アンタルヤ
都市を選択
スコアは世界共通の尺度による研究推計です。R は作業中を示します。旅行の助言ではありません。
場所を調べる
ホテルが見つかりましたか?予約前に周辺エリアを確認しましょう。
検索サービスの方針
検索すると入力内容と選択都市を OpenStreetMap Nominatim に送信します。個人の住所や機密情報は入力しないでください。 検索サービスの方針
スコアは世界共通の尺度による研究推計です。R は作業中を示します。旅行の助言ではありません。
ホテルが見つかりましたか?予約前に周辺エリアを確認しましょう。
検索すると入力内容と選択都市を OpenStreetMap Nominatim に送信します。個人の住所や機密情報は入力しないでください。 検索サービスの方針
旅立つ前に、知っておこう
出典を伴う研究推計です。地域資料は不完全で、必要に応じて広域の代替値を使用します。
都市全体の研究推計:68/100。モデルの尺度では高いほど安全です。 根拠日付: · 資料の確かさ: D
研究推計:地域資料で裏付けられた1項目のみが変動し、他は都市・国の基準値を引き継ぎます。 空白の場所は地域資料がなく、安全を意味しません。
5地域を掲載 ·
境界: OpenStreetMap contributors · Five Antalya central districts (ODbL 1.0; © OpenStreetMap contributors)
都市スコアは個々の街路、ホテル、時間帯を表しません。レイヤーの出典、日付、制約を確認してください。
Compare Antalya central districts, including long-term earthquake exposure and source-linked safety context.
Five central Antalya districts: Muratpaşa, Kepez, Konyaaltı, Aksu and Döşemealtı. The layer does not cover the whole Antalya province or outlying resort districts. ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance. The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision. Only disaster_and_environment varies locally; the citywide estimate and other dimensions retain the existing Türkiye country research calibration. This map does not measure district crime or compare hotels. Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement. OpenStreetMap administrative boundaries retrieved 2026-10-27, generalized 10 m with less than 0.5% area change; © OpenStreetMap contributors, ODbL 1.0.
Five central Antalya districts: Muratpaşa, Kepez, Konyaaltı, Aksu and Döşemealtı. The layer does not cover the whole Antalya province or outlying resort districts. ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance. The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision. Only disaster_and_environment varies locally; the citywide estimate and other dimensions retain the existing Türkiye country research calibration. This map does not measure district crime or compare hotels. Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement. OpenStreetMap administrative boundaries retrieved 2026-10-27, generalized 10 m with less than 0.5% area change; © OpenStreetMap contributors, ODbL 1.0.
Five central Antalya districts: Muratpaşa, Kepez, Konyaaltı, Aksu and Döşemealtı. The layer does not cover the whole Antalya province or outlying resort districts.
ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance.
The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision.
Only disaster_and_environment varies locally; the citywide estimate and other dimensions retain the existing Türkiye country research calibration. This map does not measure district crime or compare hotels.
Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement.
OpenStreetMap administrative boundaries retrieved 2026-10-27, generalized 10 m with less than 0.5% area change; © OpenStreetMap contributors, ODbL 1.0.
alerts are not long-term baseline risk; event footprint may not equal traveler exposure; alert severity cannot be copied directly into Safrom score
country-level only; humanitarian risk framing differs from traveler exposure; composite inputs can overlap Safrom dimensions; current event conditions require separate signals
country-level only; reporting and justice-system differences; latest year differs by country; not traveler-specific
country-level only; availability does not measure emergency accessibility; latest year differs by country; distribution within a country is hidden
country-level only; collection is not annual for every country; some values are modeled estimates; resident exposure differs from traveler exposure
Syria and Iraq border restrictions do not describe Istanbul; legal risk differs from ordinary city crime; advisory level is not an absolute safety score; U.S.-traveler perspective
country-level only; modeled perceptions rather than traveler incidents; cannot represent neighborhood variation or current events; confidence intervals must not be discarded
ESHM20 mean peak ground acceleration (PGA, units g), annual exceedance probability 0.002103 (approximately 10% in 50 years / 475-year return period), reference rock Vs30=800 m/s. This is long-term modelled shaking, not earthquake prediction, observed damage, local soil amplification or building resistance.; The model uses a 0.1-degree grid (roughly 9–11 km here). District values are area-weighted nearest-cell aggregates in UTM 36N. Administrative outlines locate the aggregates and do not imply street-level seismic precision.; Danciu et al. (2021), The 2020 update of the European Seismic Hazard Model: Model Overview, EFEHR Technical Report 001, doi:10.12686/a15. CC BY 4.0 https://creativecommons.org/licenses/by/4.0/; Safrom computed district aggregates and research scores. No EFEHR endorsement.