Jordan Pond
Jordan Pond is an oligotrophic tarn in Acadia National Park near the town of Bar Harbor, Maine. The pond covers to a maximum depth of with a shoreline of .

The pond was formed by the Wisconsin Ice Sheet during the last glacial period. Penobscot Mountain (1194 ft) rises to the west, while Pemetic Mountain (1247 ft) rises to the east. Two roche moutonnées known as The Bubbles (North and South) rise above the northeastern shoreline. The southern end is constrained by glacial debris and an artificial dam.

The pond has clear water, with visibility normally and occasionally recorded up to , the deepest recordings in Maine. The pond exhibits high levels of dissolved oxygen, and low levels of plant nutrients and plant life.

Some types of boating are permitted, but people and pets are prohibited from entering the water as it is the water supply for the village of Seal Harbor.
None
oligotrophic
UNK
Q1851937
tarn
Concept
Q337396
Acadia National Park
LOC
Q1672375
Bar Harbor
LOC
Q724
Maine
LOC
Q2094246
Wisconsin Ice Sheet
Concept
Q190559
roche moutonnée
Concept
Q2610088
glacial debris
Concept
Q3053737
Seal Harbor
LOC
Q6276889
Jordan Pond
LOC
+1194^^http://www.w3.org/2001/XMLSchema#decimal
1194
NUMBER
+1247^^http://www.w3.org/2001/XMLSchema#decimal
1247
NUMBER
located in the administrative territorial entity
significant place