O€ 886E0 is Presented to the UNI VERSITy OF To RONTO LIBRARY by the ONTARIO LEGISL ATIVE LIBRARY 1980 ' ‘ OTL ~ : THE SILVER LINING ae, Digitized by the Internet Archive in 2012 with funding from University of Toronto http://archive.org/details/withscottsilverOOtay| <2 ta Fett 4) ) - eT ences” oh ihy 3? ee 3 a : ae 4 ~ yas . M i a od a q 4 SO ty) 5, ye ; a x m, & aa - a - eke 3 a et —_ 7 * kre” 4 F n > os Lagat i -_ ad é ‘ Lay Low if ks 7 hae ; , - - of, it ; - =- . a a age. Photo by Stearn & Sons, Cambridge ] SLEDGE-MATES AT CAMBRIDGE, Novemser, 1913. (Standing) Debenham and Wright of Caius ; (sitti itl Priestley of Christ’s. ) Taylor of Emmanuel and 34 asi” ai WITH SCOTT:/3%% br, , cfr Om, are THE SILVER LINING — Voeyace BY faePrith TAYLOR, D.Sc., Ere. WITH NEARLY 200 ILLUSTRATIONS AND MAPS LONDON Seer BILDER & CO., 15, WATERLOO PLACE 1916 All rights reserved — fy ake a & le ‘ | fi, \\s % INTRODUCTION Tue great adventure of Scott’s last expedition has been given to the world in the faithful simplicity of the leader’s own words, as they were set down from day to day. His diaries were but the basis of the book that should have been written. We have not the half of what he could have told us. But in another sense, that half is greater than the whole. Here stand first impressions, not retouched: the ebb and flow of his hopes and fears, the lights and shadows of the moment, never reviewed in later perspective after the event ; thumb- nail sketches of character, vividly set down; notes of the day which reveal his spirit entering into the spirit of his men : and at the end, the singleness of heart that could give all and accept all for one high purpose. I have often liked to think—surely it is true—that the universal thrill awakened by his example strung up the soul of the nation unawares for the great call so soon to be made upon it. The other half of the picture has been partly filled in. Others have given the history of outlying explorations with their tale of human resource and endurance; they have recorded scientific results or described special branches of natural history in the Antarctic. Something, however, is still left to be told. No one will forget Captain Scott’s almost incredulous delight at the goodwill and harmony of his little company under the trying conditions of Ross Island. It is for Mr. Griffith Taylor to tell of the daily life of that company from within, to tell in careless detail its lighthearted cheerfulness lining solid effort, which the cloud of English earnestness so constantly turns out upon the night. The “ other side of the shield” is too often a byword for irreconcilable contradictions. It is not so here. The reader Vv vi INTRODUCTION is doubly grateful. He is grateful for the details of the daily round as it passed in the explorers’ hut; he is grateful for the sense that new testimony only bears out former report. Nor are these personal impressions all, though they extend over a longer period than that covered in the “ Last Expedition.” Mr. Griffith Taylor also gathers up what has in large measure appeared elsewhere, the story of his own explorations and much of his general scientific results in geology and physiography, so that his Antarctic experiences stand together as a union in thought and action of all that is typified by the old name and the new, Cambridge and Melbourne, each his Alma Mater. The book makes its appearance in the midst of a great war, when books are too often regarded as a first luxury to be cut off. Nevertheless I hope that many will be able to find in its pages some refreshment of mind, some relaxation from the long strain, some strengthening of faith in the latent spirit of the Greater England which has sent its sons from the four quarters of the world to stand beside the Old Country in the hour of destiny. LEONARD HUXLEY. February, 1916. CONTENTS Getrinc To kKNow THE MEN F P 5 F E ; : II Tue Tzérra Nova cors Soutu i. The Geologists visit the New mei Glaciers : ii. Ship Life in Calm and Storm ii. Learning the Ropes iv. Blocked by the Pack Ice v. Through the Ross Sea . vi. Making Winter Quarters at Cape oe III Firsr Western Expepirion, January—Marcu, 1911 IV A Monts in tHe Otp Discovery Hur, Marcu—Arrit, IglI. V In Winrer Quarters with Caprain Scott, Aprit—Novemser, 1911 VI Granire Harsour Expepition . Vil Tue Voyace Back, Fesruary—Marcu, 1912 ; : : : Vill Tue Enp of THe Expepition . : - ° ° : : APPENDIX 5 Inpex . PAGE 113 187 211 329 413 437 449 456 LIST OF ILLUSTRATIONS FULL PAGE PLATES FACING PAGE Sledge-mates at Cambridge . 5 . Frontispiece Officers and Crew, Captain Scott’s Anes Pepeditihas Ig10 . Icing Ship in the Pack on the Starboard Quarter : : The Norwegian Dinghy or Pram retrieving Birds in the Pack os . A Quiet Sunday Evening on the Terra Nova . . ‘ é D. Lillie, Ship’s Biologist . : : The Northern Fringe of the Pack Ice penine ic Wake of ie Ship through Open Pack . : : : ; . . . Catching the Fish in the Pack . ; - ' Surveying the North Coast of Ross Island from the Terra Nona | : Photo from the Ship of Cape Evans. . ° . : . The First Hour Ashore ; : : : ° Two Motor Sledges on the Beach at en: — 5 : ; . Photo of the Hut showing the Ramp and Erebus. , : . Penguin Courtship on the Ice-foot near Cape Evans A . Ship aground on a Reef off Cape Evans close to the Tunnel Bete . Griffith Taylor in Summer Rig (on a Keen day) on Cape Evans . ; Model of Country traversed on First Journey . . . ° My First Camp in Antarctica at the Snout of the Ferrar Glacier ° Photo taken just before we packed the Sledges for the First Sledge Journey . . : ° ° : : : Trying Times on the eeuies Gace F F ; ° Tables of Ice “‘ Mesas” in the Lower Koettlitz cut out of ‘Thaw-water Alph River cutting through the Moraines and Ancient Ice . ‘ Discovery Hut . Crater Heights, the Gap ae isenra ae Hill as Hg from the old Discovery Hut Mount Erebus from the Old Bitcovery ae ix 16 61 61 65 66 66 70 88 88 g2 92 106 106 108 108 118 126 126 163 163 189 189 196 196 x LIST OF ILLUSTRATIONS PACING PAGE Bowers’ Party adrift on the Sea-ice Over the Hutton Cliffs to test the Sea-ice Captain Scott wearing the Wallet in which he ee ‘te Sedging Journals . J - - - Simpson sending up a “ Ballon Sond a The East Corner of the Hut showing the Eddy Trench compe out by Blizzards on the Windward Side of the Hut Captain Scott’s Autograph List forthe Aurora Watch . : : Some Antarctic Archives > ee on Cape Evans, sie the Deep Bday on re Windward ide Debris Cones on eae s End re mile par of 1 Hut) “« Blizzometer Record ” during the Search for Atkinson Lakelets of Cape Evans A fine Steam Cloud blowing South ia ickinn ‘ : A Glacieret near Island Lake (C. Evans) due to Wind-blown sale : Ice-quakes in the Sea-ice A = The Tide-crack at the North-west Cisse of Cane Rises ‘ High Cliff and the South End of the Barne Glacier “The Barrier Silence” Bernard Day on the Motor Sledge just bliin he dint for ies South The Start of the Motor Sledges Wilson packing his Pony Sledge the Day Ketidh the ket for re Pole . ‘ The Hut after the Winter Relief Model of the Region traversed in re Seibel sini The Second Western Party the Day they were picked up by the Ship . A Panorama of Cape Roberts, where the Western med was isolated for Three Weeks. Looking North : : 3 Avalanche Cliffs on the South Side of Granite anaes k The Field of Crevasses (Skauk) at the Foot of bai Tongue . Granite Hut, Cape Geology : Forde cooking Seal-fry on the Blubber-stove at en Rais , Heavy Sledging off Sey se! — ay where we tried to a to Land : - . The “ Half-Ton ” after Nelson left us of nd Mouth of Dry V alley “ A Tight Corner! Crossing the Forty-foot Tide-crack off Point Disappointment, Granite Harbour ; : : : The First Western Party in a Natural Ice-tunnel amid the Pinnacles of the Koettlitz Glacier . The Second Western Party at Cape Geology ee Harbour, on Christmas Day, 1911 . ‘ ; . 198 207 214 218 218 226 266 380 LIST OF ILLUSTRATIONS x1 FACING PAGE Gran’s Midsummer Bath The Couloirs of Mount England Glick ane into efi ee The Rush to Safety : over the Edge of the Blue Glacier . Engineer Williams at the Winch Bernard Day on the Capstan A. B. Cheetham, who holds the Record for crossing ae ats Circle G. C. Simpson 5 A very “Ordinary Seaman ” Pennell on Bridge Photo of Crew off Akaroa . ILLUSTRATIONS IN THE TEXT Block Diagrams illustrating the Basins, Gorges, and Riegel in the Val Ticino below Saint Gothard ; Section across Poop of Terra Nova Harbours visited on the Voyage to New mika The Cuspate Peaks of Mount Cook and the Matterhorn The Snout of the Tasman Glacier from Sebastopol . : , Glaciers in New Zealand visited in November, 1910, by the Geologists Looking down the Snout of the Mueller Glacier from the Stocking Plan of the Deck of Terra Nova . : : : ‘ Vertical Section of Terra Nova illustrating Incidents in the Great Storm, January 2-3, 1911 Figures of Latitude and Longitude Iceberg Forms Sounding Apparatus . ‘ ; ‘ , Course of Terra Nova through ie Antarctic Pack as far as Cape Evans, Dec, 7, 1910—Jan. 4, 1911 . Coasting Ross Island, Jan., 1911 Life’s Round in the Antarctic Cape Evans from Inaccessible Island Sun-holes . Antarctic Spoor : : - F : . ; ; Iceberg Equilibrium. The Tilting of the Tunnel Berg during the Winter, 1911 . : - : » : . : : a9 Sip 411 418 418 426 426 428 428 435 PAGE xii LIST OF ILLUSTRATIONS Sketch of T'wo Grottoes cut in Glacieret near the Hut, Jan. 15, 1911. Sketch Map of Cape Evans, Jan. 21, 1911 Geological Sketch by Captain Scott ; Facsimile (reduced) of Captain Scott’s Sledge hemeaiss Geological “Sandwich” near the Dun and Hedley Glaciers Moraine Material at the Taylor Glacier, looking West Crater on the Flank of the Taylor Valley 3 The Avalanche-fed Lacroix Glacier in the Taylor ue. 122, Sketch Section across the Taylor Valley at Suess Glacier, showing the Nussbaum Riegel which bars it . . Looking west up the Dry Valley below Taylor Glacier “The Compleat Explorer” “« Anarthoclase”’ Felspar : The Age of Rocks above the Tay tsi Glacier : Plan of the bygone Twin Glaciers of Lake Luzern The Morphology of Frozen Ski-boots . “My Footgear” Empty Hanging Valley on in North Wall of the Davi is Gude “ How Evans won his Bet ” The “ Palimpsest” theory. Genesis Sketch PRE shane re chief types of Valley Erosion Forks for Blubber . ‘ “ 3 : Map showing our Journey round the Breaking Barrier Sketch Map of the Environs of Hut Point . Plan of the rejuvenated Discovery Hut The Blubber Stove in the Old Discovery Hut . Steig-eisen The Sackcloth Fete Blubber-Lamp made from ‘Tin Misiiebne Testing the Sea Ice off Castle Rock From Castle Rock to Cape Evans . The Two Tents on the Ice-shelf at Little mae Isle . Plan of Hut, 1911, showing Nicknames and Bunks of Explorers The Electrical Breadmaker : : : x k : Changes in Wind Direction Simpson’s Clue Simpson’s Instruments - : The Arch Berg before it fell in sea sega tie Gate Berg “ Balloon Meteorograph PAGE 102 107 114 123° 131 135 137 140 141 142 144 145 147 149 154 159 161 163 175 176 178 190 igi 193 197 200 201 205 206 208 212 216 217 218 221 227 234 LIST OF ILLUSTRATIONS Evans teaches us to Cobble Temperature Curves , Sections of Fossils, Beardmore Glacier . i Fossil “ Sponge-Coral ” from the Beardmore Glacier Archeocyathinac Marble set ina Ring . Bill’s Nose-nip : ‘ A Characteristic Portrait in a Bliz! Vertical Temperature Gradient in Hut How we found Midwinter The Night Watch Supper . Lost in the Blizzard . The Twin Glaciers . The Future Ice-age . : : Reversal of the Steam Banner of mee The Mouse-trap Camera ‘ The Wind-ridge on Inaccessible Isle th Tracks : The Dissected Debris Cone A Peculiar Animal seated on the top of 2 a Debris Gone Book-plate illustrating Polar Clothing . Robinson Anemometer Sunshine Recorder . “'Taylor’s Patent Heel-tips ” The Waved Edge of Glacier Tongue The Seal’s Method of rasping away the Ice “ Polar Wireless ” Ice Crampons . : Our Water Ep) The G Granite Ce at Cine enlehy Gomphocephalus, Antarctic “‘ Springtail” 3 Pressure-ridges in the Sea-ice looking West from Cape Gesiogy to bie Punch Bowl Cwm ; ; Pulpit Rock, the home of the Sea-kale . Ironclad Boots for Antarctic Geologists Looking North-west from Cape Geology, setts He Gtanite Clift of the Kar Plateau capped by dolorite Gran’s Béte Noire : Sketch Map of Region near the Devil’s ee Boi Mount Suess Nunatak looking West from Redcliff . Sketch Map of Mount Suess Nunatak and Gondola Nunakol * Erratic” perched on Six Small Stones, Gondola Ridge . xiv LIST OF ILLUSTRATIONS PAGE Sketch-diagram of South-west Face of Mount Suess, showing the Fossil- bearing Beacon Sandstones . . - 389 Gondola Ridge from the top of Mount a king icant aes . “ggu Sea-kale at 77° - e 5 Z 5 - « 393 Flexure in 30-feet Berg, Cape ea: s : 403 Diagram illustrating the Way we managed to “ Raise nt date a re a Laff upon Luff”, : : : ; ; : : - 420 Method of fixing Ice Anchor ; : ; ; : . 421 Trimming Coal in the Starboard Main Hold ; : : é 5 Beg Chart of Bay of Whales’. : ; : : : ; or ae Chart of Parties (Amundsen reaches the Pole) ; : : - 439 Chart of Parties (Scott reaches the Pole) ; ‘ : ; - 441 Chart of Parties (the Last Camp) E : : ; : -) gage Clossopteris - : - : : : F ; : - 444 MAPS PAGE . The Chief Travels of the Sixteen Officers at Headquarters, Cape Evans, Ig1I_ .. : . < E < : < A 12 . Map of Antarctica showing Localities of Recent Expeditions . S| ei? . Map of the Coast from Cape Royds to Hut Point : Facing 86 . Physiographic Features of Cape Evans due largely to the Retreat of the Erebus Glacier. : : : . : » 299 . Return Voyage of the Terra Nova in March, 1912 : : « 414 . Recent and Future Exploration : : : 2 : « 450 . Map of the Region traversed on the Western Journeys, 1911-1912 At end of text Ls he ’ > ry ‘ i ‘ - ' = - = t - > o ‘ . bs i . iT *po=~tt eo: 64 sal Wd ing d Ai Pel or ee 1022S aad 7 as tease ah) NG TO KNOW THE MEN” * “GETTING TO KNOW THE MEN” “ Wuere can I find Dr. Wilson ?” I had just entered the quadrangle of the Biological Schools at Cambridge, when a door opened quickly, and a well-knit, wiry individual ran down the steps towards me. “ Which Dr. Wilson ?”’ said he. “Wilson of Antarctica,” I replied. With a quizzical smile that | was soon to know well, he returned, “1 am Dr. Wilson.” It was in this way that I made the acquaintance of the Scientific Director of the expedition ; and in the ensuing con- versation at Christ’s College I learnt the requirements of Captain Scott. But the steps leading to this Sunday interview were rather amusing to look back on. On a Saturday afternoon of December, 1909, I had been having tea with Wright of Caius, and we discussed many topics, such as cancer and Canada, eugenics and Shackleton. He remarked that he would like to go with Scott next August, and that he would go if I would! However, we did not discuss this topic, for I left to dress for the Philosophical Society’s Dinner at John’s. In the old Combination room were most of the scientific dons, and Dr. Marr beckoned to me. ““] wanted to see you. Would you like to go with Scott to the Antarctic as English geologist ?”” He was pleased to say that my glacial work and travels suited me for the post. I said I had not thought of it at all. He added that Dr. Wilson would probably call on me on Sunday, to which I replied that I had intended to be off to the Alps at 9.30! I departed, only to fall into Professor Seward’s hands. He asked the same question ; and Hutchinson of Pembroke came up a moment later and said, “Don’t you think Taylor ought to go to the Antarctic?” I suggested that I felt as if I were being pushed out into the cold ! B 2 4 WITH SCOTT: THE SILVER LINING I postponed my trip to Grenoble for half a day, and had a long talk with Wilson. He gave me a letter to Captain Scott, which I presented after my return from France. We had a fine trip! Four Australians cycling through the High Alps in mid-winter. When it did not snow it rained—and mostly it did not snow! At the pass of Croix Haute we had to traverse thirty kilometres of heavy snow, and later in the Auvergne we found that snow formed quite a good surface for a bicycle, which discovery nearly led to a fatality in the Antarctic, as will appear later. On my return to London a month later (8th January) I called at the Antarctic offices and had an interview with Captain Scott. I soon gained an insight into the multifarious occupations of a Polar commander. The offices of the expedition were in Westminster, at 36, Victoria Street, halfway between the Abbey and the vast railway station at Victoria. They were situated in a district peculiarly devoted to the empire’s interests, for most of the colonies have their representatives there ; and that greatest boon to travellers, the Army and Navy Stores, is just across the way. I will try to give some idea of the appearance of the expe- dition’s headquarters during the busy months of preparation. In a large room occasionally sat Captain Scott, but he was usually busy with some ingenious foodstuffs or patent ap- pliance in one of the other rooms. Adjacent was the secretary’s office, and there he was to be seen, inter alia, wading through some of the eight thousand applications from eager souls anxious to get out of the rut by joining the expedition in one capacity or another. Naturally enough, the names of naval officers were numerous, both on the staff and among those applying. In fact, the navy could beat any other team that the expedition could get together at any game whatsoever. An explorer friend of mine had no great opinion of navy men, and strongly advised me to learn boxing to uphold the dignity of science. So I started a boxing club at Cambridge among the scientists, but we did not know then that navy champions like Parny Rennick and Dr. Atkinson were to join the expedition. Here let me add that arrogance was the last attribute of my dear naval friends down South. In a third room at headquarters were samples of patent “GETTING TO KNOW THE MEN” 5 foods. One open tin discloses shrivelled root-like objects about the size of lead-pencils. This was desiccated rhubarb, and it seemed merely concentrated sourness in its present state, though it furnished many dishes at headquarters later on. Cabbages and greens too much resembled coarse leaf tobacco to be eulogized bya non-smoker. A Cambridge friend —doing physiological research—was extremely pleased when he heard I was going South. ‘“ Ah,” said he, “ you can try my patent food all next week ; you'll need nothing else for any of your meals, and I can give you a full supply for the Antarctic.” Owing to various contingencies, the tin remained unopened, and I left it, with my blessing, for the landlady. In another corner of the same room an eager inventor is explaining the excellences of his patent stove, which burns almost without fuel and is guaranteed “ to produce little or no carbon dioxide” ! Here I first saw Dr. Simpson, who was wrestling with this invention, which—apart from its chemical peculiarities— seemed suitable for warming his magnetic hut. The equip- ment of this mansion seemed to occupy all his waking thoughts, while his chief exercise seemed to be taken by whirling sling thermometers. The other room was almost filled with a huge petty officer who was sorting gear for the sledges. I looked at his sturdy proportions with considerable respect, which would have been increased had I known how invaluable “ Taff” Evans was to be on my first expedition in the Antarctic. An old 1902 sledge was lying in the passage, whose splintered runners and weather-worn appearance told graphically of the screw-pack and “ bottle-glass ”’ ice it had surmounted in the past. Captain Scott was busy at first, but I soon had a long talk with him. In my journal I wrote as follows :— ** Scott is just what I expected, a sturdily built, clean-shaved naval officer, with plenty of humour and decision. He told me that Mawson was coming over from Australia immediately. His idea was to have two geologists on the Erebus side of the Barrier, and one on King Edward VII. land. The latter party would have wireless if possible. He drew a moving picture of me wiring signals of wind velocity, etc., to Mawson. «Just like old times, a friend at each end,’ said he. Scott is going to try for the Pole along the old route, I gather, and , 6 WITH SCOTT: THE SILVER LINING not vid King Edward VII. land. The ship will leave in July and make a long trip vid Madeira and Kerguelen to enable the men to shake together.” Lieutenant Campbell was often in and out of the offices. His was an independent command, and he was collecting his stores and labelling them with a distinctive broad green band. The cases were made of Venesta—a patent three-ply material, extremely light and extraordinarily tough. One could hardly break into them with a pick-axe! They were bound with iron and made to contain about 4o lbs. weight, to facilitate handling. The question of Antarctic clothing greatly interested many ladies of my acquaintance. Some of them, indeed, were so urgent that I should look into this matter, that I began to get alarmed myself. On inquiry 1 found that the fur boots were carefully arranged to go over four pairs of socks and a layer of senna-grass ; which seemed to point to a somewhat wide margin of safety. Of the Antarctic suits—trousers, jerseys, and overalls—I was told there was a supply in two sizes— long and short! I looked at the scientific director as he smilingly gave me this information, and judged what would fit him would suit me, so that no measurement was necessary in this class of tailoring. The first order from Captain Scott concerned the purchase of clothing for the voyage to New Zealand. For this £8 was allowed by the Expedition. I told Captain Scott that I was not making the voyage in the Terra Nova, and had a kit of tropical gear already. He remarked with a twinkle in his eye, “Never mind about that, I dare say you will be able to spend it on something useful !” A few days later 1 went to the West India Dock and saw the Terra Nova for the first time. Here was Lieutenant Evans “ merry and bright” from the start! He was assisting Captain Scott to chalk out cabin spaces on the deck. In a later section I describe her equipment very fully, so that there is no need to dwell on it here, save that amongst the large liners in the dock she had somewhat the appearance of a minnow among the Tritons. At any rate, the “leviathan ” is half as large again as Shackleton’s Nimrod, and if Columbus could board her no doubt he would feel himself on a Lusitania. “GETTING TO KNOW THE MEN” 7 About this time I received a cable offering me a post on the Commonwealth staff. Through the kindness of the authorities concerned I was able to hold both positions concurrently ; and I went South with a definite commission to study all the scientific factors—but especially the meteorology—which might concern Australian interests. Early in February Mawson came up to Cambridge to stay a few days with me. We had passed through Sydney University together, and done our early geological field work under Professor David. We had kept in touch with each other and had many common friends. During my cycle trip through the Alps, Glasson (from Adelaide) told me that when any of Mawson’s acquaintance at Adelaide University wanted chocolate, the explorer would take an ice-axe and break a lump off the huge block he had looted from Shackleton’s Expe- dition! I felt that an expedition of this type had peculiar attractions for me, but, alas! our chocolate supply was never on such a prodigal scale. Mawson gave us a talk at the Research Students’ Club that evening. He told us many harrowing tales, and glances of pity were bestowed on Wright and myself by the other members of the club! The next afternoon he was persuaded to give a lecture in the geological school, so that we knew a lot more of Antarctic conditions before he left. By this time he had decided not to accept Scott’s offer of a position on the staff, but he gave all of us much useful information as to equipment and research, Two other Cambridge men—both biologists—were ap- pointed to the staff. I had heard of Lillie’s adventures in the Atlantic, where he had carried out anatomical dissections with an axe! His subjects were whales, on which, I take it, ordinary instruments would have had but little effect. He was a John’s man, while Nelson came from Christ’s. Nelson had been “down” for some time, working at the Plymouth biological laboratory. I had heard of him from a friend of mine who had worked there also, Wright, of Caius, had been a mate of mine for several terms. He was a leading light in our Peripatetic Club, and was in fact the best walker among the members, Wright and I heard so much of the prowess of the naval men in every branch of athletics that we decided to show them that the scientists had 8 WITH SCOTT: THE SILVER LINING some muscle. One morning we set off from Cambridge at 5 a.m. with some boiled eggs and chocolate and walked to London, where we reached St. Paul’s, Islington, at 5 p.m. It was a non-stop effort, and Wright came through “ smiling,” but my feet were so sore that I could hardly stand next day. My chief recollection is one of loathing for hard-boiled eggs, and of the relief with which I dropped three-quarters of our provisions in a secluded corner of King’s Cross ! During the Easter vacation | planned a trip to the Enga- dine and Como to study glacial erosion in some detail. I had already spent some months in this part of the Alps, and wished to gain fresh data on many questions. A college friend accompanied me. Professor Bonney was kind enough to give us advice as to the best routes during March, for my previous trips had been in summer. He also discussed the questions of valley erosion at some length, and I was glad to hear that they would form the basis for his presidential address to the British Association at Sheffield. He was strongly opposed to W. M. Davis’ views on the subject, holding that water and not ice had cut out most of the Alpine valleys. 1 had learnt my glaciology from the eminent American while in the Swiss Alps, and was naturally Davisian in consequence. However, Antarctica led me to place more stress on frost action as an eroding agent, so that my position is now between the two schools ! We had an interesting and useful trip lasting for six weeks. This is hardly the place to discuss the results of this journey, though in some sense it belongs to the Expe- dition, for Captain Scott paid the bulk of my expenses. I visited for a second time the wonderful valleys north of Bellinzona, the Val Mesocco to the north-east and the Val Ticino to the north-west. At Mesocco and Faido are two of the most striking bars or “riegel” across the Alpine troughs, and later in Antarctica I was to find a third even more striking example. Thus, about twenty miles south of Saint Gothard is the dasin of Piotta, a trough with vertical walls two thousand feet high and a flat valley floor. This is analogous to the Antarctic valley containing Lake Bonney (77° 30° S.). Then at Fiesso this basin is bounded by a great bar or riege/, through which a narrow defile passes at one side; so also at the Nussbaum Riegel in Antarctica. “GETTING TO KNOW THE MEN” 9 Below Fiesso is the broad trough of Lavorgo closely paralleled by the broad “dry valley ” in the southern continent. Rirolo Madrano Fiotta Fiesso Prato Lavorgo Block diagrams illustrating the basins, gorges, and riegel in the Val Ticino below Saint Gothard. (Cf. Taylor Valley, Antarctica.) On my way back from Italy I stopped for a few days with the glaciologist Nussbaum at Bern, and explored the queer drainage in the, valleys near that city. In the last Ice Age all this fertile country lay below the Rhone Glacier, and I was to find that many of the features in Antarctica reproduced, in the present, the past history of the Swiss scenery. I reached London on the evening that Peary gave his lecture in the Albert Hall. Mawson had given me his ticket and I decided to go, though I had to appear in my touring rig of puttees and peletin. I heard that Bernard Day—our motor expert and lately with Shackleton—had the next seat. It was a tremendous crowd and a very interesting lecture. As is somewhat usual with Americans, he gesticulates more than is common among British speakers. He had just received the medal (which was designed by Lady Scott) and expressed his sense of the honour done him and the care with which he would cherish this token of the Geographical Society’s esteem, when the medal dropped violently from his hand amid audible amusement from the thousands comprising his audience. However, he picked it up and proceeded with his remarks with the greatest sang froid. Day and I were much impressed by his method of relaying with dog teams, and felt that he deserved full credit for his long-sustained attack on the North Pole. Three years later I was to be again in the Albert Hall to hear Commander Evans describe the British conquest of the Pole; but Bernard Day had now settled “on the land” near my own home in Sydney, New South Wales. Before I left England I had met most of the officers, Bowers I first saw at dinner one evening with Captain Scott. 10 WITH SCOTT: THE SILVER LINING Lady Scott was coming out to Australia, and was much in- terested in the political and social questions of the “ British continent.” She had done some long tramps in Switzerland, and told us much about the Fabian Society and about her art life. She had heard of our tramp to London. “ Did you really walk sixty miles in ten hours?” So had rumour: reported it. It was mortifying to confess to a bare fifty miles in twelve hours! Birdie Bowers appeared in the full insignia of a Lieutenant of the Indian Marine. He was at this time so busy loading the ship at the docks that I did not see him again until I joined the Terra Nova in New Zealand. On the 12th of May I joined the Orontes and I reached Melbourne at the end of June. For the next three months I was busy at the new Federal capital—then unnamed,—where I carried out various surveys for the Commonwealth. In July Professor David sent me some microscope slides made from a limestone obtained by Shackleton’s party on the Beardmore Glacier. To our delight I was able to identify them as fossil “corals” of Cambrian age, of the same genus as those from South Australia on which I had been working at Cambridge. Some account of these Antarctic fossils which Wright also discovered in some of his specimens from the Beardmore is given in the account of our life at headquarters. Professor David gave me invaluable advice on Antarctic matters. At the School of Geology at the University of Sydney is a large “ Antarctic Room” filled with specimens collected on the 1907 Expedition. Here Priestley had been working out results for many months, and here he presided over informal “tea” at 4.30 every afternoon! Here I met Alan Thomson, a geological scholar from Oxford, who was to have been one of us, but that he developed lung trouble at the last moment. In consequence of Thomson’s illness, Priestley obtained Shackleton’s permission by cable, and thereupon accepted Captain Scott’s offer to join us. Many were the yarns Priestley told us of his 1908 experiences. He said that the young Eskimo dogs, born down there, never knew water, yet they held out a water-can for a drink when they saw it! More credible was the story of how they buried the water-can (containing a future drink) and were profoundly disgusted on digging it up to find that their refreshment had vanished! The yarn which I fear I completely disbelieved— “GETTING TO KNOW THE MEN” II anent killing skua gulls by throwing a slab of rock vertically upward—I proved practically a few days after landing at Cape Evans, as will appear in its own place. Meanwhile the Terra Nova had left Cardiff and slowly sailed by the “ wind-jammers’” route to New Zealand. They had an exciting time at South Trinidad—a lonely island off Brazil—swimming through shark-infested surf to the shore. Here they made some biological collections, and on the remainder of the voyage many of the land-lubbers became respectable sailor-men. I hardly knew Wright when I saw him reefing sails and running up the ratlines as if to the manner born. The third geologist appointed on Professor David's recommendation, was Frank Debenham, scholar at my old university, and a family friend for many years. Indeed, the three sons of each family had gone to the same school, and five of us to the same university. It was extremely pleasant to be associated with men like Debenham and Wright, and I was indeed fortunate to have them as sledge mates in the difficult times to come. By degrees all the party were assembling at the Anti- podes, Meares had been collecting dogs and ponies in Manchuria. He had spent several years in this part of Asia, and was already renowned for his journeys into unknown Tibet. He passed through Sydney in October—accom- panied by Lieutenant Bruce—a few days before I arrived. Captain Scott, Wilson, and Simpson were now in Australia busy on various matters. During the voyage Simpson and Wright had carried out experiments on the electrical state of the air, and the latter was now engaged on testing and standardizing his pendulum apparatus before he left civilization. On the 22nd of October, 1910, Debenham and I left Sydney for New Zealand. We were to join Captain Scott at Christchurch, and the Terra Nova was now lying at Lyttelton—the port of that city. Some of the officers I did not meet until I reached New Zealand. There was Ponting, whose beautiful book on Japan had just appeared. He had had a most varied experience, including mining and ranching in California, before his genius in artistic photography manifested itself. He and Meares THE SILVER LINING WITH SCOTT 12 (osje umoys *€ 161-0161 ‘vaoy vusa7, Jo yous) BY) "1161 ‘sueag adv ‘ssoyzenbpvazy av srodqJo UD>IXIS OYI JO sfaavny yoryo oy, oc uosiiM 2 -- te ee 1 ee a a6 + 2 josh tet vol P S42"0H Ps Vasey 2 “GETTING TO KNOW THE MEN” 13 were old friends, and had travelled together in many Eastern countries. Indeed, this fore-knowledge was a usual thing among members. Simpson had almost accompanied Scott in 1902. Wilson, of course, made his name on that expe- dition; and had been chiefly connected with the Grouse Commission since. Cherry-Garrard was making an extended tour of the world when the expedition was started, and volunteered from Australia. He was the sole representative sent by the University of Oxford. He came out from home on the Terra Nova, and was one of the landsmen who took kindly to a sailor’s life. A characteristic of Cherry’s was his never- ending series of gifts to his mates. A most acceptable pair of huge Jaeger socks brought about our real introduction ! Captain Oates had seen service in many parts of the Empire. With difficulty one could get him to talk of his experiences in India (in the province of Indore) or in the South African war, where he served with distinction. He was very busy with the ponies during the voyage south, and I hardly spoke to him until we were marooned together in the Old Discovery Hut. One heard that he was a keen yachtsman, but his strong character and real sense of humour were hidden under a very quiet exterior. Our naval surgeon, Dr. Atkinson, and myself had no work in common until the same month of March at Hut Point brought us together when the Western and Depot parties joined forces. Perhaps the most interesting career among the younger officers was that of Trygeve Gran. He was only a few years over age, and yet he had seen more of the world than any member except Captain Scott. Born in Bergen, and educated in Switzerland, he had travelled all his life. He knew Europe from Turkey to Iceland, and shared with Simpson and Campbell a knowledge of Arctic life. He had fought rebels in Venezuela, tramped across South America, spent several years in the merchant service and navy of Norway, and was now a sub-lieutenant and a B.A. of Christiania. His chief record hitherto had been that of winning the Blue Ribbon of Norway, the Holman-Kol cup for ski-running. This narrative will have much to say of him, and will show that his versatility and willingness to help were remarkable even among the group of men who were my mates in Antarctica. 14 WITH SCOTT: THE SILVER LINING People have often asked me what attraction Antarctica had for me personally. It was purely scientific at first, but now I realize that the companionship with such ideal mates was the chief joy in Antarctic life. I have not, up to the time of writing, felt any of the “call to the Antarctic” that others describe ; but travel anywhere with my mates of the South would be equally attractive. At the risk of being tedious, I will try to describe the chief problem in science which | hoped to help solve by my sojourn in Antarctica. Briefly, it is the study of the effect of ice (chiefly as glaciers) in carving out the features of the earth’s surface. It may quite legitimately be asked, “ What is the value of that knowledge? What bearing has it on science and human interests ?” Most people know that Europe has passed through an Ice Age comparatively recently, but few—even among geo- logists—would be prepared to agree that almost every factor of human environment in Central Europe has been affected by this ancient ice-cap. All inter-communication, much of the agriculture, all the scenery ; nay, even the very possibility of continuous habitation is due to the work of the ancient glaciers. The Gothard, Simplon, and Mont Cenis railways pass along deep glacier-cut gorges (see p. 9) until they reach comparatively narrow ridges which can be pierced by tunnels. The great Alpine passes are but cols due to glacial erosion. The fertile uplands (the true “ Alps”), where the Swiss flocks pasture, and the extensive deep-lying plains of deep rich soil are glacial debris. The magnificent waterfalls, the tributary valleys “ hanging ’’ over the main gorge, are only found in regions where ice has played an important part in its past history. In winter it is only in these deep gorges, excavated two thousand feet below the general level in countries like Switzerland, that the inhabitants and their flocks can hibernate until the grass covers the country in the succeeding spring. There can be no more valuable branch of geology than one which tries to chronicle the actions which have made the Alpine countries of the world so different from the more normal regions. But it is by no means universally allowed that this work is principally due to ice. One school of geologists maintains that water can carve out a land surface “GETTING TO KNOW THE MEN” 15 in a simliar way; and in Switzerland, New Zealand, and similar regions, it is difficult to decide whether the living waters or the long-vanished glaciers have cut out a certain gorge or canyon. Where, then, is the solution to be found? We cannot observe Europe in the clutch of an Ice Age; but it is possible to find a region—once, no doubt, as warm as portions of Europe—now undergoing its period of intense cold and accompanying glacial erosion. In almost waterless Antarctica the land is being slowly carved out into features which must be related to those obtaining in Alpine Europe and other elevated regions, if (as I believe) the Great Ice Age has left an unmistakable imprint of itself in a characteristic topography. I may fittingly conclude the “series of introductions” by a list of the officers. This gives their positions ; and, what may be found more useful to the reader, their nicknames and the personnel of the various parties into which the expedition split up on arrival in Antarctica. LIST OF OFFICERS AND THEIR PARTIES. Leader.—CartTaiIn Ropert Fatcon Scort. Second in Command.—LiruTENANT E. R. G. R. Evans. Chief of Scientific Staff.—Dr. E. A. Wison. SHIP. Harry Pennell, Commander R.N. Henry de P. Rennick, Lieutenant R.N. Wilfred M. Bruce, Commander R.N. Francis Drake, Assist. Paymaster R.N. (retired). Dennis Lillie, M.A., Biologist. James Dennistoun (1911-12 voyage). Alfred B. Cheetham, R.N.R., Boatswain. William Williams, Engineer. SHORE ParrIEs. A. Northern Party (Jan. 1911—-Nov. 1912). Victor Campbell, Lieutenant R.N. G. Murray Levick, Surgeon R.N. Raymond Priestley, Geologist. (And Abbott, Dickason, Browning.) 16 WITH SCOTT: THE SILVER LINING B. Depét Party (Jan. 1911—April, 1911). Robert Falcon Scott, Captain, C.V.O., R.N. (The Owner). Edward R. A. R. Evans, Lieutenant R.N. (Teddy). Henry R. Bowers, Lieutenant R.I.M. (Birdie). Lawrence E. G. Oates, Captain (Titus). Edward L. Atkinson, Surgeon R.N. (Atch). Edward A. Wilson, B.A., M.B., Chief of Scientific Staff (Uncle Bill). Cecil H. Meares, in charge of dogs (Mother). Apsley Cherry-Garrard, B.A., Assistant Zoologist (Cherry). Tryggve Gran, B.A., Sub-Lieutenant (Trigger). (And Keohane, Crean, Forde, and Demitri.) C. Western Party (Jan.—March, 1911). Griffith Taylor, B.Sc., B.E., B.A., Geologist (Grif). Frank Debenham, B.Sc., B.A., Geologist (Deb.). Charles Wright, B.A., Physicist (Silas). (And Edgar Evans.) D. At Cape Evans (Jan—April, 1911). George C. Simpson, D.Sc., Meteorologist (Sunny Jim). Edward W. Nelson, Biologist (Marie). Herbert G. Ponting, Camera-artist (Ponte). Bernard C, Day, Motor Engineer (Rivets). (And Lashley, Hooper, Clissold and Anton.) All those in lists B, C, and D were united under Captain Scott at Headquarters during most of 1911. E. Midwinter Party (July, 1911). E. A. Wilson, H. R. Bowers, A. Cherry-Garrard. Pott Party AND SUPPORTS. A. Pole Party. C. Summit Party. Captain Scott. E. L. Atkinson. E. A. Wilson. C. S. Wright. L. E. G. Oates. A. Cherry-Garrard. H. R. Bowers. P. Keohane. Edgar Evans. B, Last Support. D. Dog Sledges. E.R. G. R. Evans. C. H. Meares. Lashley. Demetri Gerof. Crean. E. Motor Party. B. C. Day. F. J. Hooper. ‘oplog “sonig Soyer ‘sarvayAy {jauueg ‘piemey-Auayo Aeq ‘ueyuagag “surumoig ‘uetg ‘Suljuog ‘yoruuay ‘saravq “{aqdureg ‘33099 “‘UOSIIMA ‘Stamog ‘sueaq ‘sa1eQ ‘yoraaT ‘uosjany ‘uosdunrg Sysiay ‘tojde yp + 747320 07 LPT ‘or6r ‘NOLLIGHdXA OLLOUV.LNV S.LLOOS NIVIdVO ‘M4YO GNV SuaoIddO [ZN woyanty ‘wopsyipt yy <9 o10yq “Ty ‘uojeg = *s2a'T y ry ' “GETTING TO KNOW THE MEN” 2np WestTERN Party (Nov. 191 1—February, 1912). Griffith Taylor. Tryggve Gran. Frank Debenham. R. Forde. At THE Hout (Nov. 1911 to Jan. 1912). George C. Simpson. Clissold. E. W. Nelson. Anton. H. G. Ponting. Tue Hur Party puRING THE SECOND WINTER. E. L. Atkinson. C. S. Wright. E. W. Nelson. A, Cherry-Garrard. F, Debenham. T. Gran. Crean, Forde, Lashley, Hooper, Archer, Williamson and Demetri. They were joined by the Northern Party late in 1912. seve J ai II THE TERR-L NOUVcL GOES SOUTH * * My thanks are due to the Editor of the Me/bourne Argus for permission to reprint this section. CHAPTER” I THE GEOLOGISTS VISIT THE NEW ZEALAND GLACIERS On the morning of the 4th of November the Australian contingent reached Lyttelton. The first ship we saw was the Terra Nova snugly berthed alongside the wharf, and separated by a few feet from the shed No, 5 in which most of the gear was stored. She was readily recognizable by her characteristic rigging surmounted by the crow’s nest. The funnel is painted a rather vivid yellow, and is decidedly abaft of the centre of the ship, a feature which is usually represented wrongly in the models of the ship displayed in some of the Dominion’s shops. Technically the Terra Nova is a barque equipped with an auxiliary screw. She was built at Dundee, and carries three masts (two square-rigged), of which the mizen, for reasons explained later, is rarely used. Socially she is a Royal Yacht, which means that she may fly the white ensign, a privilege only accorded to, certain favoured vessels of the Empire. In fact, I think, apart from our barque, all the units of the Royal Yacht Squadron are on pleasure bent ; and certainly no other is frozen in the Antarctic Pack as we are at the time of writing. Originally she was used as a whaler, and differs little in general arrangement from the Nimrod (Sir Ernest Shackleton’s ship), though she is approximately twice as powerful a vessel. Almost the only wooden vessels now built are those used in the polar seas, and as no steel vessel could stand the wear and tear caused by the constant collision with ice, it follows that an Sete expedition usually makes use of a converted whaling vesse When I first saw her in the West India Docks at London, she had a wide and spacious poop and a distinctly narrow and confined saloon. Now the proportions are reversed. The poop-deck consists merely of the space around the wheel and 21 22 WITH SCOTT: THE SILVER LINING binnacle ; all the remaining area has been filled with labora- tories and with two central structures, the deck-house and chart-house. Below, a relatively noble room has been pro- vided ; with an enclosed balcony much more useful and not much less ornamental than the classic specimen in Verona ! In naval parlance, our saloon is dignified by the title of “‘wardroom,” and has none of the inconveniences usually associated with polar exploration. It is plainly furnished with a long centre table and two lateral leather-covered seats. The stove (not yet needed) certainly blocks the passage behind the Steuer Lia eurregey Section across poop of Terra Nova (not to scale). head of the table, but under normal conditions, especially before the expansive after-dinner moments, there is sitting accommodation for seventeen officers. Three more sit on boxes at three corners—the fourth being left open as a breathing space for the steward. Hence twenty of the twenty- four constituting the “afterguard” are accounted for, and the remainder are usually on watch, and arrive uproariously hungry after the majority have reached the tobacco stage. On our early appearance we were cheerily hailed by the two officers on board, One had just converted the deck- house “balcony ’’’—which overlooked the wardroom—into a bathroom, the other was devouring ham and eggs down THE TERRA NOVA GOES SOUTH 23 below. But most of the officers, after their four months’ voyage, were staying in Christchurch some eight miles away, and came into the ship by early train. Lyttelton is a mag- nificent harbour of extraordinary origin. Port Phillip, it is well known, is a drowned coastal plain, hence its low banks and rounded contour ; Port Jackson is a drowned river valley, as is obvious from its winding outline and deep frontage ; while Wellington Harbour occupies earthquake landslides. But Lyttelton Harbour is a drowned mountain valley, with hills rising fifteen hundred feet almost continuously around the elongated basin. The eastern flanks of this isolated mountain (Banks Peninsula) are drowned in the Pacific; the western flanks are buried, several thousand feet probably, in the silts and shingle of the Canterbury Plains. The fair city of Christchurch, which has arisen on an even plain stretching twenty miles north, south, and west, has a wonderful harbour at her door, owing to this unique juxtaposition of plain and buried mountain. Most of the members of the Expedition tramped over the old bridle-track to see the view from the top, but all traffic passes through the railway tunnel—one and a half mile long—cut deep in the volcanic rocks of the Peninsula. The office of the Expedition was close-to the cathedral in Christchurch, almost in the shadow of the steeple, which has a habit of toppling down under the stress of earthquake shocks. Here was the secretary struggling with a mass of correspondence—very largely letters asking for autographs, penguin eggs, and rocks from the south. These modest requests, however pathetically they are worded, cannot be attended to in the last few days of preparation of a large expe- dition. More annoying were the sheaves of letters sent later on board the Terra Nova, addressed in such terms as “ Mr. Wood-B. Pole-seeker, King Edward VII. Land.” The addressees not being known, they will probably languish in a New Zealand Dead Letter Office. Captain Scott arranged that those scientists who were specially engaged in glacier investigation should immediately proceed to the New Zealand Alps to study polar conditions amid somewhat less strenuous circumstances than in Antarc- tica. Ido not propose to do more than give a brief outline of the features of this region, which may reasonably be “pur[vaZ MON 03 adeAOA ay} UO PatISIA siMOqIL}y a PON PY ——— PAS UNA, etim\ nee OS ATTY Ry UOS/OYIIN fC pp shar LA27 LE ll Wp Yoey paumos( Syueg” SS Z we J = ae ATH UL, M1 SE, 7 = = F7 -_ Je Hay LZ : eS : —— irs LZ OTe S, MTEL. — — ee | f : ide Gy we ——— Weal Lig ty) 10/9 FP» — ——— ee GE OLY Loy —Vifssea : - gE Weller Br) sf ig Wj 4zj YY), Xi Wii aS =i hf te Pip :

Ana ae shumb s make Oke ben Vins and Re Seals And whales ee Along comes the Orca et “g Ae eae Rem down feload, ‘wale up ebove Me Afterguard attack Phem on the fee A bd wx ployer fiwbles dew : and slaves the mushy back 19, He's cvumpled up betw ean Te Poe And so qt Heer shack mn. And there's no dovbt Re soen Lecems 3 P a paleek fer iiiser Invigorating diatoms , al though they*re none Be wiser ~ So the prefeplasm pe Sses OmnlS ey hever- ceasing rovnd, Like ahvuge recYMing deci- mal, te which noeng ‘Ss found (As will be seen later, the human element in the cycle was nearly supplied !) One never sees the penguins swimming on the surface. Occasionally a snake-like head pops up and looks around for a few seconds, but usually they are swimming rapidly with THE TERRA NOVA GOES SOUTH 85 their flippers a foot or two below the surface, or imitating the — dolphins in curving leaps through the air. On the shore near the rookeries the snow was worn into long gutters where the penguins promenaded to and fro. The winds are too strong for any economic deposit of guano to arise. We saw brown patches driven by the wind on to a snow bluff five hundred feet above the rookery. About 6 p.m. on the 3rd Erebus came into sight. We approached it from the north-east—an unusual direction—and so, perhaps, obtained a more comprehensive view of the outer crater than previous observers, It is a wonderful ‘“‘Somma”’ ring, like that of Vesuvius, and being composed of dark steep rock, it stands out in strong contrast to the inner white cone and the outer snow-covered slopes. Ponting got a fine photo- graph of it, which will be of interest to vulcanologists. Having given up all idea of wintering on the north-east quarter of Ross Island, we immediately steamed west to McMurdo Sound. We were engaged on a survey of the north coast of Ross Island. Bowers with sextant, Pennell at the compass, Camp- bell at the range-finder, each with an assistant, formed a busy group on the ice-house. All that night we steamed steadily west to Cape Bird, passing Beaufort Island on the starboard, and then turned south again to Cape Royds. Beaufort Isle was the scene of an exploit of one of our seamen (Paton), who was shut in by pack some five miles away from the island in the whaler Morning. He and a mate broke leave to try and reach the isle across the floes, but had to return without accomplishing their wish. On his return to civilization Paton found he had become a proud father. The child was christened Beaufort Paton on the suggestion of Lieut. Evans. About 5 a.m. we came into sight of the western face of Erebus. McMurdo Sound was closed in here by loose pack, but the ship threaded her way through fairly readily. We were keenly interested to see the condition of the ice at Cape Royds, and two of our afterguard (Priestley and Day) have a personal interest in the headquarters of Shackleton’s expedi- tion. Soon after the queer volcanic knob on the end of Cape Barne hove in view we sighted the meteorological screen, and immediately afterwards the hut of the 1907 expedition. But 86 WITH SCOTT: THE SILVER LINING the bay, instead of its old-time surface of sea-ice, was a sheet of open water, with two stranded bergs in one corner. Obviously it was no better as a landing-place than Cape Crozier had been. The hut looked in good order, though the door had apparently been broken in, but we could not see many details, for it was essential to push south and see how much ice had broken away. An hour later we reached Inaccessible Island, and here a solid wall of sea-ice prevented all further progress. Forty-eight hours of coast observation caused one watcher to retire to his bunk. On returning to the deck I found that the Terra Nova had come to a standstill against the sea-ice, about a mile south-east of Inaccessible Island, and the same distance from the shore. Here on a large area of dark eruptive rock—freed from snow at this season—we are building our hut. In the future the locality will be known as Cape Evans. CAPE EVANS : ei. Lands End | ‘inaccessible Is. KS 500 Ft Tent IC Pes Z 1910 Hut ee EREBUS VOLCANO Bkittie 2) 500 Ft. ‘© and A “Big a Razorback \ . Tf | -=- oe ee ~- Broken of f 3-11 : THE OY Turtle Is. g@ ur Chee ees ae BARRIER « tere t+ « ve ; PRAM ROINT 4UT POINT ‘ Y \ 5 q Yilfg ‘ - CAPE iP ARMITAGE 13 MAP OF THE COAST FROM CAPE ROYDS TO HUT POINT: 2"4 Crafter Active ae 133550 ” CHAPPER? VI MAKING WINTER QUARTERS AT CAPE EVANS On the morning of the 4th we carried out hawsers, and put in ice anchors in the ice, over which so many journeys were to be made in the next fortnight. Captain Scott, Evans, and Dr. Wilson went off to choose a suitable site for the hut, and returned very pleased with their brief survey. Let us look landward from the Terra Nova, and examine the locality where the expedition will spend some six months of the ensuing twelve. We are drawn close to the ice, which stands about eight inches above the sea, and some eighteen inches below water-level. It is variable in texture, that near the ship being rather mushy and honeycombed below—while several large cracks traverse it. Further away is a belt of clear hard ice, and then bands of snow-covered and clear ice for a mile or so, until the shore is reached. Here along the western slope of Erebus extends a belt of the dark volcanic rock, kenyte, and in consequence of the rapid heating of dark objects by the continuous sunshine, this is largely free from snow. Immediately at the shore-line is a belt of very soft ice, fantastically honeycombed, and threaded by streams of fresh water. Crossing a snow-bank, we rise slightly, and reach the kenyte gravel on which our hut and the head- quarters generally are placed. Walking along this gravel slope, we come to a flowing stream, falling over a little water- fall—a rarity, as may be imagined, in Antarctica. Moreover, this stream rises in quite a respectable lake—which, if not large enough for a regatta, at all events affords good exercise in chasing the skua gulls, which have been attracted by the Open water. Continuing eastward, the steeper lower slopes of Erebus are reached. The lower portions are of the same dark eruptive rock; but a few hundred feet from the sea- 87 88 WITH SCOTT: THE SILVER LINING level these are covered bya pall of snow, which extends almost uninterruptedly to the summit of Erebus. The slope steepens considerably at an elevation of some five thousand feet, and when the top is clouded over, the lower portion is not unlike the base of Fujiyama in Japan. On a clear day the steam-cloud capping Erebus is very obvious. Usually it is seen drifting to the south from a sharp vertical column arising directly above the crater. Sometimes, however, the steam-cloud spreads out fairly symmetrically, and on one occasion it simulated a gigantic cedar-tree, with a central trunk and spreading branches. To the south are two stranded bergs, which I shall describe in detail later. As a background to these dazzling white pyramids is the sombre ridge of Inacces- sible Island, which some of us before long—in spite of its name—managed to conquer. To the north-east is the cliff- like edge of the Cape Barne glacier, reaching almost to the curious dark erratic outline of Cape Royds. Fifty miles away to the west, across the sound, the wonderful glacial valleys of the western mountains are seen veiled in clouds. Now began a strenuous time for all on board. It was necessary to get the heavy cargo off the ship while the floe remained firm. Though the weather was excellent there was no telling when a heavy wind would send all the sea ice into Ross Sea. Gang-planks were run out, and the wildly excited dogs pulled, pushed, and tumbled into the hands of men on the ice. Then they went at a gallop over mushy ice to the bow ice-anchor chain ; there they were tethered at intervals of a foot or so. We had not been at work long when inquisitive visitors turned up. These were the Adelie penguins, who waddled eagerly forward, and promenaded about, with their heads bent on one side in a very critical fashion. Unfortu- nately the dogs were as keenly interested in them, and simultaneously twenty of them rushed at the nearest penguin. A scene of wild confusion ensued. The heavy cable was jerked about so violently that the end dogs were lifted several feet into the air and hung there a moment suspended by their chains. Whips, yells, and curses were of no avail until the miserable bird had been torn limb from limb. For some hours one man had to be on the watch to warn off trespassers and prevent penguin suicide. The ponies, with one exception, were much less trouble, SURVEYING THE NORTH COAST OF ROSS ISLAND FROM THE TERRA NOVA, JAN. 3, 1911. Photo looking aft from the foc’sle, showing six officers at the standard compass, [See p. Ss. PHOTO FROM THE SHIP OF CAPE EVANS, Jan. 26, 1911. The Tunnel Berg appears on the right. Behind is the dark line of the Ramp, and twelve miles away the cone of Erebus with a small steam cloud, THE TERRA NOVA GOES SOUTH 89 and were swung out ina box on a rope from the yard with great ease. The motor sledges were transhipped in their cases—which had hitherto formed efficient walls to the dog “hangar.” Three ropes attached to the mainyard, and manned by ten men, enabled the case—weighing about a ton —to be swung up, outward, and downward on to the floe without a jar. The motors were then taken from their cases, and run further on to the floe, where Day and Nelson soon had them running. It was their buzzing which annoyed our high-spirited steed, ‘Hackenschmidt.” He careered about the waist of the ship, and was more trouble to land than all the other sixteen. He continued his career of uselessness during the following busy season. Ponting found much material here for his cinematograph, and had the machine clicking merrily most of the forenoon. He has literally miles of films, and it is amusing to see the way he snips off a foot or so of an exposed film quite callously to develop it and judge the result. As he says, it only represents a second which will never be missed in a series of several minutes. It was a large hauling job that confronted us. Material for a hut, 50 by 25 feet, with walls and roof of six or eight layers; sledging equipments, tents, etc., for thirty men ; food for two years; fuel (chiefly a patent coal com- pound) for the same period; and fodder for the seventeen horses and for the dogs. All this had to be carried nearly two miles across the sea-ice on sledges, What now were the means of haulage? We had many and varied methods. Firstly, the motor sledges ; secondly, the ponies ; thirdly, the dogs; and fourthly, man power. Each has something in its favour. Speed of transit goes to the dogs, non-liability to accidents to the man-power ; gross tonnage to the motors, and general efficiency (with decent specimens) I should award to the ponies. The man-sledges got to work very early in the campaign. The sledges are nine and twelve feet long, with runners four inches wide, and upturned somewhat at both ends. There is a flexible bent prow, and six or eight vertical stanchions, which Support the upper frame—as simple a design as one could devise. Everything is secured by leather lashings, the abut- ting ends being sewn into a sort of leather bucket. A rope loop projects trom the front, but is fastened to the forward 1161 ‘$ Asenuef “urd 11 ‘yq1ou Suryooy ‘suvag ode punose uorgor oy1 pure ‘snqa1gy WO pNojr-UlvaIs PEplAlp 24) Zurmoys ‘purysy a[qisseovuy Woy YoI9xg Pra S401 DYyIG-HIVV S| 9|4!ssa>2eu| Jorjnsuns THE TERRA NOVA GOES SOUTH gI stanchions, and not to the prow-piece, which serves chiefly to guide the sledge over hummocks of ice. A long rope with broad canvas belts (attached thereto by tributary ropes) con- stitutes the harness. When the load has been tied on by a piece of spun yarn, the leader steps into his belt, adjusts it over the hips, and, grasping his ski-sticks firmly, gives the word and plods on. Many a mile have we covered with bodies hanging forward over the belts, and our spiked boots and ski-sticks barely enabling us to pull the heavy load through a patch of snow-drift. But over moderately smooth sea ice it was quite easy for four men to pull a 1000 lbs. load on two sledges for a distance of a mile and a half in twenty-five minutes. There were two dog teams in constant use, one driven by Meares, and the other by the Russian youth, Demetri. Their sledges are Siberian, and somewhat higher in the frame. The chief difference consists in a high hoop or arch of wood, which is placed two feet from the prow. By this the driver can twist his sledge around. He also carries an iron-pointed staff, to be used as a brake and also to guide the sledge to some extent. The dog teams consist of five dogs—one leader who is specially trained to obey commands (and sometimes scorns to pull), and two pairs of dogs toggled to a central rope much as in the man harness. These dog sledges career about in long sweeping curves, and the air resounds with barbaric cries of “Ky! Ky!” or “Chui! Chui!” while the ice screeches under the impact of the driver’s pointed staff. His chief difficulty is to steer clear of penguins, for awful is the result if they sight an unfortunate bird! A dog team pulls the driver, so that 150 lbs. must be added to their load. Each dog pulls about one quarter that moved by a man, but at twice the speed. The motor 'sledges took some little time, naturally enough, to swing into the ranks. They have fourteen horse-power motor-car engines, four cylinders, magneto ignition. Most people have seen illustraticas of them, for they have been run in Norway and England previously, though designed for the expedition. The two axles bear two pairs of cog wheels about eighteen inches diameter. Around these run two end- less bands—one on each side of the sledge—which carry flat square plates. These plates constitute the bearing surface, 92 WITH SCOTT: THE SILVER LINING and each plate is actually stationary on the ground until it comes under the rear cog wheel, when it is caught up and passed forward to the front cog-wheel. Hence the car runs on its own platform. The flat square plates grip the snow by diagonal bars. There is a large tool box in front of the engine, and a small elevated padded seat at the back. Otherwise no top hamper obscures the mechanism. When not in use the motor wears a huge quilted hood which keeps the cylinders from freezing. In work two men are necessary. One drives from the seat, and another holds the end of a rope fastened to a pro- jecting bowsprit. The latter is the helmsman, for at a pull sideways the sledge slews around without the expenditure of much effort. The camber on the plate belts also helps the turning of the heavy mechanism. The two motor sledges were in frequent use for the first few days, and hauled most of the hut material to the shore. They pulled about two tons, and one of their functions (most fully appreciated) was that of hauling back empty man-sledges—empty except for the wearied pullers who lay back on the sledges and dreamily regarded the clear sky on their welcome rest between pulls. The ponies had been standing continuously for five weeks, and were therefore not very fit for a few days. They were given a short rest at the pony-lines on the snow behind the hut, but soon came into requisition, and have done the greater part of the hauling since. The ponies had, however, many little peculiarities which were troublesome, not only to those uninitiated in the mysteries of pony-driving, but to the experts as well. I shall have more to say on this later. Let us accompany a man-sledge from the ship to the hut. The question of knots troubles a landsman. At first it was not uncommon for the first jerk to result in the rope parting company with the sledge! The start was always difficult, for the sledges froze to the ice, and it was necessary to “‘ break them out”’ by extra help. We had not much eye for the beautiful scenery around, but were very keenly and vitally interested in the surface over which we had to pull the load. Ten feet of clear ice were less difficult to traverse than one foot of snowdrift only an inch deep. The party all wore snow-goggles of amber or green glass to prevent snow-blindness. These fogged from THE FIRST HOUR ASHORE. Demetri preventing penguin suicide, TWO MOTOR SLEDGES ON THE BEACH AT CAPE EVANS, JAN. 20, IgII. The tabular berg has just grounded where the ship lay at anchor and so she has steamed off to the north. The motor engine is covered by felting. The sea ice can be seen breaking away. re s Oo s oie i J ¥ 4 b. @ aa oe Wo i Ae ed ; S ent > a ait Cs : + o] wy 1 a“ lad THE TERRA NOVA GOES SOUTH 93 perspiration, and required frequent cleaning unless the sun were very bright, when luckily they warmed up somewhat, and the moisture did not condense so rapidly. At first we would follow the motor trail marked by staves and empty oil drums. But this was too heavily drifted in places, so we deviated south to reach clear ice. All goes merrily until we reach a snow belt. The first sledge touches the snow, and a slight jerk makes us pull to our belts. Another jerk announces the arrival of the second sledge, and if we are pulling three sledges the combined resistance reminds one of hauling three ploughs through stiff wet clay. On this snowdrift we see the pony hoof-marks and the long furrow cut by the dog-driver’s staff. Then on to clear ice again, where spiked boots are essential, We reach a broad band of troubled ice crossing the Svun-holes Se pit smooth surface. This is a recemented crevasse, and is practi- cally as strong as the rest of the surface. The older ice near the shore is “pitted” in a curious fashion. Imagine a red-hot horse-shoe planked down on the ice, with the front forced deeper into the ice. This is the shape and size of these holes, and it seems probable that they might save a man’s life in a blizzard ; for they are all directed to the south, and would form a sort of compass if he had no better! The explanation is that they are due to the action of the hottest solar rays, which, of course, occur when the sun is in the north. Curiously enough, those small holes have no effect on the sledge haulage, except that they tear the runners somewhat. On another patch of snow is a queer “ spoor.” A serpentine trail of four or five parallel lines, with large 94 WITH SCOTT: THE SILVER LINING three-toed footprints, alternating with the curves of the con- tinuous serpentine trails. Suddenly it changes into a broad, shallow gutter in the soft snow! What strange beast has made this? It is of course due to the penguin. As he ponderously heaves from foot to foot his stiff tail feathers swing in unison. When he is tired of this method of progression he drops on his breast and propels himself by his toe-nails. Hence the broad gutter! This trail is very like those fossil prints set down to gigantic Plesiosaurians in bygone times. Ew S : SS 3 Antarctic spoor, January 12, 1911. To our right is a patch of very dark ice with an evil crack leading to a small pool. We skirt this warily, and are not much surprised to hear a sudden plop ! as two or three penguins shoot out of the water and land at our feet, and often right in the way of the sledge. A pony-sledge passes us and then stops—amid our jeers—to breathe the steed, for the ponies are short of wind at this early stage. We hear a steady droning, and the motor rolls by. But we beat across country, while the helmsman is hauling the behemoth on to a new course. The belt is beginning to cramp our muscles, and the steady stab and drag of the ski-sticks at first blister the hands. Soon the welcome bamboo at the camp comes into sight. Snow bridges have been built across the tide-cracks just below the hut. Here the ice rises and falls a couple of feet during the day. We save a little “go” for the last hundred yards, and rush her at the tide-cracks. ‘Up she rises,” and several willing helpers from the hut lend a hand, and so our load pulls up on the belt of snow by the hut. Here Bowers takes charge, and his gang puts the wood near the hut site, the food on another spot, fodder here, and oil in the far corner. Then we run the sledge out of the way to the ice, and if there is no motor returning, pull it back with light loads and rapidly easing muscles to the ship. We were returning on Friday evening, somewhat wearied, THE TERRA NOVA GOES SOUTH 95 when Ponting met us and told us the “ owner”’ wished every one to hurry to the ship, for the killer-whales were breaking up the floes, and the stores on the ice would be lost! We ran on and found the sea-ice all broken away at the stern ; but Ponting had not explained his own very exciting adven- ture. Two dogs had broken loose and were racing about at the edge of the ice, when a party of eight killer-whales ap- peared at the stern of the ship, evidently attracted by these strangely active “seals.” An orca is twenty to thirty feet long, and has the most fearsome jaw of all the creatures that hunt in the high seas. Thirteen long conical teeth are set in each jaw, each projecting a couple of inches from the bone— and (unlike those of the crab-eater) built for business. Pont- ing, ever keen on good photographs, took his camera along to get a close view of these fellows. He narrates that they lifted their wicked-looking heads above the water to look at him, and he was just pressing the button, when he felt as if an earthquake had hit him. The whole floe was being broken away by the orcas, and he was separated from firm ice by two feet of water. He did not stop to finish that photo ! After dinner Debenham and I made a trip across the ice to Inaccessible Island. This rises sharply from the sea, about one mile south of the ship, and is usually surrounded by a belt of water—due to the warming action of the very dark rocks of which it is composed. Here we came across our first “sastrugi.” They are long, deep furrows cut by the drifting ice crystals in the sides of snow-drifts as they are driven onward by the blizzard winds. Thus they lie on the windward sides of the drifts, and make sledge-travelling very difficult if they face the sledge. If the drifts are across the path of the blizzards the sastrugi may cut right through the former. Inaccessible Island was almost covered with the debris of kenyte lavas, though here and there bosses of solid rock remained, especially towards the summit ridge. In these cold latitudes the frost action breaks down the rocks very rapidly, without destroying the mineral structure to such an extent as is the case in warmer regions. The kenyte weathered into blocks, which irresistibly suggested the Easter Island “ idols.” Every variety of this rock was found. Some with large crystals an inch long, others like glass, of a chocolate colour ; vesicular lava, full of bubbles, looking like petrified bath- 96 WITH SCOTT: THE SILVER LINING sponges, and pieces of kenyte caught up in a later flow of lava, and burnt just to the tint of a red brick. Just before midnight we returned to the ship, and labelled our specimens in broad sunlight, before turning in. There are two icebergs stranded off Cape Evans, and Captain Scott arranged that Wright and myself should have some time free to study their structure while the sea-ice was firm around them. He came along himself to have a close view, and Ponting brought a sledge, filled with cameras, to collect photographs. They were both pyramidal, and pro- jected a hundred feet or so above water. Most probably they had been much tilted, for a very prominent layer of snow— which from its included air melted slowly—was now almost vertical. It was obvious that they were affected by the tide, for a pool filled with brash ice almost surrounded them, and we could hear the ice fragments creaking as they rubbed together. A unique feature occupied our attention most of the time. Traversing the berg from end to end was an oval tunnel, forty feet high and fifteen feet wide, so regular in its outline that it looked as though a red-hot bar had been pushed right through (a distance of 150 feet). The scenic possibilities of this mass of shadow in the midst of the dazzling white of the berg were, of course, fully appreciated by Ponting, and I doubt if any mass of ice has ever been photographed so thoroughly, from the right, from the left, from above, below, outside and from inside, and right through it! By a stroke of almost unbe- lievable luck the view back through the tunnel just framed the ship at a mile distance. Next day the berg had swung through 180°, the ship had steamed away, and the sea-ice had moved out, so that Ponting was rightly overjoyed at the “ for- tuitous concourse of atoms,” which has given rise to one of the most interesting of his studies. We were equipped with rope and axes, and cut steps some sixty feet up the berg until we were well over the tunnel. | was much surprised when one of the blows of the ice-axe seemed to set free a strip of orange-peel! Visions of a Japanese hut far to the south floated through my mind, but on examining the object it was found to be a small fossilized fish. I dug it out six inches below the surface, and as the sun melts off quite an appreciable layer every day, this fish THE TERRA NOVA GOES SOUTH 97 may have been enclosed in the berg for a very long period. The species was probably Notothenia, and somewhat resembles Sep. lou Iceberg equilibrium. The tilting of the Tunnel Berg during the winter, 1911. N.B. The front of the tunnel broke away before September. the garfish of Australian waters. This reminds me of some rather curious biological specimens discovered by one of the H 98 WITH SCOTT: THE SILVER LINING non-scientific members in our little waterfall. They were white spherical objects, two millimetres wide, which could be peeled like an onion, and each seemed to enclose a little pearl. But Lillie identified them as crystalline lenses from the eyes of Notothenia, which were the only things found indigestible by the omnivorous skua gull, and so accumulated in the stream near their nests. Both ends of the berg tunnel were fringed by beautiful icicles, many being branched almost as much as the famous Jewish candlestick. The exterior of the berg on the more gently sloping side was armoured with a panoply of plough- shares projecting horizontally, and due probably to the sun melting the surface differentially, as described in the case of the sea-ice. It was unpleasant to climb, and a fall would have precipitated one into a most uninviting pool. As we watched it two killer-whales rose to the surface, and “ blew off steam ” through their dorsal spouts. They moved towards the south, under the solid ice, and we could see them long after spout- ing occasionally along a narrow open crack leading in that direction. We were very fortunate in our weather at this time. Bright calm days, so warm that one could sit outside in the lee of a pile of fodder after lunch—as many of us did—and enjoy a short siesta. From the first day work was carried on busily at the hut. The foundation was excellent, for the surface all round our camp consists of kenyte gravel, on which the snow melts as soon as the sun strikes it ; which is porous, so that water will not lie on it; and finally, is so springy that our food-cases were not damaged, however heavily they were dumped on the gravel. The main timbers were prepared long before we left New Zealand, and most of the matchboard was cut to size, tied in bundles, and roughly labelled. The floor area is fifty feet by twenty-five feet, and the roof is quite plain, with a central ridge. Three small windows, permanently shut, and with doubled panes, admit sufficient light in summer ; while later on an elaborate acetylene plant will come into use. Of greater interest were the precautions to keep out the cold. Vertical tongue and groove matchboard was nailed both out- side and inside the framework, an air-space thus being enclosed between them. Next, a layer of a patent quilted seaweed material, made of sea-grass sewn into jute sacking, was tacked THE TERRA NOVA GOES SOUTH 99 on in two-foot breadths. On the outside this was covered with weather-boarding, and on the inside by another layer of matchboard. The floor was made of thicker boards separated by ruberoid, while the roof has an inner matchboard ceiling— an air-space (with joists, etc.), matchboard, two layers of sea- weed quilt, matchboard, and two layers of ruberoid. Thus every portion of the hut has many layers, each of which is fairly wind-tight. The door opens into an air-tight porch, and this is protected from the south-east blizzards by a wind- screen. A large ventilator on the roof ridge is the only legi- timate air-gap, but in one corner the meteorologist has a sort of external cupboard for his instruments, which is bound to be cool. Everything went along swimmingly. The official carpenter and two of the petty officers carved out the more intricate details of carpentering, while the afterguard soon became moderately expert at nailing matchboard, chiefly with geological hammers. One of the scientists (subjected to criticism) complained that he never could drive a nail straight while any one was watching him. His tormentor declared that he must have afforded amusement the whole day, and pointed to a complete series of wilted nails due to the tyro’s efforts. For the roof-work the spiked boots of the geologists were in great request, for it was possible for us to manceuvre over the sloping boards at much greater speed than could “< Chips” and his assistants. On Sunday (the 8th) occurred an unfortunate accident, almost the sole mishap since the loss of the ponies in the gale. We swung out the third motor-car, having freed it from its case while it was inboard. It was landed on the sea-ice safely, and run smartly away to a firmer surface fifty yards away. I then left the ship with a one-man sledge-load bound for the hut. Captain Scott and Lieutenant Campbell were testing the ice, and warned me to be especially careful of certain wet patches near them. I got through to the shore without incident, but this unhappily was not the case with the motor-sledge, which started off imme- diately afterwards. I was not present, but heard that it was pulled across on to apparently firm ice near the doubtful portion, which had just been crossed safely. There one of the men went through, but was hauled out safely. He declared he felt himself being pulled under the floe by the strong tidal 100 WITH SCOTT: THE SILVER LINING current. Almost the next moment one corner of the motor- sledge sank, and then gradually the end, and finally the whole of the machine crashed through the ice; and despite the utmost efforts of the hauling party it sank in a hundred fathoms. Thus was lost nearly a thousand pounds’ worth of valuable machinery, and since it is made largely of aluminium, it corrodes extremely rapidly, and would not be worth salvage, even if it were possible—now the ice is out—to grapple it at that depth. During the building of the hut meals were eaten in a huge brown tent alongside, and many of the afterguard slept in small tents on the shore. A new type of these latter looks exactly like a rounded sun-helmet lying on the ground. The rim is represented by the broad flap, which will be covered with snow on sledging journeys, though now a handful of gravel is sufficient to keep them secure. One evening I strolled into the skuary just behind the camp. Here are hummocks of kenyte with little lakes and shelving gravelly beaches. In the lakes a reddish plant akin to seaweed coats the bottom, and dries to a leathery wrinkled mass. The skuas nest anywhere, not even a semblance of a nest being perceptible. They resent intrusion very strongly, and every one is at first slightly intimidated by the tremendous swoops, rushing wings, fierce eyes, and shrill cries of protest. I wanted a specimen, and decided to test a method of obtaining it, which smacked somewhat of Munchausen when described to me in Australia. Taking a flat slab of kenyte I waited until a skua was approaching. Then, before the bird arrived, I threw the rock into the air almost straight up. The bird collided with it as it was falling, and dropped to the ground stunned. This scheme of hunting is really much more certain than it sounds, for the bird has apparently no fear of objects above it. The ship was moved to a fresh berth, some five hundred yards nearer the hut, and also nearer the slopes of Erebus. Henceforth almost all the transport was effected by pony teams. There were many incidents at first, for the ponies did not understand the icy surface, and were by no means too subdued by their long voyage to object to most of the duties demanded of them. Hackenschmidt is still obdurate, I believe, but the others have calmed down, and done their THE TERRA NOVA GOES SOUTH 101 four trips a day as long as it was necessary. One soon gets to know their characteristics. Fiery ‘ Bliicher” trots through all the work, whether he is pulling an empty sledge or half a ton through a snowdrift; in fact, the driver is usually dragged alongside over the ten miles involved. With a slippery surface and only a single rope halter, it will readily be understood that four legs can defeat two if the whim seizes him. One gentleman, rejoicing in the name of “ Guts,” broke away three times, just as I had lugged him the weary mile to the ship, and galloped back unencumbered. But the least- envied duty in the expedition is a morning in the company of “ Weary Willie.” With drooping lip and stubborn eye, he improves on a crawl only when his driver precedes him with the halter over his shoulder, and practically drags both pony and sledge. In spite of a heavy load of patent fuel, he used to start back two steps to the minute quicker, thinking he was returning to the pony lines, but this soon degenerated to a crawl, and his objections to returning for another load necessitated special help at the turning-point. There was another pony, whom I only discovered on the last day, who was a happy mean between Bliicher and Weary. He was anonymous, but deserved a baronetcy. The last loads con- sisted of patent fuel (in foot cubes) and compressed fodder, while ballast, in the form of thirty tons of kenyte, was loaded from a snow-slide and taken back to the Terra Nova. Many of our minor pursuits irresistibly reminded me of a childhood’s day on the sands. There are little trenches to be dug, to lead telephone wires to the Observatory hill ; pemmican to be poked out of tins in solid cakes just like the little sand-heaps moulded in toy buckets; miniature bridges over the tiny creeks; and, most realistic of all, grottoes to be carved out of solid banks—not of sand, but of hard, clear ice. The track to the Observatory hill passes along a miniature glacier with a bank fifteen feet high on the nearer side. In this it was decided to cut an “ice house” for the mutton, and for seals and penguins. Next door the physicists cut out another grotto for magnetic work. Each took about a week to complete. A “drive” was made into the ice about six feet high and four feet wide. At a convenient distance this was widened 102 WITH SCOTT: THE SILVER LINING out to fifteen feet, and we should probably have cut out a prosaic rectangular chamber, but that we found that the floor of almost impenetrable frozen kenyte gravel sloped up very steeply. Moreover, the sun melted the “glacier” at a great rate, so that we had to leave a fairly thick roof. These restrictions produced a very pretty style of architecture—a sort of double crypt with a central partition, and gentle, sweeping curved roof, like an opened cockle-shell lying with the convex sides uppermost. The sunlight filtered through the roof and entrance wall, making the ice look like alabaster. It was hard work chipping the ice. We were helped by Glacier 1€& Gravel Sez SSE Sketch of two grottoes cut in glacieret near the hut, January 15, 1911. a few layers of dust mixed with skua feathers—representing very ancient surfaces—along which the ice broke readily. One half was covered with a rough flooring, and on this were deposited a hundred carcases of sheep given by the New Zealand farmers. In the other half a hundred penguins occupy one corner, and later we shall add seal-meat. A little nearer the hut the physicists excavated an |_-shaped grotto, of severely rectangular cross section, and lacking those picturesque sweeps in the roof which were necessary in the other cave. It penetrates the “glacier” for about twenty- five feet, and is entered by an aperture some three feet high. One feels very like a rabbit entering its burrow, but this THE TERRA NOVA GOES SOUTH 103 constriction is necessary to ensure equable temperature. A mild blizzard was blowing while we were cutting it out, though in the calm—not to say stuffy—atmosphere of the grotto a temperature of twenty below freezing had little effect on one’s comfort. To be sure files, and saws, and other iron tools developed an octopus-like surface, for they stuck to one’s fingers as if smeared with gum. The wall struts—for the lining—-were cemented simply and effectively by a mush of ice and water, which solidified immediately. Two large kenyte boulders formed jagged obstructions on the floor. When foundations for the instrument standards were being made, it was found that under the layer of gravel forming the floor was another layer of ice. It is quite possible that our hut may be built on gravel over a thick ice sheet. This will be tested by a shaft in the winter leisure. On the highest portion of Cape Evans is hoisted the Union Jack. Near by is the meteorological screen, and two anemometers are merrily whirling round. We have been laying telephone wires across the space between the hill and the hut to connect the instruments there to the meteorological laboratory (“ corner” would be a better term) in the hut. On Sunday 15 work was suspended for a day, for every- thing was progressing well. Many of the men took ski on to the slopes of Erebus, behind the hut, and had a pleasant time, diversified by many tumbles, in consequence. To the north of these slopes extended the hitherto untraversed Barne glacier, which formerly blocked all communication with Cape Royds during summer. Its seaward face is a high cliff of ice, strongly crevassed, and reaching from Cape Evans to Cape Barne. Wright and myself received permission to go on the glacier, and providing ourselves with an alpine rope, ice axes, food, and wind-proof clothing, we set off up the rocky slopes behind the hut. We soon reached an irregular snow surface deeply pitted where boulders had sunk, with little runnels of water murmuring below the crusts in ice in numberless little gullies. As the ice became more apparent we roped up and marched to the north, gradually ascending the slope of the glacier. Our objective at this time was the rock ridge behind Cape Barne, about two and a half miles away. The glacier came down from Erebus in undulations resembling gigantic rounded steps. It seemed probable to us that the best surface would 104 WITH SCOTT: THE SILVER LINING occur where the ice was in compression rather than in tension. Here in the hollows the crevasses would tend to close up, and we found them quite readily crossed. In the icy surface were broad ribbons of snow, slightly depressed below the surface, and curving grandly round the undulations of Erebus. These looked solid enough, but an ice axe hardly met with any resistance in the snow, and on sweeping it away one could see a chasm extending indefinitely down. Higher up the slope the snow formed bridges, but here in narrower crevasses it was only of value in veiling the depth. However, it was a mere question of jumping ; the leader gathering in the rope and taking a good leap while the follower drove his ice pick into the surface and held on firmly. If there had been any great danger involved, two men would, of course, have been in- sufficient, but we progressed in this fashion for a mile, then crossed another mile of softish snow without crevasses, and reached the Barne ridge, with rocks running from the coast halfway up to the crater of Erebus. Here to our surprise we saw nothing but kenyte hummocks and debris lying between us and Cape Royds. It would not have been human to have resisted this opportunity of visiting the headquarters of the 1907 expedition. After resting a little among the huge mounds of kenyte boulders—actually bearing small tufts of red and green lichens—we tramped quickly across alternating patches of rock and snow, past small ice-covered lakes, and soon reached Back-door Bay. Here quite a large stream—for Antarctica— was falling over an ice cliff, and we reached the first sign of another settlement. This was a bamboo pole planted in a cairn. Then we scrambled over slopes of kenyte gravel, skirting the rotten ice which filled the outer part of Back-door Bay. The narrow gulf at the north-east end of the bay still contained firm ice, and we crossed this without attracting any remark from a colony of twenty seals, and so reached Cape Royds. Here signs of occupation were very evident, though the hut was some distance away on the further (northern) slope of the hill. A sledge with cases of tinned meat, a ladder, and the tubes of the hand-boring plant, had been left close to the water of Back-door Bay. We carried off a tin of beef in case the hut contained nothing more attractive. Following some old sledge tracks we topped a rise, and were right on the hut. THE TERRA NOVA.GOES SOUTH 105 Every one is familiar with the appearance of Shackleton’s hut. It is very snugly placed in a little dell leading to a small lake, which empties into the sea over some steep cliffs a quarter of a mile away. It seemed extraordinary that so many empty boxes and such piles of debris could have been the result of fourteen months’ stay. I suppose our camp will appear the same three years after we have departed. We skirted round the ruined pony shelter, over boxes of cork packing and cases of empty bottles. The door of the porch had carried away, but the inner door was standing. A foot of ice sealed it at the bottom, but hanging on the door was an envelope addressed in Professor David’s hand, “To Any One who may visit Cape Royds.” It did not enter his mind when he placed it there that an old student of his would be the first to see this. The envelope contained a short account of the results of the 1907 expedition, left there “in case the Nimrod is lost on her return voyage.” I carried the re- cord back to Captain Scott, a very interesting document, though luckily not of vital importance, since the expedition’s success was not marred by any accident at the eleventh hour. We then set about getting into the hut. Cutting into the ice with our ice axes we came to a tightly fixed block of wood —which we thought had been placed there to fasten the door. More chips of ice were removed by the ice-axes, and we saw that it was merely a broom, which had fallen down and been embedded its whole length in a foot of ice. There was nothing for it but to cut away this stubborn sentinel, and then it was possible to open the door a foot or so. We entered with much curiosity. All the windows had been covered with battens, but I did not expect to find it so snug and untouched by the weather. Not a grain of snow seems to have entered. We opened one window, and the place might have been abandoned the day before. On the low table in the centre a meal had been left. Condensed milk, saucers, biscuits, jam, and gingerbread. The latter were very good, and not harmed by two years’ exposure. At the back was a tray from the oven with a batch of scones just cooked, and a loaf of bread. I lifted the latter, and the whole outer surface peeled away, leaving a ball in the middle. This is just the way basalt weathers when exposed to the air, and it is 106 WITH SCOTT: THE SILVER LINING known technically as “ spheroidal weathering.” I did mot eat the bread. The 1907 expedition left in a hurry, I believe, which accounts for the somewhat unkempt appearance of the hut. Boots were scattered on the floor, books over the bunks, socks drying on lines. In one corner a roulette machine, in another a packet of paper used in their printing press. I fear I was most interested in tinned fruits, and searched through a huge store of unused food in one corner of the hut. Tea, pickles, jams, milk, onions, sausages, hams, cocoa, delicatessen, every-. thing but canned fruit. Finally we saw that the dark room was built of cases of bottled fruit, and in honour of the first crossing of the Barne Glacier we broached a case and extracted a bottle of gooseberries and another of currants. It was a queer meal. I had brought bacon and ship’s biscuit. Wright selected plum-pudding, sardines, and Nestle’s milk. I found preserved ginger, raisins, and corned beef. We drank alternately of currant and gooseberry vinegar, and ate through the above menu. Antarctica is immune from dyspepsia, for we felt none the worse. We strolled round the headquarters. The penguins were very interesting, for they were busy feeding half-fledged chicks. There are no nests near Cape Evans, but the atmo- sphere is the purer! I was not prepared for the shape and size of these chicks, They were nearly as tall as their parents, and twice as large round the most important part of their anatomy. Huge balls of dark grey fluff, with feeble little squeaks no louder than a chicken’s—in strong contrast to the indignant cries of their parents. After a couple of hours at Cape Royds we turned south and experienced no difficulty until we reached the crevasses, for we followed our previous track. The crevasses seemed to have widened a little; we were somewhat tired, and the farther edge was now higher than the nearer. In some ex- amples—which we did not tackle—the difference in height reached two feet. However, we crossed them safely (though in two instances one foot went through the soft snow) and reached Cape Evans without misadventure. Captain Scott had made a journey on a dog-sledge to his old quarters (1902) at Cape Armitage, sixteen miles south of us Unluckily he found his hut filled with ice and practically PHOTO OF THE HUT, SHOWING THE RAMP AND EREBUS, JAN. 20, 1911. The south annexe built of food cases (on the right) and the stable on the left built of coal blocks are just being finished. PENGUIN COURTSHIP ON THE ICE-FOOT NEAR CAPE EVANS. THE TERRA NOVA GOES SOUTH 107 useless, so much so that they slept outside. He had never seen the locality so free from snow. On the 25th of January he hopes to make a start on the depot journey to the south, and on the same day the western scientific party sets out to explore Dry} Valley, Snow Valley, and the Koettlitz Glacier. Captain Scott has honoured me with the charge of this party, whose personnel I have described previously. We have now occupied our hut for a week. Let me close the story of these early days by describing our life in the hut. To-morrow we leave it for some months of sledge- work, so that we have been very busy for some time past. SSN Soe Two Bergs D. sip Barne. aground) 1 Glacier Al P First sketch-map made January 21, 1911 (before any survey), showing ice fronts and positions of ship, A-E. From the porch one enters the quarters assigned to the sea- men and cooks. A large galley-stove is placed on the right, and behind it is the chief touch of colour in the hut in the form of rows of tins of food, spices, and utensils. A bunk suspended high up from one corner by an iron rod marks the resting-place of Engineer Lashley. To the left are many Wire mattresses supported on neat iron frames. A queer instrument like a guitar cut in half is the cherished possession of Anton, the Russian groom. His comical little bow when you address him—for he speaks no English—reminds me of the action known as “ louting low.” “Wor some time the ship had been lying quite close to the hut—about a quarter of a mile away at the spot C (on the 108 WITH SCOTT: THE SILVER LINING accompanying sketch-map). The original edge of the ice is shown, and here the ship stayed (at A) until the motor sank. Then she moved to B, nearer the Barne Glacier. On the 18th she came along the crack which opened near the stranded bergs to the position C. But seventeen bergs came into sight, and one huge tabular, as if desirous of this site, bore right down on her. So the ship moved across the Sound to get away from the northern wind. In cruising about here, she ran aground at D off Cape Evans. There was sixty feet of water under the stern and only seventeen feet at the bows! That's pretty steep! They ‘rocked’ her by running across ship in unison, and after an hour got her off. I photographed her from the Cape where the land party watched the efforts of the seamen.” Later I heard that this collision with the reefs of McMurdo Sound tore out a small splinter a foot deep and about ten feet long! Luckily the stout old ship could spare this at her bows without grave inconvenience. A bulkhead of boxes, amid which two branded “ sherry ” mark the wherewithal of future festivities, separated the “ mess deck” from the “‘wardroom.” The latter occupies two-thirds of the hut, and here the sixteen officers live. A long table extends down the middle and reaches to a palatial inner room, sacred to Ponting, the photographer. The roof of the latter is by no means wasted, but constitutes an important laboratory. At the back are two incubators, not for eggs but for parasites, bacteria, and other pleasant creatures fondly cared for by Dr. Atkinson, whom we expect to see brooding for hours over his pets. The centre of the room is thus accounted for. The right and left are divided into cubicles. First, on the left, are five mattresses assigned to Messrs. Oates, Meares, Bowers, Atkinson, and Cherry-Garrard. The right wall was divided into three compartments, occupied respectively by Messrs. Debenham, Gran and Taylor, Nelson and Day, Simpson and Wright. We have to live in this space for six months of darkness, and as we are limited horizontally to seventeen square feet each, it will not cause surprise to find that we have imitated the New York sky-scrapers. The first few hours of our house furnishing were devoted to amassing enough thick timber to build strong frames for the mattresses. These are built in tiers, and so each cubicle has SHIP AGROUND ON A REEF OFF CAPE EVANS CLOSE TO THE TUNNEL BERG. The whale-boat is trying to tow off the ship, while a skua gull on the cape is an interested spectator. ees tae i. GRIFFITH TAYLOR IN SUMMER RIG (ON A KEEN DAY) ON CAPE EVANS, Jan. 25, i911. ay on . - - v vet! THE TERRA NOVA GOES SOUTH 109 some clear floor space. In our own cubicle Debenham has raised his bunk five feet from the floor, and underneath this will ultimately develop a whole geological laboratory! In the far corner is a little oil-engine and dynamo, providing current for Dr. Simpson’s meteorological apparatus. On a table at one of the two windows is the “counter,” an important portion of the biologist’s sanctum. The rest of it is below the counter ! Half the left side of the wardroom is in part partitioned off. Captain Scott has one portion of this, His eastern boundary is a huge drawing-table under our second window. On the other side of this, and snugly fenced in by the dark room, are the quarters of Lieutenant Evans and Dr. Wilson. Near the dark room are the stove and the pianola. The removal of the latter from the ship nearly devastated the officers’ quarters afloat. The stairs were removed, and we had to get into the ship’s wardroom down a rope during the two days while they struggled with the pianola. However, it has safely arrived, though just the last few days a new gramophone has had greater popularity. During the two months of our absence the hut will be fitted with acetylene lighting. The four officers and five men who remain have also a contract to kill (and clean) a thousand penguins and skuas, so that they will be as busy as the sledging parties. Outside the hut the sea waves now wash the kenyte gravel. In the last two days a mile of sea-ice has floated off, and now the Terra Nova is hovering around only waiting to land the three parties (south, west, and east) before she turns her prow to the green northern land. All our preparations are made, and we join her to-morrow morning. The educative value and the interest of an expedition like this is inestimable. I have tried to describe some of the features with which I have been most impressed myself. During the voyage one learns something of seamanship, of biology, of navigation, and of naval matters generally. First- hand information on every conceivable subject from men who have seen many quarters of the world with an appreciative eye is obviously full of interest. The biologist discusses those portions of his subject which touch on geology or meteorology with students who are as anxious to approach 110 WITH SCOTT: THE SILVER LINING them from other standpoints. In another way also is this expedition almost unique. It is hardly credible that twenty men should associate for three months in somewhat cramped quarters without a jar; yet I can truly say that the best of good fellowship has always existed. This is the best possible omen for success in the future. [Nore.—This narrative is left in the form in which it was sent back to Australia in January, 1911, in the belief that nothing is lost (and perhaps some touch of reality gained) by so doing. ] Ill FIRST WESTERN EXPEDITION January—Marcy, IgII FIRST WESTERN EXPEDITION On the 24th of January the ponies went over the sea-ice to Glacier Tongue ex rouse for the Barrier Depdt trip. Captain Scott and the western party sailed in the Terra Nova to the Tongue, which we reached about noon. Later we were able to study the Tongue in some detail, but we could see that it consisted of a huge pier of ice about half a mile wide, and projecting some five miles from the low cliffs south of Turk’s Head. The surface was undulating, and about a hundred feet above the sea in the centre. Its origin is doubtful. Probably it is old piedmont ice anchored on some hidden ridge, but it is added to by blizzards sweeping over the root of the Castle Rock Promontory and depositing snow on the leeward side of the cape. We saw sections of it stranded fifty miles to the north-west later, which proved its partial origin from snowdrifts. On the 25th Debenham, Wright, and myself marched to Hut Point, where the 1902 hut was situated. We took a light sledge and our sleeping-bags. It was very interesting to recognize the places of which we had read in the “ Voyage of the Discovery.” Castle Rock was very prominent, a huge dark square “keep” about two hundred feet above the promontory ; “Danger Slope”—an icy slope dropping down to 150-feet ice cliffs—on which Vince lost his life early in 1903. The conical hill, seven hundred feet high, just east of Vince’s Cross, was Observation Hill; destined to carry another cross two years later to the memory of the man who had built the hut below. Off Hut Point the sea-ice was very rotten and full of huge holes. However, we reached the ice-foot easily enough, and pulled up to the hut. The surroundings were very tidy compared to Shackleton’s quarters, which was very natural, for the 1902 expedition practically lived in the ship. It was 113 I 114 WITH SCOTT: THE SILVER LINING Original geological sketch by Captain Scott (January 19, 1911), directing our attention to an unusual outcrop at Hut Point. surrounded by tremen- dous eaves, which were meant to protect stores, etc. We found the door blocked by ice, and had to enter by a window. It was filled with snow to a depth of four feet, which had drifted in through various open- ings. We found a bul- wark of biscuit boxes in the middle, and various stores of chocolate, etc. Some brownish powder, after some cogitation, we determined to be pepper. It had quite “lost its savour” in the ten years of exposure. Alongside were the little magnetic huts. Wright comman- deered some _ asbestos sheets for our own mag- netic equipment, and then we set off to see the real object of our visit. Captain Scott had noticed an exposure of lamellar rocks of a sandy appearance among the almost uniformly dark basic rocks of this region, and, although no geolo- gist, he realized that it was possible that a frag- ment of the well-known Beacon Sandstone (a fossil-bearing rock) had been torn up by a basic lava on its passage to the FIRST WESTERN EXPEDITION 115 surface. This would show the relative age of the two rocks concerned (the lava, of course, being younger), and so was well worth investigating. We found the outcrop readily enough from Captain Scott’s sketch, but Debenham and I decided that it was a weathered variety of eruptive rock, and not of sedimentary origin. Two other appearances were noticeable here, which were worth recording because we saw them later in various other uarters of Victoria Land. We could not account for them ms our first example. On the steep face of the cliff (five hundred feet high) near where poor Vince slipped to his doom, were four long horizontal ridges—one above the other—of dark masses of rock. They resembled lateral moraines left by giant glaciers, but I believe they are due to debris rolling down to the foot of a snow-slope. The latter varies in extent with varying seasons, and so the debris ridge may be deposited at another level. Another very curious feature soon attracted our notice. All the more or less level lowland around Cape Armitage, as well as the bare plateau of Crater Heights, was marked out like a gigantic tesselated pavement. I noted in my journal, “The lowlands of loose black rock appear to be rolled by a steam roller, while the surface is broken by gutters from four to eight inches deep.” These gutters marked out hexagonal and polygonal areas some twenty or thirty feet across. When a light snowfall had collected in the gutters, the valleys seemed to have been paved with black tiles united by white mortar. These symmetrical polygons are due to a slow movement of half-frozen soil, which has been noted in polar lands, and is called solifluxion or soil-creep. We saw many examples of these tesselations in the western moraines. We walked back to the camp on the sea-ice, pulling the asbestos sheets on the sledge. There was some cold tea to spare in Nelson’s tent, and we were glad to make our meal off this and some biscuits. Then, pillowing my head on a camera, I coiled into my sleeping-bag, and so spent my first night on trek. On the next morning we were told that we could ride back to the ship on the dog-sledges. Nothing loth, we tied our sledge behind Meares’, and soon covered the eight miles. The dogs pulled rapidly, but seemed to need frequent 116 WITH SCOTT: THE SILVER LINING rests. It was much more lively than “ man-hauling.” Meares’ constant cries, “Tchui—Tchui! Ky—Ky!” directed the leading dog, and the six pairs behind him swerved left or right in unison. There were numerous seals on our route, and Meares had considerable trouble to keep the dogs to the straight path of duty. One ginger seal especially excited their interest, and ours also, for the colour is most uncommon. Usually the seals are a dull fawn brown, though the breast is often beautifully mottled with white spots. My first seal-killing had been done a day or two before. After dinner Wright and I had marched off on hunting bent. We walked over the great South Road—where we had cleared a track for the ponies over Cape Evans—and reached Gully Bay. Just over the tide-crack we came on three seals ; one beautifully dappled, one small and dark, and a huge, big fellow. We wanted the skin for making sandals, and so attacked the biggest specimen. There was not much attack about it! You just hit him hard on the nose, as Wright did with an ice axe, and then stab him under the fore-flipper, as I did with my Serbish dagger. To make sure, we pole-axed him also. Then we skinned him with consider- able difficulty, for two of us could hardly make the body budge! The skin and blubber were two inches thick and frightfully slippery; you could not grip it. We had to drive the ice axe into the loose flap of hide, and so gradually drag the carcase into the positions necessary for flaying. We left the hide on the head and limbs, and then cut through the cartilaginous breastbone and secured the huge liver— about forty pounds of it, I expect. We intended to drag the hide back with a rope, but all we could manage was the liver, of which I hung a part on each fore-finger. Then we walked back to the hut, about half an hour’s journey, and when we arrived I gave the liver to the cook. I soon found that my fingers were frostbitten, and through inexperience I stayed in the hut. For five minutes I tramped up and down with an almost unbearable pain in my fingers very like toothache. Never again did I expose my hands in the Antarctic in any constrained position, so that this first slight mishap was a good lesson to me. On the 27th of January the ship left Glacier Tongue, to carry Our party to the western side of MacMurdo Sound, a FIRST WESTERN EXPEDITION 117 distance of thirty miles. I got a photo of the face of the Tongue—showing queer little bulbous icicles where the swell of the tide had licked them. The Tongue rises and falls with the tide, and so there was no very definite crack between it and the sea-ice at its end. Little did we think that this century-old natural wharf was to be torn away from its moorings a few weeks later ! Now that all chance of adding to our equipment had passed, we found that several important matters required attention. For instance, my ski-boots—in which I had to traverse rocky slopes for six weeks—developed a hole thus early in the campaign! This apparently trivial matter bulked very largely in the succeeding journey, and though they were roughly cobbled on board and stiffened with all sorts and conditions of nails—none being very suitable—they were a constant source of worry. In the afternoon we approached Butter Point, passing through a belt of “brash ice” to reach it. This curiously named headland is where the 1902 party started to explore the western valleys. Here a supply of butter was left for the returning travellers to reward them with a toothsome dish of fried seal’s liver (if they had “first caught their geal”). Butter Point is really the north-east end of a “ piedmont ” glacier. It is a mass of ice—almost stagnant—which covers a coastal shelf some five miles wide between the foothills and the sea. The snow slopes rose rapidly to a hundred feet or so, and then more gradually to five hundred feet. Many unsuccessful attempts to fix an ice-anchor in the hard snow (covering the glacier) resulted in our moving north a short distance, where a grip was obtained when the anchors were carried some two hundred yards inshore. On the summit of the snow ridge, about half a mile away, we saw the pole of the depdt left by the 1907 expedition. This was now visited by a sledge party to depét provisions for the forthcoming northern journey in spring. In the meantime our two sledges were lowered on to the ice, and packed in readiness for our start. The sledges differed in size, one being twelve feet long, and the other only nine feet. The latter Evans evidently regarded as the apple of his eye, but weight for weight it was much less efficient than the 118 WITH SCOTT: THE SILVER LINING larger sledge, since it weighed almost as much, but could not carry three-quarters of the load. We had a heavy equipment for four men, averaging about 270 lbs. each, but as we were only proposing to take one sledge for a considerable portion of the journey, this was of little importance. Our total load was as follows :— Sledges, etc. Food and Fuel, etc. Tools, etc. Instruments, etc. Twelve-feet sledge Nine-feet sledge Two instrument boxes ... Iron under-runners Oil tins on platform One tin of spirits Seven weeks’ food Biscuits (four boxes) Ready bag (one week) ie Boxes protecting biscuit Cooker ... Three ice axes Crowbar and shovel Candles ... Lantern ... Alpine rope Bamboos Pe Tent and poles ... Four sleeping-bags Repair bag, etc. ... Theodolite Aneroids, etc. Zeiss camera Six dozen plates... Goerz camera Three dozen plates Box camera and films Polariscope Binoculars Compass, abney, etc. Total, i) 265 Total ... 696 Total’? (;. 1308 ~ ~ Nv Om = uw Total { ag | tube Qn “IED WORM = MA ‘jason wineqssnN = N “pur[s] p[eoH = H yjodag Arg surg = q ‘pray qouxyy = YJ *purysy Aapieg sa = [TC "syooy [BIpaypjwg = O “yooq jo pua ye deur Surpyoy osje vag «= *UMOYsS ‘purysy peaf{ O} JUIOg Jafjng pue duvg aroospy 0} JuIOg sapng ‘shournof preMjnog ‘AAUNYUNOL LSAIA NO CuSadAVAL AYMLNNOOD AO TAdOW at I of 7 “ . 7 coat: ‘te ieee. nl a ; | 1 oh as Poe = a — ar ’ _ FIRST WESTERN EXPEDITION 119 Personal Gear ... Aa Bee 1% bas A ae te ttc) LBS. Totals ... Sledges, etc. oN Se PSS Hood, ete.” ..: son By dicy- fo) A Golayiete! i: uy Habs fe (0) Instruments, etc. ... use fh NOE Personal... a at 50 1040 Several items in this list may be commented on. The heavy steel sledge runners were designed to fit under the wooden runners of the sledge, to take the wear and tear when we were crossing the rough ice of the glaciers. No favour- able occasion for their use arose until half our journey was completed, and then, as will be seen, the trial resulted in the smashing of the large sledge. We also carried the biscuit tins enclosed in their stout wooden cases up and down the Ferrar glacier, with the idea of preserving the biscuits from breakage. The cases were discarded on our return to Butter Point without any inconvenience from broken biscuit result- ing. These two items alone constituted one-tenth of our load, and we were glad when trials showed that we could get along much better without them. It will be noticed that an exceptionally large photographic battery was carried. This was necessitated by the character of the problems which engaged our attention. For instance, Wright was chiefly interested in the forms of ice structure which we encountered. The most delicate ice-crystals, which withered at a breath, must needs be photographed in situ. There was no possibility of his bringing back specimens for study in the hut during the dark winter months. For similar reasons a somewhat bulky polariscope—in which sheets of ice were examined in polarized light—formed part of Wright’s load, and accompanied him in a ruck-sack wherever he went. Debenham was engaged on the more usual work of collecting specimens, mapping their occurrence in the field, and studying the relations of the various rocks. For this purpose another camera was essential, since in general his investigations were carried out in the cliffs at some distance from the rest of us. The subject which primarily interested myself may be popularly 120 WITH SCOTT: THE SILVER LINING described as the bearing of geology on scenery—in other words, “ How has the land surface been affected by the flow of glaciers, by the action of wind, frost, water, and ice ? How do the resulting features differ from those observed in more temperate regions where water plays such an important part and ice erosion is absent ?” During February we obtained nearly a hundred photo- graphs illustrating the typical valleys, glaciers, moraines, and general topography of the western mountains, which it is hoped will help to settle the question, “ How do glaciers erode the deep valleys they occupy?” But early in March our cameras became practically useless, for the cold stiffened the shutters and the snow obliterated the details of the land- scape. I asked Pennell to take some soundings off the glacier mouth, for it has been supposed that glaciers cut their troughs out even below the surface of the sea. Rivers, of course, cannot erode below this level, so that this investigation was of importance in connection with the Ice versus Water Erosion hypotheses. He found only seventy fathoms (420 feet), which bears little resemblance to the glacier-cut fiords of Norway, some 6000 feet below sea-level. There is often so much silt and debris washing down from these valleys, that it may be possible that a deep rock trough has been filled thereby. But I think it improbable for reasons which will appear later. Debenham went off with the eastern party to examine the depdt on Butter Point. Priestley was able to identify many of the articles here as having been left by David on the magnificent magnetic Pole journey. Meanwhile, Wright, Evans, and I got our stores and sledges on to the ice and started packing. Some of the seamen went off to kill a seal, accompanied by our doctor, Levick. The latter was to show them a humane and speedy way of ending the seal. He described the method to us on his return, but the effect was spoilt by the butcher declaring that the seal had travelled a hundred yards after Levick had officially killed it ! Debenham had arranged his northern depét by six o'clock, and then our party put the finishing touches to our two sledges. With the zeal of a new leader, I advised donning wind-proofs as evening drew on ; but experience showed later that they were rarely needed until mid-February ! FIRST WESTERN EXPEDITION 121 I left my trusty “ mousetrap ” camera on board, some one snapping a photo of us just before the start. About 6.30 we pulled off from the ship across the sea ice which separated us from the glacier. The surface was good, and we dragged the sledges about five miles before camping. We headed for the northern side of the glacier. The southern side of the Ferrar was really more direct, but it was cut up into gullies and pinnacles such as made sledging almost impossible. I asked Evans to cook during the first week ; and Deben- ham was cook’s mate, to follow on later. So upon halting Evans took charge of the cooker and proceeded to light the primus, while Wright and I erected the tent overhim. Deben- ham filled the outer cooker with ice and then joined us in piling snow blocks on the flounce of the tent. After seeing that all was secure on the sledges we dived into the tent, and sitting on our rolled-up bags proceeded to change our socks. All of us, except the unfortunate cook, who was too busy mixing pemmican and salt and pepper and thickers—measur- ing out chocolate and cocoa, etc.—to have any time to attend to socks! This was one reason why cooking was not more popular! Our wet socks were hung on a rope slung upon the sledges, and by morning the frozen moisture had evapo- rated (ablated) completely off. However, on this particular evening, while the pemmican was being cooked, Wright and I walked amile or so to the south and reached a lateral “tongue ” or prolongation of the main glacier. There was a sudden rise of some three feet, and the surface, in place of being level and comparatively smooth, was carved out into deep irregular bowls with over- hanging margins, These were in all probability giant “ sun- holes,” and their floors were covered with a most beautiful carpet of snow crystals. Examined closely, each crystal plate was like the segment of a fan strengthened by cross-ribs. These plates were often half an inch across. The whole structure of sunholes, crystals, and hummocking ice reminded me of nothing so much as the appearance of a coral reef, and I suggested the name “ coral-reef surface ” for the type of ice and snow weathering. We returned and found the “hoosh” nearly ready. 1 read the sledging orders which Captain Scott had given me a few days previously. netter of Instruction to Griffith Taylor. Bea. "Terra Nova” aki : pee 26° Iq u Dear Taylor, I ptrpose to disembark a sledge party of which you will have charge oh the sea ice 6f koe Surdo Sound as near the Ferrar Glacier as possibleM Your companions will be Messrs #emssee, Debenhum, Wright and Fetty Officer Evans. You Will have two sledges with food and equipment for 8 weeks. The object of your journey will be the gecologigal exploration of the region betwecn the Dry Valley and the Koettlitz Glacier. Your movenents must depend to gome extent on the breaking of the sea ice. Your best and safest plan aprears to ie ae carry atl Provision up the Ferrar Glacier to a point in the medial moraine abreast of Descent Pass and to make a depot at that point. With e fortnigit's food yon could then continue the ascent to the junction cf the Dry Valley Glacier and descend the valley of that Glacier. On returning to your Depot you will be in a rosition to observe thé extent of the open water and you can either descend the gY¥&cicr anc pass to the East Ln Geb Point or climb Descent Tass descending by the Blue Glacier or by one of the more Southerly foothill glaciers and thus continue the examination of the Koettlitz Glacier area. On completion of your work you shculd cross to Hut Point RS careful not to camp hear the open water. Supplies v0 pet cf provision will be found at-#ut Point ert snoicté—-be-weed seating 138 - = 4 Stems remaining from the And deals Cec ram, Ce formes, trtont Pome Pret Discovery Expedition. I regard it as practically certain . that Cape Evans can be safely reacked over the new sea ice ke before the third week in March provided that the party keeps well within the bays. __ ahe safest course would be t> climt the ridges Nbeyond Castle Rock, te continue on the sea ice’ ~ —— behind Arrival Height,amd descenca to the sea cof to a point one or two miles from the end of Clacier Tongue and from thence to the South side of Cape Evans, Winton Jom Br but~ Gf lure ” Yours sincerely, 124 WITH SCOTT: THE SILVER LINING As usual we found the pemmican too rich at first, and I note that I could only eat three of the biscuits! This delicate appetite did not survive many days of Antarctic sledging. I slept soundly, only waking once at four ; but the thought that I carried the chronometer and was responsible for the punctual rising at 7.30 (6.30 local time) made me uneasy for many ensuing mornings ! We did not expect to return by this route, so that I thought it advisable to investigate the physiography of the lower end of the glacier. After breakfast we all went over to the south side of the valley. Wright was soon busy on hands and knees investigating the beautiful “fan” crystals. Deben- ham and I walked on further to some isolated moraine heaps, which projected about ten feet above the ice. I made a traverse over the glacier as far as the lower slope of the hills with the following results. The moraine heaps seemed to be the outward and visible sign of a large continuous ridge—or sheet—most of which was buried in old ice and snow. The mingling of fine silts and huge boulders, some four feet long, was characteristic of a glacial deposit, and a few doubtful striae were present. Many varieties of rock were represented, granites, recalling the famous “ Shap” of the Lake District ; splendid porphyries with large almond-like felspars in a brown matrix ; gneisses of many varieties with parallel layers of glistening mica and dull black hornblende; and some crystalline limestones and much dolerite; both of which occurred in situ about ten miles further west. These elon- gated silt and boulder ridges showed deep cracks along their sides, indicating, 1 imagine, considerable movement of the glacier which bore them. The next half a mile was rather difficult travelling, through pinnacle ice and through large lately frozen pools of water. Very striking were some of the ice-forms here. ‘“ Topsy- turvy”’ icicles, whose original support had almost melted away—leaving them attached below and surmounted with knobs like hatpins, and unsupported crusts of ice which dropped one into a pool of water, were types that made the most lasting impression. I soon reached the land—a sunny slope facing the noon sun. Here several merry little brooks hurried down over the powdery silt to hide themselves beneath the glacier. To be sure, they were only an inch deep e FIRST WESTERN EXPEDITION 125 and meandered across little channels a couple of feet wide, but they were unusual enough to excite interest. Gradually the silts changed into a pebbly soil, and this into a uniform layer of coarse gravel as I ascended the slope. Larger stones and boulders became common, and one specimen seemed of special interest. It was a fragment of coarse granite some six inches long, with its upper surface weathered to such an extent that every felspar appeared as a separate glistening brick ; yet the moiety of the granite buried in the silt was as smooth as any pebble from the beach. I consider it by no means improbable that this relatively large amount of “ weathering’ had been accomplished while this fragment lay in its present insecure situation, A little higher up the slope I was amazed to see a carpet of green moss, as flourishing as any in more temperate regions. I sat down on a granite erratic, and noted that three types of vegetation were present. One was a veritable moss, to my unbotanical eyes, the ordinary moss of universal distribution. Of the other two species, which may have been algez, one resembled the seaweed called U/va, and the other had a some- what fibrous structure. The patch of green was sixty feet long and about fifteen feet wide, and is possibly the largest area of vegetation south of 774°! I was under the impression that these forms were quite common around MacMurdo Sound, but if I had known that they were inhabited by a most interesting primitive flea, 1 should certainly have added some to our load. However, we obtained thousands of the insects next year at Granite Harbour. On my return I found that Evans had laboriously collected the fragments of a shell, which, pieced together, built up a red scallop. He picked it up on the moraine, where it may have been blown by the wind. We inspanned at noon, and before lunch reached the low ridges marking the junction of the centre of the glacier with the sea ice. Here we obtained fresh water for the cooker, b cutting some three inches through the sea ice. Evidently at this season the sub-glacial drainage overpowered the sea-water at this spot, which was eight or nine miles from the open sea. To the north of this was that remarkable “ Double Curtain” glacier, which is photographed in the Discovery volume. After lunch Wright and I decided to walk in that 126 WITH SCOTT: THE SILVER LINING direction, and we soon saw we should be justified in devoting some hours to its examination ; while Debenham came along later and collected the varied rocks in the vicinity. As we approached the northern slopes the surface of the Ferrar Glacier altered in character, and gave place to large lake-like areas of ice, which exhibited most beautiful figures on close examination. In the upper layers of the ice were included radiating designs which resembled a miniature Hampton Court maze in porcelain embedded in glass. These intricate patterns—which are characteristic of glacier ice—I termed “ Arabesques.” They are due, I imagine, to some variation in the solidifying water, perhaps owing to air being squeezed into the latest ice formed—or again show where stones have sunk deep into the glacier. Somewhat nearer the shore there were more unpleasant surfaces met with—large dome-covered ponds into which we fell at frequent intervals. We decided that a tramp over the Crystal Palace would give rise to the same sensations. Bounding the glacier and separated from the debris slopes by a wide stream was an avenue or colonnade of gigantic ice pinnacles thirty feet high. These were traversed by narrow crevasses, down one of which I had to climb to rescue an ice axe. The sun glistening on the icy minarets and beautiful icicles made a most impressive sight. This ice ridge is due to pressure from the glacier piling the ice against the cliff higher up. This crenellated selvage to the more level central level centre of the glacier—moves to the sea with the main body, and so preserves its lateral position, though no pressure can exist where we saw it—for it is many yards from the rock. Between the pinnacle ridge and the slopes was the water- bearing channel which invariably accompanies a large glacier in these regions. This physiographic feature is one of the most interesting and most important in connection with the char- acteristic topography of Antarctic valleys. The small valley bounded by ice on one side and rock on the other is conveniently termed the Lateral moat. Hereabouts it was rather complex, but further up the main glaciers its valley occupied merely a simple V. After crossing the pinnacles we had to negotiate a stream in which the water lay in pools several feet deep—though its flow was comparatively small. Then over a silt moraine and so across another slight MY FIRST CAMP IN ANTARCTICA AT THE SNOUT OF THE FERRAR GLACIER. Over a mile away is the Double Curtain Cliff Glacier. The Kukri Hills are 3000 feet high. The Snout is only ten feet above the sea-ice on which is the tent. The socks are hung out to dry on the sledge. Griffith Taft Wright. Debenham. Taylor. Evans. PHOTO TAKEN JUST BEFORE WE PACKED THE SLEDGES FOR THE FIRST SLEDGE JOURNEY, Jan. 27, 1911. Note the biscuits in the four venesta cases. ‘The men are wearing windproof blouses. [See p. 120. FIRST WESTERN EXPEDITION 127 ’ depression to the talus slopes below the ‘‘ Double Curtain’ tributary glaciers. It seemed a simple matter at first to investigate the glacier front, but it lay much further up the slope than I had imagined, and was moreover protected by an icy mantle of frozen thaw-water which surrounded the snout. Wright cut steps across this “ mantle,” and found that the almost vertical face of the glacier was forty feet high, and composed of layers of snow which had only lately reached the condition of ice. Meanwhile I climbed up the steep rock slopes alongside the glacier. At first the rocky debris was a confused jumble of granites, dolerites, and basalt, with occasional limestones and gneisses. At 2500 feet elevation I reached the top of the slope and stood on the great shoulder which characterizes the Kukri Hills hereabouts. Here solid rock was plentiful—the same gray granite traversed by long dykes of dark basic rock. A wonderful panorama was spread out before me. I could see up the Ferrar Glacier as far as Knob Head. To the south- west jutted out the three giant gables—like the roof of a Gothic cathedral—which were so appropriately named Cathedral Rocks. I was much interested in my first view of Descent Pass, by which we proposed to reach the Koettlitz Glacier. Still further to the south-west the spurless wall of the Ferrar was notched by the “Overflow.” The latter appeared to spill out through a gloomy curving gorge which indisputably showed evidence of water erosion. In the far west towered the massive Royal Society Range, culminating in Mt. Lister. Its eastern face was carved into rounded “armchair” valleys (cwms) and deep razor-back ridges—another type of topo- graphy which has been recognized in temperate regions as characteristic of glacial erosion. On descending to the main glacier I found that the others had collected several small sponges and shells from the small silt moraine in the lateral moat. These organic remains are puzzling, for it is difficult to imagine that such light and fragile specimens indicate a sea-beach, which could only have raised so many feet above the sea at some far distant period. Objects of greater biological interest had been encountered on our walk to the side of the glacier. In the rough ice we saw many Emperor Penguins, stolidly motionless and 128 WITH SCOTT: THE SILVER LINING obviously awaiting the end of their moulting season. We crossed over towards them and found that there were several flocks, probably totalling one hundred. In the nearest group were thirty-six individuals, only one of which had completed moulting. He was singled out for sacrifice and fel] by a blow on the neck. Evans and I dragged him to our camp, where I skinned and cleaned the carcase in preparation for a change of diet if our appetite failed on apemmican regime. The limbs I hacked off with my new bowie knife, and I was chagrined to find that penguin bones can chip the best Sheffield blade ! Already my boots began to give trouble. The soft leather sole would not hold the short nails, which only were available on the Terra Nova, so that I attempted to mend matters by driving in some Canadian lumber spikes supplied by Wright. After Wright had taken another round of angles with the theodolite we moved on up the Ferrar Glacier. The surface degenerated rapidly. The flatter portions were sun-carved into serried ranks of projections like plough-shares, and we used the term ‘‘Plough-share Ice” to describe this feature. Although this was unpleasant to walk on, yet the sledges travelled over it readily—for as a general rule bad walking meant easy pulling, and vice versa. But great holes, two or three feet deep, were cut out below the general level, and these were closer together as we moved further west. They were crusted with fan crystals, and indeed represented a stage of surface evolution which I have described as “coral reef structure.” We had much difficulty in guiding the sledges, and they capsized several times before lunch. Every now and again the sledge runners would jam, sending a jar through one’s frame, so that this unpleasant experience became known —quite naturally—as a “ jam-jar.” Towards evening we approached the first series of pressure rolls. Crossing diagonally (from south to north) were four frozen rivers which formed tempting surfaces, but unfortu- nately in the wrong direction, for they led to the broken ice of the Overflow. We camped in an undulation filled deeply with hard snow, a little below a fine tributary glacier and nearly opposite the Overflow. FIRST WESTERN EXPEDITION 129 On the 30th we started up some steep undulations. We had anticipated easy going, for Evans, on his 1902 journeys, had always encountered clear smooth ice here. But the ice was buried under a foot of snow and only showed in oc- casional holes. I made brief notes of the surfaces throughout the day, at our various halts, and they are characteristic of glacier sledging and so are here reproduced. “ First Halt, Heavy going up the undulations ; three of them traversed already ; the surface is smooth but the runners stick to the snow. “Second Halt. We have crossed the head of quite a deep snow-covered valley crossing the glacier,—on both sides were numerous crevasses, but they were not wide, the largest being under three feet. I slipped in twice, and Evans and Wright had similar mishaps (in no case, however, did both feet go in). Definite snow bridges over crevasses. We halted at a dead seal, obviously a young specimen and yellowish in colour. “ Third Halt. We can see a good lateral moraine at the foot of the cliffs, for we are gradually rising up a steep slope with a bad surface. Only a few narrow cracks. “ Fourth Halt. Still on the same slope, which is hard going and causes much sweat, chiefly owing to our rather heavy loads, as the slope is only three degrees. “ Fifth Stage. Same surfaces ; stopped for lunch, having done 3600 paces in three-quarters of an hour (fide pedometer). “Sixth Stage. ‘The surface became less damnable and we did a mile in which short patches of ice appeared under one inch of powdery snow. Some ‘glass-roof’ ice is appearing into which we fall, and the snow is still one foot thick in many places. “ Seventh Stage (5 p.m.). Weare reaching plough-share ice. “ Eighth Stage. Snow is falling on the northern slopes, but does not reach down to our level. “ Ninth Stage. Much better surface, nearly all ice, though the snow has powdered it to a greyish colour. “Tenth Stage. ‘ Arabesques’ are showing in the clear ice underfoot, they seem to mark fairly old solid ice and indicate good travelling. “Eleventh Stage (8 p.m.). Crossing the glacier to Cathe- i aon ; surface good, but the moraine seems a long way ahead. K 130 WITH SCOTT: THE SILVER LINING “ Twelfth Stage (9 p.m.). Stopped near the big moraine after heavy pulling over two inches of soft snow. Camped on big patch of hard snow by a huge boulder.” We spent the forenoon making our depét at this camp. It lay four miles north-west of Descent Pass, and would be on our route if we decided to return to the sea by the Pass. We left here what we did not require during our fortnight in the Dry Valley region. We piled three biscuit boxes on the smaller sledge, and packed the smaller provision bags under the sledge. We put the butter inside the instrument-box with the spare photographic plates. Also I decided to leave the heavy steel under-runners, for so far we had met with no rough ice. The penguin had been lashed on behind the sledge and had suffered considerably from the capsizes! Him we buried under some blocks of snow, pending a “ hoosh” on our return. We took a fortnight’s provisions in addition to the “ready-bag,” and I tied a note to our depét flag, mentioning the 11th as the probable date of our return. Just to the west of the main Cathedral Rocks was a very interesting tributary valley—the first real low-level tributary of which we had had a good view. Obviously owing to some difference in the snow-supply, this tributary is keeping pace with the main glacier, and enters the latter “at grade.” The majority of the other tributaries have not entered the Ferrar on a level (at grade) since it was two thousand feet thicker. The sun was quite powerful, and we had to wear goggles in consequence, but during our ensuing stay in Dry Valley there was so much bare rock that we had no need for them. At lunch my unlucky boots fell to pieces again, and Evans put some scientific sewing into them. But no sewing held, until continual frost turned the leather into a material almost as strong as steel. Towards six o’clock we reached the top of the steeper portion of the Ferrar Glacier, and found ourselves on a small ice plateau about 3200 feet above sea-level. On the south it rose to the south arm, while to the north was the entrance to Dry Valley. The col of ice leading in this direction is of considerable interest, for it shows what conditions were like near Luzern in the Great Ice Age. However, I will describe this form of “ Twin Glacier” in a later paragraph. A few miles before we camped we were hauling the sledge FIRST WESTERN EXPEDITION 131 along the foot of the grandest geological section I have ever seen. The cliff was 3300 feet high (as determined by Abney level), and was divided into so many distinct layers that it resembled a gigantic sandwich! It was capped by a little triangle of yellowish rock, which represents the most eastern exposure of the Beacon Sandstone in the valley. Beneath this were two wonderful “sills,” or horizontal sheets of the basic lava called dolerite. They could be traced in the cliffs for miles and miles, and represented flows of lava wedged in between the granites and sandstones. These dolerite sills were strongly columnar, and near by some isolated pillars of enormous size were visible on the sky-line. Above and below the lower of these black sills were layers of grey granite, and

Looking Wesk up te Dry Valles below Tayler Glacier, WITH SCOTT: THE SILVER LINING where we were about 300 feet up, and so moved east down the other slope. We reached another lake nearly a mile long with a splendid gravelly shore, on which I decided to pitch the tent. We had brought no floor- cloth ; but after the wet and icy floor in the “alcove” we found the warm gravel most comfortable. We had a frugal meal of biscuit, butter, and cold water. Our beverage from the lake was distinctly medicinal, and as the latter had no outlet we called it Lake Chad. I was distinctly troubled over the topography of the day’s march. We had left a huge open valley—a suit- able outlet for a large flow of ice like the Taylor Glacier —and had arrived at a narrow defile completely blocked by the tributary Suess Glacier. We reckoned we must be near the sea; but where was the large open moraine-strewn valley described by Professor David in 1908? 1 won- dered if we had got into an unimportant tributary and missed the main outlet of the valley altogether! So after dinner Evans and I made straight for the top of the ridge (immediately south FIRST WESTERN EXPEDITION 143 of the tent) which seemed to block the great valley. It was a stiff ascent of 1600 feet over rough blocks of slate. There we reached a flat, bare ridge with a further ascent to 3000 feet a little further west. To my surprise I saw that imme- diately to the south was a broad high-level valley gradually sloping to the east. I thought at first I was looking into the Ferrar Glacier, but soon saw that here in Antarctica was an example of the extraordinary valleys which are so characteristic of the Italian Alps. As shown by the cross-section, the dry valley is barred by a huge Riegel, which is traversed by a deep defile at the north, and scooped out to some extent into a huge elevated, rounded channel on the south. From this ridge, above the mile-long defile, Evans and I at last saw the sea gleaming in the east across some twelve miles of moraine- strewn valley. On the sth, Wright and Debenham remained near the camp, while Evans and I marched down to the sea to tie the survey on to Ross Island—if we could recognize any portion of that far-distant feature. We each carried much gear, and the annexed rough sketch shows how a geologist is loaded when “ on trek.” It was extraordinary to find two more very large tributary glaciers on the south side of the valley—reaching some way into the ice-free main valley, and blocking up the main drain- age to form a series of lakes. We named the first the Canada Glacier, and Wright later on clustered the names of various Canadian men of science on the adjoining peaks. The second we called the Commonwealth Glacier ; and to the small glacier which we ultimately reached, on the north-east end of the Kukri Range, I gave the name of Wales Glacier, so that our party’s homelands are well represented in Dry Valley! We had to climb 400 feet up the slopes here before we could see any- thing definite to the east ; but then I was able to sight the theodolite on to Mount Bird, Cape Bird, and Beaufort Island. It was a long and rough tramp back—across numerous little streams, running as usual to the north-east,—but we reached camp again at 9 p.m. and turned in thankfully. After a somewhat dry breakfast, Wright and I took the theodolite up to the top of the Riegel. We climbed some 2400 feet, but did not reach the top of Mount Nussbaum— the central summit,—which I estimated at 3000 feet high. 144 WITH SCOTT: THE SILVER LINING When we reached the scarp facing up the valley to the west the wind was tempestuous, so that we could not stand against it, much less use the theodolite. We sheltered under the lee of some projecting dykes of dark rock for some little time. There came a lull, and almost before we got the theodolite ready the gale had veered to the east—diametrically opposite on $5 The Grpleat Expleve/ 8-2-0 —and continued to blow almost as fiercely from that quarter. This violent storm would have been unsupportable on the Barrier, but the party in our camp below practically felt none of it. Our apparent fine weather was due less to absence of wind than to the absence of loose snow, and to the abundance of shelter. I tramped to the south and found that the “‘ Round Valley” FIRST WESTERN EXPEDITION 145 ended in a 1700 foot scarp above the trough containing Lake Bonney. There was little wonder that we had not realized on our seaward tramp, vid the defile, that such a high-level valley existed. This elevated ridge was comparatively free from debris, but there were huge erratics of granite with large felspar crystals three inches across. They were wonderfully scooped out by the wind, and were nearly twenty feet across in some cases. We also found small kenyte erratics containing large felspar crystals. These may have been carried across from Mount Erebus, or some unknown locality in the south. After supper I took the prospect- ing dish (which was the last article purchased in New Zealand) and washed for gold in the gravels along- “Anorthoclase” _felspar, side the lake. There were numerous thrown out of Erebus, quartz ‘“‘leads” in the slates and AS ies ea SO nee metamorphic gneisses, and eruptive in kenyte. rocks and limestone were in the vicinity. This is a juxtaposition which is always promising, and furnishes the “country rock”’ of most gold fields. But the quartz was too glistening and pure. It had not the “kindly” rusty appearance which the gold-seeker admires, and so I was not very sanguine. However, water was abun- dant in Lake Chad and I washed out many pans of dirt. The “tails” of heavy sand were not promising, even pyrites and magnetite being almost absent. We knew there would be no water available on the remainder of our journey, so I depdted the “ pan” on a boulder by Lake Chad, where some future archeologist will discover striking evidence for the lost kingdom of Sheba ! Next day we started back to Alcove Camp, buoyed by the thought of hot pemmican after nearly a week’s cold “ tucker.” We lunched just at the east end of Lake Bonney on our old site below the peak of the Matterhorn. The latter is the most striking mountain in the region. The conical summit (formed of black dolerite columns) perched on a broader i 146 WITH SCOTT: THE SILVER LINING granite base, certainly gives it a resemblance to its forerunner in the Alps. We estimated it to be gooo feet high. Luckily we took careful angles which we worked out later in the hut. To our chagrin all observations resulted in a poor 5000! Such is the effect of lack of trees or any standard of com- parison in Antarctic scenery. Continuing west we found that the penguins seemed to have the same queer habits as the seals, for we found a skeleton some fourteen miles from the sea. We reached Alcove Camp about 5 p.m. and saw that our camp site was ruined by thaw water. We hunted around for a new floor, and the only available one seemed to be a pile of moraine rubble just like a heap of road metal! This we levelled off, and when the ice had melted away in the sun, we pitched our tent upon this stony bed. Then we had a hot meal, much appreciated after our days of cold food. We were up at 7.20, Greenwich time (really 6.20, local) and shifted our gear from the heap of road-metal to the surface of the glacier. We had a good breakfast, though I noted that twelve lumps of sugar did not seem to sweeten the cocoa. It was difficult to move the sledge, for the dark straps had sunk two inches deep in the hard ice and there frozen in again. We managed to get everything ready by IO a.m., and moved up the glacier. It was very sunny, and Evans wore a huge “ Madeira”’ straw hat, quite a yard across —a queer but useful article that his previous experience had led him to add to his kit. We had lunch about six miles up the glacier in the medial moraine. I took careful notes of the latter, which differed conspicuously from those of temperate glaciers. It consisted of huge blocks of granite with smaller pieces of dolerite and sandstone. They were often 100 feet apart, so that this moraine compared with Swiss examples was a very “ tenuous thread.’’ Comparatively little material can be supplied to these slow moving or stagnant glaciers, and all the small stones have undoubtedly sunk into the ice long ago. The upper portion of the Kukri Hills hereabouts showed by the fragments of the Beacon Sandstone torn off by the intrusive eruptive rock dolerite that the latter was newer. The relative ages of the other rocks could be deduced in the same way. For instance, the dolerite sent “dykes ’’ into the FIRST WESTERN EXPEDITION 147 granite, so that the latter was older. These points are well shown in the section I sketched. Near the Solitary Rocks the glacier was moulded into a gigantic furrow or longitudinal undulation. We followed this up toward the ice-falls from the upper glacier and camped for the night on a small patch of snow in the lee of some large boulders of the medial moraine. These boulders had lee- ridges of snow, which, we were interested to see,-were gene- rally turned into solid ice and formed part of the glacier itself. This shows that nothing but a maturing process (resembling that of wine !) is necessary to convert snow into glacier ice. << Ih; hi) Ij Hl m Rte ic it “sin Hf fk Vali im a hi i I | ieee ! TA i { i } | | 4 Pi ty Ua ys ba PROT CR nt At IL Ari ve oh nue Wy aM: Seal Hy 1. HY Ny il } | nil || oA) uf baa Ty" iyi ate d "hy ‘ i 57k a ae Glacier . ~ a ¢ is Se: ee ( The age of rocks. ‘The granite (Gr.) is the oldest; it is penetrated by flat sheets of dolerite (D) at the junction with the main mass of the latter. The beacon sandstone (B.S.) has also been torn up and surrounded by the dolorite (below A and B), and has probably been lifted up by the lava (to B.S.). The talus (Ta) of loose rock is the latest deposit. From a sketch of the new end of the Kukri Hills made February 1, 1911. Wright and I went over to the Kukri Hills while the others pitched camp. I wished ‘to measure the “lateral moat.” Near the edge of the glacier there was a thick coating of snow. At the actual edge there was a sharp curve down- ward, and carefully peering over we could see that there was a frozen stream at the bottom of the gully, over 150 feet below us. I determined to measure the slope and angle accurately, and for this we had brought the alpine rope and ice axes. Wright lowered me over the edge, which I found was a snow cornice projecting over six feet. Under the 148 WITH SCOTT: THE SILVER LINING cornice was a well-defined platform a few feet wide—which, however, narrowed on either side—and then came a long slope to the bottom. Wright paid out the rope, and I let myself down to its end. There I started to cut steps, but un- fortunately slipped and fell the last thirty feet—luckily without damage except to my knuckles. I can remember thinking that an ice-axe was an uncomfortable companion in this roll down the slope and so threw it away for fear lest it should claim close acquaintance with my person. The stream was over a hundred feet wide, and then I reached the foot of a steep rocky slope formed of dolerite blocks fallen from a bold crag a few hundred feet up. I climbed up the glacier side again, and then found that the large snow-shawls of the cornice prevented my getting back—for as Wright hoisted me the rope merely cut deep into the snow and soon my head was pulled into the lower parts of the huge cornice! I crawled along under the cornice, devoutly trusting it would not avalanche on me, but ulti- mately had to retrace my steps down to the stream. Again I slipped, and this time lost the skin off my other hand as I rolled once more into the moat. Luckily some few hundred yards north I saw a place where the cornice had fallen off, and here I was pulled up by Wright with such vigour that the ice-axe entered my leg ! The huge cross-section of these “moats” is worthy of note. They definitely prove that no /asera/ erosion of any importance is occurring in this portion of Antarctica. After returning to the tent the glacier treated us to rounds of volley-firing! These were due to the opening of contraction cracks as the ice shrank in the colder night temperatures. Wright and Evans spent the morning of the gth over near the ice falls from the upper glacier. These we named after the famous Cavendish laboratory in Cambridge. They had to cross a surface compounded of “ plough-shares”” and “thumb-marks,” which they found intensely slippery, so that even surefooted Evans fell and nearly broke his elbow. Debenham and I cracked sandstone boulders, but found nought of interest save worm burrows in some shaly bands. However, these indicate damp conditions for some portions of the Beacon Sandstone, and so show that the latter is not perhaps of desert origin. ? FIRST WESTERN EXPEDITION 149 The most extraordinary feature in this small ice plateau near Knob Head Mountain is that the moraines here lead down into Taylor Glacier. Hence they cut right across the upper portion of glacier above Cavendish Falls, and show that the ice west of the latter is almost wholly flowing into the Dry Valley region and not into the lower Ferrar, as was supposed. This looks as if the “South Arm” and the glacier from the north side of Mount Lister formed the main supply of the Lowerzer See oo NS Plan of the bygone ‘win glaciers of Lake Luzern, whose overflow led to the break through the high range near Vitznau. A close parallel with the conditions near Knob Head between the Ferrar and Taylor Glaciers. Lower Ferrar, while the northern portion (vée Upper Ferrar and Dry Valley) is a distinct glacier now temporarily united with it after the fashion of the Siamese twins. This type of union is by no means unknown, and indeed explains the structure of Lake Luzern—that beautiful high-cragged chain of lake basins in central Switzerland. Here also two inde- pendent glaciers (the Reuss and the Aar) cut out deep parallel gorges as they moved to the north. They spread out laterally, and ultimately the Reuss Glacier overflowed to the west, and cut through the high ridge forming the picturesque cliffs of the Rigi and opposite shores. 150 WITH SCOTT: THE SILVER LINING As I have explained elsewhere (p. 280), when, after our return, I described this interesting parallel between Lake Luzern and the “opposed” glaciers at Knob Head, Captain Scott was good enough to honour me by naming the northern “twin ’’ the Taylor Glacier. That evening we camped near the ice divide between the glaciers. We had intended to ascend the South Arm, but after making our way in that direction for some time, we saw that a snowstorm was brewing, and so turned towards the Kukri Hills. They seemed to me less than a mile distant, but knowing the difficulty of judging distances, I suggested we should camp under the slopes, “about a mile and a half on.” Wright, with his Canadian experience, thought this would be well over two miles, and I remember the distance turned out to be three miles! Thereafter I calculated apparent distances with great care, and when convinced I had allowed for everything I would use a “ factor of safety” of 3—-and come out about right ! Debenham finished cooking, and being already an adept, had very properly saved some “ thickers”’ for his final “ flutter ” at breakfast. So Wright started with the evening meal. He imparted a scientific and physical aspect to the operation by suggesting a “drop test” to estimate the viscosity of the pemmican ; an observation of its meniscus (or curved surface) to see its sticking power; notes on colour and taste ; and— added one of his hungry audience—“I suggest 50 per cent. be subtracted from the cook’s allowance on account of rits !” " Perhaps as a result I had a dream in which my astral self did some logical reasoning! It is a fact that the fossils called trilobites gradually become more supple and less clumsily built as one traces them through newer formations, It occurred to me in the dream that this also held true for man and his monkey ancestors, and that the stiff, clumsy orang-outang, etc., developed into the limber human acrobat. Not a very epoch- making correlation, but the best my astral self has accom- plished to date ! On the evening of the roth we reached our depédt at Cathedral Rocks. We could see our flag from five miles off with the glasses. On arrival we found the food uncovered, so that the sun had melted the pemmican and butter. The skua a FIRST WESTERN EXPEDITION 151 gulls had found the carcase of the Emperor, and our chance of a variation of the menu had departed with the skuas. That evening we discussed literature. Seaman Evans had read many popular works, and was far superior in this respect to any of the other seamen with whom I had much to do. He had read some of Kipling’s poems, and “had no use for them,” nor did Dickens appeal to him. As was perhaps natural, he preferred books with more “ plot’’ in them ; espe- cially did he delight in the works of the French writer whose name he anglicized as Dum—ass ! Our sledging library was quite extensive, for each of us had devoted a pound of our personal allowance to books. I will give the catalogue, if only as a caution to later explorers. Debenham took my Browning and the “ Autocrat’’; Evans had a William le Queux and the Red Magazine; Wright had two mathematical books, both in German ; I took Debenham’s Tennyson and three small German books. The Red Magazine, the “ Autocrat,” and Browning were most often read ; Evans’ contribution being an easy winner. Somehow we didn’t hanker after German. On the 11th Wright and Debenham carried out a very important operation to determine the movement of the Ferrar Glacier. They fixed stakes right across the glacier which were aligned on two prominent peaks. Some six months later Captain Scott re-measured this line, and found that very con- siderable movement, amounting to thirty feet, had taken place during the winter. Meanwhile P.O. Evans and I prospected for a route up the steep snow slope of Descent Pass. Evans had been with Armitage when he used this route in 1903. We found the conditions very different. Soon we were sinking nearly two feet at every step in soft snow, through which I knew it would be almost impossible to drag the sledges. The slope soon increased to 11°, so that we found some difficulty in progressing even unencumbered. There I first made the acquaintance of the “‘ Barrier Shudder.” Every now and then a shiver would shake the surface, and we could hear the eerie wave of sound expanding like a ripple all around. Sometimes one could see the whole snow surface sinking slightly, and at first the effect was very unpleasant. We had been roped for two miles and were still ascending. 152 WITH SCOTT: THE SILVER LINING We now began to get among crevasses, though few were visible through the thick sheet of snow. Quite suddenly I slipped in to the thigh, and sounding with the ice-axe just in front found two inches of snow over the crevasse and very little more behind me, I was evidently standing in a narrow bridge. At the same time Evans called out that he was over another about fifteen feet behind, so that for a few moments things were rather involved. He got back on to firmer ground and hauled me back, and when we saw the surface begin to cave in bodily we decided, in Evans’ graphic language, to “give it a miss.” We seemed to be in the least impossible part of the pass, and I could see plenty worse ahead. So I decided to abandon this route and continue down the Ferrar to Butter Point, and so reach the Koettlitz Glacier vid the Piedmont Glacier. During our absence Wright had also slipped into a cre- vasse while fixing the stake nearest Cathedral Rocks. We inspanned after lunch, and moved down the glacier to our old camp at the mouth of the Ferrar. The morning of February 13 was bright and clear. We could see no change in the sea-ice filling New Harbour where we had crossed it a fortnight before. 1 therefore headed south-east towards Butter Point. Here we had an experience that might have ended our journey prematurely. We got along at a good rate for two miles, when Evans drew my attention to something black sticking up in the ice just ahead. We had noticed an unusual creaking sound, which I put down to ice crystals falling, but this strange object demanded investigation. I ran forward a little, and the black spike was obviously the back fin of a killer whale. The creaking was really a warning that the bay ice was on the move. Meanwhile the ice I was on moved off with a jolt, a mark of attention from the killer which we did not appreciate. However, I jumped the three-foot crack which resulted, and we hastened to the fixed ice nearly two miles south. It was a case of “ festina lente.” We could not drag the heavy sledges more than two miles an hour, and were continually crossing cracks where the oozy snow and creaking showed how insecure was our passage. Soon after we reached the Butter Point piedmont the whole bay ice moved off in great floes to the FIRST WESTERN EXPEDITION 153 northward, so that seven miles of it had broken away since the ship landed us. It is quite impossible to tell whether sea-ice is solid or not, for the first cracks are so small and the eleva- tion of the eye so little that the only safe way to traverse sea-ice in late summer is to keep off it ! We expected to find the Butter Point piedmont an easy level surface, but of its kind it was the worst I met with down south. All the afternoon we were plugging up an interminable snow slope. Just as one got one’s foot braced to draw the sledges through the clinging snow, it would break through a crust and sink nearly to the knee. Then we would meet a few yards of firmer surface and bet whether we could make a dozen steps before the soft “ mullock” started again. Even worse was the jar when you expected deep snow and found a firm crust one inch below the surface. I carried a pedometer, and when we had done 27,500 of these paces I felt we had earned our supper. Blue Glacier now confronted us. P.O. Evans and I pros- pected across the snout, and were glad to find that though it showed crevasses in places, yet it was so free from snow that we should have no great difficulty in crossing them. They curved round parallel to the coast, and, of course, lay along the line of our march, so that we came on to them end-on and fell in several times. But by the evening of the 15th we were safely camped in the rugged ice south of the crevassed portion. Evans as usual enlivened us with navy yarns. He illustrated the kindness of the sailorman by a story of a mate of his who started a poultry-farm. To Jack’s disgust the ducks in his yard had no belief in altruism and with their broad bills gave the hens no chance. “So,” said Taff Evans, “‘evenchooly he gets a file and trims their bills like the hens, and then everything went all sprowsy !” If any one had asked us what we should like sent post haste from civilization, there would have been a unanimous yell of “Boots!” The rough scrambling over the rocks and jagged ice of the past fortnight, and the alternate soaking and freezing they had experienced, had ruined mine completely. Deep constrictions formed in the leather across the toe and behind the ankle and raised great blisters, and even boils in Debenham’s case. I had no sole on the right foot, but within the next day or so the temperature fell considerably 154 WITH SCOTT: THE SILVER LINING and the thin leather lining froze as hard as steel and so pro- tected my foot. For days a loose boot-nail which had acci- dentally been pressed sideways into the sole when it was wet clung like a leech ! . Each morning we had a painful ceremony when it was necessary to don our frozen boots. Remarks more fervid “Wm Wair. Sock frozen fight Wrighhs & Ae ah en Taylor's ConslFicfion 8 gE ee ~ - e Jhe Morphology of frozen Ski - books. IS 201 than polite flew about the tent, and some of us found that quotations from the poet philosopher lubricated the process. “. . . Gritstone,—gritstone a-crumble : Clammy squares that sweat, as if the corpse they keep Were oozing through ” was supposed to be a very potent incantation. We carried no blacking, but this ceremony was called ‘‘ Browning the Boots.” Open water washed the face of the Blue Glacier. Black snaky heads—reminding me of prehistoric plesiosaurs—could be seen darting about amid the brash ice. They were Emperor penguins, which swim with their bodies submerged. To the south of us stretched the sea ice, which was evi- dently rotten and ready to move north. Beyond the Blue Glacier on the right stretched a broad fringe of moraine which extended fairly continuously along the north side of the Koettlitz Glacier. Immediately ahead of us was a fifty-foot ice cliff, but some distance to the south we found a lower place and managed with the Alpine rope to lower the sledges down to the sea ice. We crossed the “ pressure ice ”—where great cakes had been up-ended to form a frozen rampart—and reached a good sledging surface at last. Near by was a great pool of water containing many seals, where jostling ice pan- cakes were surging about, so there was obviously no time to FIRST WESTERN EXPEDITION 155 lose. We pushed gaily south and camped that night in a little gravelly dell among the moraines. This crater-like dell was occupied by a frozen lakelet of greenish ice, the colour being due to alge. On the slope above the lake was a blanket of alga forming a sort of peaty layer an inch thick. The latter was apparently im situ, for it extended uniformly for about ten feet. This occurrence of peat points to an ele- vated old lake bottom, and we saw similar examples later on our journey. Even in Antarctica at present we see that con- siderable organic material is deposited, which might form a thin coaly layer in succeeding ages under suitable conditions. Indeed, the kerosene shale deposits of Australia are supposed to originate in some lowly plant-form like these alge. February 17, 1911.—We had a calm, clear night, and all slept very well on the soft sand of the moraine crater. Just to northward was a little bay filled with pancake-ice having two- feet motion. We made south across little bays over a very good surface, which was intersected by cross-channels of clear ice. Seals were very numerous along this coast. We counted one group of thirty. We could now see the first of the Ice Slabs (described in 1902), which seemed in its lower portion to run parallel to the coast. Wright espied some white material in the moraines, and we walked across to see this. It turned out to be a huge deposit of Mirabilite (sodium sulphate), about ten feet across and fifty feet long. It was granular in texture, and the dip of the bed was quite high. The Mirabilite was originally a level deposit in a saline lake, so that, just as in the case of the alge, we have evidence of strong upheaval of the moraine silts, since they experienced a long-continued phase of equilibrium. The granular mass was not unlike rock-salt in appearance. We proceeded south and crossed the mouth of the large bay marked on the Discovery map. We halted off the southern headland for lunch. I had a small adventure which might have been serious. On outspanning—which consisted in freeing one’s harness from the sledge—I walked over to look at a seal which had crawled about a hundred feet from the tide crack. He shook his head angrily at me, so that I made a loop on my harness—still attached to my belt—and lassoed him with unexpected ease. 156 WITH SCOTT: THE SILVER LINING The seal bolted for the tide crack—and for a short distance they can “lollop along”’ fairly rapidly. It was amusing, at first, being pulled by an angry seal; but it suddenly struck me, “ What will happen when the brute dives into the pool ?”’ I could not get the loop off his neck, and had as much chance of stopping him as a railway train. I experienced some anxious moments before I managed to get ahead of him and jerk off the lasso, for it was impossible to slip out of the broad waistbelt in time. This adventure furnished considerable amusement to my unfeeling comrades, and became the subject of one of Wilson’s sketches in the South Polar Times. After lunch we took a round of sights from this low head- land. It was composed of moraine heaps with numerous circular sheets of water, which reminded one most strongly of crater lakes. On descending from the cape, Debenham found that the steep little cliff near the tide crack was formed of ice covered with a mere veneer of moraine silt. Probably a large portion of the promontory was ice, and we saw other examples of this pseudo-moraine further up the Koettlitz. As Deben- ham suggested, the crater lakes were due, in all probability, to the melting of the foundation ice. Probably the sun’s rays acting on the silt in a shallow pool have a powerful effect in deepening the lake when it is once initiated. The drainage of such a lake presents some difficulties, for though there was usually an apparent outlet, many were quite enclosed by a circular wall of debris. Steps of silt, appearing as small terraces, were common among the heaps. These probably represent crevasses in the underlying ice, and we actually saw several such crevasses in the ice exposure noted above. Per- haps these crevasses account for the (hidden) drainage, for ablation could not empty many of the lakes. The whole question of the origin of these unusual lakes is of great physiographic interest. We could see fairly rough ice ahead, but hoped to be able to get the two sledges several miles further before depéting one during our work on the Koettlitz. We proceeded somewhat to the east over blue ice. This soon became rippled and degenerated rapidly into a fearful “ olass-house”’ and “ bottle-glass” surface. We started to fall through the ice into hidden channels, and in some cases there was a foot of fresh water awaiting us. Things got FIRST WESTERN EXPEDITION 157 worse and worse. We wriggled round ice “ mesas” with vertical walls, over huge curved platforms which threw us all together in the centre and then dropped beneath us. We thought it might be better nearer the land, but at last had to lower the sledge down two feet to the lower level, which was silt covered and all the harder to sledge on for that reason. The “ mesas”’ showed three layers. A flat cake of solid ice on top, then a few inches of very much weathered ice, and below a solid pedestal about three feet high. We hoisted the bamboo and flag and spread out to prospect. The ice became worse towards the coast, but Wright reported some- what better going towards the centre of the gulf. However, it was obviously unwise to drag our unnecessary sledge further, so we turned in our tracks and crossing many “ glass- houses” (into most of which we fell, though with little damage) we made for the headland where we had lunched. It began to snow and looked very threatening around Mount Discovery, There was an ugly luminous patch in the sky to the south-west, and a heavy snow cloud with a very ragged edge. On Erebus alone was a red-gold ray of sunshine. From these portents Evans prophesied a blizzard. We reached land without undue difficulty and crossed the pressure ice, pitching our tent in a dell not unlike our last camp, though it was flatter and more exposed to the east. We carried the smaller sledge well inland, but left the large sledge below on the sea ice, for we should have had to manceuvre it round an open channel, and we did not need it for laying our depét here. This channel along the coast was about twenty feet across with a five-knot current in it, which was flowing strongly north. Seals swam up it quite frequently, and often used to halt and observe the strange visitors alongside. While the pemmican was cooking I went on to the ice and killed a seal and extracted his liver. This camp marked the end of the third week. We celebrated it by eating a pound of mixed chocolates. Wily Evans led us to believe that Ae was the donor; but as a matter of fact, each sledge had a box of them packed in for birthdays and feastdays. The snow stopped about 8 p.m., but later in the night a strong wind from the south-east blew much sand on to the tent. We had an argument as to whether this was a blizzard 158 WITH SCOTT: THE SILVER LINING or not, for there was no snow in the wind. Personally I now think it tends to prove that the snow in the blizzards is largely old snow caught up again, for the force and direction of the wind were just those of typical blizzards. We were protected from the open barrier surface by Brown Island and the Koettlitz glacier, and this region is one of small snowfall in any case. So we were not inconvenienced by such blizzards as blew on this western coast. The food was lasting out well. The first tin of biscuits was finished, and had lasted from the 3rd instant. (We had, however, an extra bag of loose biscuits.) 1 started my week of cooking on the 18th, and as we reached Hut Point in the seventh week I had only one turn at this duty. February 18, 1911.—It seemed advisable to get a good view of the Koettlitz from some high peak, so I decided to spend a few days in the vicinity of this camp before marching up the big glacier. We had a “ make and mend” morning— sadly needed by our boots. I had saved some staples from the venesta boxes (thrown away at Butter Point) and found they were satisfactory in holding the soles together. Luckily the others’ boots were very much better, though Debenham’s were much improved by some of Evans’ sewing. We had a large fry of |seal’s liver in butter, and Debenham and myself decided that as raw blubber tasted passably, we would fry liver in blubber for the next meal off seal meat. In the afternoon Wright and I crossed Davis Bay to the mouth of Hobbs Glacier (about two miles to the north-west). The promontory on which we were camped was about a quarter of a mile across, chiefly built of basalt fragments rich in olivine. The shore of the bay below Hobbs Glacier was in the form of an extraordinarily flat alluvial fan. This uniform level extended almost to the glacier for three-quarters of a mile, though it narrowed greatly away from the bay. It was mapped out in square “tesselations,” and at the sides were striking terraces about five feet higher with strongly marked, clean cut edges. The whole topography had a very recent appearance ; but the only explanation I can give for these levels points to a period when Davis Bay was dammed by ice so as to raise the waterline to the levels of the various terraces. A parallel case of terraces in a waterless region is given in FIRST WESTERN EXPEDITION 159 Utah, where the hills around the great basin are fringed by similar deposits indicating a bygone lake. Down the fan ran a creek from the glacier, which cut into the silts at the shore to a depth of several feet. Evidently the base-line has been lowered by this amount since the fan was deposited. From the hill above the bay it could be seen that there were two fans, one of a lighter coloured silt being derived from the next valley to the south. We could also see that our camp was really on an island which corresponded to the stranded moraines south of Butter Point. February 19, 1911.—I cut out some sealskin from the carcase near-by to make a pair of “brogans” to cover my boots, lashing them over the sole with yarn, and over the sealskin | bound my iron crampons (steig- eisen) on. Then we all started to explore the valley immediately west of Davis Bay and south of the Hobbs Glacier. Leaving the sea-ice we reached a lighter coloured “fan” by a sharp step of five feet. Emerging through _ this broad gravel fan were “nunataks” of large stones which had evidently been deposited before the fan. They rose twenty or thirty feet above the fan, forming ridges lead- My footgear, 9-2-1 ing towards the valley. We reached a gully about 500 yards from the bay, which was entirely water-cut, and was fifty feet deep. It had steep sides and its bed sloped considerably. The latter was filled with large rounded boulders, one or two feet in diameter, obviously waterworn. The account of the summer streams in 1903, given by Dr. Wilson, explains this striking example of ordinary water erosion, which I was unprepared to meet in icy Antarctica. The gully wound about through the morainic foot-hills, _ and widened considerably about a mile higher. Here it was occupied by an ice-sheet some 300 feet wide. In this sheet narrow little canyons four feet deep had been cut by the water, and very generally these canyons were roofed with ice. 160 WITH SCOTT: THE SILVER LINING In other places the whole ice-shell had been undercut for thirty or forty feet by the relatively warm water. Gradually the valley—which I named after Professor W. M. Davis—became wider, and a tributary joined it from the north. (See folding map at the end of the volume ; and also p. 175, section No. II.) It drained the lowest slopes of the foothills, which extended to the scarp of the Western Mountains. These lowest slopes are largely covered by a gigantic deposit of moraine matter. This deposit extends many miles along the foothills, and can only be due to the great Koettlitz glacier. Four or five miles from the coast the steep hill-sides formed of solid rock rise somewhat abruptly from the moraine slopes to a fairly uniform height of 3000 feet. The sides of the valley along which we were walking were marked by lateral ridges in several tiers. These were about thirty feet high, and in some cases certainly contained much ice. At one spot the silty covering of the side of one of these lateral ridges was marked by vertical stripes of darker silt, as if the whole ridge had moved slightly and cracked along these lines. These ridges followed the contour of the hill between the tributary and the main valley, and reminded me of the parallel roads of Glenroy (though on a very small scale, of course). They are, I think, like terraces or beach deposits due to a bygone ice dam across the mouth of the main valley, such as one sees in the Marjelen See above Fiesch in Switzerland. Later we saw “ pocket editions” on Cape Evans. Continuing up the valley we found it bounded between solid cliffs of limestone, which were altered in places to a marble. We called these the marble cliffs, and they culmi- nated in a double peak of a fawn tint, which we called Salmon Peak from its colour. I kept along the base of these cliffs while the others walked up the thal-weg 200 feet lower. We soon saw that the upper portion of this “dry” valley was occupied by a glacier whose snout was forty feet high. ere light snow had fallen lately and occupied the furrows of the “ tesselations ” which ornamented the floor of the valley. For some reason (probably the direction of the wind and sun’s rays) only the north-south furrows were now filled, FIRST WESTERN EXPEDITION 161 and these white zigzag markings on the black basalt-debris resembled so many white snakes ! The Davis Glacier snout was about six miles from the sea. A range of mountains 4000 feet high blocked the upper end of the U-shaped valley. I was very anxious to see whether the glacier really came into the valley from some hidden angle, for if not this glacier was of great interest. Here was a glacier which could not be more than eight miles long, which had cut out a valley 3000 feet deep and a mile or so broad. We separated here, Wright and the others taking the theo- dolite up a 3000 feet hill to the south, while I went a couple ——$——— SS Empty hanging valley, on north wall of the Davis Glacier, showing catenary curve due to former glaciation, February 19, 1911. of miles further into the range to see the head of the glacier. Everywhere were the signs of recent recession of the Davis Glacier. First I had to cross the mouth of a side valley opening 600 feet above the glacier. This was quite free from ice, and was a perfect “ bowl-valley”’ or cwm. On the opposite side was another “ hanging valley ” at a lower elevation, with a most symmetrical U-cross section. It was abruptly trun- cated by the plane surface (35°) of the marble cliffs under Salmon Peak. I now climbed round the top of a cliff of ice which descended smoothly for 1000 feet to the glacier at an angle of 30°. After ascending over many outcrops of lime- stone schist, granite, and basic dykes, I reached the head of the glacier and saw that it originated in a cwm about three M 162 WITH SCOTT: THE SILVER LINING miles from its snout. Its snowfield was very circumscribed, but reached the summit of the bounding ridge in several places. The glacier up here was not crevassed, and the main surface lay only two hundred feet below me. After making some rapid sketches I returned to the snout of the glacier where the others had already arrived. This Davis valley contains a typical example of the “ ice- slabs” mentioned by Ferrar. But I do not agree with his description of them. He writes, “They are the relics of glaciers which once drained the snow valley ; but owing to diminution of ice-supply, this has now become an inland basin, and its overflows have slipped away from it, leaving a subsidiary watershed bare.”’ In the first place, the head of this glacier was a typical cwm, with steeply sloping sides, and to all appearance a sharp crest to the ridge at the back. It did not resemble the dis- continuous lower portions of the Lacroix and Sollas Glaciers in Dry Valley, which fully deserve the title of ice-slabs. The latter lie supinely, one might say, on a gently sloping hill- side, in which they have cut no definite trough. The method of erosion of these curious valleys became clearer to me as we saw other examples in the next fortnight. Monday, February 20.—We spent the morning making a depét on the Ice-Borne Moraines. We left the camera legs with a flag thereon, and cemented them into the gravel by the simple method of pouring a cup of water on to it! The seal’s liver we put under the food stacked in the small sledge, and I left a note of our whereabouts in the instrument box. We took eighteen days’ food with us. We crossed about one mile of good surface and then reached ‘‘glass-houses,” “craters,” “pools,” etc., through which we struggled till two o’clock. After lunch Wright and I prospected and found some “ plough-share” ice about a mile to the south-east. We made for this, having to cut tracks along the bottom of the channels connecting “ glass-house ” areas. Debenham and I pulled on short traces while the others lifted the sledge over the constant succession of obstacles. The sledge fell two feet into a hole and capsized, but the brunt of the shock was absorbed by the empty oil tins. We were always falling, and occasionally disappeared a foot below the glass-house surface. TRYING TIMES ON THE KOETTLITZ GLACIER, Fes. 2, 1911. yy. The sledge has fallen through “glasshouse” ice into a thaw-water channel. TABLES OR ICE “MESAS” IN THE LOWER KOETTLITZ CUT OUT BY THAW-WATER. [See p. 157. FIRST WESTERN EXPEDITION 163 Later we halted in a slight snowstorm. We were cheered to hear Evans say that it was the worst sledging sur- face he had ever seen, even though he added that it was not fit for sledges. I wore my iron steig-eisen all day, and so was able to hold my own somewhat ; but the others preferred to slip about, for the irons certainly made one’s feet very sore. For an hour we had fair going over “ plough-share”” and shallow glass-houses, during which we changed direction somewhat to the south. A thick snowstorm blotted all ahead, and we reached a region of “ basket-work”’ ice structures, which we called “ fascines,” and all sorts of ice tables. One shaped like an Armadillo standing on a pedestal was especially noticeable, and after pulling the sledge over three “ roof- pillars” (the roof having long ago fallen in) we cried “enough,” and camped in the shadow of the “‘ Armadillo.” “Tt is fairly warm to-night, the others smoking peacefully. They have almost given up trying to make me smoke. I had a difficulty in getting Wright to eat some extra pemmican ! ‘Sugar Vat,’ ‘Liver Chewer,’ and ‘Pemmican Tub,’ are common ekenames. And so to sleep.” During the next four days we struggled up the middle of the Koettlitz Glacier. It was a strenuous time, but I recall a pleasant noon halt when P.O. Evans earned an _ honest penny. We saw him playing with the rope which lashed his sleeping-bag. Says Evans, “Ill show you how to make a clove-hitch with one hand, and I bet you a 1s. 3d. dinner (our usual currency) you can’t do it after you’ve seen me do it six times!”” Debenham took the bet, and we all watched Evans closely. Then “Deb” tried, and to our joy succeeded, for the handy-man was rarely “done.” But he never turned a hair, and booked the bets that now filled the air. Again Debenham proceeded to try, and failed—and Wright and I were equally unsuccessful. Evans made quite a haul, but One - hand Clove Hitch How Evans won his bef. 20-2-4 164 WITH SCOTT: THE SILVER LINING after saying he had never seen any one do it by sheer luck before, he proceeded to teach us the dodge ; and later Deben- ham became quite a knot-master under his willing tuition. “A fine sunny morning, the first for many days. Even this scene of desolation looks cheerful.” Thus my sledge diary for the 21st. But the route did not improve. I wrote : “We got going on awful stuff—rounded pools of ice, between tables. It got worse and worse, and after many bumps and leaps and falls I decided to prospect. We had done half a mile in the hour. . . . We started again about 3 p.m. Awful heavy work over ‘ glass-house’ and leaping three-foot chasms, between high fascines and across decomposing rivers of i¢e.”” About 4.30 we saw a ragged piece of skin projecting from under an ice-table, and found that it was part of a large fish. We spent half an hour chipping it out, and recovered the dorsal spines, skin, tail, and the vertebra. These were pre- served in a yellow fatty substance smelling like vaseline and quite soft. I made rather a ludicrous mistake here. I care- fully preserved a very hard irregular mass coated with this flesh, thinking it was a bone, but later, after we had carried it for days on the sledge, we found that this “ pelvic bone,” as we called it—melted in warm water! No head was found, and in this respect the fish—which was possibly about four feet long—agrees with the four large headless fish found by the Discovery Expedition. We had a hot discussion in the hut as to this problem of decapitation, but came to no definite conclusion, for it seemed too far for seals to carry it. That night we slept at Park Lane Camp. We had been traversing a frozen park, set out in circular beds with winding paths in every direction. The “flower-beds” were repre- sented by elevated masses of ice thirty feet across, exactly like an apple-pie with a raised crust—even to the four cuts made by the housewife across the top! The last two days we had only progressed seven miles, and for five of them we had carried the sledge rather than dragged it. Next day, however, we found that to the south the glacier was nearly continuous. It had not been dissected by thaw- waters to nearly the same extent, and by 4 p.m. we managed to advance ten miles to the south-west. We camped on a platform of weathered ice, so rotten that it resembled a layer FIRST WESTERN EXPEDITION 165 of honeycomb. We found that this honeycomb ice was very common in this part of the Koettlitz. We tried to find an easier way out of the numerous undu- lations which now characterized the surface, but unsuccessfully, and so plugged on south-west. We used to “ pully-haul” up one side (i.e. hand over hand) and then toboggan down the other. P.O. Evans was an expert steersman, while we others used to keep the ropes clear. But we had some nasty falls, especially Evans, who got a cut deep in his palm from a piece of “ bottle-glass”’ ice, in spite of his thick mits. At noon we came across a picturesque tunnel in the ice, about three feet wide, seven feet high, and one hundred feet long. It had been cut out by thaw-waters which had now drained away. In and out wound the lanes, forming a regular network through all sorts of picturesque pinnacles. Here was one like a yacht on stocks, there a perfect wedding-cake twelve feet high, again a lady’s bonnet, and so on, in infinite variety. The long promontories of “ bastions” along which we skirted are probably dissected undulations of the original glacier surface, fifty to a hundred feet high. They are all steep to the north, and covered with sloping plough-shares on the south. The bergs which we left ten miles back were like jumbled blocks, and were not separated by simple channels— which looks as if they had been floating separately at some period and then frozen together again. This may explain the presence of the sponges and fish which we found so far from any open water. On the 24th I wrote: “This is the day of my release from the joys of cooking! We have done four weeks. A rotten night, cold, and pillow (of books, etc.) slipping away on the smooth surface. Every one restless. Smooth ice no good to sleep on, though I had a jersey under me. Bright next morning, and we took photos till 10 am. Then we made across country towards a hanging valley. Some of the lanes were overhanging, and I took a photo of Debenham and Evans sitting under a ledge. Sheets of plate-glass pro- jecting from low bastions were common, but there was no undulating country. More common were sharp bottle-glass angles sticking up abominably from about eighteen inches to ’ 166 WITH SCOTT: THE SILVER LINING two feet, and impeding the sledges, while pot-holes (due to the sun eating round black silt) caught one’s boots. “‘Lunched in this mullock about two and a half miles from the coast. Then on practically straight, making fair progress with Evans and C. S. W. at the sledge, lifting while we pulled. We had several upsets, and the rucksack was jerked off, but the fossil fish has survived so far. “‘ After a final dash up over steep silt bank between pin- nacle ridges (where the sledge balanced rockingly!) we reached a broad avenue between moraines and Stonehenge pinnacles of ice. I went back for my brogans, and fell a frightful ‘cropper,’ getting a spike in my fifth rib. “After half an hour or so we plugged on steadily up a beautiful surface for two and a half miles. The moraines were getting bigger and wider, and were now about three hundred yards across. We finally reached a fifty-feet silt ‘col,’ and had to portage the sledge. It was mighty heavy, and flattened our crampons. Later we reached a cul-de-sac among the moraines, and after a survey I decided to make a final camp, as we were now favourably situated to explore ‘Snow Valley’ and Heald’s Island. I don’t understand the ice-slabs or the promontory on the 1902 map. I guess it is wrong. “The sun clouded and snow began. We put the tent in a sandy dell. It was so small that we had the tent like an old sock at the side! However, we are on earth again, and not on cold wet ice, even if one post of the tent is on a huge stone. “T cooked my last meal. Raisins in excess ( X 2), sugar- dust about right, cocoa X 2, chocolate short #, cornflour three portions left, cheese short 3, biscuits right, and pemmican two feeds left. Butter short owing to seal-liver feast. We had a good hoosh and drank thick chocolate. ““My week’s cooking done, Praise Be! 9.20, snowing now and pretty cool.” Next morning was devoted to a “make and mend.” All our sleeping-bags and finnesko were wet with the sloppy ice- floors of the last week—for we had not been able to find any snow-drifts on which to camp. They are much warmer and drier than ice. Behind the tent to the north were slopes about 1000 feet FIRST WESTERN EXPEDITION 167 high leading to empty “hanging” valleys. These radiated from the base of the Lister scarp, which rose in one steep face 10,000 feet to the summit. This face was pitted by gigantic “armchair” valleys or, as they are technically called, cwms, and presented a spectacle which probably could be paralleled nowhere in the world. Looking southward across the Koettlitz from the mouth of one of these hanging valleys one could see some sort of plan in the icy maze which had so bewildered us. Above Heald Island the valley was filled with the glacial stream in a normal uniform mass, interrupted only by crevasses and falls. But to the east of Heald Island it took the form of a glacier “ delta.’ Below the falls the ice descended to the east in a series of broad undulations, a portion of which we had traversed on the 23rd. Long promontories of ice fifty feet high extended from the unbroken glacier mass and probably represented the crests of the undulations. These degenerated at the ends into icebergs and monoliths of ice, and these again had weathered into the bastions and pinnacles. Lower down the thaw waters had etched these into still smaller units, and along the coast just below me the streams had formed a well- defined if narrow avenue of smooth ice, which promised us an easier return, On these slopes I found an ice-scratched block—the only specimen I had seen in a hundred miles of moraine debris. I walked along the margin of the glacier, and was amazed to see seal-tracks in the fresh snow. We were over twenty miles from the sea, and had not seen any possible route for seals on our outward journey. Yet here were two seals— asleep as usual—on the old glacier ice. I disturbed one of them to see what it would do. He sneezed and grunted at me. When I teased him further he began to warble! 1 heaved a lump of ice at him, whereupon he lolloped twenty yards to a wet patch, lay over on his side, and produced a whole octave of musical notes from his chest, ranging up to a canary-like chirrup. Finally he crawled under a deep ledge, and vigorously butting with his shoulders, opened out a hole and flopped under the avenue ice. Later I came out among the moraines, and was unable to make out where our tent was. Soon I saw Wright’s foot- prints in the snow—two sets, one going each way. By 168 WITH SCOTT: THE SILVER LINING Sherlockian logic, I decided to follow the shorter-pace footsteps, judging that the weary owner would walk with less “‘ vim” returning, and they seemed to be “slurred” also. Finally, a mile ahead I saw some skua gulls wheeling about, and sure enough below them I found our tent. When I reached camp I found that Wright and Debenham had both met parties of seals. We all thought of the constant stream along the tide crack by our last depét, and came to the conclusion that this was largely fresh water, and formed the main drainage of the Upper Koettlitz. By this sub-glacial stream the seals penetrated nearly thirty miles inland up the Koettlitz Glacier. February 26, 1911.—-It seemed advisable to take the sledge as far up the Koettlitz as we could without waste of time. So we portaged all our loads out of the cu/-de-sac over a moraine col and so reached the outer margin of the low level moraine, where another avenue of smooth ice ran parallel to the Grand Canal which we had been using. About two miles to the west we passed a seal and its hole. Soon the pinnacle ice came in so close that there was barely room to Squeeze in between it and the moraine. We had one spill within a few yards of our final camp, and unfortunately it resulted in the destruction of the focussing screen of my camera. In a sheltered bay among the moraine heaps we pitched our furthest camp, where we remained four days. About 2.30 we started for Heald Island, which lay three miles to the south across a tumbled sea of ice practically impassable for sledges. (This island is placed too far to the south on the Discovery Map.) First we crossed the definite line of high pinnacles which extended almost continuously for twenty miles parallel to the coast. This we called Stonehenge structure, for many ice masses strongly recalled the Druid monoliths. Then over a comparatively level area of honeycomb ice between low bastions. Finally we reached wide level lanes with a thirty foot wall on the side facing the sun, while the opposite wall sloped much more gently and was fretted into plough-shares. Looking back towards our camp we were facing north towards the sun, so that we saw the sheltered side of the moraine heaps. The whole surface seemed to be snow- covered. Yet from the opposite aspect the moraines seemed FIRST WESTERN EXPEDITION 169 to be bare. I expected this constant thawing on one side of the moraines would have resulted in some asymmetry in their shape, but I was not able to detect any such characteristic. We had not much difficulty in traversing these lanes, and crossed several cols, down which Debenham and I—who were not wearing crampons—had to slide in somewhat undignified positions. Here we separated, Wright and Evans making for the lateral gully north of the island, while we moved more directly for its eastern face. We had been steadily rising up the lanes and came to the divide near to Heald Island. Here a narrow water-cut channel led down to a broad frozen river 100 yards across, which fringed the island on the east. Debenham collected along the slopes while I pushed on to get a summit view. This end of Heald Island was 1100 feet high, and the slope was very steep, for the most part reaching 30°. It was covered with a talus of schists, lime- stones, and basalt, the latter being erratic, while the former were 7m situ on the top of the hill. I got good views of the topography from the compara- tively flat top of the island. The surface was scraped fairly smooth by glacial action, and only a thin veneer of basalt rubble was present in this eastern portion. I carefully noted the features towards the S.W., and was satisfied that the slope glaciers (Walcott, Ward, etc.) headed in sharp ranges 6000 feet high, which joined to the scarp of Lister without any intermediate longitudinal valley, such as was indicated on the 1902 map as “Snow Valley.” The surface of the glacier through which we had passed was very interesting. I could now see that it would take days to get the sledge up the glacier to a spot where our view would be materially increased, and judged it better to investigate fairly fully the features in this interesting region of the valley. The island evidently blocked the glacier greatly, for this was 700 feet higher on the south-west face than where we had crossed it. Next morning was foggy and cold, and there had been snow in the night. We boiled the hypsometer and found that the camp was only 100 feet above sea-level. At 11 a.m. we started off to explore a large tributary glacier which we could see across the low-level moraine. Debenham had a sore heel, due to the deep ridges which developed in our frozen 170 ~ WITH SCOTT: THE SILVER LINING ski-boots, so that he did not move far afield for the next day or two. After crossing two miles of moraines we reached a lake. It was drained by a stream which ultimately reached the pinnacles of the Koettlitz glacier. Between the ice cliffs and the lake this stream for a con- siderable distance flowed under the moraine, and ultimately entered the seals’ sub-glacial stream and so reached the sea. Coleridge’s lines entered one’s mind : “Where Alph the sacred river ran Through caverns measureless to man Down to a sunless sea.” So we christened this stream the Alph River. We marched along the lake and up the gully beyond. Here a tributary entered from a large cave in the moraine wall to the north. The roof of this cave was coated with most beautiful ice crystals, which resembled pine twigs in shape and were about two inches long. Many brownish ice stalactites and stalagmites fringed the walls of the cave, and Wright was lucky in obtaining some beautiful photos of these structures, At 4 p.m. we reached our goal—the steep face of the Walcott glacier, but as the weather looked stormy we had to retreat immediately. Wright and I compared compass readings here. The needles swung extremely sluggishly, but we found they were reliable to four degrees—which is about eight times the ordinary error. The fact that magnetic south was nearly due north also complicated matters here! We marched back by a different route and discovered a strong outcrop of basic lava about fifty feet thick, which was rich in olivine and had caught up fragments of garnet rock in its passage through the earth’s crust. It was a cold cloudy morning on the 27th when we started off for a tramp over the ancient low-level moraines. We could see a big tributary glacier about twelve miles away, whose vertical front was separated from the Koettlitz by two miles of bare moraine heaps. Debenham, with his bad heel, stayed around the camp where there was plenty of collecting. We went a short distance along one of the moraine avenues. Then we climbed eighty feet up and proceeded FIRST WESTERN EXPEDITION 171 over the more or less level moraine debris for two miles. There we came on an interesting outcrop. It was very unexpected to find a deep gully 100 feet below the general surface with water still flowing in the creek at the bottom. The walls were largely composed of ice hereabouts, and*they were melting merrily in the sun. This stream originated in the lake which we had seen a day or two before, and we reached it vid some beautiful meanders. At its outlet was a cave twenty feet deep cut in blue ice. Evans and I had a bet as to the length of the lake, in which I recorded a win; but “ Taff” usually came off best in these encounters ! February 28, 1911.— We awoke to foggy and cold weather, which was unsatisfactory, as one of our chief objects was to climb a peak and get a good view of the hypothetical Snow Valley (between Descent Pass and the Walcott Glacier). Wright and I went back to Alph Lake some miles to the west, while Evans and Debenham made another journey to Heald Island and traversed it almost to its western end. I investigated the cave in the silts at the lake outlet. The cave seemed to be due to a block of ice breaking away at a silt band, for the roof was filled with stones, while the mass above was clear ice. The interest lies in the fact that these silts were obviously laid down in water, and the large boulders arranged in uniform layers indicated that a strong current had been operating. I left Wright at the lake, which he crossed later to examine the “crystal cave’’ we had seen previously. Mean- while I climbed up the steep delta of the stream leading to the “ Ward Hanger,” and visited the latter valley. This gully was about a mile long with steep sides sloping thirty degrees at first. I made for a black exposure which | could see ahead where the gully cascaded down from the hanging valley. This was a bed of decomposed basic lava, about twelve feet thick and pointing to fairly late volcanic action, Then I proceeded up the gully, scrambling over large rounded boulders. I hurried to the top of the slope and found that a very definite dam blocked the hanger, just as in the adjacent valley. These dams were, I think, high-level 172 WITH SCOTT: THE SILVER LINING lateral moraines left by the Koettlitz glacier, and not serminal moraines of the small tributary glaciers. I could see that the latter (Ward) glacier now lay about five miles up the valley, and resembled the others which we had observed previously. Wright and I then traced the Alph River from the lake down to the glacier opposite Heald Island. We had to climb over several rough barriers of silt-coated ice, under which the stream flowed. The relative movement of the frozen surface and overhanging ice-cliffs led to very queer twists and bends in numerous icicles, thus forming a striking example of the plasticity of ice. The water was flowing strongly with musical gurgles under a lace-work of crystal-edged ice. We got very wet boots by slipping through on our walk at the foot of the steep slopes fifty feet high. The river ended in a little round lake separated from the Koettlitz by the silt-covered pinnacle described previously. We walked along the glacier edge towards the camp. At one spot the water was welling up through holes in the ice, and appeared to indicate a slight tide, for it had spread out to varying boundaries at various times. Probably a variation in temperature would account fully for the difference in supply. We reached the tent about a quarter past six. The weather had been dull, and it was useless to expect a good view of the western scarp and valleys. I decided to wait until the 3rd if necessary to climb up for this view. The hills were now snow-covered, and we had several valleys to the north to investigate before our return, The month of March opened with a bright sunny morning, just suited for our proposed climb up one of the hinterland ranges. We climbed up the slope about eight hundred feet and soon reached the level floor of the hanging “ valley ” just behind the camp. We marched along this to the north end of the valley towards a prominent peak on the eastern ridge. A stiff climb over snow slopes and rugged granite led to the summit, which we reached at 1 p.m. The aneroid made this 3000 feet above sea-level. It was a beautiful day and we could see Erebus, Discovery, Morning, and the Pyramid up the Koettlitz. Lister itself, as usual, was in the clouds, but nearly all below was visible. We could see numerous hinter- land ridges reaching from the Lower Koettlitz to the Lister FIRST WESTERN EXPEDITION 173 scarp, and satisfied ourselves that no lateral “Snow Valley” existed below the scarp such as has been indicated in earlier maps. a was very cold on this hill (which we called Terminus Mountain) ; and after swinging the theodolite and taking several photographs we hurried back to the tent down Ward Valley. On March 2 we started our homeward trek ; nothing could be worse than our outward track up the middle of the glacier—though we were able to study the changes of the glacier ice and so did not regret it. I therefore decided to hug the coast on our return, though near the depdt the ice was so full of silt from the moraines that we had not seen any feasible route along the coast thereabouts. For the next few days we followed the course of the sub-glacial Alph River. Some four miles down-stream from Terminus Camp a rampart of ice pinnacles commenced, which recalled the monoliths of Stonehenge. These walled off the rough sea of the Koettlitz Glacier from the frozen surface of the “river.” This broad lane was here a quarter of a mile wide and consisted of a level surface broken up by deep sunken “paths.” The more elevated areas were preferable for sledging, for the paths occasionally let us through into water. The whole structure was due to the drainage of water away from rivers and lakelets whose surface had frozen. This splendid track—which we called “ Alph Avenue ”— enabled us to proceed with unexpected ease, and each day we halted and explored one of the numerous tributary valleys which characterized the hinterland. Each valley was of the same type. A great bar of debris, some three hundred feet high, blocked the mouth of the tributary. Within this was a bare rounded valley extending to the foot of Lister. Some five miles from the coast was the snout of a tributary glacier which had originally deposited the moraine, but now was shrunk back to a mere shadow of its former self. All along our route were groups of seals, and numerous skua gulls enlivened the surroundings. Coming back from one of our détours I was much amused to see Wright crawling about among the seals in his investigation of the ice—while thirty skuas were anxiously awaiting the demise of this obviously crazy seal ! 174 WITE SCOTT: THE SILVER LINING The summer was over now and we were getting fifty degrees of frost in the nights. The weather was gloomy, the sun rarely appearing till it had sunk below the level of the pall of stratus. We had an eventful lunch just before reaching our depét. We pitched the tent and fastened the door to keep out the wind. I was sitting next the door with my precious lumps of sugar on the floorcloth when I noticed that water was creeping into the tent. In a few seconds it was several inches deep. We bolted our raisins, pocketed the lumps of butter and sugar and rushed out with the sleeping-bags. There was a small lake all round us, rapidly rising round sledge and tent. The water was rushing out of a crack one hundred yards below us, probably driven back by a high tide. We had quite a pilgrimage to get our sledge packed again, having to walk round the newly formed bay. The avenue petered out here, after furnishing us with a magnificent highway for twenty miles. We had some pretty rough work for the next mile or so, but reached our depédt safely on the evening of the sth. Having now described many of the glacial valleys it is interesting to see if we can discover how their peculiar topo- graphies have arisen. One great problem confronting geologists is to explain how the giant “steps” and “ basins” of the Swiss glacier valleys were produced. In Antarctica the gradual change in the character of the valleys as we proceed northward from Mount Discovery has led me to put forward a theory which I think holds good for these huge glaciers in latitude 78° S., and may help to explain those in 45° N. In old Greek manuscripts one can sometimes discern traces of an older script half obliterated by the later writings—this MS. is called a palimpsest. Just so in Antarctica—I think that beneath the largest outlet glaciers, such as the Ferrar and Taylor Glaciers, we can perceive the relics of an earlier cwm erosion. Near Heald Island is the gigantic scarp of the Royal Society Range 10,000 feet high. Cutting into its face are simple cwm glaciers such as the Walcott glacier. This stage is shown in section I. As the snow accumulates (and turns into ice iz situ) we get a gnawing process, in the moat, etc., at the margin of the glacier, which gradually extends FIRST WESTERN EXPEDITION 175 backwards and eats out a long parallel valley such as the Davis Valley (section II). If the plateau ice-cap increases sufficiently it will drain to the sea as an ouslet glacier. This will obviously Young Icecap Wn The “ Palimpsest” theory. Generalised sketch sections, showing the chief types of valley erosion. I. Early erosion like that shown by Walcott Glacier, 78° 10'S. II. Headward erosion producing a “ finger” valley, shown by Davis Glacier, 78° S. III. Plateau ice overwhelming the cwm glaciers giving profile like the Ferrar Glacier, 77° 40’ S. IV. Pronounced erosion by “thaw and freeze” (= nivation), as shown in the Taylor Valley, 77° 30’ 8. tend to follow the lowest contours and so would naturally overwhelm a series of cwm glaciers (such as shown in II). Hence we get a glacier falling over steps (and cutting gradually 176 WITH SCOTT: THE SILVER LINING through them) which were originally heads of cwm valleys (see section III). Finally, these big glaciers may retreat very slowly, and at their snouts—in a somewhat complicated way which I have explained elsewhere—further erosion by nivation will produce basins with level bottoms, such as those in the Taylor Valley * (section IV). In the maximum of glacier flow (for which we have to go to temperate climes for good examples) there is much “ planing” by the glacier, but not in Antarctica under the present conditions. At any rate, the con- clusion 1 have reached after two summers’ sledging, is that considerable frost, wind, and water action is occurring in the Ross Sea area, and very little true glacier erosion. Moreover, the gradual succession of types of valley erosion which we investigated makes me confident that some such cycle of evolution as sketched above is not only possible, but has taken place in the south. On arrival we swept the snow from our old ground and camped on the bare gravel, for our floorcloth was quite soaked. I went over to the seal I had killed a fortnight earlier and managed to cut through the frozen hide. Evans and I then managed to prize off some blubber with the spade. The blubber was quite soft where it was protected from the air. Evans and Wright were frankly sceptical as to the value of blubber as a means of frying ! “ After cleaning out the aluminium base of the cooker, Debenham cut the blubber into strips and heated it up. It soon began to melt and gave off much steam at first. The smell was like fried herrings and not unpleasant! We had thawed out some liver from my cache, and at + 2° F. it was as hard as iron! I cut it into strips and we cooked it in the blubber for a quarter of an hour or so. Debenham tasted it, and then I ate the first piece. “Jolly good! Absolutely no taste of fish or oil, which was curious in view of the smell of herrings. Evans took his bit gingerly, and then handsomely acknowledged that he had been sold. He reckoned their * The theory of nivation would be out of place here. It is explained in Hobbs’ “ Existing Glaciers,” and I deal with it fully in the official memoir. forks r Blubber 53-1 FIRST WESTERN EXPEDITION 177 cook had tried to poison them in 1902. We used safety pins as forks, and my bowie knife to turn it over. A vote of thanks to Deb was passed by the company ! “With luck we shall camp in the middle of the Dailey Isles to-morrow (Monday). On Wednesday get to Hut Point, and then two days to Cape Evans.” This prophecy was rather feeble! We took nine days to reach Hut Point, and five weeks elapsed before we saw our own headquarters ! March 6, 1911 (Monday).—A fairly sunny morning with a temperature of — 8° at 9.30. We spent some time in packing all our depéted goods. I carried an empty biscuit tin to the nearest large moraine heap, and buried it halfway in the gravel with a note of our journey. The sun, glancing on the bright metal surface, made this a very distinct landmark some distance from the moraines. We had now two sledges to pull, but the surface was very ood. We made for the nearest Dailey Island. After one and a half hours we reached old ice at a higher level than the sea-ice we had just left. Here I mounted a hummock and saw that open water extended to Davis Bay, and was practically within one mile of our track. We were rather astonished, for this ice (around Blue Glacier) had not been out for several years. We pushed on and camped two and a half miles from West Dailey Isle for lunch. Another two miles brought us to a most interesting locality. All around us were heaps of large sponges half buried in snow and ice. The three largest heaps were about 8 feet long and one and a half feet high. The sponges were a foot in diameter, and among the long spicules we found Bryozoa, Brachiopoda, Serpule, Molluscs, and a fine solitary coral. How did these marine animals come to be entangled in the old ice on which we found them? The ice was apparently normal fresh-water glacier-ice, but may have been originally sea-ice from which the salt had drained out. At any rate, it was floating—for half a mile further east was a succession of grinding ice-cracks, 1 believe the sponges were pushed up (from a depth of twenty feet or so below water) by the edge of the Koettlitz glacier, in some palzocrystic age when its snout was much less advanced. We pushed on about a quarter of a mile, and reached N 178 WITH SCOTT: THE SILVER LINING irregular ice crossed by a deep gully due to tide cracks. Here we left the sledges, and all climbed up the West Dailey Island. We attacked the nearest snow-covered slope, though later we found it was the steepest portion of the island. There was a fair route along the snow, however, and we soon reached the top. Two asymmetric valleys crossed the island, whose cross section seemed to indicate glacial erosion from the south-east. Blocks of marble, kenyte, and gneiss were scattered over the island, which was itself composed of basic lava. We were most interested, however, in the view towards Erebus, for we hoped to see a clear route to Cape Evans. 5, Caskle ' Z : Rock ‘gts 443 : ri 473 2 s S44 § \ : Bhazard a ~ t % id 177% a “ 12-173 © : J Camp Pref | - Bea A A i, e* er G & ) od “ Or Brown = White A Map showing our journey round the breaking barrier. Four miles north of us was a prominent crack leading east and west. All the ice to the east and north-east was rough, pinnacled stuff as far as we could see. In the distance Inaccessible and Tent Islands appeared clearly, and also a curtain of frost smoke. We could not detect the latter much south of Tent Island, and hoped this meant that the ice had not gone out behind Glacier Tongue. I decided to camp after another mile, and then skirt along the pinnacle (bearing towards Cape Royds) until it appeared feasible to cross to the east. I photographed the little valleys on the island, and then we returned down a much easier slope FIRST WESTERN EXPEDITION 179 to sea-level. Here we saw a young skua practising its first flights under the eye of two older birds. We camped in the snow amid troubled ice just off the north-east corner of West Dailey Island. March 7, 1911.—We had a wakeful night, for the pressure ice at 2.30 started groaning and creaking just under our heads. We had a temperature of — 13°, and the night was quite dark, though a glow was apparent to the south. In the morning a cold wind from the south-east arose. I had to prospect across half a mile of bad surface, but found a fair route for a single sledge before the packing was concluded. The sledges stuck badly on sharp snags, and we had to relay through tables and over snow-covered ledges and crevices. Then we reached a glass-house surface, which was fairly stable owing to the thick covering of snow. We held along the west side of the broad tongue of bad ice and made fair progress. It was pretty cold, however, and Debenham suffered two frostbitten toes. About 4.30 I felt that we ought to be near the end of the Pinnacle Ice as shown on the map. So we pulled towards it, and reached high ridges rather suddenly. We camped here, and Wright and I penetrated the ice for a mile, making for a specially high pyramid. The surface was frightful, consisting of big rough undulations much broken into snags and pyramids, and crossed by frozen rivers with window-glass buried in snow- drifts. We could see no difference in the distant east. It was evident that we could not cross. here, and must make still farther north. We felt that the whole broad tongue had moved north, It was necessary, therefore, to turn back and go rather to the north-west, Hence we called this Keerweer Camp, after the Cape Keerweer where the old Dutch captain retreated from Australia. _ March 8, 1911.—We moved off along the edge of the pinnacle to the north. We did about one and a half miles, and got bogged in bad country. A prospect ahead showed that we had entered a sort of cul-de-sac. We could see frost smoke rising all around us, and heard seals; and, apparently, orcas blowing and grunting, much closer than we could explain, for we could see no water. Finally, we decided to keep to the smoother ice, and so for the next mile or so were heading for Butter Point, directly away from our destination at Hut 180 WITH SCOTT: THE SILVER LINING Point. Soon we turned more to the east, and topping a small rise, were confronted by a large bay of open water in the pinnacle ice, in which several orcas were apparently enjoying our discomfiture. The water lay right across our path, and we made as rapid a course as we could lay for the further side of the bay. Before going many yards into the pinnacle ice we came on a labyrinthic river of salt water fifty feet or so below the general level of the pinnacle. Luckily the pancake had jammed in this valley, and it was strong enough to carry the sledges. We had to haul up the sledges by hand on the further (southern) side. Here we lunched, and soon after came to a fifteen-foot drop, which necessitated casting off one sledge. 1 prospected ahead, and the other three followed almost as quickly as I could pick out a feasible route. Every now and again I climbed a pinnacle, and got a fair view, and so we got along much more easily than | had anticipated. The grade was good, but necessitated much winding about, and very often drifts of sand covered the ice and played havoc with the runners. The drifts of snow, eighteen inches deep, were no trouble compared with a thin film of sand on an ice ridge. “We could hardly get a fragment of ice hereabouts which was not full of sponge spicules, which did not improve the hoosh. It was very curious to see the skuas pecking at the numerous sponges lying around, while they neglected the small frozen fish (Notothenia), of which I saw a dozen ! By six o'clock we brought up our second sledge to the site I had chosen for a camp. Just north of the camp was a large cavern excavated in the side of a thirty-foot cliff by a meandering river, now frozen. We had a fairly sheltered position for the tent, but there was no snow for the flaps. However, ice blocks made that all secure. Before turning in we took a round of angles, which should fix the position of the edge of the open water quite accurately. March 9, 1911.—A comfortable night, the temperature only falling to —3°. We picked a pretty fair route across the meandering gully. At one place a snow-drift had built up a track above the undercut edge of the river. Then we went down-stream a quarter of a mile, and then hauled the sledges up the further bank. We could see quite a large FIRST WESTERN EXPEDITION 181 patch of smooth snow towards Observation Hill, and made in this direction. As we were not more than sixty feet above sea-level, I judged this to be four miles off, which turned out to be the case, though it took us nearly two days to reach it. We pulled in relays, doing one and a quarter miles with the light sledge in less than an hour, and then returning for the heavy sledge with some knowledge of the conditions ahead. Twenty-five minutes took us back to the other sledge, and sixty-five minutes more with the heavy sledge brought our whole equipment one and a quarter miles nearer Hut Point. Bad sandy patches still annoyed us, but the ice was gradually becoming more level as we penetrated further south. In the afternoon we did a longer relay, with less sand but more snow. We had to cross several creeks, and had some upsets, but at the end of our day’s work a climb to a pinnacle showed up smooth sea-ice no great distance ahead in the direction of Tent Island. Six hours’ hard work—largely hand-hauling—had only given us three miles of progress, However, we were able to enjoy the chocolate provided by Evans in honour of his own birthday, and we christened the camp Birthday Camp in consequence. ‘ I feel that I cannot more fittingly describe the last few days of our First Journey than by transcribing my sledge diary. The style is “choppy,” but if the reader will picture the conditions under which the journal was written he will perhaps excuse lapses. We were now coasting the breaking Barrier edge, just where Bowers’s party had gone adrift a week before (see p. 197). It was getting very cold, and we had been sledging six weeks—over really awful surfaces since mid- February—and were feeling stale and in need of some com- fortable rest at night. “. . . Friday, March 10.—I am writing this on the morn- ing of the 11th, after a rotten night. The tent is flapping and C. S. W. wears a worried look as the icy aluminium pot sticks to his finger. I have filled the cooker with powdered snow. There is drift everywhere, an eighth of an inch thick in C, S. W.’s bag, who got out to survey the scene. I have a blistered ear, and am wet everywhere owing to perspiration. There is no joy in us, though sounding merry. I slept on the outside, where Debenham has slept hitherto, However, 182 WITH SCOTT: THE SILVER LINING I could get my back warm against him, which is not the case when we reverse ! “We moved off about 11 a.m. with the light sledge. Debenham prospected one-third of a mile, and then returned to say that we could go on with both. So we pulled up the heavy one, and in less than half an hour reached the level ice, about 11.45. Hence we traversed about six miles of pinnacle ice. We had heavy going for a mile, owing to deep snow between hard patches, occasionally knee-deep. “‘ Now a long argument arose as to the course. Debenham wished to head straight for Glacier Tongue, and reach Cape Evans same night maybe. I judged it not much further to Hut Point, and we were rather near the sea edge. Evans felt frost-bite in toes, but said later it was due to chocolate-paper stuffing ! “We camped for lunch at 1 p.m., with good hopes of getting all ‘sprowsy’ by night. The others put on finnesko, as all very cold. My feet troubled me least of all. Good ho! so I didn’t change from boots, though blisters very raspy when one’s foot slipped into a deep crack! Left about 2.30 and surface got much better—patches of hard white snow and some ice. We decided to get to Hut Point or bust! About 5 p.m. we decided to bust, for there was apparently five miles of open water before the Hut! So we deviated with what speed we might to the south, gradually veering further south in the teeth of a young blizzard, which made much drift and at times obscured land. We donned coats and windproof, and during the last hour got very wet with sweat. Rather tired when at 6.30 we stopped near snow-drift, being four miles from the sea. “We had to put up the pole first and then the tent, which nearly blew away, and the floorcloth afterward. I got into finnesko and got fairly warm, though the primus went out several times through draught, etc. Huge blocks of snow on flap. Rather slow prospect of a week or two at Hut Point, when we felt yesterday pretty sure of getting to Cape Evans in two days! Wind moderated at intervals in the night. Good sunset and fairly clear, so this is not a true blizzard. “ Saturday, March 11.—Fairly clear, still some snow-drift and gusty. Up early. Every one uncomfortable in the night. Hope to reach the Hut vid Pram Point about 4 p.m. FIRST WESTERN EXPEDITION 183 “ Drift packed hard round the tent, and had to dig out it and sledges. “‘ Made an early start at 9.45 a.m. Saw mists rising appa- rently all way from Hut Point to White Island. One column of dark cloud very persistent, the rest varied with wind some- what. So we made for east centre of White Island over poor surface owing to fairly soft snow. “‘ Finnesko nice and warm, felt as if one’s feet bare after boots. We did six miles and camped where we seemed to see the crack petering out. Then two miles in the hour to (3.45) where we deviated from White Island. Here Castle Rock was occulted by Observation Hill. 1 thought end of water would be only three-quarters of an hour away! We saw a black dot and cairn of snow and decided it was the Barrier depot. Me We had crossed one crack, probably an old one. The depét turned out to be a fawn-chested seal, active and bold, which moved off rapidly (4.30). (The open water was here only half a mile away.) The cairn was pressure ice, probably old line of permanent ice. About a mile further came on sledge tracks of depét party.* Don’t see their depdt anywhere. Not possible it has gone out, as undoubtedly some of Barrier has. At 5.30, after doing about four and a half miles, we reached southern end of broad bay of water. “C. S. W. took photo here, but so cold that spring shutter didn’t work, I fear, Then on for two miles further to our Barrier camp. “ Sunday, March 12.—Rotten night; slept about four half-hours and shivered, sore ear, cold knees and back, every- thing wet (on outside), Helmet a mass of ice, and so wrapped my head in wind-proof pants. Others better. Dreamt six individual dreams, including our relief by a rival party of kids! I got up to read aneroid and so acquired merit ! “‘ Primus a great bother in the morning. “Quite foggy and snowing considerably. Not safe to say where we'll be to-night ! “We left about 10. Foggy everywhere and drift blow- ing, but could see sun. Went (S. 40° W. magnetic) for two miles or so, then steered by sun. We saw a black object on * These tracks were made by the Rescue party, in their attempts to save the ponies, ten days earlier. 184 WITH SCOTT: THE SILVER LINING ahead. Evans said an icefoot; I said boxes. They turned out to be bales of fodder nearly covered and an empty dog- biscuit box. From here tracks of five sledges (no ponies) lead to Pram Point. We piled up fodder higher, and left map and note tied to our depédt pole.* By this time wind getting stronger. “We marched on over undulations, mostly heavy going. Wind from the south-east. About 11.30 a.m. followed sledge track right to a narrow gulf leading into Barrier, with broken block sticking out. Ice twenty to thirty feet above water, some snowy, new ice in the open gulf (elsewhere all clear water). The shore went nearly due west from here. We crossed a strong crack rising several feet. C. S. W.’s foot went in here. I deviated to north-east from here, and pulled three-quarters of an hour in worse wind and drift. Camped at 12.45, about four miles from main edge and one and a half from crack (and edge). Very blowy and blinding, and cold. Had lunch and no better! Stayed in tent, and here we are held up indefinitely only six or seven miles from the Hut! We tried dancing to warm feet. Played cards, sang, changed socks. Finally, about 4.30, all went outside and filled cooker with snow. We decided to have an early supper and turn into our wet bags. We lit the Primus, and let the flames singe our feet to warm them. Talked of Cambridge cake and tea and other delights. I put on pyjama pants for the first time. Jt may prevent chills to-night, but I doubt it. Evans told cheerful tale of snow wall round tent at Cape Crozier, when they were pinned in for five days in September in 1903 ! “We can’t see a hundred feet anywhere. The rime is dripping down my neck and covering our bags. Drifts are slipping off the tent. Wind veering somewhat southerly from south-east. Now and again we peeped out of doors. No improvement. Couldn’t get into shore probably to camp, as water is evidently exceptionally far to east. No camping on slopes, I understand, and daren’t try to reach the Hut (eight miles or more round) in this damned young blizzard. Guess we'll shiver it out. Underpants make much warmer, but toes nearly as cold as ever. 5.30 p.m. Booming of lid of biscuit- tin outside is like Inchcape Bell.” * The other parties had all returned from the Barrier a fortnight before to Hut Point. FIRST WESTERN EXPEDITION 8s [N.B.—13th and 14th written later in Hut.] “ Monday, March 13.—Pretty miserable all day. Stayed in bags till ro or so. Tent flapping wildly. There had been a lull in the night ; slight shift to south-west at times set the door swinging. Couldn’t get going at all. Had lunch at 12 (no breakfast). I didn’t like the idea of Barrier edge being only one mile away, and we are on a bad crack ; but as thirty feet cliff, probably ice is eighty feet thick. Couldn’t see the sun all day till late in the pm. Evans told yarns as usual. We had supper about 5 p.m., after trying a melancholy game of Rickety Kate, in which we couldn’t deal in mits, and got frost-bitten if we took them off. I managed to read a bit of “The Great Plot.” C. S. W. cursed baccy, and Deb lay low and felt cold. We turned into the bags very early, though the sun appeared about 5 p.m., and could get a sight of land above the drift. «< Evans said curious wind never to south-west, and so xot a real blizzard.* “ Tuesday, March 14,—Another night nearly as bad as the previous, with sore backache added, for everything damp. Used to put head and all inside bag for ten minutes and hot up bag. Then open nose hole to get oxygenated again ! “We got up at 7 a.m. and had early breakfast, but it came on very badly about ten, and as we knew directions we decided to make for Castle Rock anyway within half an hour. We dug out sledges and the tent flap. A long lee snow slope lay a hundred feet to north of sledges. Instrument boxes and tank full of drifts of snow, of course. “‘ Bags thrice proper weight. Mine worse split than ever, so I have no hood now. We marched on rather difficultly, but wind helped us considerably over small sastrugi and drifts. Helmets tight over head, but under chin (i.e. not coldest). All our duds on—a mistake as one gets so sweaty and it 1s tiring. Went onand on. Could see ice bluff on left, passed it and approaching slopes. Wondering if we'd have trouble at the tide cracks, which Evans described. All lost to sight in fog about 1.30. Plugged on steadily, had hallucination of hawthorn trees just behind one. (Why?) Told C.S. W. * His meteorology was incorrect. tT In the coldest weather the helmet covers the chin and a nose-nip protects the nose. 186 WITH SCOTT: THE SILVER LINING we were ascending, and wondered where the tide crack was. We had steered for the cone all the way to reach the incline as used by Evans (day of Vince disaster, 1902). “Just about 2 p.m., I guessed we were over the tide crack, and the sun appeared and showed us we were one-third way up the mountain! So we joyfully had lunch in the strong wind. Then transferred all necessaries to the big sledge (including ski boots), and left about 3.30 for the climb to Castle Rock. Not half so bad as expected, steady pull up eight degrees (about four miles), only two stops. Reached the top at 5.30, without trouble except for some slipping on hard snow. We zig-zagged a bit. Castle Rock is composed of agglomerate with brownish outer zone, over a darker centre. Height about 150 feet (boss). We had a short rest. A very strong wind blowing across us now. Evans evidently had Vince in mind, and wouldn’t let us pull quickly, though on a broad platform. We saw here a team track, apparently a dog team with sledgemeter. We had arguments as to its meaning and decided only one unit back. C. S. W. reckoned all the ponies ‘gone under’ as no tracks. Plateau one and a half miles long and one thousand feet high. Then we saw four men over towards Crater Heights. A great sight, though comic, to see arms swinging and fat wind clothes. Not like Penguins! They came towards us. We guessed the names all wrong, except Birdie. (They were Dr. Bill, Atch, and Cherry.) We heard all were safe and back, that the queer tracks were due to rescue of Bowers, Crean, and Garrard. They took our sledge down Ski Slope. Dr. Bill said, ‘Go and see the Owner.’ They were just expecting us. I put on crampons and met Scott. He told me of loss of ponies. Of the eight, three died in blizzard, three lost on floe, so only two left. We got to the hut about 7 p.m. Found it all cleared out by Atch and Keohane ; very dark and sooty from the blubber stove. Only one lantern, we sat around ; and pots served out in fixed order. Owner arranged for us to sleep in the ‘Sanctuary,’ opposite window. We had one lantern over stove, and then turned in to wet bags and slept fairly. Gran gave us finnesko. Will get Gran and Garrard’s yarns after.” 1V ‘H IN THE OLD DISCOVERY HUT MarcH—ApriL, I9I1 d ot) VW ALPH RIVER CUTTING THROUGH THE MORAINES AND ANCIENT ' ICE. [See p. 170. ae “DISCOVERY” HUT, Jan. 25, 1911. Showing the ice-slope above the bay leading from the Gap to the Hut. Note the eaves of the hut on left. A MONTH IN THE OLD DISCOVERY HUT Wuize we had been engaged on the western journey, Scott had made his depot at One-Ton Camp, and had returned north to Ross Island, a fortnight before we arrived. During February the sea-ice had broken away far to the south of Glacier Tongue—which marked the water’s edge in January —and it was now impossible to return to Cape Evans by the route they had marched south. Moreover, the icy slopes of Erebus were seamed with crevasses, and many ice-falls lay at the root of Glacier Tongue, so that an overland journey was out of the question also. Luckily the old Discovery Hut had been placed on the long rocky southern promontory of Ross Island named Cape Armi- tage, and even under present conditions, with the water reach- ing to Pram Point, it was possible to get to this hut from the Barrier surface—as, indeed, the last chapter has shown. A queer little hut indeed is this, compared with our palace on Cape Evans! It is square in plan, and rises to a central peak. All around is a sort of verandah, with outer walls reaching halfway to the ground. This was designed to hold stores and protect them from the blizzard snows. But the hut was hardly used at all by the 1902 expedition. When we first saw it in January, 1911, it was filled with snow and ice to within a few feet of the ceiling, and did not look by any means an attractive place of abode. During February, Dr. Atkinson and Crean had spent a large portion of their time excavating the hut, and had ulti- mately cleared it completely of ice. A great heap of ice blocks and chips marked the extent of their labours. They had piled up the boxes of captain biscuits into a barrier enclosing the north portion of the hut, and in this dark retreat the western party found the depdt party on the 15th March. We reached our refuge about 7 p.m. It was almost dark 189 190 WITH SCOTT: THE SILVER LINING outside and quite so inside. An acrid atmosphere of blubber, smoke, and soot enveloped us as we occupied the rough planks grouped around the heart of the hut. Here was built up a primitive blubber stove, crowned by a chimney whose vagaries formed the chief topic of conversation among the Ry Yy, NK a cuts AA ‘AAAS My f) \\Wi KN dpe RS we sii : s. Wht WU Ye AMIN) “uy, if / Cd Vy ‘y Y 4 ‘yy Ps ~—_— Y=, - a LS ££ a7 J AZ => Lz » \ A\\ \\ \ 7 NY hd \\ \\ \\ SOO SS S CLIFFS TO TEST THE SEA-ICE. OVER THE HUTTON From a drawing by D. Low. A MONTH IN THE OLD DISCOVERY HUT 207 near Hutton Cliffs, but north of Glacier Tongue the sun was in our eyes and we could not see if ice or water lay between the Tongue and Cape Evans. On the 11th of April nine of us started for our own head- quarters, leaving Wilson in charge of a party to bring over the dogs and two ponies. [The track is shown on the map, . 88. i The ‘relics’ helped us up the two snow slopes. Birdie and Bill arranged signals with fireballs at 10 p.m. on the first clear night in the next three. Dr. Bill had an under- standing with Scott that he should not move with the ponies and dogs until the sea-ice had stood a blizzard. We passed Castle Rock and were going strong at noon. I had been leading, giving Scott my shoulder, but here he shortened my rope and I pulled just behind him. Beyond Castle Rock all the land is untraversed. We kept for one mile along a steep snow slope, seeing no crevasses, and easily reached the flat top of the promontory. After about four miles we ap- proached Hutton Cliffs and could see patches of blue ice on the slopes ahead. Soon we met some crevasses, and both of us fell into small ones. We got to a ridge of boulders which showed where we were to get down to the bay ice, if anywhere. “ Quite suddenly it began to drift heavily from the south, and we had to put up the tents and camp. We had some tea and then prospected for a route to the cliff edge. There were huge crevasses zigzagging across the blue ice below us, but when the drift stopped we found a good track and soon reached the cliff edge. Here it was thirty feet high with snow whirling over on to the bay ice. Further south it was a little lower, and here Scott lowered me on to some fallen blocks on the sea-ice. Then Evans, Wright, and Bowers followed, and we guided the sledge down, fully loaded, without difficulty. Two bamboos were stuck in and the rope passed round. Crean arranged this, and Scott came last, being lowered from below. “We left the Hutton Cliffs about 5 p.m. and pulled north over two miles of soft sea-ice to Glacier Tongue. We anticipated trouble climbing the Tongue, but found a spot where its edge was only ten feet high. Evans and I were lifted up, and in ten minutes both sledges and men were on 208 WITH SCOTT: THE SILVER LINING the Tongue. It was good fun crossing the Tongue, for there were numerous crevasses to jump, none of which was particularly risky, though Evans fell into one. We camped on the north side about 6.45. It was pretty dark, but after some tea Scott decided to push on for the remaining five miles. ‘““We had to steer across the bay ice by observing a star, for it began to grow thick near the surface. I tested the ice with my axe fairly frequently. We pulled all we knew, for occasionally our only beacon (the star) was almost obscured. About 10 p.m. a black patch showed up, which we guessed must be Little Razorback Island. Here Scott decided to open water The two tents on the ice-shelf at Little Razorback Isle, April 12, 1911 (looking south). camp. We had a difficult job gathering mushy-ice to weigh the tent-flaps, but all turned in on the wet ice before midnight.” I don’t think many of us enjoyed the situation. We were camped on new ice and had not the faintest idea how far off the open water lay, and we had practically no food with us. Next morning, before it was properly light, a blizzard came up to add to our discomfort. We could not see Cape Evans or tell whether there was ice or sea in the intervening two miles. I climbed up the Razorback, cutting steps up the soft ashy rock with my bowie knife. Bowers and I explored an ice- ledge on the south side of this little islet. On reporting to A MONTH IN THE OLD DISCOVERY HUT 209 Scott he inspected it, and in the afternoon we shifted camp up on to the ledge, whence we could not drift out to sea if the blizzard increased. “TI snoozed about an hour during the night, pulled the flaps of my bag tight, and apart from frozen toes—partly owing to my home-made sealskinjfinnesko being too tight—and shivers in the back, and the soppy nature of all my clothing, I was pretty comfortable ! “We roused at 7 a.m., and I had to wait half an hour before my fur mits thawed out enough to be wearable. We finished up our pemmican and biscuits. Birdie was cook, and as usual took too little for himself, and made a fuss about filling up his own pot. “We packed up at 8.15, and found that the wind helped us materially. The ice seemed firmer here, and near Inac- cessible Island we crossed tracks and a silk line, evidently due to Simpson’s balloon experiments. We rounded Cape Evans and saw the open water less than a mile off, so that we were pretty close to it at Razorback. “Another hundred yards and we saw the hut with two men moving about. We went on silently (by order), and saw Lashley stand up, look our way and stand rigid. Then he spoke to Anton (who phlegmatically took no notice) and bolted into the hut. Soon they came streaming out in all sorts of overcoats, etc., Demetri and Lashley leading, Day next, Ponting, Anton, Simpson, and Hooper !” Nelson was asleep, and Clissold too interested in some cooking ! We learnt that all had gone well except that one pony (Hackenschmidt) had died of inanition and a bullet ! We pulled on, and Birdie fell into the broad tide crack. I got across safely with the ice-axe and so to the hut. I noticed the fine door-knobs, and the wooden number )_ | on our front door. The kitchen looked O.K. with ] bright tins and acetylene lighting, and all else was much about the same. Postscript (that evening). “Here am I in the hut, using my fountain-pen again after twelve weeks without refilling—only it’s made a blob! P 210 WITH SCOTT: THE SILVER LINING It is midnight and I lie in my bunk. ‘ Marie’ Nelson is taking meteorological readings, and remarks that the Skua Gull (z.e. G.T.) has resumed his predatory habits. The others are sleeping except Ponting, from whom I got my candle. But everything feels too warm and clean for sleep! Clocks are ticking everywhere !”’ Moe eee | yam en iv) ; Ad t io © Ponting's £ : a £ L : 7 2 Dark 2: a ca 5 Room a: Chart Table Captain Scott Mother Meares sover Jane Atkinson "Deb over Geological Lab. Titus Oates Be) L 4a 2 io) L £ a i< Birdie Bowers over Cherry- Garrard Taff Evans Stores Crean “Messdeck Table Keohane Forde Plan of hut, 1911, showing nicknames and bunks of Explorers. Sewin é “Machine Annexe built of Anton over Demitri IN WINTER QUARTERS WITH CAPTAIN SCOTT Arter our return from the summer’s sledging a new phase of Antarctic life began. For the next seven months we were practically confined to Cape Evans, and often to the hut itself. During our “ habitation enforced” it was rare for any man to be addressed by the name inherited from his parents or chosen by his godfathers and godmothers! The nicknames of the fifteen of the afterguard had by this time become standardized, and I| think merit a little attention. Captain Scott was invariably known as The Owner, a naval term always applied to the captain of a warship. Dr. Wilson (baptized Edward Adrian) was always known as Bill. Doctor Bill at first, Uncle Bill later, as one grew to rely on him more and more. Lieutenant Evans had four pre-initials, but was always called Teddy, which eminently suited his cheery frame of mind. Dr. Simpson was early caricatured as Sunny Fim by Lillie, and soon every one, in- cluding our leader, called him nothing else. Captain Oates was Titus to all of us, except to Bowers, who called him Farmer Hayseed, while Captain Scott usually referred to him as Soldier. Ponting was Ponko, and his chief aim in life (to get us to pose for him in all sorts of uncomfortable places) is perpetuated in the verb “to pont.” Nelson was Bronte naturally, and more obscurely Marie from some theatrical star met with in his varied career. Bowers was Birdie, from his outstanding features and Titian crest. Atkinson was shortened to Ach, or at times Fane. We were short of female society—which lack also accounts for fessie Debenham as an alternative to Deb. Cherry-Garrard was always Cherry—though an affectionate variation was Cheery Blackguard, while the seamen—baulking at the hyphen— called him Mr. Gerard! Our Canadian Imperialist, Charles 213 214 WITH SCOTT: THE SILVER LINING Wright, bore with equanimity the name of Cousin Silas, though perhaps Carolus and Tranter (Toronto) were more to his taste. Bernardo Day and Trigger (Tryggve) Gran were less remarkable ekenames. I gave up counting my own. McCormick (Skua—alluding to the rapid disappearance of some apricots), Keir-Hardy, Sharn-Gatch, and Old Griff were but a few. Before we had time to change into semi-civilized garb the indefatigable Ponting had us outside to “pont” er him. Luckily there were no melting icicles available, and he was content to get us standing near the sledges. Some of the others had already shaved off their beards, much to Ponting’s disgust; but mine was so rudely criticised that I kept it most of the winter to show my opinion of it! I assisted Ponting to the best of my ability by adding a touch of verisimilitude to Debenham’s photograph, and threw some snow at him at the critical moment ; but most of us looked such pirates, that there was no need for any further touch of Antarctica about us. I spent the day sorting gear, “. . . and about 1 p.m. I had a gorgeous bath—the first for three months. Funny thing, no effect from no wash, no change, no hair brush, etc.” I suppose the cold accounts for no ill consequences, but I have ever since felt more sympathy for the Southern European peasants, for their ablutions are equally simple ; they also do without a lot of impedimenta, and are equally healthy ! Ponting took his plates off to the dark-room, and sub- mitted proofs next day! ‘‘ Debenham says he looks just like an aboriginal—and far be it from me to contradict him.” Captain Scott and Seaman Evans seemed to develop an Irish appearance, while I scorn to repeat the comments on my portrait. On Sunday afternoon I had a stroll with Nelson, who told me how the nine at the hut had spent the time. Dr. Simpson was in charge, and had converted the newly built hut into a palace of mystery. In his corner to the south-east a small Gardiner oil engine was clacking away. This was used primarily, in conjunction with a dynamo, to charge accumu- lators for his electrical recording instruments. Mysterious clicks and gasps and ticking galore warned us that chrono- graphs and other wild fowl, to be described later, were brooding t Sis ee = ~ Photo by H. G. Ponting. CAPTAIN SCOTT WEARING THE WALLET IN WHICH HE CARRIED HIS SLEDGING JOURNALS. ; IN WINTER QUARTERS WITH CAPTAIN SCOTT 215 over meteorology yet in ovo. Ponting had “raked in every little bit” available, including some magnificent studies of surf breaking on the ice-foot. Day and Nelson roused our envious admiration chiefly by the condition of their common cubicle. No old beams from the stable framed their bunks! They were supported by carved and polished standards, encased in veneer (of venesta casing) ; and below were some fine specimens of joinery in the shape of two capacious drawers ! Day had equipped the hut with acetylene. The generator occupied a corner of the enclosed porch, where one could hear it gurgling as one entered the hut. If the outer door were not shut properly the fact was made evident by the dimming of the light! For the water in the generator soon froze if a blast of —40° struck it from the outer darkness. We were prohibited from carrying candles through the porch into the verandah storeroom for fear of explosion. Nelson and I initiated the survey of Cape Evans on that stroll. The lakes had diminished greatly ; not by ordinary evaporation, but through the removal of ice particles by the rocess of ablation. The margin of the lake ice was fringed by “ blobs ” of ice united into a lacework, and day by day one could see this fringe vanishing. It was curious that the small animalcule (//agellata, etc.) should in some cases belong to the same genera as in English ponds ! Cape Evans is a low promontory of triangular shape. Its average height is only about twenty-five feet above the sea, though Windvane Hill rises to sixty-five feet. The south- western portion consists of rocky ridges of kenyte with steep cliffs adjoining the sea, but to the north-east is a gravelly plain surrounding Skua Lake. Quite abruptly on the east and about half a mile from the western extremity, rises a steep bank of gravel (the Ramp) to a height of 150 feet. A few hundred yards of slope studded with quaint cones of rubble brought one to the edge of the great sheet of glacier ice which covers the whole western side of Mount Erebus. This was our domain, and to this cape we were practically confined during the ensuing six months (see Map No. 4). Patches of ice covered portions of the cape, but the rest of the surface consisted for the most part of kenyte gravel with ridges and bosses of solid lava (kenyte) projecting through it, especially to the south-west. These dark lavas undoubtedly 216 WITH SCOTT: THE SILVER LINING represented an earlier offshoot from the volcano of Erebus, probably a subterranean flow ; while careful mapping later on showed us that the little sheets of ice were not haphazard, but were “ glacierets”’ fed by blizzard snowdrifts. The most ingenious apparatus in the hut was due to Clissold the cook. This was an electrical device to tell him when the “ bread was riz.” He used to make the dough in the galley and place it in a big pot, puncheon, or pan. This was supported on a little trolley and stood at his bedside. The dough mixed, Clissold turned into bed, and left the rest to the yeast cells. When the dough rose sufficiently it pushed up a disc pat eddie date : | he Wc trcol Yeadmakey f 17-4 ott which overbalanced a gutter. Down this ran a lead ball which made contact and rang a bell! Further, the bell actuated a pulley and wire and made another contact whereby a red light appeared at intervals above his head! All this apparatus was made in the hut, and we never found out where certain of the “works’’ were hidden. Anyhow the bread was very satisfactory. On the 17th April Scott took a party back by the same route to the Discovery Hut. Scott, Bowers, and Crean returned there, accompanied by Day, Nelson, Lashley, Hooper, and Demetri. Debenham and | went in charge of two ponies who were to pull the sledges as far as possible. IN WINTER QUARTERS WITH CAPTAIN SCOTT 217 There was a fine moon, so that it was quite light at 8.15 a.m. We crossed several cracks, and 1 tested the ice with an axe. A moderate wind was blowing from the north— always a safe direction, for the blizzards invariably came from the south. The surface had improved greatly in the last few days, and the ponies had no difficulty in pulling along at about four miles an hour. Erebus was clouded, but occasionally we could see a red glow when the mists dispersed. Rarely was there so much sign of heat visible, though the steam banner often spread out a hundred miles. Opposite Turk’s Head (six miles south) the wind changed /nacce ‘Ale ~, ‘ste Bais Qe Lye /s/e =H Changes in wind direction, March 17, 1911. to a west breeze and then lulled, but a little further, near Glacier Tongue, there was quite a strong southerly, and we could see the drift sweeping over the promontory above Hutton Cliffs. Here Scott sent the ponies back in our charge. The others marched on, and had a cold, rough time reaching the Discovery Hut. Their difficulties in climbing the ice rampart at Hutton Cliffs in the teeth of a smart blizzard is well shown in one of Dr, Bill’s sketches in the South Polar Times. A small villa had been erected in our absence, to carry the magnetometers. This was built of asbestos or similar material, 218 WITH SCOTT: THE SILVER LINING and held together by brass nails. It also formed a camera obscura for meteorological purposes. A lens in the roof pro- jects the clouds on to a sheet of squared paper. This sheet is rotated until the clouds appear to move along a set of lines, and by comparing this with a compass the direction of their movement is obtained accurately and quickly. That evening I helped to festoon the hut with telephone wires. While so engaged I saw my first aurora, and it did not impress me. “ Like a huge broad cirrus cloud right across the sky from W.N.W. to E.S.E. No colour or movement, and it only lasted five minutes.” Wright and I assisted Simpson to send up a ballon sonde. This seemed a complicated business at first. We had to carry 9 out a queer theodolite with the “ eyepiece inserted at right angles oa to the telescope at the side; and = a large tank for generating the hydrogen ; and the inner tube of a bicycle tyre—and various reels of silk, etc., etc.; not to mention a small tissue-like de- flated balloon of red gutta-percha. = = The tank was filled from a Ss. ——— ep convenient tide-crack in the ie ferens Clie, sea-ice, and then Charles filled A sketch ne sr pees the cycle-tube with calcium unwinding the ack Sl “ ; i threads ae the two conical hydride. This compound r Seis analogous to carbide, but gives off hydrogen instead of acetylene. He attached it to the top of the generator, and squeezed it to push the lumps of hydride into the water. The balloon was attached to an outlet pipe, and gradually lost its dejected appearance and became a red sphere of some two feet diameter. In about ten minutes the balloon was inflated. This was merely a test, and after tying a piece of silver paper on the balloon it was set free and rose rapidly. With the theodolite the vertical and horizontal angles could be plotted, and thus the path of the balloon charted approximately. The sun was setting (at 3 p.m.) while we were doing this, and gave a yellow glow to the steam-cloud on Erebus, which was drifting to the south-east. When the balloon was about SIMPSON SENDING UP A “BALLON SONDE,” Nov. 12, 1911. The meteorograph stands on the box. Inside the latter are the two conical reels of silk. In the background is the magnetic hut, the Grotto Glacier and Vane Hill. ge BOL pass Sy MI Soh .. ee wR & y * THE EAST CORNER OF THE HUT SHOWING THE EDDY TRENCH SCOOPED OUT BY BLIZZARDS ON THE WINDWARD SIDE OF THE HUT, Sept, 14, 1911. The stores annexe appears just on Clissold’s right, and the “weather cupboard ” on the right of the picture. IN WINTER QUARTERS WITH CAPTAIN SCOTT 219 4000 feet up we could follow the flashing paper, and saw that here the air currents were opposed to the direction of the steam-cloud at 13,000 feet elevation. The next afternoon there was a furious blizzard of fifty miles an hour, and a temperature of —7°. We kept to the hut, and made a start at winter occupations. I was busy writing a narrative of the western journey for Captain Scott. In this I proposed to discuss the physiography in some detail. When I had written twenty pages on the first day and a half, I wondered if the “ Owner” would live through a report 840 pages long! Luckily the rule of three responsible for this forecast did not hold throughout ! Inside the hut the temperature was +47°. This was not exactly hot, and poor Ponting was delighted when some of the new-comers advocated lighting the small stove near his dark room. He said that developing photographs with water down to 47° was not the pleasantest job on earth. The blizzards hit his side of the hut, so that the inside of the dark room was festooned with icicles, giving it a most picturesque but uncomfortable appearance. Things were getting straight in our cubicle. Our floor space was about eight feet by eight. We built a small table opposite the door and put shelves over this. Gran occupied a bunk over mine, and the legs of his wire bedstead hung over my head and feet, and caused many bruises at first. Debenham’s bunk was raised six feet off the ground, and was supported on two stout wooden cylinders, on which the linoleum had been rolled. He climbed into it by a primitive ladder. His sea-chest was under the table, while mine half blocked the doorway. On the rubbish-heap outside I found a small tin which served as my wash-basin. In this I kept a sponge, and normally it stood on my chest below Debenham’s bunk. We were able to get about half a tea-cup of water if we found the cook in a good humour, so that it was rather a dry rub. Secretly I was rather proud of my morning wash, but it did not seem to improve my appearance. I soon discovered the reason. Watching Debenham one morning before I arose, I saw him finish his ante-breakfast pipe and casually knock it on the edge of his bunk. The ash obeyed the laws of gravity, 220 WITH SCOTT: THE SILVER LINING and fell into my sponge with great accuracy, and as if it were accustomed to do so! When the chest was thereafter freed from my ablutions, it was seized by Debenham as a petrological laboratory. For hours he might be observed rubbing down fragments of rocks on a glass plate with carborundum powder. He had a microscope, and was able to examine the many thin sections thus produced without awaiting his return to civilization. It is most interesting to see a dark rock gradually becoming transparent as the section gets thinner. First the quartz and felspar show up like clear and milky glass respec- tively. Then the green or brown colours of the mica horn- blende or augite appear, while the characteristic green fringes to the clear olivine crystals or the absolute opacity of mag- netite define those minerals. And then under the polarized light of the microscope even the colourless minerals show wonderful colours—from the pale greys and yellows of quartz and felspar to the vivid blue and purple of the olivine and pink and neutral tints of white mica. Thus Debenham classified the numerous rocks from the western mountains. Kemytes rich in lozenge crystals of a beautifully banded felspar; granites showing brown cleaved crystals of hornblende and mica among the quartz grains and simple felspars ; dasa/ts with numerous crystals of olivine and magnetite in a felted mass of little felspar laths—gneisses, granulites, etc., etc., each and all can be pigeon-holed by picking out the relative proportions of the few minerals specified above. By far the most interesting instrument in the hut— consulted by scientist and layman alike—was the “ blizzo- meter.” Such was the name we used for “ Dines Pressure- tube Anemometer.’”’ We could all see a roll of paper on a rotating drum, on which a pen was always scratch- ing lines giving wind velocity. But the expert could tell lots more. He could say not only how heavy each individual gust had been during the past twenty-four hours, but he could tell from the character of the graph whether the wind were from the north or south, and, more awkward still, he could tell when the night watchman had neglected his duty and let the inlet become choked with drift ! You could not bluff Simpson or the blizzometer. The IN WINTER QUARTERS WITH CAPTAIN SCOTT 221 Rotahng Lever and Pen Alcohol Thermograph. Graph | Pen , | < Pisfon rising with float alcohol mercury Piston rising with drum rofafed Clock which lowers pencil | Wind Direction Recorder Dines Blizzometer External Tubes within Fhe Hol Above Hut Copied from Simpson’s diagrams at his lecture in the hut, June 3, 1911. 222 WITH SCOTT: THE SILVER LINING blizzard gave a thick series of vertical lines, so close together that a broad ribbon almost resulted. The north wind was never so strong, and the lines were shorter and less close together. To understand the working of the blizzometer, let us accompany the night watchman. He has been engaged on his diary, maybe, till nearly midnight, when a complete set of observations are to be taken. He goes to the blizzometer to see what particular virulence of blizzard he has to face, and sees that the pen is motionless at the bottom of the paper— having dropped down after tracing gusts of sixty miles an hour. The night watchman feels depressed. He has to go and inspect thermometers and barometers and various other -ometers, but had hoped he would be spared “clearing the head” of the blizzometer. However, he wraps up well, and, carrying an electric lamp, ventures out round the south of the hut. He reads the thermometer at the most exposed corner, and then glances up to the roof-ridge and wonders whether he'll be blown off or not. In a sheltered nook he finds a brush of wires, and clutching this he climbs up a ladder to the roof. He feels the hut vibrating under the blizzard, and the drift shoots past him to the north. He clutches a metal tube projecting two feet above the ridge, and proceeds to prod the Wires into its orifice, which faces the blizzard. A plug of drift snow breaks loose, and the wind once more drives freely into the nozzle of the blizzometer. It rushes down the tube into the hut and enters the base of the instrument. Here it passes under and into a metal bell floating in paraffin. The pressure raises this float, and of course raises a piston attached to it above. The piston passes through a gland to the outside and carries the pen at its upper end. Thus with every gust the piston (and pen) rises and falls, and a record is made directly on the rotating drum. The watchman warms his hands inside his jacket, and when feeling has returned to them he trudges into the hut, and devoutly prays the “head” will remain unchoked all night. At this period our hut interior looked neat but not gaudy. Later, the continual tramping in of boots carrying snow and gravel, somewhat detracted from the neatness ; but luckily, in the absence of brilliant illumination, no one was perturbed by the accumulation of “ matter in the wrong place” which soon IN WINTER QUARTERS WITH CAPTAIN SCOTT . 223 collected in the corners. But one object in the hut looked rather incongruous, and that-was the Broadwood Pianola, lent us by the Broadwood Company. It was intended to keep this on the ship, but our unloading was done so successfully that some time could be devoted to transhipping the pianola. By dint of dismantling the wardroom—removing the stairs bodily—Rennick and his assistants managed to hoist the pianola on deck, and so got it eventually into the hut. We were a strikingly unmusical crew. Ponting on the banjo and Nelson on the mandolin were the best. No one but myself ever used the piano. I had three pieces of music and speedily lost one—it was found under the pianola buried in grime six months later,—so that there was rather a same- ness about my performance. I grieve to state that my two pieces became less rather than more popular as_ winter advanced ! However, I rather thought I might shine as a pianola player, and started to practise as early as April. After listening for some time, my scientific colleagues, who occupied bunks immediately back of the pianola, were moved to remark, “‘ For Heaven’s sake, Griff, give that a miss, and let some one play who can keep time!” Perhaps I should have persevered, but they could throw too straight, and I never attempted pianola-playing again. On the 21st Scott returned from Hut Point, leaving Meares, Nelson, Day, Forde, Keohane, Lashley, and Demetri in the 1902 hut with the ponies. They had had bad weather going—as I expected. Very thick drift hampered them, and the new chums, especially Hooper, had been severely frostbitten. The latter had two angry red sores on his neck where the blizzard had caught him between his helmet and jersey. To climb the cliff at Hutton Cliffs they had to empty a sledge. Crean and Lashley held it up at arms’ length like a ladder, and Scott managed to climb up it, and cut steps over the cornice. They reported that the others expected to stay a fortnight more, and they augured badly for the commissariat under Meares, because “he’s so very sparing with the butter !” Ponting kindly developed my western negatives in his dark-room. They were no worse than I expected, being, however, all rather thin. Half a dozen were broken, and I had 224 WITH SCOTT: THE SILVER LINING improved on a common error by putting three on one plate. We had such a rush before starting our journey that neither Debenham nor myself could test a single plate under Antarctic conditions. It seems simple now, but we had many failures before we gauged the best method. Previous Antarctickers had recommended plates and not films. I now disagree with this advice im to, at any rate for sledging. We broke the plates. They scratched easily. Changing them in our bags was an unmitigated nuisance and filled the dark slides with hairs. Lastly, the glass plates weighed so much that they were always left behind when we had to cut down weights. We had an idea that the quickest exposures would be advisable with snowscapes. Ultimately we took most of them at half a second or thereabouts ! A typical scene would largely consist of a skyline of snow mountain backed by a blue sky more or less covered by grey or white clouds. The foreground was usually also snow with bluish shadows. Everything was blue or white. There was little contrast, and owing to the photographic value of d/ue being almost the same as that of wire, the resulting photo- graph was of a dismal flatness and one could not distinguish land from sky. Of course this pointed to yellow screens to cut out all blue and give it the effect of black. We had much better success thereafter, but this necessitated the slow exposures I have mentioned previously. My chief camera was a Zeiss Minimum Palmos equipped with all modern features, taking telephoto pictures, stereo- scopic, } plate or panorams (73 inches long). It had a focal plane shutter calculated to give yso of a second; but the rubber shutter froze stiff, and my exposures were largely made with a red handkerchief presented to me by Wright. At the east end of the hut Ponting was busy at a huge instrument which looked like a cross between a barrel organ - and a butter churn. It was really a “washer” for cinema films. The films were wound on a cylinder, placed in the washer, covered with a lid, and then rotated by a handle. When this operation was finished we all admired Ponting’s ingenuity, for he emptied out the water and placing a rug inside the hybrid, converted it into a most comfortable lounge chair. The 23rd was Sunday, and Scott held Church service as IN WINTER QUARTERS WITH CAPTAIN SCOTT 225 usual. He and Dr. Bill would consult as to the hymns, and Bill acted as choir-master. He and Scott would test the key by striking several notes on the pianola before service. Then just before we started the hymns Bill would sound the note again and Scott would lead off with the first line. He hada tenor voice and could sing much higher notes than most of us, and made no ado about remarking, “ We'll have this a few notes higher,”’ between the first and second verses. Early in the winter Dr. Atkinson started physical measure- ments, which were always the source of much interest and amusement. They were taken every alternate Sunday or Monday, and a list of the figures for those present on the 24th April may be of interest. In addition to ordinary measurements, tests of the grip by the dynamometer and breathing power by the spirometer were also recorded. In the former an oval spring-frame is compressed and a rachet and cog actuates a finger which indicates the grip. The spirometer consists of a _ small enclosed vane which is blown round by the pressure due to One expiration. I got the heights of the officers and recorded them on the wall of the “owner’s”’ cubicle. The other measurements are given in the table herewith. APRIL 24, IQII. Name. Height. Weight. Dyn™.| Waist. Arm. Chest. Spir™. Calf. Fr. in. Stone lbs. Ing. Ins. 7 dns, Ins, Captain Scott 5 g'05 11 64 320] 30% 143 394 294°5 154 Dr. Wilson ... peso Iie or 275 zo) ns "36° “289°3) 154 Lieut. Bowers 5 4 12.0 | 280°) gzF 132 go. 230 164 Cherry-Garrard Os tn 6 300] 30, 19+ 362 267 a5 Atkinson & 675 11) OF 270 | go. 132 362 265 154 Debenham 5 84 «11, oF 305 | 29h 124 384 261 132 Taylor [moo rr 7 Bho | 352" 19° "36% 307 144 Ponting Bee SG rg) WN eh erg | Zoe x44 37 «-258°5 4h Oates... i. 5 35 TA 4a 270i FIRS TBR 40) 266° 15d Evans BOs EI MGal 2kO aa te. 40k. 270 Ase Gran... 5 11°05 13 3% 300] 31% 122 40 335 154 Wright BGS) Tip fz) 945°) sok 222 38 329 149 Simpson ,TO'Qs rE ee! 260") igo Sag” gy 408 13+ Day Nelson pabsent at |Hut Point. Mears * The waist measurement caused great amusement. Evans and I were Q ~ 226 WITH SCOTT: THE SILVER LINING Wilson, Bowers, Taylor, Ponting, Gran, and Meares were non-smokers, and Wilson, Bowers, Taylor, and Simpson were teetotalers, though several of the others swore off alcohol except on high days. At noon the northern and western sky was very beautiful, and I made an effort to record the colours by means of chalks in my diary. The dominant note was yellow shading to lemon-green in the west. Over the western mountains was a rose-pink flush verging into lilac-grey through salmon-red. To the north the band of salmon-red flanking the yellow changed into slate-blue and pale blue overhead. The sun’s rays shone gold through clouds over the Barne glacier, which exhibited magnificent purple and blue shadows. It is sad to think that Bowers’ sailor-like criticism of the magnificent study in reds and yellows was that it reminded him “of a mess of eggs that had carried away,” meaning thereby a dish of fried eggs which had been upset. Captain Scott instituted an aurora watch on this date. It was desirable to discover if periods of great magnetic disturb- ance (as shown by the magnetometers in the ice grotto) were accompanied by striking displays of aurore. There were fifteen officers in the hut, so that each man’s turn came along about once a fortnight. He was to go out at every hour and sketch the aurora if present, and of course attend to the meteorological instruments, inspect the ponies, keep up the fire, and generally mount guard from 8 p.m. to 8 am. A feast of sardines heated on a bunsen burner was promised to the gallant watchman. The most imposing objects near the cape were the stranded icebergs. Ponting and I walked across to them in the after- noon. First we reached the Arch Berg just before it fell in and became the Castle Berg, the Arch Berg, in which the major portion of the arch had fallen, leaving only a narrrow elevated strip uniting the two moieties of the berg. There was a magnificent view, looking back at Erebus through this white measured first, with the result above recorded. Wilson came next and basely proceeded to constrict “little Mary” to an incredible extent, so that he had apparently five inches less corporation than Evans and myself. Every one else followed suit, and many were the jeers at our expense. However, I got Gran to measure me according to Wilson’s method, and dropped to 30} with ease ! . Mnaey Yet fact ae Jul fn Que dasa vee sol Tag Ce Te SO ae b 4 26 - t A Pee Oey i Aish 38 | 27 Festus Rea kK a zz ee Gi tS 71D 260 10 $ hee } ci ES cg eas, % # fr Cafetl Pe ee 2k ee 8 ld ey od wk Teg a 2h 1 9g 2 4 1 2 a , / _ Wretpd Paseo ta oe (eee: R26 ; Cran {6 ee ry Zoot 28 B29 QZ. Cot ly) Ts a [ae eee ae) 228 a, is 3 ee ieee Be pee Ss Page Be a Ig 4 Boe I fp Sr wae pa LA on, AP GLIS cs Sate lar Wag inet Wer ¥o 246. % PD, | : 2h 6 22. ) Ne 3 CAPTAIN SCOTT’S AUTOGRAPH LIST FOR THE AURORA \WWe IC lst. 7 ° a | 7 oe pire IN WINTER QUARTERS WITH CAPTAIN SCOTT 227 arch, and Ponting promised himself some particularly pleasing views when the sun returned. Later we went over to the tunnel berg, which Wright and I surveyed in January. It had also broken up, and had tilted up some twenty feet on the southern side, owing to readjustments in the equilibrium. The once vertical tunnel was now only half its length, and lying at an angle of 45° (see Fig. p. 97). ME Two seals were lying in the lee of a small berg near by. As we approached they took to the mushy water immediately surrounding the berg. They lay there on the sea ice sub- merged by the pressure of the berg above it, being just under Sen ‘ee = ees ss SS The Arch Berg just before it fell in and became the Castle Berg, April 27, 1911. water, and not worrying to get through the ice into the Sound beneath. Later in the day a wandering Emperor was led in by a strap round his neck, and I held his wings while Dr. Bill pithed him by a lancet in the brain. “The last bunk has been added by Oates. He brought in some boards from the stables—not needed now owing to the decease of the six ponies—and has built an erection which presumably satisfies him. We all remark that it is only held up by a small plank nailed to Bowers’ bunk ; but Oates is quite imperturbable as usual, and no whit disturbed by ribald remarks as to a ‘ deadfall’ trap baited with oats.” I had been reading Cherry’s set of Kipling, and there was such a clatter of talk from our rivals across the hut that I* publicly christened them the Banderlog. Birdie retaliated by criticizing my pronunciation ; but I said I had no objection 228 WITH SCOTT: THE SILVER LINING to calling them the “ Bunderlohg,” and did so for the rest of the winter. Debenham fixed up a terra-cotta curtain across our entrance which had been presented by Ponting, and now we were hidden from the vulgar gaze, though one frank critic said our sanctum looked like nothing so much as an opium den. Day had run in a branch acetylene light, and Debenham had stained everything stainable a dull red-brown with that beauteous dye, “ Condy’s Fluid.” Not to be outdone, Gran fixed red linen borders on the shelves made from photographic “ window” material, while I draped my bunk with a deep blue hanging, which had originally formed part of the Sunday tablecloth. We put down all captious remarks to jealousy ; and the “Ubdugs”’ were more secluded than any other coterie in the hut. Immediately north of Cape Evans the coast-line con- sisted of alternating rocky crags and snow-drifts, but about half a mile away this gave place to the vertical wall of the Barne Glacier. In places this ice barrier rose to 180 feet, and was fissured with crevasses from which frequent falls took place. These varying features were named later on, and Wright, Debenham, and myself were never tired of examining the silt bands, and included blocks, crevasses, debris slopes, etc., which characterized the vicinity of High Cliff. The summer sun acting on some of the dark boulders included in the ice face had etched them out until they appeared like giant gargoyles projecting three or four feet beyond the general plane of the ice wall. I made a rough pencil sketch of these “ gargoyles,” and on my return to the hut asked Dr. Bill to show me how to improve on this attempt. On the 27th an important institution was inaugurated, which was afterwards called Universitas Antarctica. Captain Scott had sounded Wilson, and then he called up Simpson and myself and asked us if we would be willing to help carry out a scheme of winter lectures which he had drawn out. We had a notice board on the side of the “ Owner's’ cubicle, and on this he appended the following notice :— IN WINTER QUARTERS WITH CAPTAIN SCOTT 229 WINTER LECTURES. Some members of the community have very kindly consented to give a series of lectures during the forthcoming winter, the programme of which is attached hereto. These lectures are arranged for each week, to be given on Mondays, Wednesdays, and Fridays, after the evening meal. It is proposed that each lecture should be followed by a discussion, conducted on ordinary debating lines, and regulated by myself as chair- man. ‘The time occupied by the lecturer will be about one hour. It it not thought advisable to attempt to impose a time limit on the subsequent discussion. Attendance at lectures is purely voluntary, and neither the lecturer nor the chairman will feel aggrieved if any person prefers to read a novel or otherwise employ his time. WINTER LECTURES AND DISCUSSIONS. Subject. Lecturer, Monday, Mayr. Antarctic Birds ... E. A. Wilson. Wednesday, ,, 3. Halos and Auroras G. C. Simpson. Friday, » 5. Physiography G. Taylor. Monday, » 8. Future Plans of the Expedition,,. R. F. Scott. Wednesday, » 10. Illustrated Lecture a: kd. Gy Ponting. Friday, 5 12. Mineralogy F, Debenham. Monday, » 15. Penguins ee ar E. A. Wilson. Wednesday, », 17. Management of Horses ... LL. E..G.!Oates: Friday, » 19. Ice Problems C. Wright. Monday, », 22. Evolution of Sledge Rations H. Bowers. Wednesday, »» 24. Parasitology 4) !4] PIRQ' 4? yt tlie | 2 | ea IN WINTER QUARTERS WITH CAPTAIN SCOTT 277 He got back quite safely to the tide gauge, which was only a stone’s throw from the hut. Then he was completely lost. The wind had dropped somewhat. He tried to keep it full in his face ; and, perhaps, owing to eddies around the cape, he must have wandered due west away from the hut and towards the opensea. After some hours of helpless wandering, where he had to keep moving to prevent his freezing to death, he came to some high cliffs. He thought these might be the walls of Inaccessible Island, but there is little doubt that he had wandered south now, and was skirting Tent Island. He tried to burrow into the snow-drifts here, and so got his hand badly frostbitten. Then the moon showed faintly, and he owed his life to the fact that he remembered to have seen the moon over Erebus (and therefore east) on the preceding night. So he staggered towards the moon, and after about an hour and a half he reached Cape Evans, and was safe. We had imagined that the blizzard, constantly blowing from the south, would have enabled him to steer east to the coast ; but, owing to lulls and to eddies, and finally to his dazed condition, he lost all sense of direction, and would have undoubtedly perished but for the moon. The search parties got in by 2 a.m., and then the blizzard fury increased nearly to gale strength, and continued all next day. It was only during the six hours while Atkinson was lost that it lulled sufficiently to permit of any one venturing away from land. If it had kept up to its original or final strength, we might easily have had other casualties in the search parties. The recital of dreams, as furnishing outside interests of a sort, was occasionally tolerated in the hut. I wonder if most people go through my dream evolution? Asa child, a feeling of terror, often that primitive idea of falling and never hitting anything, which is a survival of tree life. Later, the growth of a belief that the dreamer himself never gets hurt. And then in the late ’teens the comfortable realization that it’s only a dream, to be followed by “dreams within dreams” ; and, finally, at the age of thirty by logical reasoning while dreaming. I noted that we had been south six months before I began to dream of snow and ice, and this perhaps is of psychological interest. In one dream “TI was climbing up above Grindel- wald, aided by a New Zealand guide, in company with Dr. 278 WITH SCOTT: THE SILVER LINING Bill. We got ‘bushed’ on a high peak near a hay-stack. I had a talk with Dr. Bill, in which I said that I had dreamt that the guide was going to take us down an easy way, which he wanted to keep dark, as he’d discovered it and wanted to keep it for rich tourists. We both smiled at this fool dream. Then I really awoke, and I suppose my sub-conscious self is still smiling on ‘Hay-stack Mountain’ in the Grindel- wald!” The ponies were snugly housed in the stable along the lee side of the hut. Their stable was built of the blocks of compressed fuel, and was quite a snug abode. They were rather vicious little beggars, and a walk down the narrow “aisle’’ meant a risk of a bite or a kick. Oates and Meares spent a lot of time in the stable making blubber and seal pemmican for the dogs. The western party had nothing to do with the ponies, for only those who were leading the ponies south were responsible for exercising them. In mid- winter some “ fearful wild fowl” took cover in their shaggy coats, and occasioned Captain Oates much trouble. I noted this in my journal as follows— “Baron Bernard du Day, Messenger from Captain Titos Oates. “Greetings to Debenham. “ Wilt thou peril thyself so far as to visit the stable, and for payment of one straight-cut cigarette an hour, comb the manes of ye Siberian ponies to catch ye intrepid and adventur- ous louse ? “Debenham meekly leaves his rock sections, and hies him hence!” Some of the game from the Pony Coverts was exhibited by Atkinson under his microscope. They resembled white ants in wind-helmets! No legs appeared in the specimen, so I asked if they had been worn off in the chase, but the indignant exhibitor was silent. During the autumn another grotto had been added to our outlying villas. This had been cut out in the glacieret to house Wright’s pendulums. We called it the “Cave of Pendullum.” It was usually drifted up, and we had to cut down to the sacking door, being careful not to chop the tele- IN WINTER QUARTERS WITH CAPTAIN SCOTT 279 phone wires. Inside, in one corner, was the telephone box, well crusted with ice, through which he could hear the ticking of the sidereal clock in the hut. There was also a delicate apparatus from the Cavendish Laboratory at Cambridge to register the “ionization of the air,” and a microscope and micro-camera. On an ice bench was the chief instrument, a stand carrying four short pendulums. Each was mounted on an agate knife-edge, and was surmounted by a mirror. The time of swing of these pendulums was very delicately measured, and gave the pull of gravity at Cape Evans, thus leading to an estimate of the shape of the earth. This account is somewhat brief, and this is explained in my journal as follows: “This description has been greatly interrupted by the irruptions and incursions of the Anti- Feminist, who wi// pour out his antiquated views on ‘ Woman’s Mission in Life’ into the unwilling ears of Debenham and myself. His only semi-sane argument is, that as all laws rest On an appeal to force, and as men are physically stronger than women, therefore men must protect, must rule, and (apparently) therefore must control and administer all the laws! The rest is pure selfishness.” Tuesday (11th July) was Jam Day, as I write with glee. There are two articles of diet to which I am not particularly addicted, and they are cheese and sardines. We got cheese solus for four lunches a week, and sardines every night watch. So that I used to reckon by Tuesdays! I proceeded to translate German glaciology as usual, but unfortunately Debenham and Nelson started a cag on the merits or demerits of Australian tennis champions ; and when that was over we had another as to which was the worst storm in the Terra Nova. Nelson said it took place off Cape Town, Wright said off St. Paul, Atkinson said south of New Zealand. All this talk occurred in our cubicle, and as Debenham and I had not experienced the two earlier excitements, we were not violently interested, and tried to push the debaters out, with complete lack of success. I did very little German ! On the 12th of July we had a record blizzard. For over twelve hours its mean velocity was above forty miles per hour, and it rose above seventy miles per hour at 9.15, 11.15, and 5.30. At 9.15 p.m. it fairly boomed over the hut. Luckily the hut is so surrounded by “lean-tos”’ and great snow-drifts \ 280 WITH SCOTT: THE SILVER LINING that the wind is led gradually on to the Hut, else it would surely have blown us into the sea. This blizzard was accompanied by relatively high tempera- tures. It roared all that day, but after lunch, on 13th, I write: “. .. it is getting cooler; none of that oppressive heat of +8° F. (24 degrees of frost), and is now much nicer (—7°); so that the leaks have stopped, after damping Gran’s mattress considerably.”” The lunch was evidently cheese, so that I confined my attention to brown bread, dripping, and cocoa. We were able to leave the Hut in the afternoon, and walked up to Bertram. Skua Lake was so brilliant, I thought at first it had melted, but it was merely polished like plate- glass by the furious drift. Teddie Evans had been engaged for some days on plotting the chart of Dry Valley on the first western journey. He made a fine drawing, with “form-lines” inserted, so that the shape of the glacial valley showed up splendidly. Captain Scott, Evans, and myself discussed the nam- ing of the new glaciers, etc., now first charted. We had given some of them pro- visional names on _ our journey, and the Owner chaffed me somewhat, but said he didn’t mind a bit. There were two distinct glaciers included in the Ferrar Glacier, which Scott had named in 1903. He asked me if the one entering Dry Valley was going to be described as a type; and I said that its exposed bed was probably unique in Antarctica. Then he said, “ We'll call it the Taylor Glacier.” So that on 15th July I became a cartographic entity ! One of the most interesting paragraphs in the German tome through which I was laboriously wading tended to show that the world was approaching another Ice Age rather than leaving it behind. In the Swiss Alps the Germans have shown that there were no less than four Ice Ages included under the last glacial The Twin Glaciers (copied from diary, July 15, 1911). IN WINTER QUARTERS WITH CAPTAIN SCOTT 281 epoch, separated into three inter-glacial periods. The general temperatures can be obtained by studying the depression in the snow-line and the position of the moraines in these four Gunz Mindel Riss — Wurm Wow She futore lce-age 1e-70 Ice Ages. It really looks as if we were now in an inter- glacial period, rather than permanently free from glacial con- ditions. However, the next Ice Age is seventeen thousand years off, even by the lowest computation. I was able to make a characteristic sketch of Erebus on the 18th July. The steam cloud extended across an arc of 90°, Similar reversal of the steam banner of Erebus at noon, May 1, 1911. and appeared to be drifting “ the south. The banner was possibly a hundred miles long. On the surface there was a cool southerly wind, in just the opposite direction. Several fine undulations showed in this banner, and at times a hummock of steam over the crater pointed to extensive outbursts of vapour. Far to the south the banner was very faint, and reminded one of the Milky Way. The dawn colours were very beautiful. We were not to 282 WITH SCOTT: THE SILVER LINING see the sun for over a month, but over his position were belts of crimson lake, dull red and green, with pale blue above. Sometimes the dogs would accompany us up the Ramp. Atkinson and I went up to read Bertram on the 21st, while Stareek and Tsigane trotted alongside. The latter is quite sociable, while Stareek, one of the leaders, is one of the most imperturbable. According to Atch, he has been seen admon- ishing Tsigane for his undignified behaviour ! These walks were good exercise, but the weather was getting colder (though mid-winter was past) and —35° was quite common. My first occupation on reaching the Hut was to go and hold my head over the stove. After some minutes the lumps of frozen breath which surrounded my mouth would melt somewhat, and I was able to free my beard from the flannel of my helmet ! After Church service on the following Sunday (23rd), Ponting gave an exhibition of cinema pictures in his dark room. It was a very select show, as there was only room for an audience of four! His films were megatives, so that the black and white were reversed. Under these circumstances the seals appeared white and more slug-like than ever, while the white shadows following the penguins were most uncanny. While we were in the dark room Simpson called out that the wind was still rising. It reached eighty-four miles per hour at 8 p.m., which was the record during the first winter, though this was easily beaten in 1912. The 26th of July was a splendid day, and without doubt marked the return of daylight. Simpson and I visited Bertram and were able to read the thermometers without recourse to fusees. We marched on the Erebus Glacier some distance, and found numerous potholes in it, due to stones sinking therein. On our return I continued plotting the chart of the Koettlitz Glacier. Wright is obtaining interest- ing results from his ice sections by “rubbings” of the ice striae with a soft pencil. These photograph quite well. We were well stocked with books in the Hut. Almost every officer had taken down some standard novels in addition to a few text-books, and curiously enough there was very little overlapping. For instance Cherry had a row of Kipling’s works which almost all of us appreciated, Day had Dickens, Debenham had four or five poets, and more popular still—a IN WINTER QUARTERS WITH CAPTAIN SCOTT 283 collection of thirty ‘“ paper-back sixpennies,’’ which every one was always borrowing. He kept them in a box under his elevated bunk, and I remember one evening after we had turned in, some one came into our cubicle and started burrowing about. Debenham said, “ Now then, what are you after down there?” A voice replied, ‘‘ Where do you keep those sixpenny novels, Debenham?” It was Scott, who couldn’t sleep, and wanted some light literature ! I had two or three of Wells, Browning, Tennyson, and “‘ Martin Chuzzlewit.” However, though my library was small, I used the official library more than any one! I have mentioned elsewhere the splendid little library of standard fiction presented largely by Mr. Reginald Smith. This con- sisted of about 250 portable volumes published by Smith, Elder and Co., and by Nelsons, There were Merriman’s, Bronte’s, and Conan Doyle’s, and all the shilling editions of noteworthy books by authors like Gosse and Belloc. Mr. Mackellar gave us many other volumes, especially some small art books. These lived in Day’s bunk. Then Admirals Markham and Beaumont presented us with many rare copies of books on Polar Exploration. These were constantly being read, especially by Bowers, whose lectures on sledging rations and polar clothing led him to read every word. Candidly I must admit that it was not cheering—when the blizzards were booming over the hut and all was dark around us—to read of Greeley’s awful suffering in the Arctic, where forty out of fifty men perished ; or of the loss of the feannette and her crew in Siberia; but still the volumes were always being referred to by one or other of the officers. We had several larger books, Haydn’s “ Dictionary of Dates,” which didn’t seem to be much troubled, and Harms- worth’s Encyclopedia, which was always in demand. Cherry had the large Times Atlas, and we had Paul’s “ History of the 1gth Century,” and Harmsworth’s “ History of the World.” Oates brought along Napier’s “ Peninsular War,” and rarely seemed to read or need aught else. I had a bet with him that I would finish Paul’s six volumes before he had read through Napier. However, neither was completed, though Oates was along way ahead! Scott had a shelf of poets and a number of foreign novelists, chiefly Russian and Polish. I had finished all the lighter literature in about three 284 WITH SCOTT: THE SILVER LINING months, and thereafter was able to advise some of the others as to works meriting their fleeting attention! It occurred to me that it would be amusing to try and discover the tastes of the fifteen officers of the hut. Books were naturally often discussed. Oates must have been reading some of Merriman, for I find that Simpson took exception to his praise of the latter's works on meteorological grounds! This seems rough on Merriman ; but Simpson said it was not possible to see the midnight sun at Tver, and he also objected to the wrong use of the word parhelion. I’m afraid I’d missed these “ pro- fessional errors,” but I remember what seemed a serious flaw to me in Davis’ “ Soldiers of Fortune” (otherwise a rattling yarn), was the author’s weird geological description in the first chapter! Similarly we expected Captain Scott and Seaman Evans to revel in Kipling’s sea yarns, whereas they were not enthusiastic. Both made the same criticism ; Evans saying that there seemed to be a lot made about a little, and that, “anyway things isn’t so concentrated-like in the Navy!” I hope living authors, if they ever read this, will rise superior to our criticism ! Debenham didn’t like “ Kipps”’ ; in fact, except for Wright I couldn’t get a word in favour of Wells. Even Nelson, who liked reading “ Anne Veronica,” declared it was a piece of satire from beginning to end, in which Wells was obviously gibing at his readers! The only book Nelson and I liked in common was Gissing’s “ Born in Exile,” and I grieve to state that the “ Owner ’”’ characterized this as “ Tosh!” ‘Richard Yea and Nay” is loved by Debenham. I couldn’t read it, and declared it was not free from gross errors. (Pace Hewlett!) Challenged thereon, I said I had visited the castle at Gisors, and that it was still a well-preserved ruin, whereas in the novel it is “razed to the ground.” ‘This, of course, led to a cag on the meaning of the word razed, in which all the hut took part, and I’ve no recollection as to who was supposed to have won! Any Canadian novel that was appreciated by one man, would be caustically slated by Wright. I think we were all better at criticism than appreciation. Chambers’ “ Fighting Chance” was damned “‘ because the hero kisses a girl under water” ! However, as a result we began to get some idea as to each other’s tastes in literature. I was a sort of referee, in that Ponting, Day, Debenham, Wright, and Simpson, would some- IN WINTER QUARTERS WITH CAPTAIN SCOTT 285 times read a book on my recommendation, while Meares, Oates, and Nelson, always went for what I didn’t like ! We had very strong winds about this time, and were very anxious to know how the Cape Crozier party were pro- gressing, They were due back, and had had awful weather judging by our experience. On the 29th Atkinson and I made our usual excursion up the Ramp to “ Bertram.” There was no drift, but the wind rose to fifty miles per hour at times. We could hardly keep up on the ice, and I was actually blown bodily off the little cone on which Bertram was erected. Later we went out to “Archibald,” letting the wind blow us there. Scott said he saw us start, and when he looked again in a few minutes we “ were mere dots on the horizon !” But it was not so easy getting back, and I only managed it by bending double and watching our outward tracks. On the 1st of August I went on night watch at 8 p.m. Most of the men were turning in, when Hooper called out, *‘ Here’s the Cape Crozier party.” So we all rushed out and there were the three of them. Cherry staggered in looking like nothing human. “ He had ona big noseguard covering all but his eyes, and huge icicles and frost stuck out like duck’s bills from his lips! They had been away five weeks and a day, and it had been hell all the time practically. After leaving Meares and Sunny Jim, they had pushed on and camped four miles this side of the 1902 Hut. The next day they camped on the Barrier. There had been but little snow on the sea ice, though a snowdrift led them up on to Barrier. Here awful soft snow began, and it was very cold. They had to relay most of the way, and sometimes even with one sledge they could hardly get a move on. It was like pulling in soft sand, and often they only seemed to be marking time. “It took them three weeks to get to Cape Crozier, and they remained there ten days. They were unable to get any blubber and had to return when only one tin of oil was left. Blizzards held them up off Mount Terror, and here Birdie is credited with sleeping three days and nights (bar meals). The other two didn’t! They spent three days building a stone igloo, and pitched the tent to leeward. A tremendous blizzard came up and blew their tent away! They had now a poor chance of getting back, and proposed to dig snow holes 286 WITH SCOTT: THE SILVER LINING each night and cover themselves over with the floor cloth. Luckily they found the tent a quarter of a mile away, just on top of the sea cliff! They had camped just south of the big cliff under which we had rowed in January, 1911. “All the ice blew off the Ross Sea with the force of the blizzard. They were only able to get down to the Emperor penguins on one day. These were nesting—if such it can be called—on a piece of old sea ice between the cliffs of Cape Crozier and the high Barrier Ice. They had to crawl down between the Barrier and the Rock Cliffs, and here Birdie stuck as his clothes had frozen so stiff! There were only a hundred penguins there, instead of 1000 as they had expected. They spent two hours getting down and could only carry away six eggs, of which three broke. Cherry says his mits were made warmer thereby! The temperature was down to —77° F. (a sledging record) and often below —60° F. Their sleeping bags froze stiff, and they couldn’t roll them up, while Cherry’s was too big and never thawed except where he touched it ; moreover, they tore badly when they were getting into them. “On their return they could only make one mile on the first day, and Birdie went down a crevasse to the length of his harness. They managed to get him up by a bowline on the alpine rope. On the last three nights Cherry said that no one slept. They used to doze on the march and over their meals, but were too cold in the bags. On emerging from their tents they had to be careful to hold their heads as they would bear them later, for their clothes froze and held them like a coat of mail !”’ About three miles to the south lay Tent Island ; so called because in 1904 the men cutting a canal through the ice had their tent there. Atkinson and I walked over there early in August, to see if we could find his belt, which he had lost on July 4th. I carried a plane table to continue my survey of these islands. It was. extraordinary to see footprints in the gravel, which must have been made by Priestley in 1907, though they looked as fresh as my own. We visited Clarence on our return, and found it to be much less imposing than Archibald or Bertram. Merely a little box at sea-level, containing two thermometers, but no stand or cairn. It was getting gloomy and we just returned IN WINTER QUARTERS WITH CAPTAIN SCOTT 287 in time, for Atkinson’s feet were pretty well gone in his old finnesko. It is a queer fact that both Atkinson and myself dreamed that the Cape Crozier party were returning on the night before they arrived. In my dream I modestly went out and pulled their sledge back. However, 1 don’t think we pub- lished their approach on the strength of these dreams, else we might have claimed some credit for our superior intelligence ! When there was no wind it was quite pleasant strolling about by the light of the moon. In the long winter night it was cheering to realize that we could tell where the sun was even if we hadn’t seen him for over three months, for the moon’s brighter face of course points to the sun. This com- forting deduction led to the following astronomical effusion in §.P.T. :— THE ERRANT SUN, Throughout the night, Nor life nor light, E’er chases gloom away ; But still the moon Foretells full soon, Arrival of the day. For each bright ray Shot to the day, By Luna’s silver bow, Transfixes straight Her lucent mate, The errant sun below. I wrote at the foot for Dr. Bill’s edification— “If your artist can rise to the occasion will he please illus- trate this poem (sic) with a sketch?” and to this note there hangs a tale as shall appear later. Wright and I went off for a tramp towards Inaccessible Island. We came across some of the queer snow stalactites which I called “Cold Feet.” They were due to snow col- lecting on the ends of icicles where they were somewhat sticky. The snow built out a “ foot” to windward, and they looked exactly like long white stockings. Near the big icebergs Gran pointed out to us an Emperor penguin and yelled to us to kill it. On approaching it, 288 WITH SCOTT: THE SILVER LINING however, it objected strongly, having legs and arms and answering to the name of Lieutenant Evans ! The pressure of the sea ice had raised great ridges of ice around Inaccessible Island. Some cakes of ice were most precariously perched on the top of these six-foot hummocks, The queer structures resulting from the buckling and cracking of this six-foot thick sheet of ice reminded the geologists very strongly of the type diagrams used to illustrate the major folds and earthquake cracks in the earth’s crust. On the 4th of August we made a real start for the summer campaign by taking the two motor sledges out of their winter quarters. “It was frightfully heavy work and took about twenty of us to move one a foot. I wouldn’t care to go over a snow-lidded crevasse in one.” Simpson gave us a good lecture on General Meteorology in the Antarctic. I thought Simpson didn’t lay enough stress on the purely local character of our storms. I said that he reminded me of a minnow living behind a stone in a big river, wildly excited over every eddy and paying more attention to them than to the river as a whole. This “cag” between the scientists greatly delighted certain of the ribald, and Simpson was referred to as the “ minnow in the eddy” for some time thereafter. The usual occupations filled our time during the first fortnight of August. I was busy mapping the vicinity, trans- lating German geology, calculating sledge stores, and writing a long article on the Inmates of the Hut for §.P.T. On the 14th I wrote, “ To-day is a beautiful day, with a tempera- ture of —38° F.; but with no wind, so that one can stay out quite comfortably. It is very light now, for the sun is due in five or six days. Erebus is very active, and is puffing up big gouts of steam. Debenham measured one which rose 4000 feet in ten seconds! The banner then sweeps south and east. It is lit up by the hidden sun in a most beautiful manner. I say the colour is tawny, Atch says russet, Birdie burnt sienna, while Bill says it’s a mixture of vermilion and yellow ochre! Anyway it is very pretty, and Debenham says he can see inside the crater.” Through falling into a small crevasse 1 found some beauti- ful ice crystals above the Ramp. Later I turned up some IN WINTER QUARTERS WITH CAPTAIN SCOTT 289 slabs of ice which had covered old water channels and their lower surfaces were sparkling with beautiful basket crystals half an inch across. In some cases these were branched like candelabra. Wright managed to photo some of them satis- factorily, for unlike our rock collections, 4is specimens were extremely fragile and hard to preserve. I renovated my smaller camera which had suf- fered so in the gale. After I fitted it with a simple “ flip- flap” tin shutter, this piece of apparatus was always called the mousetrap. / By this time most of the = “«”¢7' "ivi diarists had lost their early enthusiasm. The Owner wrote an hour or two each day. Gran and myself were probably the most voluminous writers. Debenham, Cherry, Wilson, and Simpson also kept records ; but most of the others affected to despise diaries. Wright would bring his along once a fortnight, sometime when I was engaged on mine, and look through it for references to him- self. We often went for a walk together (invariably towards the Erebus Glacier), so his diary was often something like this— or. Jhe Mousetrap Cameva (4 Bru Aug. 1.—Went up the Ramp with G. T. » 2-—Ditto. 9 3-—Ditto. 55 4-—No entry. I suggested he should fill in his blank days with “ Did zor go up the Ramp with G.T.”! The “illiterate” took a great, if transitory, interest in our labours. Birdie seeing me stuck for copy on August 13 sang out, “ Write—Turned in, turned out ; ditto, ditto. That'll fill your diary!” Atkinson assisted as follows: “On night watch ; slept till 10.30; woke up and was very pleased to see Atkinson, because he’s such a good fellow!” Cherry’s quota, “ We have many cags on scientific subjects and so acquire much merit.” While Uncle Bill, with a merry twinkle, added, “‘ And next week we'll get on to some serious work !”’ I think the seamen enjoyed life in the Hut as much as U 290 WITH SCOTT: THE SILVER LINING any of us. The night watches must have pleased them immensely. To see a weary officer nodding and shivering all through the night, while they were snugly rolled in blankets and enjoying an uninterrupted night’s rest, was just the state of things they would appreciate! As I have noted already, some of them unconsciously imitated Kipling’s Emanuel Pycroft in “ Bonds of Discipline,” feeling they might never have the opportunity of reprimanding an officer again, they would pour out (from the shelter of a bed curtain) the vials of their wrath on any unlucky watchman who fell over the fire-irons or discomposed their slumbers! It is fair to state that in the next winter they cheerfully took on night watches, and were quite equal to reading all the meteorological instru- ments. The 15th was a rather threatening morning; the wind coming from the west, which was most unusual, ‘“ Deben- ham says this implies a blizzard. Every one has a different theory of blizzard forecasting. Mine is simple! If you've had four days fine, you’resure to get a blizzard! This works well in winter.” “Last night we had an addition to our Antarctic family. Innumerable pups accrued to us, descendants of our long- haired collie, ‘Lady,’ and the Siberian dog, ‘ Beely-glass.’ They occupy a corner of the stable, and add life to our ménage. Julik went off some time ago, and is undoubtedly lost ; though it is difficult to see how, unless he got into a deep crack. The other day Peary and Cook and another dog (harnessed to the cook’s light sledge) bolted. They tipped Clissold into the tide-crack, and made for Cape Royds. Luckily, Atkinson managed to catch them. Tsigane, Peary, and Cook are the only dogs I’d care to take back.” The others were too unsociable, and though by no means savage when well fed, they were little interested in their owners’ doings, and exhibited none of the so-called dog-like affection. Wright and I walked south over Cape Evans, and above the curious belt of moraine, which we called Land’s End. It was pretty cold, for Evans found the mercury frozen that day at Clarence ; but as there was no wind this did not affect us after the exercise made us warm. Sometimes one could feel one’s nose “go with a ping,” as if the blood had really solidified in one’s veins. But vigorous rubbing and nursing in IN WINTER QUARTERS WITH CAPTAIN SCOTT 291 the warm palm of one’s hand usually restored circulation. As long as one’s heat energy was abundant there was no risk ; but when vitality was low, through fatigue and hunger, frost- bite was certain in any cold extremity. As we walked over the Erebus Glacier we noted numerous circular dark patches in the ice. These exhibited maze-like patterns (arabesques), and marked where stones had sunk through the ice. There were no stones visible on the surface, and no source of supply, so that either these were very ancient, or else they were due to the effect of the sun on stones deep buried iz the glacier ice. The Land’s End Ridge was a mile long and only a hundred yards wide. It was most pre- cariously placed between the glacier and the deep sea, and was perched on a line of cliffs which were just uncovered by the retreat of the glacier. Monoliths of kenyte lava and ash (tuff) were scattered along the moraine. Great debris-cones, capped by huge un- weathered blocks of kenyte, rose to thirty or forty feet high. The Land’s End cliffs abutted on the crevassed piedmont glacier to the south, and from their 150-feet elevation we could see the curving crevasses crossing the glacier, and could determine that the “ ice-caves” were but these crevasses seen in vertical section on the ice front. To the south extended a fine view of Turk’s Head, and the long promontory to the Hut Point. We returned towards our hut, and attempted to reach the sea-ice from the moraine. In the dim twilight we judged that there was a twenty-foot gully between us and what looked like an iceberg. When we dropped into it, it was only four feet deep! So deceptive is a snow surface in the absence of light and shade. The next day was cold again (—35°), and Gran and J climbed Inaccessible Island. I carried a theodolite, and fixed it on the top (521 feet). It was awfully cold work. I had to remove my fur gloves, and my neers “went ’’ very soon, and standing still made my toes lose feeling also. By the end of an hour I could do no more, and was so numb that I could not put the theodolite back properly in its case. My fingers and toes ached badly all the way home, but had recovered on arrival. I went out to the rubbish pile and commandeered enough material for a book-binding kit. I bound up some glacial 292 WITH SCOTT: THE SILVER LINING pamphlets into two pieces of “‘ venesta wood” from a packing- case. The rest of the case made the sewing frame. Two iron clamps, lent me by Simpson, made the press, while I had found a queer residue in the glue pot, which I used in default of better. Towelling for head border, and tent cloth for the back completed it. Next day I wrote Hoc Pegit in what is probably the first book professionally stitched and bound in boards in Antarctica. Atkinson gave us a clear and concise account of scurvy, from which I gather that our chances of seeing any are few. LECTURE ON SCURVY By ATKINSON History: Scurvy was a dread disease about the end of the 18th century. Anson lost 300 out of 500 men from scurvy in 1795, but about that time Blaine introduced the use of lime juice, and since then it is practically unknown in our navy. Symptoms : It is a general non-febrile disease, and not contagious. It is marked by mental depression, syncope, and debility, and the morbid blood arising often causes characteristic patches on gums, thighs, etc., like bruises. Atkinson modestly ascribed the cure to the Naval Medical Corps (loud cheers !). He said that immunity was possible, and was assisted by plenty of lemons and other vegetables (sic /). Detection: Ralph found that if you gave too much acids to animals they got scurvy, and Wright also believes it is a form of acid intoxica- tion. Serum is obtained from the clotted blood of the patient. This should be alkaline in reaction, and its alkalinity is tested by neutralizing it with various strengths of sulphuric acid. Thus 4, or ¥ normal] strength of acid should be neutralized by alkaline serum. If only J, » . : « ” normal acid oo 1S necessary to neutralize, then “you have your scurvy. Prevention: Fresh meat alone does not prevent scurvy, since they had plenty of horse in the siege of Paris, and yet sa heavily. Possibly it is too acid. Fresh vegetables seem to contain an alkaline salt which is helpful, and possibly sodium lactate is a useful drug. Nansen, however, believed in change of diet as being very helpful. In the discussion Uncle Bill said that many of the symptoms noticed after sledging were purely due to the lowering of tone. If one entered upon hut life gradually by living for a day in the annexe you wouldn’t feel funny feelings in your toes ! “T asked if a vegetarian diet would do down here? We IN WINTER QUARTERS WITH CAPTAIN SCOTT 293 have no fresh vegetables, but we have bread, butter, cocoa, sugar, jam, porridge, tinned fruit, tinned milk and cheese. (I lived on a less varied diet in Cambridge, only I still don’t enjoy the cheese lunches where the pungent stilton stalks around, and the exclusives have to collect together and wave the phantom off.) Bowers said that Bill developed spots on his face on the Crozier journey; but Bill swore they were beard sprouts. Birdie had been nodding a bit, so I said he was evidently scorbutic, as he exhibited a tendency to syncope, deposit of fat, and an inflamed head (a cruel hit at his red hair). Ponting had been listening anxiously to the doctor’s criticisms of sausages, and various potted meats, and then read us a cable he had received in November announcing that a friend meant to send a half ton of sausages by the Relief!” On Saturday night (19th August) we experienced the maximum wind pressure of the winter. “It rose from forty- five miles per hour to eighty-six miles in one fell shriek.” There was such heavy drift that it blew through the outer walls (of cases) and filled the annexe. The temperature had risen astonishingly, for we found “Bertram” registering +4° F., whereas a day or two before mercury was freezing! The blizzards were sometimes accompanied by a sort of “ foehn ” wind warming affect, and nearly always raised the temperature slightly. They swept away the stagnant heavy cold air which 7 at sea-level, and which normally surrounded the ut. The 21st of August was a calm, clear day. The sun was due in a day or two now. Nelson was having some trouble with his soundings at the “Igloo.” So seven of us marched out to help him free his rope. It was quite a procession, Nelson going first to fix a block and tackle (pronounced saikle/) on his obdurate rope. Then Atkin- son and Clissold—-who worked the fish trap, and so were professionals in such jobs—walked along in a dignified way. Then long Day on ski, followed by Debenham also on ski, and causing some amusement by his ‘ croppers.” Finally, “Trigger” Gran started long after us, and “ flapping ” along on his ski easily caught us up. I could easily keep up over a couple of miles without ski, but over a longer distance there is no doubt as to the advantage of the ski. We all hauled on the “taikle,” and so broke Nelson’s rope away 294 WITH SCOTT: THE SILVER LINING from the bottom, where it seemed to have frozen in. Then dropping the “earth” wire of his telephone circuit into the water I rang up Simpson in the hut, and heard him with great ease through the bare aluminium surface wire. Debenham and I climbed Inaccessible Isle to try and see the sun first. Wewent up by the usual route, but had to kick steps in the thick snow which now covered the gravel slopes. There is a magnificent windblown gravel ridge on the lee side of Inaccessible Isle. The blizzards shoot up the southern face and drop their dust contents beyond the central notch on the northern slope in the form of a long ridge about fifty feet high. We obtained a fine view of the western cwm valleys below Mount Lister from this elevation (520 feet). To the north we could see a bright glow over the Barne Glacier and good 520' 4, Ay 500 (OEE: Zz ia £ ———— : = SS ZZ WY —— > We ~G, Wy lg he i ra ee sail pe, N vid G Meinl iN \) ' _> SS XY ms = wy Jhe wind-ridge on Inaccessible Isle , with racks 21-86-41 sun shadows on Mount Lister, the first time for four months ! But we did not see the sun’s disc at all. The sun was due on August 22, so it was natural that a blizzard should spoil all chances of seeing him! We took him on trust to the extent of champagne at lunch, when Scott toasted Lieutenant Campbell’s birthday also. “‘ A snorting blizzard:; never saw such thick drift. It wet one, so that one’s hands froze in no time. None went out- side the hut.” The table resembled a grocer’s shop from now on, for Birdie started bagging provisions for the sledge journeys. Pemmican was taken out of the tins, broken up, and bagged first, and then cocoa, butter, sugar, in fact everything but biscuit, which was left in the 40-lb. tins as sent to us. “2.30 a.m. on the 24th.—It is now my night-watch, and IN WINTER QUARTERS WITH CAPTAIN SCOTT 295 I have finished making the slides for my next lecture ; I have read M. Beaucaire, had two slices of toast, gone on the roof and cleaned out the blizzometer tubes, and washed my feet. The sooner 3.30 arrives (and Nelson with it) the better ! “Tn two months we shall be away on the veldt again. I have lots of prints to make, and must continue my German and physiography ; but I have done about as much as I intended, and found the winter a very pleasant and busy time. It is wonderful how exhilarating a fine day is, though the last few days have been the limit.” Next day it was still blizzing, with the temperature up to +11°! The drift was lower, and Nelson managed to get out to his igloo on the sea ice. Captain Scott asked Debenham and myself to map Cape Evans in considerable detail ; while Lieutenant Evans carried out the coast survey and Wright obtained heights and ice- cliff data. As a result Debenham and I were out with our plane tables fairly continuously in the next few weeks and got to know almost every rock upon our little promontory. Wright and I climbed the Ramp in our anxiety to see if the sun was still alive! but without avail. The clouds on Erebus were worthy of note. During the day huge billows collected to the south below the summit, and at 7 p.m. these disappeared, and the steam cloud (which had hardly showed before) shot up several thousand feet and then spread out as a banner to the zorth. This latter direction was unusual, as the upper air currents usually went due south. On our return we found that Simpson had seen the rim of the sun about 3 p.m. from Wind Vane Hill (at noon it was hidden by the Barne Glacier), so that the meteorologist was the first to welcome His Majesty’s return. On the 24th I gave a lantern lecture on Polar and Tem- perate Glaciation. As usual Ponting kindly made most of the lantern slides and operated the lantern. Afterwards he showed us some of his magnificent Swiss slides. On the 26th I managed to improvise a satisfactory plane table from a telescope tripod and my drawing board. We had a spare sight-ruler, and with this primitive instrument I successfully mapped my section of Cape Evans. We could always orient on far distant peaks, such as the Matterhorn, fifty miles north-west ; or Castle Rock, twelve 296 WITH SCOTT: THE SILVER LINING miles south ; and this saved a lot of trouble with the usual “three-point resection” method. I climbed up the Ramp and read “ Bertram.” I could see the sun shining on Inacces- sible Isle, and even on Hut Point far to the south, but it would need to get considerably higher before it illumined the Ramp. Lieut. Evans was setting up signal flags on the prominent debris-cones, and we returned together vid the “ Slippery Slopes,” Evans justifying the name ! “ Just before I reached the Hut I felt exactly like Peter Pan, and saw that I had regained my shadow! I walked up to Wind Vane Hill, and there was the old sun showing half his disc over Cape Barne Glacier! About 2 p.m. I went out with the ‘ mousetrap’ camera, and took some photos to celebrate the event. I gave four seconds (with F. 45) on snow banks, etc., lit by the low-lying sun. This was too much, I believe, but the photos were fairly satisfactory and worth the trouble considering when they were taken.” Wilson reported some queer alge deposits above Gully Bay, so we went off to investigate them. There were two layers (about fifty feet above the glacieret) in the soft kenyte gravel. I had little doubt that they were lake alge which had grown when the water was held in by a larger ancestor of the present glacieret. Just to the west were beautiful ex- amples of these ice-dammed lakelets, with “ Glenroy terraces ”’ marking various contours on their shores, just as in the historic Glenroy region in Scotland. Only in these Antarctic specimens the ice dams are still evident, whereas their absence in Scotland made the origin of the Scotch terraces a puzzle for many years. I have made frequent mention of the debris-cones on the Ramp. Their origin was often discussed by Scott, Wilson, Debenham, Wright, and myself. Scott and Wilson believed they were dumped over at re-entrant angles in a bygone ice- barrier wall. Debenham compared them to the cones and hollows we had seen over in the western moraines and thought they were due to the melting of submarine ice. Wright and I believed them to be due to the weathering of huge erratics. On the 27th Gran and I made the rather obvious test of cutting one open. It was six feet high and lay just on the edge of the steep slope of the Ramp, whence all debris would “Jsam oy 0} sivadde dot-vas ay Ul Sieg foUUNT, aYJ, “3s9M pu ysva Ayaryo uns vary ayXuary Jo sdosoyno paSSni ayy, “purljoog ‘soovsia yp, Aoruapy jo Wonvutioy ay urefdxa surep aor asayy, (‘ya1ou ay} 0} uMOlq shee ore syyTIp oy.) *sAarpns [[eus ssosoe Surtu10y Mous pailip JO sjartaioer[s 0} ang "1161 “6z “1aag “SNVAA AdVO JO SLATANVI IN WINTER QUARTERS WITH CAPTAIN SCOTT 297 slip down the Ramp and save cartage. The upper face was a friable dry gravel. We heaved out two huge blocks the size of a man’s body and found them fitting into other blocks of the same rock. We cleared away the top portion of one half, and then came to a huge block evidently extending to the foot of the cone and right through it. All this was frozen stiff into the kenyte soil of the Ramp, and it was beyond our powers to shift it. However, we had definitely proved that this symmetrical cone was solid, and was piled around a core of kenyte blocks. <<] met the ‘Owner ’ after lunch and introduced him to the ‘dissected cone.’ He seemed to think it a strong argument The Dissected Debris-Cone, 288-1 in favour of our long-held theory. Wilson basely hit back at me for upsetting his argument with a caricature in the South Polar Times, which is here reproduced. ‘The difficulty in disposing of all the instruments needed by a geological surveyor is also hinted at in the gear encrusting the queer object on the debris cone.” “August 30.—A cold day, —33° with wind. Natheless, Deb and I went outabout noon plane-tabling. I had finished my stations and carted the table about, filling in details. But it was mostly a ‘cabman’s war dance,’ jumping and flapping one’s arms to keep warm. I found that a great deal of the ice sheet to the north was only six inches thick over gravel, the latter appearing in the eddy gutters to the south of every big boulder. “It got too cold to work, but I swore I would stay out as long as Debenham, Finally, at 1.15, 1 could stand it no longer, and made a beeline for the Hut, finding he had returned a minute or two earlier!” The next few days were similarly occupied. I made a pantograph (to reduce or enlarge drawings), and so obtained a 298 WITH SCOTT: THE SILVER LINING fairly accurate plot of all the sections of our map. The result is given herewith. One can readily see some method now in the queer physiographic features of Cape Evans. It can be subdivided into several zones, which may be tabulated as follows, pro- ceeding inland (east) towards Erebus :— 1. Kenyte cliffs and ridges, of rock in situ (about fifty feet above sea-level and chiefly to the south and west of the Cape). 2. Low-lying plains with lakes about twenty feet above sea- A Peculiar Animal seated on the Top of a Debris-Cone. level, due to erosion and deposition from 1 (chiefly in the north-east of the cape). 3. Glacierets and ice-dams running north and south, and due chiefly to drifts distributed by the southern blizzards. On the low cape and on the Ramp also. 4. The continuous “Ramp” ; a steep slope (30°) extend- ing from “Low Cliff” practically to Land’s End Cliff, ie. about two miles. It varies in height from 100 to 150 feet above sea-level. Partly composed of rock im situ and partly of moraine just uncovered by the retreating glacier of Erebus. Barne Glacier High Cuff Low Cliff SS a VY Sea tce = ees | Feel Q ° (000 2000 Cape Evans Physiographic features of Cape Evans, due largely to the retreat of the Erebus Glacier. 300 WITH SCOTT: THE SILVER LINING 5. The boulder-strewn plateau parallel to and east of the latter, and about 150 to 200 feet high. It is largely ground- moraine, but contains some ancient ice masses, and is affected by soil-creep or solifluxion. 6. A zone of large blocks (with ice between) which occurs chiefly in the north-east, and merges into the Erebus Glacier. Both 5 and 6 contain numerous debris cones, which are especially large in the south-east over Land’s End cliffs. 7. The continuous Erebus Glacier which extends un- interruptedly from Cape Barne to Turk’s Head, and walls in Cape Evans to the east. There is not much movement in it just behind the cape, for there is no ice “ wall” but a gradual merging of rock and ice. My diary proceeds as follows :— “* September 1.—I fear I must give this a miss. Titus Oates says, ‘You were probably caulking and coughing, or blatting. But if the latter you’d remember!’ (These rude words refer to a slight cough that worried me at this time. ‘Caulking’ is sleeping, and ‘blatting’ is arguing.) The Conservatives were evidently waking up, for I note one of Atkinson’s remarks. Colonials go to London and murmur ceaselessly, ‘Change and decay, in all around I see, Except in me, O Lord, except in me!’ This misquotation afforded the ‘ True-Blues’ (Cherry, Birdie, Titus, and Atch) great joy about twenty times a day. We Liberals scorned to use such feeble wit in upholding our principles.” The next lecture was one delivered by Birdie Bowers on the Evolution of Polar Clothing. I took fairly full notes of this lecture, which represented much reading on Birdie’s part in our extensive library of Polar journals. LECTURE ON “EVOLUTION OF POLAR CLOTHING” By Bowers. September 1, 1911. There are many fabrics which can be used, for instance, cotton is very satisfactory for some purposes, as we see in our windproof overalls. Fur was naturally first used, and Ross, on his magnetic pole expe- dition, was the first to employ fur sleeping-bags. Weddell found boots a great difficulty, and had to cut upall his gear to make new ones, Some Arctic explorers used blanket squares (sixteen inches across) instead of IN WINTER QUARTERS WITH CAPTAIN SCOTT 301 socks. One must be careful not to have boot-soles too rigid, for this induces frostbite. It is curious that the Eskimo garments leave the skin completely bare at back and knee. , Bird-skin clothes are very warm and very light. In one expe- dition devices were painted on the backs of the white jackets to give the SSS fi 2 SS TS TS eS (es E.P.froma sketch by G.T. 1913. A book-plate illustrating Polar clothing. men behind something dark to look at, and so minimize snow- blindness. With regard to mits, thumbless gloves are best for very cold weather. Greely had gloves with two thumbs, so that they could be used on either hand, It is foolish to rub frostbites with snow, for the skin is chafed ; flannel or a bare warm hand, etc., is better. Wool absorbs perspiration the best of all textures. White cotton does so to only half the amount. So the latter evaporates quicker, and soon feels chilly. Nansen says 302 WITH SCOTT: THE SILVER LINING goat-hair socks attract the moisture. “Oh! as you were!” No, I don’t mean that! (G. T.—I find I’ve omitted the correction, how- ever!) Personally, I think that an old sock makes an excellent nose-nip ! Sverdrup used to use a double tent for warmth with good results. I think we might modify the tent opening, and make the tent floor- cloth wider. If the sleeping-bags were provided with a separate hood, they would not get so wet. On our midwinter trip we found that eiderdown inner bags were no use after fourteen days. It was best to change sides with the fur bags and scrape them. ‘The hair inside was warmer, but held the perspiration more. The wind helmet should certainly be made fast to the blouse ; and I think lanyards fasten the bag-flaps much better than toggles. These are the only improvements I can suggest in our clothing. The seamen played six-handed euchre most evenings, while the two Russians looked at illustrated papers and turned in somewhat early. The mess-deck used to read the books in the library, and especially Debenham’s paper-backs. When l ran short I raided their small private stock. I was assured by Taff Evans that one by Hichens “is no good, for no one in the mess-deck can read it!” Needless to say I did not always agree with this stalwart board of navy critics. On the 8th of September the second volume of S. P. T. appeared. Cherry wrote the Editorial in the best style of the Times. Some eighteen pages were devoted to a skit on life in the Hut, called the “Bipes.” Its redeeming feature is a series of coloured illustrations by Uncle Bill. In it I gave a somewhat garbled but recognizable view of various person- alities at headquarters. The tenants of the Diarist’s Den (i.e. our cubicle) as well as the Conservative party (the “ Bunder- lohg ’’) came in for their share of attention on the part of the inquisitive rabbit ; who is here supposed to observe the habits and customs of the so-called Bipes. Simpson contributed a gruesome account of the decline and fall of the human race in the last days of the earth’s habitation. The only panacea seemed to be certain elixirs to be obtained near Mount Erebus. There was a beautifully illustrated rhyme dealing with the midwinter party at Cape Crozier. I could never discover who was the writer unless it was the Owner himself. Simpson’s career was described in a semi-serious article, “Celebrities in Glass Houses.” There were two poems called into being by the return of the sun, IN WINTER QUARTERS WITH CAPTAIN SCOTT 303 both due to Australians. Some one, I suspect Nelson, wove Uncle Bill and myself into a “nightmare interview.” There were some beautiful photo plates by Ponting and three of Wilson’s inimitable Egyptian tablets ; besides various cartoons and silhouettes by Wilson and Lillie. Guessing at the authors furnished considerable amuse- ment. Even the astute Nelson fell in! On p. 1g there is a plan of the hut showing inter a/ia the engine in one corner. Nelson made the rash statement that Uncle Bill had drawn it the wrong way round. I immediately bet him that Bill hadn’t. Nelson went over to the engine and came back ready to stake his life on it! Then I told him that I had drawn the plan; so that Bill couldn’t have made a mistake! He proceeded to say that he would have put me down as the author of the “ Bipes,” only I was so unmercifully described therein ; while Simpson amused me by assuring me that Scott wrote the poem, “The Errant Sun.” I gave the palm to Nelson’s poem on “ Uncle Bill,” “ You are old, Uncle William.” Captain Scott was now preparing for a fortnight’s sledge- trip over to the west. He proposed to Simpson that he should take this chance of some sledging, and so the meteor- ology was left in my hands. Simpson kindly coached me in the special minutiz, and I started the records on the 11th (before he left), so as to get into swing. Nelson gave us a particularly well-illustrated lecture on the 11th on Invertebrates generally. He told us of the pleasant habit of the Zydra which turns itself inside out, and converts its skin into a stomach lining, and vice versa! He discussed the huge arthropod, remarkably like a flea (but eight inches long), which Meares declared was found in a bunk in the hut, though Ponting said he obtained it on the beach. We envied the Pycnogonids (sea-spiders), which grow an extra pair of legs in Antarctica, though they have only eight in less strenuous latitudes. Two more limbs would help us so greatly in sledging! He called on me to lecture on the corals, and I gave a brief account of the biology of the forerunners of this family (the Archeocyathine), which occur fossil on the Beardmore Glacier. I discussed Darwin’s and Murray’s theories with special reference to my 304 WITH SCOTT: THE SILVER LINING observations on the coral reefs of the Great Barrier. Debenham instanced Funafuti—that coral islet bored by Professor David to show the depth of a reef formation. Birdie wanted to know why a sea anemone wasn’t a plant? And some one thereupon asked Nelson if he could explain why a Birdie wasn’t a cabbage? But this problem proved too difficult for the lecturer. Wilson with his usual kindness was now copying some of my western sketches and turning them into splendid pen- and-ink drawings. He spent many hours coaching me in drawing, but indeed he would always help any one if it lay in his power. I think what touched some of us as much as anything was his willingness to take the last and longest hour of any one’s night-watch ! He used to say, “I don’t mind getting up at seven ; I’ll get on with my painting. Just put a kettle on to boil, and wake me, and then you can turn in!” I’m afraid I took advantage of this, when my watch lasted through to the morning, though usually I shared it with Nelson. About this time Scott and Bowers spent their leisure in photographic work. Ponting was untiring in coaching them, and the excellent results obtained by these absolute tyros on the southern journey speaks well for teacher and pupils. Bowers handed over the pony “‘ Chinaman” to Wright, who “sets run away with, with great regularity.” Cherry was typing out those sections from the “ Heart of the Antarctic” which would help Scott in his southern journey. On the 15th of September Captain Scott set out for a trip to the Ferrar Glacier and thereabouts. They carried about 200 Ibs. of food for us to Butter Point, where we were to pick it up later. Nelson and I helped them along for three miles, though the party, consisting of Scott, Bowers, Simpson, and Taff Evans, needed us little. It was —4o° starting, but luckily there was no wind. A big shear-crack about two and a half miles out marked a permanent crack in the sea-ice extending between Inaccessible Isle and Cape Royds. It had developed into a fractured wall, as much as ten feet high in places, where the floes ground together, and gave us some trouble. However, Nelson and I were able to steady the sledge and guard the sledge meter, and so they soon nego- tiated it. IN WINTER QUARTERS WITH CAPTAIN SCOTT 305 On the 17th of September we actually had a “fine bright sun, so that films of snow melt on the black rock.” This is an interesting date, for though the air temperature was only +7°—that is, twenty-five degrees below freezing !—yet the radiant heat from the black rock produced a little water. Let us accompany the meteorologist, and see how a first- class weather station is run at 774° S. lat. The weather man has to rise about an hour before the others. (It was pleasant to see Sunny Jim lying in his bunk till 8.30 on the 14th—as he pathetically put it—for the first time since he’d landed !) I find I am dressed five minutes too soon, so I hit Wright with a book to get him up in time to check the chronometers, which is his “ pigeon” ! 1. When I hear the automatic signal I have to fly around and mark all the recording instruments to show exactly eight o'clock on their charts. 2. I read the large standard barometer and its attached thermometer. 3. Change the chronograph papers and put ink on the pens, for the blizzometer, thermograph, barograph, and wind velocity charts. (In all these chronograph drums the “clock”’ part (carrying the paper) revolves about the central axle— which is just the opposite of an ordinary clock ! 4. Wind up the various chronograph clocks (once a week, on Monday). Then I muffle myself in wind-clothes and gloves, and collect the gear for the outdoor apparatus. A. A clock set to nearest half-minute. B. “ana paper for the record burnt by the glass all. C. Tablet and pencil. 5. I stagger up to the top of Wind Vane Hill—a long operation and a cold one in September, for it is not far from August, the coldest and roughest month. At a definite minute I read the anemometer figures alongside the anemo- meter cups. 6. Then I press four times on a button alongside, and this is electrically transmitted to the record in the hut, and so gives a datum each day on that record, 7. | walk across to the screen and read the three Xx 306 WITH SCOTT: THE SILVER LINING thermometers—present, maximum, and minimum. Then I readjust the two latter and read again. 8. By this time three minutes have elapsed, and I return a few paces to the anemometer and read the latter figures again. ; Push Maegan | RA Tae . ZA “Robinson cor Anememeter— (This gives the revolutions in three minutes, and therefore the velocity per hour at that time. This is another check on the automatic record.) g. Read the wind direction from the arrow on the hill, and note the steam-cloud direction on Erebus. 10. Change the blue paper in the sunshine recorder and clean the glass sphere. ¥, This is an awful job, fo for the frost crystals eee eee cling like glue to the five-inch glass __ ball, and have to be melted off by rubbing with the bare hands. A slow and painful job at —40°! 11. Read the out- Sunshing Recovols 1, side thermometer at the south-east corner of the hut, just below the anemometer tubes. Each morning at 8.15 I used to predict the weather, as I went out to Wind Vane Hill. This was received with great joy by the mess deck. Crean was especially congratulatory. I have explained my method—z.e. “that after four days’ calm A FINE STEAM CLOUD BLOWING SOUTH FROM EREBUS, SEPT. 19, 1911: The illustration shows also the station on Wind Vane Hill. The thermometer screen on the left, the flagstaff and the wind instruments on the right. One anemometer is rotating ; the other is blocked (for the photo). 5) A GLACIERET NEAR ISLAND LAKE (C. EVANS) DUE TO WIND- BLOWN SNOW, SEPT. 23, rg11. The blizzard builds and also prunes these small glaciers. In the distance are the debris cones on the ramp and the south-west slopes of Erebus. IN WINTER QUARTERS WITH CAPTAIN SCOTT 307 ’ it’s certain to blizz ;” and it worked as well as most weather rules. However, even when this standby failed, Crean was always consoling. At last the other seamen got nettled. “Go on, sir! he’s only kidding; he wants your long sea- boots when you return!” It was “cupboard love,” I fear ! , On Thursday (21st) I believe the wind was blowing seventy miles per hour when I reached the screen. The temperature was pretty high (— 7°), but a wind that nearly blew me away soon robbed one of one’s bodily heat. My fingers took about ten minutes to “come back,” and only by degrees lost their dead feeling, though they did not reach the dead-white colour of bad frostbites. The early morning sun was throwing fine earth shadows, which moved round quite rapidly. Thus on the 24th, at 8 a.m., Erebus cast a shadow right over the western moun- tains, while at 9 a.m. the shadow could be seen to the south- west of Erebus itself. Debenham had been doing long-distance geology! He fixed up a telescope and trained it on the south slope of the crater of Erebus. He could see hundreds of snow structures on the side, each representing the vent of a “ fumarole” from which steam was issuing. This side of Erebus must resemble a gigantic pepper-box ! Inside the hut Day was doing some ingenious turning. His lathe was certainly unique! Many of the hardwood rollers for the motor sledges needed renewal. So he attached a block of hardwood to the flywheel shaft of the oil-engine, and he sat on the floor and, using a box as a tool-rest, he turned out rollers quite successfully, if not very rapidly. The morning of the 24th was quite clear, so 1 got my camera into working order, only to find the sky clouding over for a blizzard so soon as 1 ventured out, about noon. Ponting was lost for about two hours in the thick fog in the evening. We fired off guns, and it looked as if Atkinson’s mishap was to be repeated. However, luckily he had a compass, and so got back to the hut quite safely in the end. The weather was hopeless, and the coast survey party very sensibly returned to await better conditions. The following i eaae rhyme pinned to Gran’s diary affected them not a whit :— 308 WITH SCOTT: THE SILVER LINING “Three bold explorers hied them forth For to explore the plain; Although so bold, They found it cold, So hied them home again !” Next day was again gloomy and cold. It took me ten minutes to rub the sunshine ball clean. The record for yesterday showed clearly the sudden cessation of sunshine about noon, just when I was ready to use my camera. Every one was now busy with sledging outfit. Bernard {by mnUeeyZ :)