. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. rcle-like spine, \y gibbous, and iriorly. A nar- i8t opposite the md arching, at '^ards the outer ing that point, ous set of fine ected outward ar to bifurcate immencement, Bnileyi. It is le whole uuter lised points cr iistinct under ute pi -iCtures. I cf the shield, as well as the minute, short ⢠appearance, cheek-lobes, »s. They are its. >emi-c
. The geology of Nova Scotia, New Brunswick, and Prince Edward Island, or, Acadian geology [microform]. Geology; Geology, Stratigraphic; Paleontology; Geology, Economic; Géologie; Géologie stratigraphique; Paléontologie; Géologie économique. rcle-like spine, \y gibbous, and iriorly. A nar- i8t opposite the md arching, at '^ards the outer ing that point, ous set of fine ected outward ar to bifurcate immencement, Bnileyi. It is le whole uuter lised points cr iistinct under ute pi -iCtures. I cf the shield, as well as the minute, short ⢠appearance, cheek-lobes, »s. They are its. >emi-circular, more convex picuous. bundant and iraate friend non at Rat- slight differ- able cheeks, t, where the il to breadth s so inclined ery convex; about one- :wards, and 18 distinctly , appearing. FOSSILS OF THt! ACADIAN GROUP. Occipital ring narrow, convex, widest in the middle, narrowing towards sides, which are turned forward, giving to it a crescent shape. Occipital furrow deep and well developed, widest in the middle, where it slightly impresses the base of the glabella; narrow and slightly bent forward at the ends. The ring bears a little short conical tubercle-like spine in the middle, directed slightly backwards. Fixed cheeks, frontal limb one-third to one-fourth of whole length of head, with a narrow, high, convex border, inside of which is a moderately deep furrow; :heek-lobes depressed, convex, meeting in front, rising abruptly from the deep dorsal furrow, on the borders of which they reach their greatest elevation, which, however, is not equal to that of glabella, and sloping thence roundly towards the sides and front. The posterior limb bears a deep, wide, furrow, which widens somewhat near extremity. The marginal fold is very narrow and of little prominence; and widens a little in the outer half. The posterior margin bends slightly backwards at extremity of limb, which is rounded. RatclifTe's Millstream.âN. B. Survey and J. W. Hartt. Conocephalite
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Keywords: ., boo, bookcentury1800, booksubjectgeology, booksubjectpaleontology
