Geomorphology of Stansbury Peninsula, Nelson Island, Antarctic Peninsula

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F25%3A00141831" target="_blank" >RIV/00216224:14310/25:00141831 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/10.1080/17445647.2025.2532561" target="_blank" >https://doi.org/10.1080/17445647.2025.2532561</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1080/17445647.2025.2532561" target="_blank" >10.1080/17445647.2025.2532561</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Geomorphology of Stansbury Peninsula, Nelson Island, Antarctic Peninsula

Popis výsledku v původním jazyce

The proglacial landscapes of Antarctica offer critical insights into past and ongoing deglaciation processes and the impacts of climate change. This study presents the first geomorphological map of the proglacial part of Stansbury Peninsula (Rip Point) and Cariz Cabo Cape in the northern part of Nelson Island. We identify and characterise a variety of glacial, proglacial, paraglacial, and periglacial landforms using high-resolution drone imagery, fieldwork, and geological data. The defined landforms presented reflect a complex interplay of erosional and depositional processes shaped by multiple glacial advance-retreat cycles since the Last Glacial Maximum, with evidence for significant glacial activity during the Holocene. The presence of hyaloclastite and crystalline erratic boulders further contributes to the reconstruction of glacial dynamics in the region. Our findings provide a crucial dataset and baseline for studies on future Antarctic deglaciation, periglacial processes, and the expansion of proglacial landscapes driven by ongoing climate change.

Název v anglickém jazyce

Geomorphology of Stansbury Peninsula, Nelson Island, Antarctic Peninsula

Popis výsledku anglicky

The proglacial landscapes of Antarctica offer critical insights into past and ongoing deglaciation processes and the impacts of climate change. This study presents the first geomorphological map of the proglacial part of Stansbury Peninsula (Rip Point) and Cariz Cabo Cape in the northern part of Nelson Island. We identify and characterise a variety of glacial, proglacial, paraglacial, and periglacial landforms using high-resolution drone imagery, fieldwork, and geological data. The defined landforms presented reflect a complex interplay of erosional and depositional processes shaped by multiple glacial advance-retreat cycles since the Last Glacial Maximum, with evidence for significant glacial activity during the Holocene. The presence of hyaloclastite and crystalline erratic boulders further contributes to the reconstruction of glacial dynamics in the region. Our findings provide a crucial dataset and baseline for studies on future Antarctic deglaciation, periglacial processes, and the expansion of proglacial landscapes driven by ongoing climate change.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Maps

ISSN

1744-5647

e-ISSN

—

Svazek periodika

21

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

15

Strana od-do

2532561

Kód UT WoS článku

001542191800001

EID výsledku v databázi Scopus

2-s2.0-105012189178