References                                               

1. Rupke, N.A.,  “A Study of Cataclysmic Sedimentation,” Creation  Research  Soc. Quarterly., Vol. 3, 1966, p. 21.

2. ibid. ref. 1,  p. 23. See also:  Bolsche, W., 1918, Im Steinkohlenwald, Stuttgart, Franckh’sche Verlagshandlung, 16 th impr. P. 34;  
   This is discussed in more detail in Part Two of this paper.
3. ibid. ref. 1, p. 23; See also:  Nelson, B.C., (1931), The Deluge Story in Stone, Minneapolis,  Augsburg, 1962, 16th impr. p. 111; 
   and Taylor, W. E., 1857, Voices from the Rocks..., p.?;  Various other upright trees from 25-50 feet long have been documented
    as well; this will be discussed in greater detail in a subsequent publication.

4. Dawson, John W., 1868,  “Acadian Geology,” 2nd ed. Macmillan & Co., London, pp. 151-178. For example, Dawson states:

      "We thus see a  series of  beds  amounting  to  more  than  14,000  feet  in  vertical  thickness, and 
        extending  from the marine limestones of the Lower Carboniferous series  to the top of the Coal
        formation. In the cliff and on the  beach, more  than  seventy  seams of coal may be seen, with their 
        roof  shales  and  underclays,  and erect plants appear  at  as many distinct levels..."  
       Acadian Geology, 1868, p. 151.  Emphasis Added
   

5. Dawson, 1854, Quart. Jour. Geol. Soc. London, Vol. 10,  p.26.  Regarding  the  Drifted  Trunk deposits see pp. 4-27.
6. Dawson vaguely described at  least nine different deposits at  Joggins that  contain large drifted trees; however,
    the  actual  number is almost certainly larger.  For example, on p. 178 of  Acadian Geology (1868), we are told that 
   there are 1224 feet of  "Gray  sandstone  with  gray  and  red shale" with "Many drifted trunks of Sigillaria and 
   Calamites, and an erect Sigillaria in the lowest bed  of  sandstone."  No other details are given. The other drift 
   deposits are described in  similar fashion with few details.  No drawings (or pictures) of these deposits were provided.
7. Dawson, John W., 1868, “Acadian Geology,” 2nd ed.  Macmillan &  Co., London, p. 188;  Lyell,  Sir Charles, 1881,
    Life of Sir Charles Lyell, Vol. II, p. 65; Bell, W.A.,  "Joggins Carboniferous Section of Nova Scotia," Canada Geol. 
   Survey Summary Report; 1912, p. 328.
8. Dawson, John W., 1868, “Acadian Geology,” 2nd ed.  Macmillan  & Co., London,  p. 151-203;  
   See also:  Helder, Margaret, Ph.D.,  “At  Joggins:  Look  What  The Sea  Uncovered,” Creation  Science Dialogue, 
   Vol. 19, No.3, 10/92; pp. 4-5. Dunbar, Carl O.,  Geology, 2nd  Ed., 1960, Wiley  &  Sons, pp.  227-228.  
   Coffin,  Harold,  Origin  by Design, 1983,  Review and Herald  Publishing  Assn.,  Hagerstown,  MD 21740, pp. 117-133. 
   See also Appendix  A.
9. Another place where large tree stumps are preserved without  their  roots  is  Axel Heiberg Island in Northern Canada.
10. ibid. ref. 4, pp. 151-202.
11. ibid. ref. 4, pp. 406, 408-410.  See text (refs. 80 and 109) for actual quotes.
12. Nöggerath, Jakob: Ueber aufrecht im Gebirgsgestein eingeschlossene fossile Baumstämme und andere Vegetabilien. 
    Bonn: Weber, 1819., 65 S. Also: Scheven, Joachim, 1986, Karbon -studien: Neues Licht auf das Alter der Erde; Hänssler 
    Verlag, 94 pp.
13. Rupke, N.A., Creation Research Society Quarterly,  Vol. 3, 1966, p. 25.
14. Schrock, Robert R., 1948, Sequence in Layered Rocks; McGraw Hill, p. 293.
15. Schuchert, Charles, 1915, "A Textbook of Geology", Pt. II, p. 714.
16. Ferguson, Laing, 1988, The Fossil Cliffs of Joggins, Publ. by the Nova Scotia Museum, pp. 9-11, 27
17. ibid. ref. 14, p. 296.   This drawing first appeared in the 1868 Edition of Acadian Geology, by Dawson, Sir William J., p. 198.  
    An earlier  version appeared on p. 172 of the 1855 Edition.
18. Berthault, Guy:   http://www.answersingenesis.org/home/area/magazines/tj/docs/v11n1_sedexp_reply.asp
19. ibid. ref. 5, p. 26;  Acadian Geology, 1855, p. 172, and 1868, p. 198.
20. The reason this coal does not appear laminated is because the drawing in the text is from microfiche. The laminations do 
    not appear in  Shrock's reproduction either--perhaps for the same reason; however, they are present in both the 1855, 
    and 1868 editions of Acadian Geology.
21. ibid. ref. 5, p. 11;  see ref. 33 (in text) for actual quote.
22. Dawson, John W., 1855,  Acadian Geology,  p. 159;  See also ref. 4 p. 188.
23. Lyell, Sir Charles, "Life of Sir Charles Lyell," Vol. II, 1881, p. 65. See also:  Bell, W.A., 1912, “Joggins Carboniferous Section
     of Nova Scotia”, Canada Geol. Survey, Sum. Report; p. 328.
24. Page 164 of  Acadian Geology 1868 Ed.. says four inches, while page 199 says one inch.  An earlier publication (ref. 5, p. 4) 
    also indicates one inch.  Furthermore, we are told on page 164 that there is an underclay beneath this coal, while on page 199
     we are told there is not.  Logan  refers to the  underclay as a  "Gray argillo-arenaceous shale, with stigmariae. " 
     Logan's measurements indicate  that  this seam was four inches thick. In either case the evidence  suggests  that  this  tree
     probably crossed this seam that  was  full  of  Poacites (ref.5 p.4) long  striated  leaves  now referred to as Cordaites
25. ibid. ref.5, p. 26.  See also note on ref. 26 below.
26. According to a Nova Scotia Dept. of Mines  Website:  See ref. 162 for URL. 
      "... (Fallen logs up to 13 m long have been found in former coal mines in  the area)."
    
    Note:  With regard to this 13 m (40 foot) tree: I  contacted  Mr Calder to ask if he saw it himself, or, if not to provide a reference.
      Mr. Calder said that he did not have first-hand knowledge  but that  he would ask the person who told him and get back to me.  
    So far he has not done so; however, some light was added on this in a recent discussion that I had online with Bill Birkeland.  
    Here is a Link to this part of our discussion.  The entire discussion is  Here,.
    
27. ibid. ref. 5 p. 8.
28. ibid. ref. 4 pp. 164-165.
29. ibid. ref. 4, p. 165.
30. Dawson, John W.,  Acadian Geology 1855, p. 173.
31. ibid. ref. 5, http://www.talkorigins.org/faqs/polystrate.html" p. 21;  This drawing also appears in Lyell and Dawson, 1853, Vol. 9, 
    Quart. Jour. Geol. Soc. Lon., p. 62; Dawson, J. W.,  Acadian Geology, 1855 and 1868 Eds., and Calder, J. H. and  Scott A. C.,  
    Geology Today, Nov.-Dec. 1994, p. 214.
32. ibid. ref. 4, pp. 157-178.  See also ref. 5 pp. 3-10, and Logan, Sir William E., appendix to the first Report of Progress of the 
    Geological Survey (of Canada), 1843 (published in 1845), pp. 92-156.  Logan's report is reprinted in the Proc. and Trans. of the
     Nova Scotia Inst. of Science, 1908, Vol. XI, pp. 419-499.  See also Appendix  A.
33. ibid. ref. 5, p.11
34. ibid. ref. 4, p. 168.
35. Lyell, Sir Charles, and Dawson, Sir John W., 1853, Quart. Jour. Geol. Soc. London, Vol. 9, p. 58-62.
36. ibid. ref. 1,  pp. 24-25
37.  Fauth, Ph. 1913, Hörbigers Glacial-Kosmoganie.  Eine Neue Entwickelungs-geschichte des Weltalls und des Sonnensystems, 
    Kaiserslautern, Kayser, p. 445.
38. http://www.answersingenesis.org/Home/Area/Magazines/docs/cen_v18n1_forests.asp  
39. The "river / flood plain" scenario for the Joggins deposits is quite popular. See also ref. 16, pp. 8, 11, 17, 42.
40. http://www.talkorigins.org/faqs/polystrate/trees.html.
41. ibid. ref. 16, p. 11.
42. ibid. ref. 16, p. 27.
43. Bell, W.A., “Joggins Carboniferous Section of Nova Scotia,” Canada Geol. Survey Summ. Rep; 1912,  p. 331.
44. Helder, Margaret, 1992, "At Joggins: Look What The Sea Uncovered," Creation Science Dialogue, Vol. 19, No. 3, p.5.  Helder 
    also provides the following reference: Gibling,  M.R., 1987, "A Classic Carboniferous Section: Joggins, N.S. Geological Society
     America Centennial Field Guide, NE  Section," 5(88): p. 411.
45. Duff, P. McL. D., and Walton, E. K., 1973, "Carboniferous Sediments at Joggins, Nova Scotia", In: Septieme Congres 
    International de Stratigraphie et de Geologie du Carbonifere; Compte Rendu; 7; 2, pp. 355-379, See pp. 370-372.  Note: 
     Congres International de Stratigraphie et de Geologie du Carbonifere = International Congress on Carboniferous 
    Stratigraphy and Geology.  See also ref. 66.
46. Archer, W., Calder,  John H., Gibling,  Martin R., Naylor,  Robert D.,  Reid,  Donald R., and Wightman, Winton, G.,  1995,
     "Invertebrate trace fossils and agglutinated foraminifera as indicators of marine influence within the classic Carboniferous
     section at Joggins, Nova Scotia, Canada, Canadian Journal of  Earth Science, Vol. 32, pp. 2028-2029.
47. Calder, John H., "The impact of climate change, tectonism and hydrology on the formation of Carboniferous tropical 
    intermontane mires: the Springhill coalfield, Cumberland Basin, Nova Scotia," Palaeogeography, Palaeoclimatology, 
    Palaeoecology, 1994, Vol. 106, p. 323.
48. http://www.gov.ns.ca/natr/meb/ONE/98ofr5.htm
49. White, Judith C., Gibling, Martin R., Kalkreuth, Wolfgang D., "The Backpit seam, Sydney Mines Formation, Nova Scotia:
    A record of peat accumulation and drowning in a Westphalian coastal mire," Palaeogeography, Palaeoclimatology,
     Palaeoecology, 1994, Vol. 106, p. 223.
50. http://www.talkorigins.org/faqs/polystrate.html">Acadian Geology, 1855, pp. 129-130.  See also ref. 5 above, p. 3.
51. http://www.talkorigins.org/faqs/polystrate.html"> ibid. ref. 5, pp. 28-29.
52. ibid. ref. 4, p. 179.
53. ibid. ref. 5, p. 29.
54. Brown, Richard, 1849, Quart. Jour. Geol. Soc. Lon., Vol. 6,  p. 129.
55. ibid ref. 54, p. 131
56. Brown, Richard, 1847, Quart. Jour. Geol. Soc. Lon., Vol. 4, p. 49.
57. ibid. ref. 39.
58. Personal correspondence with author.
59. ibid. ref. 16, pp. 13-18.
60. ibid. ref. 4, pp. 169-176 and 181-188; refer to Coal Groups 18-45 of the Division 4 Coals.
61. ibid. ref. 4, p. 188.
62. ibid. ref. 5, p. 30
63. Lyell, Charles, 1871, The Student's Elements of Geology, p. 379. Also: http://www2.cddc.vt.edu/gutenberg/etext03/geogy10.txt ; 
    Or go to:  http://promo.net/cgi-promo/pg/t9.cgi  and search for Charles Lyell.
64. Brown, Richard, 1846, Quart. Jour. Geol. Soc. Lon., vol. ii, p. 395, Fig. 2;  See also ibid. ref. 4, p. 406-B
    See also Appendix A for a bed by bed  analysis of Coal Groups 1-12 of the Joggins strata.
65. ibid. ref. 42, p. 332.
66. ibid. ref. 44, p. 370.  Note: A reference for Lyell's quote is provided in their paper.
67. Calder, John H.,  http://www.gov.ns.ca/natr/meb/ONE/98ofr5.htm 
68. Coffin, Harold, Origin by Design, 1983, Review and Herald Publishing Assn., Hagerstown, MD  21740, pp.120-121.
69. ibid. ref. 4, p. 186.
70. Brown, Richard, 1849, Quart. Jour. Geol. Soc. Lon., Vol. 5, pp. 358-360.
71. ibid. ref. 4, p. 183.
72. Lyell, Sir Charles, 1845, Stigmaria in micaceous sandstone; Travels in  North  America, Canada, and Nova Scotia, with Geological
     Observations, p. 151, Fig. 20.
73. ibid ref. 68, pp.120-121. See also : http://www.icr.org/pubs/imp/imp-316.htm 
74. Lyell, Sir Charles, 1845; Travels in North America, Canada, and Nova Scotia, with Geological Observations, pp. 151-153.  
    This illustration also appears in "The Natural History of Coal," by Arber, E. A. Newell, 1911, Cambridge Univ. Press, p. 103
     It also appears in ref. 152, (p. 265) of this paper. See also Lyell, Sir Charles, 1871, The Students Elements of Geology, Lon.,
     pp. 392-393.Geikie, Sir Archibald, 1903, Text Book of Geology, p. 655. Note:  Geikie gives reference to a Memoir by M. Fayol 
    from which this photo may have been taken. He also informs us that this tree is from the Nova Scotia coal-fields.
75. ibid. ref. 74.
76. Brown, Richard, 1846, Quart. Jour. Geol. Soc. Lon., Vol. 2, p. 394-396.
77. ibid. ref. 4, p. 406-B. Note: This page is between pp. 406 and 407.
78. Although Dawson does tell us that Figs 1, 2, and 3  "are from papers by  Mr. Brown  quoted in the text," he does not say 
    which ones.  In other words, the inquisitive reader is forced to look up all of Mr. Browns papers (listed in Chapter 1) in order
    to find any other details about  this tree.  This is also the case for the tree in fig. 9 (above ref. 78) in Part 1 (of text) -- which  
    Dawson  also had  re-drawn  and  is pictured on the same page.
79. ibid. ref. 4, p. 406.
80. Dawson, John .W. Acadian Geology, 1855, p. 54; and 1868, p. 81.
81. ibid. ref. 68.
82. Dawson, J. W., 1866,  "On  the Conditions of the Deposition of  Coal...of  Nova  Scotia,"  Quart. Jour. Geol. Soc. Lon., Vol. 22, 
    pp. 127-128.
83. ibid. ref. 5, p. 34.
84. ibid. ref. 4. p. 183.
85. Scott, A. C. and Falcon-Lang, H. J., 2000, "Upland ecology of some Late Carboniferous corditalean trees from Nova Scotia 
    and England,"  Palaeogeography, Palaeoclimatology,  Palaeoecology, Vol. 156, pp. 228-230.
86. Austin, Steve, 1986,  "Mount St. Helens and Catastrophism,"  ICR Impact Article 175.
87. Morris, John D., The Young Earth, 1994, p. 103.
88. ibid. ref. 86, p. 230.
89. Dawson, John William, 1846, Quart. Jour. Geol. Soc. Lon., Vol. 2, pp. 132-134.
90. ibid. ref. 4, pp. 179-183.
91. Lacefield, Jim, 2000, Lost Worlds in Alabama Rocks, The Alabama Geological Society, p. 61.
92. Calder, John H., Nova Scotia Dept. of Natural Resources website, at: http://www.gov.ns.ca/natr/meb/ONE/98ofr5.htm
93. Dawson, John W., 1865, Quart. Jour. Geol. Soc. Lon., pp. 103-105.
94. ibid. ref. 4, p. 172.
95. ibid. ref.  68, p. 120.
96. ibid. ref. 4, p. 185.
97. ibid. ref.  94.
98. Coffin, Harold G., "A Paleoecological Misinterpretation".  Note that this is only a summary of Coffins article.   
    See also "The Spirorbis Problem" -- also by Coffin.  
99. ibid. ref. 86, pp. 225-234.
100. Darwin, Charles.  More Letters Of Charles Darwin -- Volume 2,  LETTER 555.  TO J.D. HOOKER;  May 22, 1860.
101. More Letters Of Charles Darwin -- Volume 2,  Letters 552, 553, and 555  To J.D. Hooker;
     May 1846, June 2nd, 1847, and May 22nd, 1860.  This may also be found online at:
     ftp://ibiblio.org/pub/docs/books/gutenberg/etext01/2mlcd10.txt ;  Or go to :
     http://promo.net/cgi-promo/pg/t9.cgi  and search for Charles Darwin .  See also:  Binney, E. W., 1844, The London, Edinburgh, and 
     Dublin Phil. Mag., Vol. XXIV, p. 173.  And: Binney, E. W., 1848,  “On the Origin of Coal,” Mem. Literary and Philosophical. Soc. of 
     Manchester; AKA : Mem. of the Manch. Lit. and Phil. Soc.; Vol. VIII, pp. 148-193 ?
102. http://www.answersingenesis.org/Home/Area/Magazines/docs/cen_v18n1_forests.asp
     See also: Wieland, Carl,  "Forests that grew on water," Creation, Vol. 18, No.1, Dec. 1995- Feb. 96, pp. 20-24.
103. Kunze, Otto, 1884, Die vorweltliche Entwicklung der Erdkruste und der Pflanzen Phytogeogenesis.
104. ibid. ref. 4. pp. 151-211.
105. ibid. ref. 4, pp. 158-159; ibid. ref. 5, pp. 13-14. 
106. ibid. ref. 4, p. 167
107. ibid. ref. 4,  p. 169
108. ibid. ref. 44. p. 356. 
109. Price, George, M. 1923, The New Geology, pp. 462-3
110. ibid. ref. 4, pp. 408-9.
111. ibid. ref. 68, pp. 132-133.
112. ibid. ref. 54, p. 120.  According to Brown, section 174 is 2 feet, 7 inches thick and composed of  Argillaceous shale," and  section 
     175 is 4 feet thick and composed of "Arenaceous shale"  (with) "(Erect Trees)."
113. ibid. ref. 54, p. 130.
114. ibid ref. 4, p. 164
115. Personal communication with author.  The 1995 paper referred to is ref. 46; the 1998 paper is ref.  152. Faure, G. Principles of Isotope
      Geology, 2nd edition, 1986, pp. 309-340.
116. Skilliter, Deborah M., 1997, Geol. Soc. Amer. Abstracts with Programs, Vol. 29, p. 80
117. Nevins, Stuart E., 1976, "The Origin of Coal." ICR Impact Article 41; Available online at:  http://www.icr.org/pubs/imp/imp-041.htm
118. A. D. Cohen, 1970, "An Allochthonous Peat Deposit from Southern Florida," Geol  Soc. of Amer. Bulletin, Vol. 81, pp. 2477-2482.
119. Rupke, N. A., Oct. 1969,  "Sedimentary Evidence for the Allochthonous Origin of Stigmaria, Carboniferous, Nova Scotia," 
      Geol. Soc. Amer. Bull., Vol. 80, pp. 2109-2114.  See also Coffin, Harold G., 1983, "Origin by Design", pp. 41-53 and 117-133.
120. Ferguson, Laing, 1970, Geol. Soc. Amer. Bull., Vol. 81, pp. 2531-2534.
121. Rupke, N. A., 1970, Geol. Soc. Amer. Bull., Vol. 81, pp. 2535-2538.
122. Williamson, C. W., 1887, "A Monograph on the Morphology and Histology of Stigmaria ficoides," p.12., Lon. Palaeontograhical Soc..
123. ibid. ref. 123, pp. 40-44.
124. Lesquereux, Leo, 1880, "Description of the Coal Flora of the Carboniferous Formation in Pennsylvania and Throughout the U. S.,
     Vol. 1, pp. 510-513.
125. ibid. ref. 44.
126. ibid. ref. 68, pp. 125-127.
127. ibid. ref. 88, pp. 100-103
128. Austin, Steven A., 1986, "Mount St. Helens and Catastrophism," Impact  Article 157, Published by the Institute for Creation Research.  
     See also Dr. Austin's 1992 video presentation on Mount St. Helens.
129. Coffin, H. G., 1968,  "A Paleoecological Misinterpretation," Creation Res. Soc. Quart.,  Vol. 5, pp. 85-87;  
     See also  http://www.creationresearch.org/crsq/abstracts/sum5_2.html , See also Barnes, R.  D., 1963, Invertebrate Zoology, p. 205; 
     and Thorson, Gunnar, 1957, Geol. Soc. Amer. Mem. 67, p. 480.  Also ref. 4 pp. 151-207, For Dawson's Comments on Spirorbis, esp. p. 181.
130. ibid. ref. 4, p. 181.
131. ibid. ref. 4, pp. 205-206.
132. It is almost certain that Sigillaria trees had hollow (or semi-hollow) trunks.  This is because in virtually  every case where they are found,
     they are either "flattened" (when prostrate) or filled with sediments  (when upright).  See also ref.  4 pp. 151-203.  See also ref. 167 below.
133. ibid. ref. 101 and 102.
134. ibid. ref. 103, 104.
135. ibid. ref. 130
136. Schultze, H. P., and J. Chorn, 1997, "The Permo-Carboniferous genus  Sagenodus and the beginning of  modern lungfish," Contributions 
     to Zoology,  Vol. 67 (1), pp. 9-70.  For a summary see: www.uba.uva.nl/ctz/vol67/nr1/art02/6701a02#Spirorbis.html.
137. ibid  63. p. ???
138. ibid. ref. 46, pp. 2027-2039.
139. Wightman, W. G., Scott, D. B., Medioli, F. S., and Gibling, M. R., July, 1993, "Carboniferous marsh foraminifera from coal-bearing 
     strata at the Sydney basin, Nova Scotia...", Geology, V.21, pp. 631- 634.
140. Price, George M., 1923, The New Geology,  pp. 400-401, 417.
141. ibid. ref. 92, pp. 43-45.
142. Dawson, Sir William J., 1868, “Acadian Geology,” 2nd ed. Macmillan & Co., London, pp. 165, 206.
143. Moore, Raymond C., Lalicker, Cecil G., and Fischer, Alfred G., Invertebrate Fossils, 1952, MaGraw-Hill, p. 560.
144. Van Nostrand's Scientific Encyclopedia, 1958, 3rd Edition, p. 897.
145. ibid. ref. 4, p. 175.
146. ibid. ref. 4, p. 162.
147. ibid. ref. 4, p. 164-5.
148. ibid. ref. 4, p. 209.
149. ibid. ref. 4, p. 209.
150. Copeland, M. J., 1957, “The Arthropod Fauna of the Upper Carboniferous Rocks of the Maritime Provinces,” Geol. Surv. Can. 
     Mem. 286, 110pp.  
151. Calder, John H., 1998, "The Carboniferous evolution of Nova Scotia," in Lyell: The Past is the Key to the Present, Blundell,
      D. J., & Scott,
      A. C., editors, Geol. Soc, Lon. Special Pub. 143, pp. 261-302. 
152. Tibbert, Neil E. and Scott, David B., "Ostracodes and Agglutinated Foraminifera as Indicators of Paleoenvironmental 
     Change in an Early
      Carboniferous Brackish Bay, Atlantic Canada," 1999, PALAIOS v. 14, pp. 246-260;  a summary of this paper is available at: 
     http://www.ngdc.noaa.gov/mgg/sepm/palaios/9906/tibert.html.
153. ibid. ref. 153, p. 268.
154. Tibert, N. E., 1996,  "A Paleoecological Interpretation for the Ostracodes and Agglutinated Foraminifera from the Earliest Carboniferous 
     Marginal Marine Horton Bluff Formation, Blue Beach Member, Nova Scotia, Canada." MSc thesis, Dalhousie University, Halifax.
155. ibid. ref. 144, p. 574.
156. Skilliter, Deborah, at:  http://www.gov.ns.ca/natr/meb/ONE/98ofr5.htm
157. Dawson, John W., 1866, Quart. Jour. Geol. Soc. Lon., Vol. 22, p. 143.
158. ibid. Ref. 158, p. 126.
159. ibid. Ref. 158, p. 144.
160. Condra, G. E., and Elias, M. K., 1944, "Carboniferous and Permian Ctenostomatous Bryzoa." Bull. Geol. Soc. Amer., Vol. 55, pp. 517-568.
161. http://www.gov.ns.ca/natr/meb/ONE/98ofr5.htm
162. ibid. ref. 152, pp. 267-268.
163. Archer, et al. 1995, Geol. Soc. Amer. Abstracts with Programs, p pp. A31-A32.
164. ibid. ref. 94, pp. 103-105.
165. Gessner, Abraham, 1836, Remarks on the Geology and Mineralogy of Nova Scotia. 272 pp.
166. Price, George, 1923, The New Geology

**  = Emphasis Added

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