| Marla Glacier | |
| Map: | Antarctica |
| Mark: | Blue_pog.svg |
| Location: | Trinity Peninsula |
| Coordinates: | -64.0083°N -58.8833°W |
| Length: | 8nmi |
| Width: | 1nmi |
| Terminus: | Prince Gustav Channel |
Marla Glacier (-64.0083°N -58.8833°W) is a glacier long and wide on the northeast side of Detroit Plateau on the southern Trinity Peninsula in Graham Land, Antarctica.
Marla Glacier is in Graham Land on the southeast coast of the Trinity Peninsula, which forms the tip of the Antarctic Peninsula.It is situated south of Aitkenhead Glacier and north of Diplock Glacier. It drains southeastwards along the east slopes of Povien Peak, then turns east between Mount Roberts and Bezenšek Spur, and flows into Prince Gustav Channel in Weddell Sea.
Marla Glacier glacier is named after Marla River in Northern Bulgaria.
-63.9667°N -112°W. A nunatak, high, rising northwest of Mount Roberts, on the south margin of Aitkenhead Glacier. Named by the UK Antarctic Place-Names Committee (UK-APC) for Hugh W. Simpson of the Falkland Islands Dependencies Survey (FIDS), a member of the Detroit Plateau reconnaissance party from Hope Bay in 1957.
-63.9822°N -58.97°W.An ice-covered peak rising to high in the northeast foothills of Detroit Plateau. Situated between the upper courses of Marla and Diplock Glaciers, southwest of Mancho Buttress and, west-northwest of Mount Roberts. Bezenšek Spur projects east-southeastwards from the peak. Named after the settlement of Povien in Southern Bulgaria.
-64.0208°N -58.8667°W.A long and high wide rocky ridge rising to high in the northeast foothills of Detroit Plateau. It projects from the southeast side of Povien Peak eastwards between Marla Glacier and Diplock Glacier. Named after the Slovene-Bulgarian linguist Anton Bezenšek (1854-1915) who developed the stenographic system for the Bulgarian language.