Low-scarp morphology on Holocene-raised coral reef terraces in Kodakara Island, the central Ryukyus, Japan

Nozomu Hamanaka, Takehiro Okamoto, Tomoya Ohashi, Hironobu Kan

Research output: Contribution to journalArticle

3 Citations (Scopus)

Abstract

Numerous active faults in the Ryukyu Islands have been identified. However, relatively few studies and reports on the Holocene activity of these faults have been reported. Kodakara Island, which is part of the volcanic inner arc of the central Ryukyus, is fringed by well-developed Holocene-raised coral reef terraces, Terraces I, II, III in ascending order, that were formed by co-seismic uplifts. We found two continuous low scarps across the Holocene terraces. We verified whether low scarps are tectonic in origin or not on the basis of detailed field surveys such as mapping and measurements around the scarp, affirmations from inhabitants, and previous earthquake records. The low scarps are usually associated with ground fissures. The vertical displacements of T I and T II are 1, 5-1. 7 m and 0, 7 m, respectively, which indicate the accumulation of displacement. These characteristics indicate that the scarps may have formed by normal faulting during the Holocene. However, based on the presence of trees (Ficus microcarpa) with recently altered orientations beside the scarps, affirmations from inhabitants, and previous earthquake records, it seems likely that the scarps formed during seismic events that have occurred over the past three to four decades. Moreover, the timings of the scarp formations correspond to swarm earthquake activities, and their focus is not located on Kodakara Island, but near the island. This indicates the scarps have been formed as a result of swinging during recent swarm earthquake activities, not by faulting. Hence, we define the scarps as a landslide scarp associated with the characteristics of normal fault morphology. Our results imply that the area in the vicinity of Kodakara Island is currently tectonically active and that the scarps are likely to be displaced in future swarm seismic events.

Original languageEnglish
Pages (from-to)125-135
Number of pages11
JournalChikei
Volume30
Issue number2
Publication statusPublished - Apr 2009
Externally publishedYes

Fingerprint

coral reef
terrace
Holocene
earthquake swarm
faulting
earthquake
active fault
fissure
normal fault
field survey
landslide
uplift
tectonics
inhabitant

All Science Journal Classification (ASJC) codes

  • Earth-Surface Processes

Cite this

Low-scarp morphology on Holocene-raised coral reef terraces in Kodakara Island, the central Ryukyus, Japan. / Hamanaka, Nozomu; Okamoto, Takehiro; Ohashi, Tomoya; Kan, Hironobu.

In: Chikei, Vol. 30, No. 2, 04.2009, p. 125-135.

Research output: Contribution to journalArticle

Hamanaka, Nozomu ; Okamoto, Takehiro ; Ohashi, Tomoya ; Kan, Hironobu. / Low-scarp morphology on Holocene-raised coral reef terraces in Kodakara Island, the central Ryukyus, Japan. In: Chikei. 2009 ; Vol. 30, No. 2. pp. 125-135.
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