Oak street unclassified BULLETIN NO. 8 \J South Dakota School of Mines Departments of Geology, Chemistry, Mining „nd Metallurgy. u[)lvER j lTy OF ILLINOIS THE PRESIDENT’S OFFICE, Cement Resources OF THE Black Hills. Including Tests on Cements Made from Black Hills Material BY CLEOPHAS C. O’HARRA, Ph. D. M. F. COOLBAUGH, M. A. M. A. EHLE, Jr. E. M. CHAS. H. FULTON, E. M. RAPID CITY, S. D. JULY/ 1908. BULLETIN NO. 8 South Dakota School of Minty 1 ’' OF ILLINOIS PRESIDENTS OFFICE Departments of Geology, Chemistry, Mining and Metallurgy. THE Cement Resources OF THE Black Hills. Including Tests on Cements Made from Black Hills Material. BY CLEOPHAS C. O’HARRA, Ph. D. M. F. COOLBAUGH, M. A. M. A. EHLE, Jr. E. M. CHAS. H. FULTON, E. M. RAPID CITY, S. D. JULY, 1908. Rapid City Printing Company, Rapid City, S. D. Letters of Transmittal. SOUTH DAKOTA SCHOOL OF MINES. Rapid City , S. D., July i, 1908. Dear Sir I have the honor to transmit herewith a paper by C. C. O’Harra, M. F. Coolbaugh, Mark Ehle and C. H. Fulton on the Cement Resources of the Black Hills of South Dakota. I submit it with the recommenda- tion that it be published as Bulletin No. 8 of the School of Mines. Respectfully, CHARLES H. FULTON, President. To The Hon. E. C. Ericson, President, Regents of Education. Digitized by the Internet Archive in 2017 with funding from University of Illinois Urbana-Champaign Alternates https://archive.org/details/cementresourcesoOOohar Introduction. The great increase in the use of Portland Ce- ment has drawn attention to possible sources of raw material. The Black Hills of South Dakota are es- pecially favored in this respect, both as regards the quantity available, and the purity of the material. In the experimental work on the cements care was taken to have it thorough and representative. Much more work was done than is recorded in the bulletin. The editor desires to express thanks to Mr. Willi- am A. Coursen for the efficient aid given in the con- struction and operation of the experimental cement furnace; also to thank Mr. J. B. Read for services in connection with the making of analysis, etc. The ed- ‘**or also expresses his gratitude to his colleagues, Pro fessors O’Harra, Coolbaugh and Ehle for their able labors in making this bulletin thorough and represen- tative. CHARLES H. FULTON, Editor. PART I. THE GEOLOGY OF THE BLACK HILLS CEMENT MATERIAL. C. C. O’HARRA, Ph. D. The Geology of Black Hills Cement Material. C. C. o'HARRA J PH. D. The Black Hills region is bountifully supplied with deposits available for the manufacture of good cement. Until recently little attention has been given to the experimental study of these materials and in this bulletin chief attention is directed toward the ex- aminations of two or three formations of special prom- ise favorably situated with reference to railroads. The formations chiefly studied are what in geo- logic literature are known as the Minnekahta lime- stone, the Graneros shale, and the Niobrara argillace- ous chalk. Experimental work indicated that by a proper mixture of materials from the Minnekahta and the Graneros formations a compound can be made, suited in every way for the manufacture of a high grade Portland cement, while the Niobrara can fur- nish material of proper composition for the making of excellent natural cement. Of the limestones, the Minnekahta is the only one of the region deemed worthy of consideration at this time. The Pahasapa is the great limestone formation of the Black Hills, making long lines of high white escarpment facing on all sides the central part of the uplift, but it con- tains much maganesia and too little attention has been paid to the possible magnesia-free portions to allow for any reliable statement as to favorable localities where this limestone might be profitably exploited. Such other limestones as occur within the region are thin or impure and are often inclined to considerable IO variation in character, hence have not been given spec- ial attention. The shale'bearing formations are abundantly rep- resented and several of them give evidence of possible value used in combination with the Minnekahta lime' stone. In addition to the Graneros already mentioned there are the Pierre, the Niobrara, the Carlile, the Mor- rison, and possibly other formations that merit care- ful examination, should an exhaustive study be made of all available materials. That the geologic position of the various formations may be better understood a complete generalized geologic section of the Black Hills region is here given. The Minnekahta Limestone. The Minnekahta limestone, known commonly in early geological papers as the Purple Limestone, although seldom more than fifty feet in thickness is one of the prominent out- cropping formations of the Black Hills region. It is a close-textured, thinly-bedded, grayish limestone with frequently a slight pinkish or more often a purplish tinge, hence the earlier name. The bedded nature of the rock is much concealed on fresh surfaces, but weathering reveals the condition in a very definite way. Near the middle of the formation the nature of the bedding is such as to allow for slightly more rapid weathering than elsewhere and this feature generally reveals itself in unmistakable manner. Near the bot- tom the bedded nature is again pronounced and the rock here contains considerable argillaceous material. The lowest beds which are generally much ironstained are not commonly exposed. In some localities where they are exposed the limestone breaks up into numer- ous small lenticular concretionary bodies within which fairly well-preserved fossils are found. In general, however, the formation is markedly free from fossils, although not quite so much so as was earlier supposed. Mr. N. H. Darton of the United States Geological Sur- vey records the identification of Bakewelha , Hdinondia r and Nuculana. Map showing outcrop of the Minnekahta formation II The Minnekahta is underlain by a thin series of soft clay shales known as the Opeche formation and is overlain by a thicker series of soft sandy shales, the Spearfish formation, commonly known as the Red Beds. The dip, sometimes steep, sometimes low, varies in a more or less undulatory manner, but in general it follows the nature of all of the periclinal sedimentary rocks of the region in that it is distinctly apocentral, that is, it dips outwardly on all sides from the higher central portion of the main Balck Mills uplift. The outcrops are unusually prominent every where. The relatively hard, more or less sharply dip' ping limestone between the soft shale beds readily lends itself to the production of a bold topography. Hun- dreds of streams, constant and intermittent flowing radially from the central area of the uplift run across the formation and each carves for itself a V-shaped gateway to the red valley beyond. On the outer slopes wherever the dip is considerable, the rock is nearly bare of soil and vegetation although the pine trees, Pinus ponderosa, cling tenaciously to it wher- ever a roothold can be secured. • The inner line of out- crops is a continuous succession of prominent escarp- ments which, facing the central area of the uplift dome, stand out in bold relief as they overlook the sharply, trenched Opeche below. The width of outcrop varies greatly. Where the dip is steep as for example along Beaver creek and the lower portion of Gillette canyon east of Newcastle and on the immediate flanks of several of the lacolithic areas which interrupt the general foothill structure, the width of the outcrop is reduced to a minimum. Elsewhere where the dip is slight and gently undulat- ing, such as in the southern Hills west and north- west of Hot Springs, in the northern Hills near Spear- fish and still better, along the western side of Cold Spring creek in Wyoming extensive areas are cap- ped by this limestone. Local irregular and isolated 12 FORMATION Character Average THICKNESS Feet AGE Laramie Massive Sandstone and Tertiary and Pleistocene Shale 2,500 Ofetaceous Fox Hills Sandstone and Shale... 250-500 do Pierre Shale Dark Gray Shale 1,200 do Niobrara Chalk and Calcareous Shale 225 do Benton Group— Carlile formation.. Gray Shales with thin sandstones, limestone and concretionary layers. 500-750 . do Greenhorn Lime- Impure, slabby lime- 50 do Graneros Shale Dark shale with lenses of massive sandstone in its lower part at some places , 900 do Dakota Sandstone . Massive buff sandstone 32-150 do Fuson Very fine grained sand- stone and massive shale. White to pur- ple color 30-100 do Minnewasta Lime- stone Gray limestone 0-30 do Lakota Massive buff sandstone with some shale 200-350 do Morrison Shale Pale, grayish green shale. — 0-150 Jurassic Unkpapa Sandstone Massive sandstone white, purple, red buff . 0-250 do Sundance Thin limestones. Dark drab shales and buff sandstones. Massive sandstone at base 60-400 do Spearfish Red. sandy shale with gypsum beds 350-500 Triassic Minnekahta L i m e- stone Thin-bedded, gray or purple limestone 30-50 Permian Opeche Red, slabby limestone and sandy shale 90-130 Permian Minnelusa Sandstones, mainly buff and red; in greater part calcareous. Some shales and thin lime- stones included 400-450 Carboniferous Paliasapa Lime- do stone Massive gray limestone 250-500 Englewood Lime- do stone Rink, slabby limestone 25 White wood Lime- stone Buff colored, mottled limestone, with green- ish shales at top 0-80 Ordovician Dead wood Red-brown quartzite, calcareous shales and sandstones, locally conglomeratic, partly massive » • • 4-150 Cambrian 13 areas are common. Such are the tongue'like extension between Hot Springs and Alabaugh canyon, the elongated irregular dome alongside the Chicago & Northwestern railway northwest of Rapid City, and the more or less circular outcrop about Green moun- tain, Strawberry mountain, Inyan Kara, Warren peaks, Elkhorn peak, Crook mountain Bear Butte* etc. The formation affords many fine springs, a feat- ure of much interest. It is the source of the abund- ant thermal waters at Hot Springs and Cascade springs and of colder waters at many other places. Analyses as elsewhere given show this limestone to be of excellent character for various industrial uses. It serves for the manufacture of high grade lime and is indeed the chief source of such material for the Black Hills region. It was used for a considerable time in the smelter at Rapid City in the reduction of the siliceous gold ores of the northern Hills, the lime- stone being obtained alongside the Chicago & North- western railroad three miles northwest of Rapid City. It is now being extensively utilized in the cyanide plants of the Homestake Gold Mining Company in Lead, their two kilns of modern make being constant- ly in operation at the quarry on Elk creek near Doyle on the Burlington railroad a short distance above Pied- mont. The following analyses of this limestone indi- cate its superior nature in the preparation of a high- grade Portland cement. Analysis No. I is by Profes- sor M. F. Coolbaugh of the School of Mines, the ma- terial coming from an outcrop alongside the Missouri river and Northwestern railroad near the old Canyon Lake site, four miles west of Rapid City. Analysis No. 2 and No. 3 are from samples taken near Newcastle. These two analyses are given in Bulletin No. 315 of the U. S. Geological Survey.* ♦Ball. Sydney H. Portland Cement Materials in Eastern Wyoming. Bulletin No. 315, U. S. Geol. Survey, p. 232-244. 14 Table No. 2. Analysis No. 1. Silica, SiC>2 Ferric Oxide, Fe2 O3 Alumina, AI2 O3 Titanium oxide, Ti02 Lime, CaO Magnesia, MgO Sulphur, S Alkalies, ^2 < 0, Phosphorus pentoxide, P2 O5 Carbon dioxoxide, CO2 Water, H2 O 1.21 Percent 0.16 0.47 trace 54.56 0.41 0.11 trace trace trace 42.30 0.91 Total 100.13 Loss on ignition 42.95 percent. Table No. 2 A. Analysis Nos. 2 and 3. No. 1. No. 2. Silica, SiCL 1.08 Percent 1.42 Percent Alumina, AI2 O3 0.33 0.68 Ferric oxide, Fei*2 O3 0.77 0.40 Manganese oxide, MnO, 0.46 0.11 Lime, CaO, 53.40 52.85 Magnesia, MgO, 0.57 0.72 Sulphuric anhydride, S03, 0.12 0.12 Alkalies, 0.36 0.16 0.76 0.30 Water at 100° C 0.20 0.10 Ignition loss 42.92 42.78 Total 100.37 100.24 The Graneros Shale. The Graneros shale is the st member of what is frequently known as the Benton group. Lying as it does just outside the main Cretaceous hogback its outcrop completely encircles the Black Hills uplift as a broad belt of low undulating hills and valleys and serves as the innermost fringe of the great plains of the Black Hills region. i5 The formation is made up distinctively of fine- grained dark gray to black shale, but there is consid- erable modification of this simple character in many places, especially in that portion of the area lying with- in the borders of Wyoming. Here a well-defined four-fold character generally shows itself, viz., first, a lower portion of fine black fissile shale 150 to 300 ft. thick; above this, massive grayish-buff sandstone of varying thickness up to 40 ft. ; following this a series 250 to 300 ft. thick of dark shales of hard texture which weather to a distinct grayish white color ; lastly, at the top a series of very black shales 400 to 500 feet thick, much resembling the shales of the lowest mem- ber. In that portion of the Black Hills region lying within South Dakota the four fold character is less prominent and particularly is this true so far as con- cerns the eastern and southern portions of the uplift. The sandstone member varies greatly in thick- ness and hardness; sometimes it stands out in bold cliffs much like the Dakota sandstone whose texture and grayish-buff color it closely simulates. Elsewhere ii is much concealed and over considerable areas it is thin or absent. Near Newcastle where this member reaches local prominence the rock contains petroleum as indicated by certain bore holes and by small flows from several natural springs. The sandstone shows in various places along the eastern side of the Black Hills, as, for example, at Rapid City and Hermosa, but here it partakes more of the nature of greatly elongated lenses and, except for a few lenticular hills, is of little or no topographic significance. The hard grayish shale member, now commonly designated as the Mowrie beds, from Mowrie creek near Buffalo, Wyoming, where it was first studied, is prominent in much the same areas as the underlying sandstone except that it partakes less of the lenticular nature of the latter. Its greatest thickness is apparent- ly in the vicinity of Belle Fourche and northwest of there along the Belle Fourche and the Little Missouri i6 rivers. Ridges often result from the more rapid wear- ing away of the softer shales and these ridges by con- trast of color, by topographic importance and by their general wooded covering serve admirably in delineat' ing the outcrops of these beds from the generally non-wooded darker shales of the lower and the up- per members. The beds are further characterized by the presence of multitudes of fish scales in almost all good exposures. Southeast of Belle Fourche the gray color and the indurated nature become gradually less distinctive and the fish scales grow fewer in num- ber until at Rapid City only the closest scrutiny es- tablishes the presence of any portion of the member. The lowest member needs little more character de- scription than already given. With the exception of the passage beds of alternating shales and sandstones near the bottom and occasional bands of fair to good sized lime-clay concretions it is practically entirely a fine fissile, black shale. It lends itself to especial at- tention here in that the shale material used with lime- stone from the Minnekahta formation in the prepara- tion of the Portland cement described elsewhere in this bulletin was obtained from this member. The follow- ing chemical analyses shows its favorable character. No. i is by Professor Coolbaugh of the Shool of Mines and represents material obtained a few hundred yards north of the Hinrichs-Lanphere saw mill in Rapid City. No. 2 represents material from near New- castle and is recorded in Bulletin No. 315 of the U. S. Geological Survey.* *Ball. Sydney H. Portland Cement Materials in Eastern Wyoming. Bulletin No. 315, U. S. Geol. Survey, p. 232 244. Table No. 3 Analysis No. 1 Silica, SiOs, 58.74 Percent Ferric oxide, Fes O 3 3.87 Alumina, Als Og" 18.97 Titanium oxide, Ti0 2 , 0.71 Lime, *CaO, 0.93 Magnesia, MgO, 1.62 Sulphur, S, 0.21 Alkalies, §2 0^ 1.49 • 0.58 Phospheros pentoxide, Ps O5 1.44 Manganese oxide, MnO, trace Loss on ignition 11.93 Total 100.24 Table No. 4. Analysis No. 2. Silica, SiOs 58.82 Percent Alumina, Als O 3 , 16.43 Ferric oxide, Ees O 3 4.47 Manganese oxide. MnO. 0.24 Lime, CaO, 0.54 Magnesia, MgO, 1.68 Sulphuric anhydride, SO 3 1.32 Alkalies, K 2 2 0 0 ’' 0.33 2.18 Water at 100° C, 6.39 Ignition loss, 7.93 Total 100.33 There is little or no reason for believing that much of the shales of the higher members of the formation would not lend themselves as freely to the production of good cement as the lowest member, although lit- tle experimental work has been carried on by way of demonstrating their real value for such purpose. The upper black shale member much resembles the lowest member. It is generally thicker and is inclined to be more abundantly supplied with lime-clay i8 concretions. These concretions sometimes reach a diameter of five or six feet or more. Thin bands of limestone are occasionally found. Some of these are highly fossiliferous and, while never of great thickness, they occasionally are able to control the topography sufficiently to out- line ridges and hills of some prominence. The formation taken as a whole is well exposed. The outcrop is generally wide. This is more particu- lary true around the northern end and along the west- ern side of the- Hills where for many miles it serves as a wide valley bed for the Belle Fourche and the Little Missouri rivers and their tributaries, the width of outcrop in places reaching ten or a dozen miles or more. Along the eastern foothills the outcrop is nar- rower. From Whitewood creek southward to Spring creek it varies from one to four or five miles. South of Spring creek it is much concealed by unconformable Tertiary deposits. Throughout the entire region allu* vial deposits cover up considerable areas along the streams and higher gravels veneer many of the gentle slopes and flat topped hills and ridges. The alluvial deposit is particularly prominent along the Belle Fourche river and the Little Missouri river in the northern and northwestern part of the area and along lower Beaver creek and certain portions of the Chey- enne river in the southern part. This covering pre- vails to a less extent elsewhere but is of significance wherever the formation is crossed by streams of a me- andering nature. The Graneros, like the Minnekahta, is favorably situated with reference to railroads. Northwest of Newcastle and between Newcastle and Edgemont the Burlington is built upon this formation, for many miles. This road could easily reach it by short exten- sion near Piedmont or near Spearfish if such should be desired. At Rapid City the formation is convenient to the Missouri river and Northwestern, to the Chi- cago, Milwaukee and St. Paul, and to the two lines of 19 the Chicago & Northwestern. South of Rapid City to Buffalo Gap the Chicago & Northwestern touches it at many points. North of Rapid City to Whitewood this road lies within the red valley but even here easy access is permitted to the Graneros by the many notches through the intervening hogback ridges. North of Whitewood the Belle Fourche branch of the Chicago & Northwestern railroad quickly passes outside the red valley to the formation. It then follows the general di- rection of outcrop to and beyond Belle Fourche, being flanked on both sides by exposures in most conven' ient mariner. In much the same way west of Belle Fourche ihe formation lies convenient to the Wyoming and Missouri River railroad. The Niobrara Formation. The Niobrara forma- tion lies just beneath the Pierre shale. Compared to the Pierre it is thin, being seldom more than 225 ft. thick and around the northern end of the uplift it is approximately 100 ft. The material is very soft, is highly calcareous, and partakes more or less of the nature of an easily pulverized chalky limestone. Fresh material is of a blun h-gray color but outcrops are generally well weathered and disintegrated and in this condition the material is of a rich creamy yellow color. The formation seldom develops any topographic features of significance but its pronounced yellow color renders the formation conspicious whenever the out- cropping surface is broken. The fossil oyster, Ostrea congesta, occurs in abundance in occasional thin in' durated bands and this also serves as a distinctive feature. Near the head of the Little Missouri river west of the Bear Lodge range and in the vicinity of Newcastle where local disturbances have given the formation a steep dip the width is only a few yards but frequently elsewhere it reaches one mile or more. In view of the fact that the formation outcrops continuously and in a fairly regular manner around 20 the Black Hills and is so readily distinguished in the field it serves nicely as a stratigraphic guide and deline- ates in an excellent manner the plain ward extent of the more pronounced structural features of the Black Hills uplift. The Niobrara is the' formation that affords much of the raw material for the Portland cement plant at Yankton in the southeastern part of the state. The interesting feature with reference to the Black Hills area is that the chemical nature of the rock 'as revealed by analysis, while not uniform, indicates that this formation can furnish in places within the Black Hills area a most excellent material for natural cement. Its physical condition is almost everywhere particularly favorable. The shaly pulverent nature of the mater- ial would allow for easy excavation and doubtless steam shovel operation could be carried on to consider- able depth. The chemical nature varies and is not ah ways satisfactory but the following analysis by Pro' fessor Coolbaugh of the School of Mines from mater- ial near Antelope creek ten miles east of Tilford shows a particularly favorable composition and indicates the possibility of utilizing this material to most excellent advantage : Table No. 5. Silica, SiC> 2 , Ferric oxide, Fe 2 On and Alumina, AI 2 O 3 Lime, CaO, Sulphur, S Magnesia, MgO, Alkalies, K 2 O, and Na 2 O, Loss on ignition Total 15.51 Percent 5.80 38.85 trace 1.08 1.50 36.67 99.41 This may be more readily compared with the analy- sis of Portland cement manufactured from the Min- nekahta-Graneros mixture given elsewhere in this bul- 21 letin by recalculating so as to omit reference to loss on ignition. The analysis thus arranged is as follows : Table No. 6. Silica, SiOs, 24.65 Percent Ferric oxide, Feg O;} and Alumina, AI 2 O;* 9.16 Lime, CaO, 61.36 Sulphur. S, (estimated) 0.20 Magnesix, MgO, 1.72 Alkalies. K 2 O and Na 2 O, 2.52 Total 99.61 Table No. 7. Silica Si02. Ferrie Oxide and 1 Lime CaO, Magnesia, MgO, Alkalies, Sulphur, Loss on ignition Total No. 4. ' Near Rapid Oity. 22.47 mina 9.80 25.01 1.54 0.75 1.84 38.25 ( 99.66 No. 5. Bear Butte Piere 6.81 3.23 46.75 0.93 1.43 trace 39.56 99.71 The Burlington and Missouri River railroad fol- lows the outcrop of the formation for some miles near Ardmore and near Newcastle and crosses it again near Moorcroft. The Chicago & Northwestern railroad crosses it near Buffalo Gap, then follows it fairly close- ly to Rapid City. Just east of Rapid City the Pierre, Rapid City & Northwestern cuts across the formation in a particularly favorably manner while the Chicago, Milwaukee & St. Paul could reach similarly good out- crops near by with little side trackage. Between Rapid City and Whitewood the formation outcrops in a wide belt several miles east of the railroad but this could be easily reached if desired through the various gaps in the hogback ridges. 22 The Morrison Formation . The Morrison forma- tion of early Cretaceous or late Jurassic age lies just beneath the Lakota sandstone. It does not completely encircle the Hills, there being a considerable space in the southeastern portion of the uplift where it is ab- sent.. Along the eastern side of the Hills it is under lain by the massive soft Unkapapa sandstone but along much of the western portion of the uplift the Unkpapa is absent and it is underlain by the Sundance forma- tion. The formation is made up of shales and thin nod- ular bands of white argillaceous limestone, the shales greatly predominating. Sometimes the clay-lime nodu- les are of little or no significance and occasionally thin shaly sandstones appear, the latter showing best in the Bear Lodge mountains. The shales carry more or less carbonaceous matter and vary much in color. Olivine green predominates in fresh exposures but pale green- ish gray, yellowish gray, pink, red, maroon, chocolate, purple, and black are not infrequently observed. A characteristic and fairly common feature of the for* mation is the presence of large saurian bones near the bottom of the formation. Several localities have af* forded good specimens. The formation where best exposed varies in thicks ness up to 160 feet or more. In the Bear Lodge moun- tains and southward it varies from 40 ft. to 160 ft. Along the northeastern side of the Hills the thickness varies in much the same way. On the Oelrichs quad- rangle it is absent. Exposures are good in many places *and conven- ient to the railroads. The Chicago & Northwestern parallels the outcrop all the way from Rapid City to Whitewood and could easily tap many of the expos- ures by short spur trackage, the outcrops being all to the east of the track and at various convenient heights above the main line. The Burlington and Missouri River railroad crosses the formation between Edge- Scale 0 10 20 30 <0 00 Julies 1 J l i J I Map showing outcrop of the Morrison formation .. K . v i 23 mont and Minnekahta and is fairly convenient to it near Newcastle and Piedmont. The Wyoming and Missouri River railroad follows the formation for some distance near Aladdin. Little experimental study has been given this for- mation but it is worthy of consideration. An analy- sis* of material obtained near Newcastle gives the fol- lowing favorable composition : Table No. 8. Silica, Si O 2 , 45.78 Percent Alumina, AI 2 O 3 12.92 Ferric oxide, Fe 2 O 3 3.95 Manganese oxide, MnO, 0.83 Lime, CaO, 0.56 Magnesia, MgO, 0.73 Sulphuric anhydride, SO 3 0.48 Alkalies, Na 2 O, 0 64 K 2 O, 0.50 Water at 100° C, 8.26 Ignition loss, largely 26.32 carbonaceous matter Total 100.42 The Carlile Formation. The Carlile formation outcrops immediately within the Niobrara and consti- tutes the upper portion of the Benton group. It is made up of a series of thin black shales with occasional thin impure sandstone and limestone bands. In places the limestone is quite argillaceous and takes on the form of large concretionary or lenticular masses. These sometimes contain fossils. In the Devils Tower quadrangle the formation is made up of three fairly distinct divisions, viz., an up- per division, chiefly shale, 300 feet thick; a middle di- vision 125 feet thick, concretions and shale; and a low- er division 200 feet thick, mostly shale. Elsewhere this threefold nature is absent or is not sufficiently prominent to disclose itself in any characteristic man- *Ball. Sydney H. Portland Cement Materials in Eastern Wyoming. Bulletin No. 315, U. S. Geol Survey, p. 236. 24 ner. The total thickness varies from about 400 feet near Buffalo Gap to about 700 feet in the vicinity of Newcastle. The shale portions much resembles the shales of the Pierre and the Graneros and doubtless the chemical composition is much the same. The formation is readily accessible to the various railroads in much the same manner as the overlying Niobrara. Since it has not been carefully studied as to possibilities in the way of affording ingredients for cement manufacture further description need not be given at this time. The Pierre Formation. The Pierre formation is the latest Cretaceous formation that outcrops within the immediate Black Hills region. It completely encir- cles the uplift as a broad belt and is one of the greatest formations of the Plains region. West of the Hills its outcrop averages perhaps five or six miles in width. Northeast, southeast, and south of the Hills it reaches several times this width while to the east of the Hills it extends far beyond the limits of the regions under discussion. Every railroad entering the Hills traverses the formation for several or many miles and good ex- posures are abundant and convenient. The thickness of the formation is given as ap- proximately 1200 feet. The material is almost wholly black shale. Weathered surfaces show lighter color and in the lower portion where some lime enters into the composition the color is inclined to a dull yellowish color. Lime and lime'iron concretions are abundant at several horizons. These are often highly fossiliferous. particularly those in the upper part of the formation and the invertebrate forms that they contain are varied in character and often beautifully preserved. The for mation is abundantly exposed and readily distinguish- ed. For further details of structure, distribution and phsical character of this formation as well as for the Carlile the reader is referred to the various publications listed on a subsequent page. 25 Little attention has been given to the accurate chemical nature of the shales. One analysis* made from material obtained one mile above Spencer siding on the Burlington and Missouri River railroad south- ly known as the “red beds.” This formation complete- southeast of Newcastle, is as follows : Table No. 9. Silica, Si02, 60.66 Percent Alumina, AI 2 O 3 22.13 Ferric oxide, Fe 2 O 3 1.21 Manganese oxide, MnO, 0.41 Lime, CaO, 1.59 Magnesia, MgO, 1.54 Sulphuric anhydride, SO 3 0.43 Alkalies, Na 2 O, 0.53 K 2 O, 3.16 Ignition loss 9.28 Total 99.97 The above analysis shows certain undesirable per- centage of ingredients but field observation furnish good reason for believing that a series of analyses of material selected from various localities would show a fair number with favorable proportions of the var- ious important elements. Gypsum. A brief word concerning the nature and occurrence of Black Hills gypsum may be of inter- est here in view of the fact that gypsum enters in a minor way into the manufacture of cement. The deposits of Black Hills gypsum occur at var- ious horizons within the Spearfish formation, popular- ly known as the “red beds.” This formation complete- ly encircles the Hills and good exposures seldoms fail to show gypsum, nearly pure white, in sufficient quant- ity and of sufficient purity to be of commercial value. The deposits are extensive and convenient. They are sometimes lenticular but more often they occur in beds *Ball. S. H. Portland Cement Mat. in Eastern Wyoming. Bui. 315, U .S. G. S. p. 238. 26 of nearly uniform thickness and in some places where the outcrop is favorable these white beds may be traced across the landscape for many miles as they stand out in prominent contrast to the enclosing red sandy shales. The gypsum is of a high degree of purity and for several years has been utilized in the manufacture of stucco or plaster. Two plants are now in active opera- tion, one at Hot Springs and one near Rapid City. The Hot Springs plant has been in interrupted operation for several years. The Rapid City plant was placed in commission early in the year 1908. Both plants are convenient to large bodies of good raw material. Analysis of the Hot Springs gvpsum made by Pro- fessor Coolbaugh show the following composition. No 1 is from a thirteen foot bed near the bottom of the ex- posure and No. 2 is from a four foot, the two being separated by one foot of red shale carrying only thin seams of gypsum. Both beds are utilized. Table No. 10. Silica, SiOs, 0.12 Ferric oxide, Fes Ob A lumina, Als Ob 0.12 Sulphuricanhydride,SOB 47.77 Lime, CaO, 83.00 Magnesia, MgO, a 10 Loss on ignition 20.85 Totol 101.97 0.09 Percent 0.06 44.86 32.89 0.28 21.41 98.59 Mr. Steiger of the U. S. Geological Survey lab- oratory gives the following analysis of material from near Cascade Springs:* *Dartcn, N. H. Gypsum Deposits in South Dakota. Bulletin No. 223, U. S. Geological Survey, p. 76-78. Map showing outcrop of the gypsum- bearing Spearfish formation Reproduced from U. S. G. S. Bulletin No. 223. New railroads inserted 27 Table No. 1 1. Lime, CaO, 32.44 Percent Magnesia, MgO, 0.33 Alumina, AI 2 O 3 0.12 Silica, Si O 2 0.10 Sulphuric anhydride, SO:* 45.45 Carbon dioxide, CO 2 , .85 Water, H 2 O, 20.80 Total 100.09 Additional Literature. The reader who may wish to examine more fully into the details of distribution and description of the various geological formations de- scribed or mentioned in this paper will find much ad- ditional information in the following atlas folio publi- cations of the U. S. Geological Survey : Darton, N. H., Oelrichs folio. No. 85, 1902. Darton, N. H. Newcastle folio. No. 107, 1904. Darton, N. H., and Smith, U. S. T. Edgemant fo- lio No. 108, 1904. Darton, N. H., Sundance folio, No. 127, 1905. Darton, N. H. and O’Harra, C. G. Aladdin folio, No. 128, 1905. Darton, N. H., and O’Harra, C. C., Devils Tower folio No. 150, 1907. PART II. OUTLINE FOR THE ANALYSIS AF CEMENTS AND CEMENT MATERIALS. M. F. COOLBAUGH, M. A. Outline for Analysis of Ce- ment and Cement Materials. M. F. COOIvBAUGH, M. A. The outline scheme for the analysis of cements will serve in many places as a scheme for the analysis of limestones v raw mixtures, shales and clays. Decomposition . — With highly silicious material decomposition can be effected by treatment with hy- drochloric and nitric acids, filtration, fusion of the resi- due with sodium carbonate, and solution of the fused mass in water and hydrochloric acid. Or the fusion may be made directly without a previous treatment with acids. For the decomposition of limestones or unburned mixtures, ignite material with one-half to an equal weight of sodium carbonate and treat mass with diluted hydrochloric acid. Silica . — Two evaporations are essential for this determination when considerable accuracy is required. Even then a complete separation is not effected, as some silica will be found with the iron and alumina precipitate. Some alumina will also be found with the dehydrated silica. Corrections for these small amounts of impurities are not, however, necessary in technical work, since the weights tend to counterbalance each other. For greater accuracy, the silica should be driven off by treatment with hydrofluoric acid and a few drops of sulphuric acid. The residue should be 32 added to the precipitates from the ammonia treatment. Iron and Alumina . — The precipitates of iron and aluminum hydroxides, which contain also titantic-acid, ferric phosphate, and a small amount of silica, is puri- fied from calcium and traces of manganese by solution in nitric acid and reprecipitation with ammonia. The calcium in the first precipitate is caused by impurities of ammonium carbonate in the ammonia, or by carbon di- oxide in the air of the laboratory. The manganese is mot separated even by two precipitations unless the content of that element is small. If this is not the case, separate it from the iron and aluminum by precipita- tion of the latter as basic acetates in a dilute acetic acid solution containing sodium acetate. The amount of silica is separated after the fusion with the acid sodium sulphate, as in (3), and evaporation of the sulphuric acid solution to low bulk. The weight found here should be added to that already found. Titanium Oxide . — The titanium is determined in the. solution from the titsation of iron in (3). Add ten c.c. hydrogen peroxide, make to a definite bulk, and compare color with that of a' standard solution of titanium treated in a similar manner. Manganese . — This is determined in the filtrate from the iron and alumina precipitation. It is precipitat- ed with ammonium sulphide, dissolved in nitric acid and determined colorimetrically by use of silver ni- trate and ammonium persulphate. Lime . — Acidify with hylrochloric acid the com- bined filtrates from the aluminum and ferric hydrox- ides precipitates, or the filtrate from the manganese determination, heat to boiling, add 10 to 12 c. c. of a saturated solution of ammonium oxalate and slowly neutralize with ammonia. The longer the time taken for neutralization the less danger there is of contam- ination by magnesium. When greater accuracy is de- sired, the calcium oxalate is filtered, ignited, dissolved Scheme for Analysis of Cement. 33 a? o cec^.2 SO 3 ^ ^ p -* 1 o 3 hSS^“ PPO - .jl & o 3 ® o © 0 ) I '
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