. The Pan-American geologist. retaceous rocks of Vancouver and the Sucia Islands, has enabled them to tie determined with much more accuracy now than was possi- hle then. Unfortunately, some of the fossils collected by Sir James I [ector cannot now he found. Notes on some Fossils from the Wanaimo formation of Van-couver, Hornby, and Denman /stands, J. F. specimens referred to in this paper are the property of the Pro-vincial Museum at Victoria, Ik (..and were obligingly lent by itscurator. Mr. John Fannin. Many of them were collected quite recentlybj Mr. Walter Harvey, of
. The Pan-American geologist. retaceous rocks of Vancouver and the Sucia Islands, has enabled them to tie determined with much more accuracy now than was possi- hle then. Unfortunately, some of the fossils collected by Sir James I [ector cannot now he found. Notes on some Fossils from the Wanaimo formation of Van-couver, Hornby, and Denman /stands, J. F. specimens referred to in this paper are the property of the Pro-vincial Museum at Victoria, Ik (..and were obligingly lent by itscurator. Mr. John Fannin. Many of them were collected quite recentlybj Mr. Walter Harvey, of They include a Gfryphaa not previ-ously noticed in these rocks, remarkably fine and perfect examples ofLytoceras jukesii Sharpe, and other interestingammonitoid forms, threeof whi(d) are probably new: also three new species of decapod Crusta-cea. Two of these Crustacea are crabs, and the other a long-tailed lob-ster-like species, apparently referable t the genus Podorates. The American Geologist. Vol. XIV, Plate THE MADISON TYPE OF DRUMLINS. THE AMERICAN GEOLOGIST Vol. XIV. AUGUST, 1894. No. 2. THE MADISON TYPE OF DRUMLINS.* By Warren Upham, Somerville, Mass.(Plate III.) CONTENTS. PageDrumlins enclosing nucleal beds of sand and gravel, but mainly com-posed of till, in Winthrop and Scituate, Mass 69 Similar drumlins, with more nucleal stratified sand, in Madison, Wis. ..73 Altitudes in Madison and its vicinity 74 Subglacial deposition of the nucleal beds 78 Accumulation of the overlying till 80 Drumlins enclosing nucleal beds k sand and gravel, butmainly composed ok till, in winthrop and s( ill ate,Mass. The earliest publications known to me of observations ofdrumlins structurally resembling those which form the sub-ject of this paper are by Mr. W. W. Dodge, of Cambridge,Mass.,f and by the present writer,* describing the oval hillsof till called Great Head in Winthrop and Third and Fourth(lifts in Scituate, Mass., each of which is nearly half washedaway by the sea. Great
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