Spath Crest (80°39′S 26°12′W / 80.650°S 26.200°W) is a summit rocks rising to about 1,450 m and marking the northwest end of Du Toit Nunataks, Read Mountains, in the Shackleton Range. It was photographed from the air by the U.S. Navy in 1967 and surveyed by the British Antarctic Survey (BAS) between 1968 and 1971. In association with the names of geologists grouped in the area, it was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Leonard Frank Spath (1882–1957), a British paleontologist and stratigrapher whose study of ammonites made possible the correlation of Mesozoic rocks. Spath was also a paleontologist for the British Museum of Natural History from 1912 to 1957.
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| - Spath Crest (de)
- Spath Crest (it)
- Spath Crest (en)
- 斯帕思峰 (zh)
- Spath Crest (sv)
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| - Spath Crest sind eine Gruppe bis zu 1450 m hoher und felsiger Berggipfel im ostantarktischen Coatsland. In der Shackleton Range ragen sie in den Read Mountains auf und markieren das nordwestliche Ende der Du-Toit-Nunatakker. Luftaufnahmen entstanden 1967 durch die United States Navy. Der British Antarctic Survey nahm zwischen 1968 und 1971 Vermessungen vor. Das UK Antarctic Place-Names Committee benannte die Gruppe am 5. Januar 1972 nach dem britischen Paläontologen Leonard Spath (1882–1957). (de)
- Spath Crest är en bergstopp i Antarktis. Den ligger i Östantarktis. Argentina och Storbritannien gör anspråk på området. Toppen på Spath Crest är 1 450 meter över havet. Terrängen runt Spath Crest är huvudsakligen platt. Spath Crest ligger uppe på en höjd som går i öst-västlig riktning. Den högsta punkten i närheten är 1 799 meter över havet, 19,4 kilometer väster om Spath Crest. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 斯帕思峰（英語：Spath Crest），是南極洲的山峰，位於科茨地，處於里德山脈的迪圖瓦冰原島峰西北端，屬於沙克爾頓山脈的一部分，海拔高度約1,450米，現時由南極條約體系管理。 (zh)
- Spath Crest (80°39′S 26°12′W / 80.650°S 26.200°W) is a summit rocks rising to about 1,450 m and marking the northwest end of Du Toit Nunataks, Read Mountains, in the Shackleton Range. It was photographed from the air by the U.S. Navy in 1967 and surveyed by the British Antarctic Survey (BAS) between 1968 and 1971. In association with the names of geologists grouped in the area, it was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Leonard Frank Spath (1882–1957), a British paleontologist and stratigrapher whose study of ammonites made possible the correlation of Mesozoic rocks. Spath was also a paleontologist for the British Museum of Natural History from 1912 to 1957. (en)
- La Spath Crest ( cresta di Spath) è una sommità rocciosa che si innalza fino a 1.450 m e che delimita il margine nordoccidentale dei Du Toit Nunataks, una serie di picchi nei Monti Read, che fanno parte della Catena di Shackleton, nella Terra di Coats in Antartide. Nel 1967 fu effettuata una ricognizione aerofotografica da parte degli aerei della U.S. Navy. Un'ispezione al suolo fu condotta dalla British Antarctic Survey (BAS) nel periodo 1968-71. (it)
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| - Spath Crest sind eine Gruppe bis zu 1450 m hoher und felsiger Berggipfel im ostantarktischen Coatsland. In der Shackleton Range ragen sie in den Read Mountains auf und markieren das nordwestliche Ende der Du-Toit-Nunatakker. Luftaufnahmen entstanden 1967 durch die United States Navy. Der British Antarctic Survey nahm zwischen 1968 und 1971 Vermessungen vor. Das UK Antarctic Place-Names Committee benannte die Gruppe am 5. Januar 1972 nach dem britischen Paläontologen Leonard Spath (1882–1957). (de)
- Spath Crest (80°39′S 26°12′W / 80.650°S 26.200°W) is a summit rocks rising to about 1,450 m and marking the northwest end of Du Toit Nunataks, Read Mountains, in the Shackleton Range. It was photographed from the air by the U.S. Navy in 1967 and surveyed by the British Antarctic Survey (BAS) between 1968 and 1971. In association with the names of geologists grouped in the area, it was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) after Leonard Frank Spath (1882–1957), a British paleontologist and stratigrapher whose study of ammonites made possible the correlation of Mesozoic rocks. Spath was also a paleontologist for the British Museum of Natural History from 1912 to 1957. This article incorporates public domain material from "Spath Crest". Geographic Names Information System. United States Geological Survey.
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* e (en)
- La Spath Crest ( cresta di Spath) è una sommità rocciosa che si innalza fino a 1.450 m e che delimita il margine nordoccidentale dei Du Toit Nunataks, una serie di picchi nei Monti Read, che fanno parte della Catena di Shackleton, nella Terra di Coats in Antartide. Nel 1967 fu effettuata una ricognizione aerofotografica da parte degli aerei della U.S. Navy. Un'ispezione al suolo fu condotta dalla British Antarctic Survey (BAS) nel periodo 1968-71. Ricevette l'attuale denominazione nel 1971 dal Comitato britannico per i toponimi antartici (UK-APC), in onore del paleontologo e stratigrafo britannico (1882–1957), i cui studi sulle ammoniti resero possibile la correlazione delle rocce del Mesozoico. Spath fu inoltre paleontologo presso il Museo di Storia Naturale di Londra dal 1912 al 1957. (it)
- Spath Crest är en bergstopp i Antarktis. Den ligger i Östantarktis. Argentina och Storbritannien gör anspråk på området. Toppen på Spath Crest är 1 450 meter över havet. Terrängen runt Spath Crest är huvudsakligen platt. Spath Crest ligger uppe på en höjd som går i öst-västlig riktning. Den högsta punkten i närheten är 1 799 meter över havet, 19,4 kilometer väster om Spath Crest. Trakten är obefolkad. Det finns inga samhällen i närheten. (sv)
- 斯帕思峰（英語：Spath Crest），是南極洲的山峰，位於科茨地，處於里德山脈的迪圖瓦冰原島峰西北端，屬於沙克爾頓山脈的一部分，海拔高度約1,450米，現時由南極條約體系管理。 (zh)
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