Julia García‐Oteyza
Biographic Data
| ID | 9111178 |
|---|---|
| NAME | Julia García‐Oteyza |
| GIVEN NAMES | Julia |
| FAMILY NAME | García‐Oteyza |
| SIGNATURE | OTEYZA J G |
| AFFILIATIONS | Universidad Complutense de Madrid |
| ORCID | 0000-0002-0187-2922 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2023 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Saimaluu-Tash I Rock Art (Kyrgyzstan)
Saimaluu-Tash I, located in a high-altitude glacial valley in Kyrgyzstan, preserves one of Central Asia’s largest and most culturally significant concentrations of rock engravings. Despite extensive archaeological research, the physical, mechanical, and chromatic properties of the sandstone substrates relevant for conservation assessment remain poorly characterized. This study integrates petrographic microscopy, scanning electron microscopy, colo…
Holocene glacial evolution in Quingaussarsuaq Peninsula (Central–West Greenland)
The Greenland Ice Sheet (GrIS) is a key component of the global climate system, and constraining the Holocene deglaciation history of its land-terminating margins is key to understanding its sensitivity to climate forcing. Here, we provide insights into landscape evolution and environmental change on the Qinguassarsuaq Peninsula, Central–West Greenland 69°N, 50°W, where we used high-resolution geomorphological surveys and extensive field mapping …
Holocene glacial oscillations in the Tyroler Valley ( NE Greenland)
Although the spatiotemporal oscillations of the Greenland Ice Sheet (GrIS) during the last millennia have played a prominent role in global environmental changes, its glacial response to the natural variability still needs to be better constrained. Here, we focused on the reconstruction of the glacial behavior and deglaciation process along the Tyroler Valley (74° N, 22° E), within the Northeast Greenland National Park. This NW‐SE valley connects…
Holocene deglaciation of the northern Fildes Peninsula, King George Island, Antarctica
The timing and magnitude of Holocene glacial oscillations in most currently ice‐free areas of Antarctica remain unknown. This work focuses on the recent deglaciation in the northern sector of the Fildes Peninsula, King George Island, northern Antarctic Peninsula. The ice cap covering ca. 90% of the island has receded since the Last Glacial Maximum and exposed ca. 29 km 2 of ice‐free land. We reconstruct its glacial history based on a dataset of 1…
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Holocene glacial oscillations in the Tyroler Valley ( NE Greenland)
Although the spatiotemporal oscillations of the Greenland Ice Sheet (GrIS) during the last millennia have played a prominent role in global environmental changes, its glacial response to the natural variability still needs to be better constrained. Here, we focused on the reconstruction of the glacial behavior and deglaciation process along the Tyroler Valley (74° N, 22° E), within the Northeast Greenland National Park. This NW‐SE valley connects…
Holocene deglaciation of the northern Fildes Peninsula, King George Island, Antarctica
The timing and magnitude of Holocene glacial oscillations in most currently ice‐free areas of Antarctica remain unknown. This work focuses on the recent deglaciation in the northern sector of the Fildes Peninsula, King George Island, northern Antarctic Peninsula. The ice cap covering ca. 90% of the island has receded since the Last Glacial Maximum and exposed ca. 29 km 2 of ice‐free land. We reconstruct its glacial history based on a dataset of 1…
Saimaluu-Tash I Rock Art (Kyrgyzstan)
Saimaluu-Tash I, located in a high-altitude glacial valley in Kyrgyzstan, preserves one of Central Asia’s largest and most culturally significant concentrations of rock engravings. Despite extensive archaeological research, the physical, mechanical, and chromatic properties of the sandstone substrates relevant for conservation assessment remain poorly characterized. This study integrates petrographic microscopy, scanning electron microscopy, colo…
Holocene glacial evolution in Quingaussarsuaq Peninsula (Central–West Greenland)
The Greenland Ice Sheet (GrIS) is a key component of the global climate system, and constraining the Holocene deglaciation history of its land-terminating margins is key to understanding its sensitivity to climate forcing. Here, we provide insights into landscape evolution and environmental change on the Qinguassarsuaq Peninsula, Central–West Greenland 69°N, 50°W, where we used high-resolution geomorphological surveys and extensive field mapping …
Cryospheric studies and observations (3 works) · Deglaciation (3 works) · Geology and Paleoclimatology Research (3 works) · Glacial period (3 works) · Glacier (3 works) · Holocene (3 works) · Ice sheet (3 works) · Moraine (3 works) · Climate change and permafrost (2 works) · Geography (2 works)