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The vents have an overall southwest-northeast alignment, which suggests that the ascending magma utilised a pre-existing fracture within the Earth's crust. Several of the craters are breached to the southeast, possibly due to the prevailing southeast winds blowing ash and
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Whitehead, P. W.; Stephenson, P. J.; McDougall, I.; Hopkins, M. S.; Graham, A. W.; Collerson, K. D.; Johnson, D. P. (2007). "Temporal development of the
Atherton Basalt Province, north Queensland".
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to the northwest and so building the cones more to that side. Parts of the rocky
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Aerial view of The
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flows are still densely forested and can be seen surrounding the
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136:(aka the Seven Sisters) are a series of seven volcanic
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Rocks, landscapes & resources of the wet tropics
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152:. They were formed more than 350,000 years ago.
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240:Australian Journal of Earth Sciences
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304:: CS1 maint: others (
193:Mount Hypipamee Crater
146:Yungaburra, Queensland
116:17.26667°S 145.55000°E
706:Far North Queensland
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183:Lake Eacham (Yidyam)
121:-17.26667; 145.55000
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221:. Retrieved
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188:Lake Tinaroo
178:Lake Barrine
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138:cinder cones
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47:Cinder cones
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427:Lake Eacham
402:Attractions
223:12 November
119: /
107:145°33′00″E
756:Categories
678:Tablelands
657:Yungaburra
602:Irvinebank
526:Millstream
464:Waterfalls
455:Windy Hill
199:References
104:17°16′00″S
709:geography
637:Ravenshoe
632:Mutchilba
597:Herberton
506:Josephine
481:Clamshell
300:cite book
292:271828487
260:0812-0099
150:Australia
652:Walkamin
592:Dimbulah
587:Atherton
571:Wongalee
561:Wallaman
546:Tchupala
511:Kearneys
172:See also
673:Mareeba
642:Tinaroo
622:Malanda
617:Mareeba
612:Kuranda
551:Tinaroo
516:Malanda
486:Crystal
476:Blencoe
371:Schools
144:, near
140:on the
566:Whites
531:Murray
496:Dinner
471:Barron
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162:basalt
158:scoria
704:This
647:Tolga
607:Kairi
580:Towns
556:Tully
713:stub
306:link
288:OCLC
278:ISBN
256:ISSN
225:2019
248:doi
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
