Translation guide
A slow earthquake is a type of earthquake that releases energy over a longer period than ordinary earthquakes, often imperceptible to humans. In Japanese, it is typically expressed using the technical term スロー地震 or the more descriptive ゆっくり地震.
The scientific term for a slow earthquake, used in seismology and earth science.
The most common technical term, a direct loan from English. Used in academic and news contexts.
Explaining the concept to a non-specialist audience.
A natural way to describe a slow earthquake in everyday language, using the adjective 'yukkuri to shita' (slow).
In scientific contexts, スロー地震 is the standard term. For general audiences, ゆっくりとした地震 or ゆっくり地震 are more accessible. Avoid literal translations like 遅い地震, which sounds unnatural.
Slow earthquakes last longer than ordinary earthquakes.
A more descriptive term using the native Japanese word for 'slow'. Less formal but still used in scientific communication.
Slow earthquakes cannot be felt by humans.
Refers specifically to low-frequency earthquakes, a type of slow earthquake. Used in specialized research.
Low-frequency earthquakes are a type of slow earthquake.
In this region, slow earthquakes occur frequently.
Short for 'slow slip event', often used in news reports about slow earthquakes that involve gradual fault movement.
A slow slip event was observed.