(しんげん)

しんげん
noun
epicenter; hypocenter; source of a quake
1. epicenter; hypocenter; seismic center
The point of origin of an earthquake, either underground (hypocenter) or its projection on the surface (epicenter). A key term in earthquake-related news and information.
震源(しんげん)海底(かいてい)だった。
The epicenter was under the sea.
震源(しんげん)(ふか)さは(やく)10キロだった。
The depth of the hypocenter was about 10 kilometers.
気象庁(きしょうちょう)震源(しんげん)内陸(ないりく)(あさ)場所(ばしょ)であると発表(はっぴょう)した。
The Meteorological Agency announced that the hypocenter was at a shallow inland location.
2. source; origin; root cause
Figuratively, the origin or source of trouble, conflict, or a problem.
(かれ)問題(もんだい)震源(しんげん)だ。
He is the source of the problem.
その部署(ぶしょ)社内(しゃない)トラブルの震源(しんげん)になっている。
That department is the epicenter of internal trouble.
経済危機(けいざいきき)震源(しんげん)がどこにあるのか、専門家(せんもんか)(あいだ)でも意見(いけん)()かれている。
Even among experts, opinions are divided on where the source of the economic crisis lies.

USAGE:
震源(しんげん) combines (しん) (quake, tremor) and (げん) (source, origin). Strictly speaking, 震源(しんげん) refers to the underground point (hypocenter), while 震源地(しんげんち) refers to the surface location (epicenter), though the terms are often used interchangeably in casual speech.

COMMON COLLOCATIONS:

  • 震源(しんげん)(ふか)さ (depth of the hypocenter)
  • 震源地(しんげんち) (epicenter location)
  • 震源(しんげん)(ちか)い (close to the epicenter)

SIMILAR WORDS:
震源地(しんげんち) specifically refers to the surface point above the earthquake origin. 震源(しんげん) is more general and is also the form used in figurative senses.