Skip to main content

Table 2 Thematic map data used for comparison with the terrain classification of the current study

From: Classification of topography for ground vulnerability assessment of alluvial plains and mountains of Japan using 30 m DEM

Data no.

Range

Dataset, map

Creator/publisher

Subject

Map scale/resolution

Usage in this study

1

Nationwide

Seamless digital geological map of Japan (SDGM)

GSJ (ed.) (2015)

GSJ (ed.) (2019)

Geology

1:200,000

Grouping decision, subdivision of the groups

2

Nationwide

Japan engineering geomorphologic classification map (JEGM) ver. 3

Wakamatsu and Matsuoka (2013)

Landform

250 m grid

Grouping decision, subdivision of the groups

3

Urban plains and their surroundings

GIS data of landform classification

GSI (maps are available on the GSI Maps (GSI 2020))

Landform

Compilation of 1:25,000 Land Condition Map and Landform Classification Map for Flood Control

Comparison, subdivision of the groups

4

Nationwide

Landslide Distribution Maps

NIED (2015)

Major landslide (often deep-seated)

1:50,000

Grouping decision

5

5 regions (total 98 km2)a

Inventory of landslides

Iwahashi et al. (2012)

Small or shallow landslides

Interpolated from 2 m LiDAR and 20–50 cm orthoimageries

Grouping decision

6

Iburi, Hokkaido (approximately 400 km2)b

Inventory of landslides

Yamagishi and Iwahashi (2020)

Shallow landslides

Interpolated from 1 and 2 m LiDAR and orthoimageries

Grouping decision

7

Western Japanc

Inventory of landslides

GSI (2016)

GSI (2018)

Small or shallow landslides

Interpolated from aerial digital photographs

Grouping decision

8

Eastern Japand

Estimated inundation areas

GSI (2019)

Flood area

Estimated by aerial photographs and 5 m DEMs

Visual observation

  1. aThe study areas include small or shallow landslides distributed in Izumozaki (caused by the August 1961 and July 2004 heavy rainfalls), Niihama (caused by the September–October 2004 heavy rainfalls), Houfu (caused by the July 2009 heavy rainfalls), Hanokidachi, and the Kurikoma-dam regions (caused by the 2008 Iwate–Miyagi Nairiku earthquake (Mw. 6.9))
  2. bCoseismic shallow landslides on the slopes covered by volcanic pumices by the 2018 Hokkaido Eastern Iburi earthquake (Mw 6.6)
  3. cThe data include landslides caused by the 2016 Kumamoto earthquake (Mw 7.0) (GSI 2016) and shallow landslides caused by the July 2018 heavy rainfalls in Iwakuni, Hiroshima, Eastern Hiroshima, and Ohsu–Uwajima regions (GSI 2018)
  4. dEstimated inundation areas caused by the 2019 Typhoon Hagibis (GSI 2019)