Yarwondutta Rock, Minnipa
Australia /
South Australia /
Port Lincoln /
World
/ Australia
/ South Australia
/ Port Lincoln
World / Australia / South Australia
interesting place
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Location:
12ha, 4km north of Minnipa on Minnipa Yardea Road, comprising area enclosed by a series of straight lines joining AMG points: 5932-3-Minnipa 147691, 147688, 151688, 151692 and commencement point.
Yarwondutta Rock is an isolated granite inselberg (or island mountain) standing abruptly from the surrounding cleared plains. The rock is cut by several vertical or near-vertical fractures, three trending north-east to south-west, two trending west-north-west to east-south-east and one aligned north-west to south-east, so that the outcrop is subdivided into several roughly quadrangular blocks. Preferential weathering has taken place along the major fractures giving rise to clefts or slots. One of the major clefts is bounded by flared slopes like those formed around the margins of the inselberg and on some of the upper slopes. Clear evidence of the subsurface origin of the flares can be seen in the reservoir (in summer, when it is dry). The upper flattish slope is poked and grooved due to the development of many rock basins (or gnammas), linked by bedrock channels. Most are of the flat-floored pan variety but those near the edges of The Summit plain take the form of the armchair-shaped hollows. The large residual boulder standing on the north-western step displays an active tafone or hollow. The entire north-western slope is stepped, which flared slopes linking flattish platforms. Good exposures of the fresh hiltaba granite can be seen in the quarry. There is also a good exposure of a regolith in granite and with calcrete (pedogenic limestone) superimposed on the weathered bedrock.
12ha, 4km north of Minnipa on Minnipa Yardea Road, comprising area enclosed by a series of straight lines joining AMG points: 5932-3-Minnipa 147691, 147688, 151688, 151692 and commencement point.
Yarwondutta Rock is an isolated granite inselberg (or island mountain) standing abruptly from the surrounding cleared plains. The rock is cut by several vertical or near-vertical fractures, three trending north-east to south-west, two trending west-north-west to east-south-east and one aligned north-west to south-east, so that the outcrop is subdivided into several roughly quadrangular blocks. Preferential weathering has taken place along the major fractures giving rise to clefts or slots. One of the major clefts is bounded by flared slopes like those formed around the margins of the inselberg and on some of the upper slopes. Clear evidence of the subsurface origin of the flares can be seen in the reservoir (in summer, when it is dry). The upper flattish slope is poked and grooved due to the development of many rock basins (or gnammas), linked by bedrock channels. Most are of the flat-floored pan variety but those near the edges of The Summit plain take the form of the armchair-shaped hollows. The large residual boulder standing on the north-western step displays an active tafone or hollow. The entire north-western slope is stepped, which flared slopes linking flattish platforms. Good exposures of the fresh hiltaba granite can be seen in the quarry. There is also a good exposure of a regolith in granite and with calcrete (pedogenic limestone) superimposed on the weathered bedrock.
Nearby cities:
Coordinates: 32°48'25"S 135°10'24"E
- Monarto Zoo 445 km
- Gluepot Reserve 470 km
- Naracoorte Caves Conservation Park 694 km
- Johnson Swamp 882 km
- Hird Swamp 886 km
- Kow Swamp 904 km
- 12/Twelve Apostles 964 km
- Cape Otway 1008 km
- Ford Proving Ground 1009 km
- Dowdle Swamp 1060 km
- Minnipa Airport (MIN, YMPA) 4.4 km
- Minnipa Golf Club 5.2 km
- Lake Yaninee 20 km
- Wudinna Airport (YWUD / WUD) 36 km
- Mount Wudinna 40 km
- Yardea Airfield (YRDA) 53 km
- Yardea Station 58 km
- Acraman crater 91 km
- Kimba Golf Course 120 km
- Gairdner Lake 142 km
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