Document Pages

45 Pages
Page 6
86 4 Derbyshire Falls. Lamell bed, lace, she clay 20 inches. From fine grained flaggy, 7 ft 6in to 7ft 9in. White Clinton or Lower Keegan, = 1ft 3in. Clinton 7 ft. 3 in. Sample I. 3 ft 9in., below Clinton lace, worn away. Sample II. 10 ft. below Clinton base contain more lime, at least fossils. Sample III. 12 ft below Clinton base Very fine grained, fairly soft massive rock, weather back. At not 2 feet of it, Below are 5 feet of material similar to Sample II with plants fossils. Next come about 5 ft of rock similar to III, which again's worn back under the more fossil aftering rock above. The level at the face of the Falls lies 15 feet lower down - a 32 ft below Clinton = 39 ft 3 in. below Clinton top, = 4ft below trans. arch top, = 48ft 6in. below clay bed at base of Lamell bed, 87 7.) Harry Manly's Quarry N of James Ch. (On S side of creek there is fully 10 feet of Judgem- note to want lamell. Waite with many chatty layers.) Stopping 12 ft clay and a little rock. Flaggy flaggy flaggy cheap, getting 5 in. A 2 in, 2 2 in. clent, 3 in, 4 in, 3 1/2 in, 3 1/2 in. with short in bottom part 6 in layer with chest or red line trip. 4 1/2 in. flaggy curbing good, 4 1/2 in. spotted calf ditch clint & pretty key 3 in, flagging. 6 in curbing 2 - 2 1/2 in light cellar flag. 8 in used for 6 in. curbing 7-9 in. used for curbing steps or lls 7-9 in. men for curbing steps, mills. 1 ft of soft blue clay. (cragged one) 3cap. 22 in. of this fine material line the bottom but under pressure 3ft 6in. three layers of soft lowerst. Den.May, 3ft 8in. Clinton. salmon form clint. reddish below, 4ft + don't like claygy material and a about 6 in layer on top of it.
Page 14
102 RR crossing over stream, 3/4 mi. EAST of deft at Greensburg, 2 feet of white sparkling stone looking like sandstone & evi- dently very crystalline, im- mmediately overlies the Laurel bed with out the intervention of the intermediate Waldron shale. Above the 2 feet of sandstone are 5 feet of limestone not in nice layers but in small lenticular masses. It is fine grained and apparently also gritty as though the sandstone below turned to limestone above. The upper stone is sometimes also white but usually it is more drab. The 2 foot sandstone contains brachiopods, Atrypa Dcn + Steph, Dcn + Favosites Large. The overlying beds contain small branching corals. 7 in capps into stone flagging caps irregularly 14 in. 5/9 in. - curb fine steps veranda blocks. 3 flag curb. 1 scale 7 used for 5 in curb. 6 flag from gutter. 17 in ledge. 6 in curb. gutter in flag. 9 in ledge jail flag cellar flooring, 4 in with flint on bottom flag. 9 in waste with flint. 4 in flag. 4 in flag. 6 in for gutter flag footing with flint on bottom 6 in 1/2 waste with flint. 6 in gutter flag. 5 in flinty, 2 in scrap flag. 7 in 4/3 [illegible] flag not good for curb. 4 flag. curb. 13 in. 4/6/3 gutter a flag not good for curb flag curb. good curb. 5 regular flag & curb. 9 hard 3/4 flag. curb. 4 in flag of flawed nature == 6 flawed, wiggly, = 2 1/2 in ledge {4/6} flag curb. gray {4/6} gutter flag. 6 blue = good 4 in curb. 14 in 7/4 freezes. blue. fine clay 16 in. / 16 in freezes. blue. Bottom 8 & aytm.
Page 15
{ "text": "104\nJ.J. Langton.\nTopi\ngraveling\n+ stone for use, used for\n7 feet of dimension as good bedding\n3/2 cwt.\n11 Milk trough, water table steps\nveranda blocks.\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n [TRANSCRIPTION_TRUNCATED_DUE_TO_LOOP]
Page 19
shale. side of road, Newton. blue shale limestone with numerous fossils (crinoid byzpranus) especially desire found. blue shale limestone as with for- made to the cliffs. blue shaly limestone, front, water lime These limes just described turn to a marlstone structure or going a slight but more eastward. immediately below the shaly limestone is the crinoidal lime- limestone which appears to be made of various fossil stems with numerous branch pieces of limestone with [illegible] the limestone immediately beneath is a buff color and is full of radiar- tes, especially Spirifera & Sterophyllum and shells. Do some places there are layers are crinoidal, and large nodules and irregular masses of clert on it various levels. The total thick- ess of the various layers is about immediately over is very fine grained shale rock with fine close bedding, claimed to be shaly. Further in the other side where more granular this is less shaly and forms three layers. this strike. The fine bedding is still shown the other grades irregularly & shaly like 6 in. of less finely stratified buff calcareous rock is found beneath. The last three layers contain very few fossils. 13 in. of buff or blue argillaceous with many fine horizontal cra- filled with calcite. 12 in. argillaceous and a blue lime- stone with irregular calcite masses. 12 in. argillaceous limestone thin with fine regular cracks filled with calcite, also small calcite specks. 11 in. argillaceous limestone. 24 in. argillaceous laminations with calcite in irregular cracks or specks. The lower half of these argilla- cious layers consists of somewhat better done than the upper half. The irregular liney contact between the fossiliferous limestone and the closely stratified crinoidal rock below should be photographed. Further eastward, the upper feet of this series are seen to be in buff & argillaceous or poor shale 4'2 feet beneath a rest of a white rock which is a