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ofthe canon beyond the main high ridge runs approximately with the strikeof the beds but in its lower portion it crosses them almost at right anglesAt its western mouth are found beds of massive compact limestone withothers of a more shaly character dipping westward and having a strikesomewhat west of north The western dip holds for about miles up thecanon when a body of white and pinkish saccharoidal quartzite is foundwhich forms the axi. Mulberry Outlet UK Store bags s of a gentle anticHnal fold This quartzite containsalmost no lime as is generally the case with those of the higher bodies Itgave by analysis nearly per cent of silica the impurities being mostlyalumina To the eastward of this the limestones come in again dippinggently eastward and showing on the face of the cliff evidences of the ver-tical movements which must have lift. Mulberry outlet site buy cheap mulberry bags and handbags ed up the ridge of Timpanogos in thecontortions and dislocations which have twisted and broken beds of massivelimestone hundreds of feet in thickness The fossil remains fragments ofProductus Euomplialus and Crinoid columns obtained from these limestonesthough too poor for specific identification were considered sufiicient at thetime of our visit . Mulberry outlet Store mulberry bags sale online to determine the Carboniferous age of these beds Withthe experience which has been since gained a careful search more particu-larly in the beds immediately overlying the quartzite which is without doubtAMERICAJT FOliK CANON the Ogflen Quaitzite would probably have yielded Devonian or Sub-Car-boniferous formsThe anticlinal structure disclosed in the Americ. http://www.mulberryfashion-uk.com Mulberry Outlet an Fork section con-tinues in the main ridge to the north but the beds rise and lower horizonsare successively exposed until at Dry Canon the granite body of the Cot-tonwood district is found at the surface a spur of which doubtless underliesthis whole ridge which we have been examining and served to detemiineits direction The contact of the lower beds . shop Mulberry Bags with the granite body at DryCanon has not been actiially observed but the lines of division between thefoiTOations at this part of the range are based on observations fi-om LonePeak and the position of these beds in contiguous portions of the rangeThe limestone body north of American Fork Canon has a general easterndip in continuation of the Timpanogos Ridge and preserves for some dis-tance the same strike; but soon the strike of all the beds bends to the north-east parallel in general to the southern line of the Cottonwood granite bodyAt the head of Deer Creek the first northern lranch of American Forkthe granite is seen to form the face of one of the spurs while on either sideit is covered by the steeply-dipping quartzite beds of the Cambrian whichwith a general in
