SECTIONS SEISMOLOGISTS 263 



Page 



Sections tlirouKli Copper Mine Hill ami ('iiiubt'i'laiHl Hill 25. 40!), 471 



Sederholm, J. J., cited on Botlniiaii slates 27, 189 



inetamorphisiii 28, 413 



— Upper Cambrian I'ocks 27, 557 



Sedimentaries and lavas in Kittitas County, Washinjiton, Relation be- 

 tween the tertiary 26, 137 



SEniMENTARY character of surnetiferons b.ornblcmle schist, Hanover, New 



Hampshire ; J. W. Merritt 25,7". 



— method in stratigraphy 27, 498 



— rock composition study discussed by .1. M. Clarke 29, 85 



— rocks 28, 163 



, Interpretation of 28, 735 



— — of I'ennsylvania 28, 150 



, Siguihcance of sorting in 28, 925 



, Symposium on the interpretation of 28. 162, 206 



, Triassic 27, 624 



— succession in southern New Mexico ; N. II. Dartou 27, 86 



Sedimentation along the Gulf Coast of the United States; E. W. Shaw 27,71 



— , Catskill 21, 286 



— , Hypothesis of origin of iron ores 23, 323 



— in diastrophism and vulcanisjn, Kole of : F. M. itandy 26, 138 



— , Laws gt)verning 25, 732-737 



— of the interior prt.vince 25, 343 



— , Rhythms in 28, 102, 776 



Sediments. Clinnitic types of 28, 920 



— , Composition of clastic 25, 655 



— , Differences between water and wind 25, 740 



— in relation to landslides 27, 58 



— , Modes of origin of 27, 352 



— of Center County, I'ennsylvania, Upper Cambrian and Lower Ordo- 



vician 24, 112 



— , Unaltered Paleozoic 26, 85 



— , Usefulness in studying earth Iiistory of 29, 84 



Seeley, H. G., cited on oolitic texture 25, 749 



Seelv, Henry Martyn, Bibiography of 29, 68 



— cited on origin of oolitic texture in limestone rocks 21, 645 



— . specimen of Stegosauria in Woodwardian Museum, Cambridge 26,332 



— , Memorial of 29, 65 



Seidel, , cited on uplifted coral islands 29, 558 



Seismograms, Plates showing 21, 375, 376 



Seismograph records and studies; Alaskan earthquake of 1899... 21,374-383 



^ Intervals and times of maxima, Table showing 21, .'>77, 378 



— , Speed of transmission of earthquake shocks determined by. . . . 21,391-395 



— stations, Map showing location of 21, 383 



— , Time of Yakutat Bay earthquake determined liy 21, 386 



Seismographic data, Tables establishing 21. 379-382 



Seismographs, Origin of earthquakes located by 21, .376 



Seismologists, Studies of Alaskan earthquake by experienced 21, 374-394 



