Field notes, undated (5)

THE MILLER STATIONERY CO. 25 East Third St. DAYTON, O.

Received of A W Heyman $30.21, expense account for trip from Annibal Arts Pueblo return via Dayton. any J Freski. 404 furs 18. 20. 40 lost ind. 30 clothes 20 inches 81 inches 3 1/2

Bailey Landing : Red Rocks Landing Resty Co. Only my own notes, in river bottom. St Mamps, St Gene Ruled to Farmington - about 3-4 miles out, as you up middle mile you find yellowish limestone & clay: ?? Wiltonburg, Walk along river bank about 1 mile, no river banks; ?kenidium(?) modoc statum Bailey Arthus mizi group. stribalrohtus elongatus. Not a Stibabo ?ystra. Bailey's Landing Red Rocks. Silicula 18-20 ft. Bowling Green l, yellow, 3-4 ft Walsum l, white patches Green - coal bedgings? N rip vobia. Black shale Ocmulgee yellow limestone crabs. Winnimeth 8:05 Am 4 PM. 9.20 PM, 11 13) 13 15 13/165-13 13 35 St Louis Linnville, 9. PM, Sat, 6.55 AM. Sunday. Room 302 Terminal Hotel Glencoe Lime & Cement Co. Byers, Missouri: 1/4 NW 1 West Kilmunswick.

Monday on RR. 26 Tuesday in lutes 27 Wednesday O'Tate fount .50 28 3:10 Thursday London 1:00 29 3:10 Friday Sinkings Spring 1:50 30 3:10 Saturday Sinkings Spring 1:50 31 3:10 Sunday London 1:00 1 3:10 Monday 3:10 18:10 CH+D 9:45 PM Dayton 11:30 PM 2:55 AM. 4:40 AM. Big 4 9:45 PM, Dayton 11:35 PM From C Murray school south 3/4 mi. then east, at first whitish clay supposed to be Cent Archad, further east is Behir Black Shale dipping 30° or more eastward. Then further east is sandy looking rock which may be Brown West Union. 3/8 mi E by S side, at right angle where road turns north, West Union lineetone, with Cladofora, small called Farmites, Half a mile S of Scurry Corner School the Corner 826, the face of the Ellen tangs is exposed at 826 USGS. and thus and the Black Shale cross the farm land as far south as the next depression in the road. East of corra 826 tip of Monroe occurs and 1/4 mile east is face of Ellen tangy at 820 about, From Scurry Corner School to house 1/2 mi NE then top of Monroe = about 8:15. Up creek SE of house, in creek bed, and about 27 ft below house level = Allen tang-Monroe contact. = dip 6 east. At house tip of Monroe is about 15 feet below house level

From Sunday Corners School 1/4 mi N & then 1/4 mi N, where 820 line touches the road, west N near this limestone rises as high as 820 along the road. From Sunday Corners School 1/4 mi W & then 3/4 mi N, to road corner 813. Eastward road corner as far as creek and for several hundred feet beyond, tip of Monree is exposed. At about 820 the Clentaugy slumps up and forms the hill as far as 1/4 mi E of the road corner. About 3/8 mi E of road corner the tip of the Monree slumps up again, & nowhere near 830 and where the creek crosses the road 1/2 mi E of road corner, the Clentaugy comes in again at about 830. From corner 813 go 1/4 mi N. At road corner is Monree which shows up as mark at house nearly 1/4 mi E of corner. Directly east of house, at about 830 is lowest Clent augy seen which continues to where road turns N, after the road goes W for 1/2 mi the light and clear Black shale shows up at about 840. From corner 81B go 1/4 mi N, to road corner. From here we examine for 1/4 mi W. At this point the road corner is Monree tip. This Monree tip sizes irregularly northward for 1/2 mi, where the road turns W. Monree is seen past of road corner. The Clentaugy goes right in east of road when road turns NW. Next Monree occurs my house on east side of road and Glen tangy comes in NW of house and continues as far as road corner 875. This 2 miles of outcrops here and to and SE of Sunday Corners School suggests that Clentaugy rests upon very irregular Monree base, but it is possible that all the ridges here are irregularly contorted and folded. From C m an ays school 1/2 mi N to corner 782, then 3/4 mi E to where road turns off straight north. From this road, westward for a short distance tip of Monree is exposed. Further west, Black shale force shows up nearly 1/4 mi W of road junction, where 820 line then line reaches road from south, and this Black shale and underlying Clent augy are exposed northward as far as both creek crossings. A short dist since not I second creek crossing a sandstone like rock,

assumed to be West Minn shms of and this sandst me like rock to followed east y road corner 782 by a whitish clay assumed to be East Orchard clay. This same East Orchard clay and West Minn sandst me was also from's of road corner 782, where another road leads off north. It should be remembered however that one mile south of the C'many school this eastward road exposed actual black shale east of the supposed East Orchard and then the unknown sandstone, here called West Minn, but crops further west. There is our draft about northwest dip in the whitish black shale at the exposures east of the creek 1 mi NE of the C'many school. Returning to the corner N of C'maway school, = corner 782, a fully 1/4 mi E of corner and south y road, on east side of highest point in road, showed Tainimus or Canada galli in sandstone suggesting Waway age in place of West Minn or that the clay section northward, which dips most norady, may also be one of The Waway clays. cast side y pike at C'many school and church is some unknown whitish clay here called Wawayly clay. Further along pike is black-black shale. Then further south is the same unknown white clay of supposed Waway age, and further south is small abandoned store where lane turns off west to several houses back from pike. SW of point where this lane starts off is a knoll exposing whitish black shale on NE side where brink flows against east side y lane. Immediately by point when this lane cuts off there is a sandstone here in turn prefixed as Wawayly. Between point where lane turns off and road corner 779 the unknown white clay (Waway clay?) is exposed along road, on E side of road, N of Crooked creek 1 mi. NE of letter F in FRANKLIN, East Orchard clay is visible on east side of road by trace of West Minn with typical green West Minn joints about 40 ft above road. This suggests East Orchard age of unknown some clay, called Waway above.

Wanted Congracchulus (Turchinus) halli, F, type locality & horizon? Mingan Islands, where? St Lawrence Large Island 1) St Lawrence Pentamerus oralis or, Clinton monon nov. Stricklandina canadensis? My collecting? centerminas el magatno Argos trivinculatus type, at Orient n? Kerr, Perfectin Imperfection Con- found. D isn't Daniel Wyz Co 12. 20 Car I. Lizzone 79th & Amsterdam Brittin Hall 86 & Beradine autumn quadruple puncture sagittal plane by definition symmetry semi-spherical.

Camarotectia acinno Sandegruit Camarotectia aequinadiata Sangroit Camarotectia emacerata Williamson Camarotectia neglecta Reyn des Sandegrut Pterinea emacerata Sangroit ? Bem Creek Brewerini Van Hornerville Phoenix Reynielwa lata Sangruit. -> Srohs ? Verma ? Rirklandia Boll'a lata ? Sagunit -> Srohs ? Williamson Caninia trilateralis (marant ?) Finnacerville Reynaies Ptryconus plurumns Finnacville. Reynales, Contrlassma calgulus ?Finnacervile Staplinella parenta ?Finnacerville Reynaies Camarotectia h'dens Reynales Atypha reticulans S rohs ? Williamson Brewerini Phoenix Sandegrut P mellv Glycospira muttens (hemi)phlebia Finnacervile Sodros plicatula Finnacerville Reynales S rohs Calymenella antrata S rohs Calymene vogdesi ? Srohs Calymene majorum's Sandegrut Calymene ab'nt mi ? Williamson [Brewerini] Rirklandia Trimerus delphinocphalus Horkemer Sandegrut. Dalmantus linnuburs Phoenix Bimastus 0x no Sandegruit Spirifera radiatus Walcott Furnace Williamson Phoenix Donelly Sandegrut Spirifra majorum's ? Walcott Spirifra crispons Sandegrut. Cityna verostriate Sandegrut. Pontanirus prolis ? Phoenix ? D mellv Stricklandia complans Reynales. Pentannern 0l inms, Reynales Walcott

stromatoporids "Ostrich eggs" WH B[or]rds farm, 2 mi W of New Londm, on 2 with side of road, m east branch of Doe Rim, about 1/2 mile above its confluence with Doe Rim, = ESE of this confluence. Top of Dornian is. with large "pillow structure, forming total thickness of 2 feet. The total thickness of the Dornian here is 15 feet. It is underlain by calcareous shale - 15 ft yellowish green shaly clay - 2 ft Top of Stewartville with Machuringa at top, and with Receptaculites and cyelstrides belli at 15 ft belw the of stewartville. At vari cyclostrides horizon are some crystal fragments (Glyptosty) apparently). The upper part of Dornian has contains Farnits perimorphice bel in the Stromatoporid layer.

quartermaster 56 ordnance 50 signal corps 56

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