Geological Map of the UNESCO site of Ḫattuša (Türkiye)

We present the Geological Map of the UNESCO archaeological site of Ḫattuša in Türkiye. The mapped ∼5 km2 area is characterized by different superposed thrust sheets of the Upper Jurassic-Cretaceous Ankara Mélange succession, which is covered by Quaternary deposits. Here, the Ankara Mélange consists of an ophiolitic sequence comprising massive, layered and pillow basalts, gabbros and serpentinites, overlain by a sedimentary oceanic succession including argillites, sandstones, radiolarites, and cherty limestones, and finally capped by channelized calcareous conglomerates. The orogenic architecture is defined by older top-to-the-S thrusts, subsequently deformed by top-to-the-N back-thrusts. High-angle normal, transtensive, transpressive and strike-slip faults crosscut the orogenic pile. The geological map of Ḫattuša represents an important contribution to the understanding of the unique and complex geological setting that characterizes this region. On the other hand, it is also a crucial piece in the mosaic for assessing the relationship between man and the environment.

Authors

Institutions

Publication Details

Journal
Journal of Maps
Published
2025-09-23
DOI
https://doi.org/10.1080/17445647.2025.2556323
Primary Topic
Building materials and conservation
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Geological Map of the UNESCO site of Ḫattuša (Türkiye)

Stefano Vitale, Giovanni Varriale, Andreas Schachner
Journal of Maps
Building materials and conservation
article

Geological Map of the UNESCO site of Ḫattuša (Türkiye)

Stefano Vitale, Giovanni Varriale, Andreas Schachner
article en

Abstract

We present the Geological Map of the UNESCO archaeological site of Ḫattuša in Türkiye. The mapped ∼5 km2 area is characterized by different superposed thrust sheets of the Upper Jurassic-Cretaceous Ankara Mélange succession, which is covered by Quaternary deposits. Here, the Ankara Mélange consists of an ophiolitic sequence comprising massive, layered and pillow basalts, gabbros and serpentinites, overlain by a sedimentary oceanic succession including argillites, sandstones, radiolarites, and cherty limestones, and finally capped by channelized calcareous conglomerates. The orogenic architecture is defined by older top-to-the-S thrusts, subsequently deformed by top-to-the-N back-thrusts. High-angle normal, transtensive, transpressive and strike-slip faults crosscut the orogenic pile. The geological map of Ḫattuša represents an important contribution to the understanding of the unique and complex geological setting that characterizes this region. On the other hand, it is also a crucial piece in the mosaic for assessing the relationship between man and the environment.

Journal of MapsVol. 21(1)
Deutsches Archäologisches Institut, Abteilung Rom (IT), University of Naples Federico II (IT)
Openalex Percentile: Top 72%
Building materials and conservation
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.

Geological Map of the UNESCO site of Ḫattuša (Türkiye) — Stefano Vitale, Giovanni Varriale, et al. · Journal of Maps (2025) | TGRS Research Map | TGRS