune of Saint-Louis, where the newly built town hall had visible cracks and the church was closed due to the potential of aftershocks breaking stained glass windows.
Boiling Lake
In the weeks following the mainshock, no abnormal geochemical or seismic activity was observed at La Grande Soufrière on Guadaloupe, but on southern Dominica near the Valley of Desolation, a flooded fumarole known as Boiling Lake was discovered empty by tourists on Christmas Day. The deep lake lies in an active geothermal area and is normally stable in terms of temperature and water level. By mid-February the lake was again full again, but the temperature had not returned to normal, and the water level dropped again following the M5.8 aftershock on February 14.
Aftershocks
By mid-February, aftershock activity had essentially ceased, with events becoming increasingly far apart. On February 14, a strong and slightly-damaging aftershock occurred. This was also a normal slip event that occurred about to the northwest of the November 21 mainshock. The damage was minimal, with cracks developing on the roads, some broken water pipes, and wall and roof damage.
Tsunami
A small tsunami took place following the shock, and while no tide gauges captured the event, scientists were on scene within several days to investigate. A large storm occurred on the day of the event, and this might have prevented visual observation of the tsunami, but witnesses on Guadelouple reported that the sea dropped "a few" to as many as. At Anse des Mûriers on Îles des Saintes, a ship captain reported that three minutes after the earthquake the sea dropped about and also receded from the coast about. Investigators documented a runup at Grande-Anse and a runup was measured at Anse Pajot, but these findings were difficult to distinguish from the storm surge.
