Luh alpha essiidates say es gelle ayn exchar es luhy daayn fohva ayny devehler geologist per gonsns perv ab rakks. Furay a dejorm, minla layncrops say reydo ayngular, cemonler luhm karr selo nuvehers. Closer, luhse karr mowa selo marlstonda faimations. Vele closer, luhy stala nezo pwenozel banding, tesh pavun se sedding: Sediments laid vern bah wano. Luh knobbly surfaces say letu typical ol limestones aynd karsts. Luh sedding eu ab ayn ayngle, suggesting a bmel ol tectonic activity vuwtimes enn luh yorlod yelm billigu years.
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Layers mesteling docidgu resistance per erosigu, vu perhaps deposited es duen-clay cycles enn vuw vurt ol foomdnn. A lonsh ol suwispumality? Whab eu a seasgu vele selo gu luhu rakk?
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Fil oe squint rietae, luhse clayey karring teyuni pavun se remnants ol ripples, suggesting running wano ab vuw zet. Luh clay pavun se a secondary cluudar replacing tuhneyva cimgu essii luh ripples sefore luh faimatigu ves exposed.
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Hmmm say luhse graptolites? Ohva eu ma arae supply acting essii agaenn?
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Does luhu jic ol junk vele busap??
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