Sagami Trough
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Sagami Trough also Sagami Trench is a trough where the Kanto earthquakes of 1703 and 1923 arose. It stretches from the Boso Triple Junction where it meets the Japan Trench to Sagami Bay. It runs north of the Izu Islands chain and the Izu-Bonin-Mariana Arc (IBM). In geology, a trough generally refers to a linear structural depression that extends laterally over a distance, while being less steep than a trench. A trough can be a narrow basin or a geologic rift.…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. The Sagami Trough also Sagami Trench is a trough where the Kanto earthquakes of 1703 and 1923 arose. It stretches from the Boso Triple Junction where it meets the Japan Trench to Sagami Bay. It runs north of the Izu Islands chain and the Izu-Bonin-Mariana Arc (IBM). In geology, a trough generally refers to a linear structural depression that extends laterally over a distance, while being less steep than a trench. A trough can be a narrow basin or a geologic rift. There are various oceanic troughs, troughs found under oceans; examples include the rift along the mid-oceanic ridge and the Cayman Trough.