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Kantō Plain

.mw-parser-output .geo-default,.mw-parser-output .geo-dms,.mw-parser-output .geo-dec{display:inline}.mw-parser-output .geo-nondefault,.mw-parser-output .geo-multi-punct,.mw-parser-output .geo-inline-hidden{display:none}.mw-parser-output .longitude,.mw-parser-output .latitude{white-space:nowrap}36°00′N 140°00′E / 36.000°N 140.000°E / 36.000; 140.000

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Kantō Plain

Nodes63
Edges62
Triples43
Avg. degree1.97
Density0.031746
Components1

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Kantō Plain

Top relations

related to Geography · 38
Kantō Plain → Abukuma Highlands, Akagi, Among, Arakawa River, Ashio Mountain Range, Bōsō Peninsula, Fuji, Haruna, In, Japan, Jōsō, Kantō Mountain Range, Kinu River, Kokai River, Kuji River, Kujūkuri Beach, Miura Hills, Most, Mounts Asama, Mounts Hakone

Important terminology Word statistics

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Important terminology

plain plateaus tokyo kantō central kanto 000 northern western hills sea part surrounding north mountains due region japan rivers river

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
the eastern margin of the Fossa Magnainstance ofLarge tectonic lines0.80text
the Median Tectonic Line are thought to exist in the central part of the plaininstance ofLarge tectonic lines0.80text
but this thick accumulation of soft sedimentary layers makes it difficult to find active faults that can cause earthquakesinstance ofLarge tectonic lines0.80text
sediment carried by rivers have been used to create landinstance ofnatural sediments0.80text
and the terrain was almost the same as it is today in the Late Jomon to Early Yayoi Periodinstance ofnatural sediments0.80text
Kantō Plainrelated to GeographyThe0.60section
Kantō Plainrelated to GeographyAbukuma Highlands0.60section
Kantō Plainrelated to GeographyYamizo Mountain Range0.60section
Kantō Plainrelated to GeographyAshio Mountain Range0.60section
Kantō Plainrelated to GeographyNasu Volcanic Belt0.60section
Kantō Plainrelated to GeographyKantō Mountain Range0.60section
Kantō Plainrelated to GeographyBōsō Peninsula0.60section

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    Min side: 3
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