INDEX.
- Absolute heating-power of ocean-currents, 23
- 〃 amount of heat received from the sun per day, 26
- Adhémar, M., theory founded upon a mistake in regard to radiation, 81, 85
- 〃 on submergence, 368
- 〃 on influence of eccentricity on climate, 542
- Aërial currents increased in action by formation of snow and ice, 76
- 〃 function of, stated, 51
- 〃 heat conveyed by, 27
- Africa, South, glacial and inter-glacial periods of, 242
- 〃 boulder clay of Permian age, 300
- Age and origin of the sun, 346
- Air, on absorption of rays by, 59
- 〃 when humid, absorbs rays which agree with it in period, 59
- 〃 when perfectly dry incapable of absorbing radiant heat, 59
- Airy, Professor, earth’s axis of rotation permanent, 7
- Aitken’s, Mr., experiment on density of polar water, 129
- Aland islands, striation of, 447
- Alternate cold and warm periods, 236
- Allermuir, striations on summit of, 441
- America, low temperature in January, 72
- 〃 thickness of ice-sheet of North, 381
- Anderson, Captain Sir James, never observed a stone on an iceberg, 282
- Antarctic ice-cap, probable thickness of, 375
- 〃 diagram representing thickness of, 377
- 〃 thickness of, estimated from icebergs, 384
- Antarctic regions, mean summer temperature of, below freezing-point, 63
- Antarctic snowfall, estimates of, 382
- Aphelion, glacial conditions at maximum when winter solstice is at, 77
- Arago, M., on influence of eccentricity on climate, 536
- Arctic climate, influence of ocean-currents on, during glacial period, 260
- Arctic regions, influence of Gulf-stream on climate of, 45
- 〃 mean summer temperature of, 63
- Arctic regions, amount of heat received by, per unit surface, 195
- 〃 warm periods best marked in, 258
- 〃 warm inter-glacial periods in, 258−265
- 〃 state of, during glacial period, 260
- 〃 evidence of warm periods in, 261
- 〃 occurrence of recent trees in, 261, 265
- 〃 evidence of warm inter-glacial periods, 293
- 〃 warm climate during Old Red Sandstone period in, 295
- 〃 glacial period during Carboniferous age in, 297
- 〃 warm climate during Permian period in, 301
- 〃 list of papers relating to, 556
- Arctic Ocean, area of, 195
- 〃 according to gravitation theory ought to be warmer than Atlantic in torrid zone, 195
- 〃 heat conveyed into, by currents, compared with that received by it from the sun, 195
- 〃 blocked up with polar ice, 444
- Armagh, boulder beds of, 299
- Arran, Island of, glacial conglomerate of Permian age in, 299
- Astronomical causes of change of climate, 10
- Astronomy and geology, supposed analogy between, 355
- Atlantic, atmospheric pressure on middle of, 33
- 〃 inability of, to heat the south-west winds without the Gulf-stream, 34
- 〃 mean annual temperature of, 36
- 〃 mean temperature of, raised by Gulf-stream, 36, 40
- 〃 isothermal lines of, compared with those of the Pacific, 46
- 〃 area of, from equator to Tropic of Cancer, 194
- 〃 inquiry whether the area of, is sufficient to supply heat according to Dr. Carpenter’s theory, 194
- Atlantic, North, heat received by, from torrid zone by currents, 194
- 〃 according to Dr. Carpenter’s theory ought to be warmer in temperate regions than in the torrid zone, 195
- 〃 great depth of warm water in, 198
- 〃 North, an immense whirlpool, 216
- 〃 above the level of equator, 221
- 〃 probable antiquity of, 367
- 〃 from Scandinavia to Greenland probably filled with ice, 451
- Atmosphere-pressure in Atlantic a cause of south-west winds, 33
- Atmosphere, on difference between black-bulbed and shaded thermometer in upper strata of, 547
- Australia, evidence of ice-action in conglomerate of, 295
- Ayrshire, ice-action during Silurian period in, 293
- Bakewell, Mr. R., on influence of eccentricity on climate, 540
- Banks’s Land, discovery of ancient forest in, 261
- 〃 Professor Heer, on fossilized wood of, 309
- Ball, Mr., objection to Canon Moseley’s results, 501
- Baltic current, 171
- Baltic, glaciation of islands in, 448
- Baltic glacier, passage of, over Denmark, 449
- Bath, grooved rock surfaces of, 464
- Bay-ice grinds but does not striate rocks, 277
- Belcher, Sir E., tree dug up by, in latitude 75° N., 263
- 〃 carboniferous fossils found in arctic regions by, 298
- Belle-Isle, Strait of, observations on action of icebergs in, 276
- Bell, Mr. A., on Mediterranean forms in glacial bed at Greenock, 254
- Belt, Mr. Thomas, theory of the cause of glacial epochs, 415
- Bennie, Mr. James, on surface geology, 468
- 〃 on deposits filling buried channel, 486
- Blanford, Mr., on ice-action during Carboniferous age in India, 297
- Borings, evidence of inter-glacial beds from, 254
- 〃 examination of drift by, 467
- 〃 journals of, 483, 484
- Boulder clays of former glacial epochs, why so rare, 269
- 〃 a product of land-ice, 284
- 〃 if formed from icebergs must be stratified, 284
- 〃 scarcity of fossils in, 285
- 〃 formed chiefly from rock on which it lies, 285
- 〃 of Caithness a product of land-ice, 435
- 〃 on summit of Allermuir, 441
- Boulders, how carried from a lower to a higher level, 527
- Boussingault on absorption of carbon by vegetation, 428
- Britain, climate of, affected most by south-eastern portion of Gulf-stream, 33
- Brown, Dr. R., cited on Greenland ice-sheet, 378, 380
- 〃 on inland ice of Greenland, 284
- 〃 on cretaceous formation of Greenland, 305
- 〃 on Miocene beds of the Disco district, 310
- Brown, Mr. Robert, on growth of coal plants, 421
- Brown and Dickeson, on sediment of Mississippi, 330
- Buchan, Mr., on atmosphere-pressure in the Atlantic, 33
- 〃 on force of the wind, 220
- Buchanan, Mr. J. Y., on vertical distribution of heat of the ocean, 550
- Buckland, Dr., observations by, on occurrence of red chalk on Cotteswold hills, 459
- Buff, Professor, on oceanic circulation, 145
- Buried river channels, 466
- 〃 channel from Kilsyth to Grangemouth, 468
- 〃 section at Grangemouth, 474
- 〃 from Kilsyth to Clyde, 481
- 〃 not excavated by sea nor by ice, 469
- 〃 other examples of, 488−494
- Caithness, difficulty of accounting for the origin of the boulder clay of, 435
- Caithness, boulder clay of, a product of land-ice, 435
- 〃 boulder clay not formed by icebergs, 437
- 〃 theories regarding the origin of the boulder clay of, 437
- 〃 why the ice was forced over it, 444
- 〃 Professor Geikie and B. N. Peach on path of ice over, 453
- Cambrian conglomerate of Islay, 292
- Campbell, Mr., observations of, on icebergs, 276
- 〃 on supposed striation of rocks by large icebergs, 278
- 〃 evidence that river-ice does not striate rocks, 279
- Canada, change of climate less complete than in Scotland, 71
- Carboniferous period of arctic regions, 298
- 〃 evidence of glacial epoch during, 296−298
- 〃 temperate climate of, 422
- Carboniferous limestone, mode of formation, 433
- Carpenter’s, Dr., objections examined, 141
- 〃 theory, mechanics of, 145
- 〃 idea of a 〃vertical circulation〃 stated, 153
- Carpenter’s, Dr., radical error in theory of, 155
- 〃 on difference of density between waters of Atlantic and Mediterranean, 168
- 〃 theory, inadequacy of, 191
- 〃 estimate of thermal work of Gulf-stream, 199
- Charpentier’s, M., theory of glacier-motion, 513
- Carse clays, date of, 405
- Cattegat, ice-markings on shore of, 446
- Cave and river deposits, 251
- Chalk, erratic blocks found in, 304
- 〃 débris, conclusion of Mr. Searles Wood, 460
- Challenger’s temperature-soundings at equator, 119
- 〃 crucial test of the wind and gravitation theories, 220
- Chambers, Dr. Robert, on striated pavements, 255
- 〃 observations on glaciation of Gothland, 446
- Champlain Lake, inter-glacial bed of, 241
- Chapelhall, ancient buried channel at, 491
- 〃 inter-glacial sand-bed, 244
- Chart showing the agreement between system of currents and system of winds, 212
- Christianstadt, crossed by Baltic glacier, 450
- Circulation without difference of level, 176
- Climate, Secular changes of, intensified by reaction of physical causes, 75, 76
- 〃 affected most by temperature of the surface of ground, 88
- 〃 ocean-currents in relation to, 226
- 〃 cold conditions of, inferred from absence of fossils, 288
- 〃 cold condition of, difficulty of determining, from fossil remains, 289
- 〃 warm, of arctic regions during Old Red Sandstone period, 295
- 〃 rough sketch of the history of, during the last 60,000 years, 409
- 〃 of Coal period inter-glacial in character, 420
- 〃 alternate changes of, during Coal period, 426
- Climates, Mr. J. Geikie on difficulty of detecting evidence of ancient glacial conditions, 289
- 〃 evidence of, from ancient sea-bottoms, 289
- Coal an inter-glacial formation, 420
- Coal beds, alternate submergence and emergence during formation of, 424
- 〃 preservation of, by submergence, 426
- Coal period, flatness of the land during, 430
- Coal plants, conditions necessary for, preservation of, 423
- Coal seams, thickness of, indicative of length of inter-glacial periods, 428
- Coal seams, time occupied in formation of, 429
- Coal strata, on absence of ice-action in, 429
- Coal measures, oscillations of sea-level during formation of, 425
- Cold periods best marked in temperate regions, 258
- Colding, Dr., oceanic circulation, 95
- Confusion of ideas in reference to the agency of polar cold, 179
- Continental ice, inadequate conceptions of, 385
- 〃 absence of, during glacial epochs of Coal period, 432
- Contorted drift near Musselburgh, 465
- Cook, Captain, description of Sandwich Land by, 60
- 〃 on South Georgia, 60
- Cornwall, striated rocks of, 464
- Cotteswold hills, red chalk from Yorkshire found on, 459
- Couthony, Mr., on action of icebergs, 275
- Coutts, Mr. J., on buried channel, 493
- Craig, Mr. Robert, on inter-glacial beds at Overton Hillhead and Crofthead, 247
- Craiglockhart hill, inter-glacial bed of, 245
- “Crawling” theory considered, 507
- “Crevasses,” origin of, according to molecular theory, 521
- Cretaceous period, evidence of ice-action during, 303−305
- Cretaceous age, evidence of warm periods during, 304
- Cretaceous formation of Greenland, 305
- Crofthead, inter-glacial bed at, 248
- Cromer forest bed, 250
- Crosskey, Rev. Mr., comparison of Clyde and Canada shell beds, 71
- 〃 on southern shells in Clyde beds, 253
- Croydon, block of granite found in chalk at, 303
- Crucial test of the wind and gravitation theories, 220
- Crystallization, force of, a cause of glacier-motion, 523
- Currents, effects of their stoppage on temperatures of equator and poles, 42
- 〃 produced by saltness neutralize those produced by temperature, 106
- Dalager, excursion in Greenland by, 378
- Dana, Professor, on action of icebergs, 275
- 〃 on striations by icebergs, 275
- 〃 on thickness of ice-sheet of North America, 381
- Darwin, Mr., on alternate cold and warm periods, 231
- 〃 on migration of plants and animals during glacial epoch, 395
- 〃 on peat of Falkland Islands, 422
- Date of the 40-foot beach, 409
- Date when conditions were favourable to formations of the Carse clay, 409
- Davis’ Straits, current of, 132
- Dawkins, Mr. Boyd, on the animals of cave and river deposits, 251
- Dawson, Principal, on esker of Carboniferous age, 296
- 〃 on habitats of coal plants, 424
- Deflection of ocean-currents chief cause of change of climate, 68
- De la Beche, Sir H. T., on influence of eccentricity on climate, 539
- De Mairan, on influence of eccentricity on climate, 528
- Denmark, crossed by Baltic glacier, 449−452
- Denudation, method of measuring rate of, 329
- 〃 as a measure of geological time, 329
- 〃 measured by sediment of Mississippi, 330
- 〃 subaërial rate of, 331
- 〃 law which determines rate of, 333
- 〃 marine, trifling, 337
- Deposition, rates of, generally adopted, quite arbitrary, 360
- 〃 rate of, determined by rate of denudation, 362
- 〃 range of, restricted to a narrow fringe surrounding the continents, 364
- 〃 area of, 365
- 〃 during glacial epoch probably less than present, 366
- Deposits from icebergs cannot be wholly unstratified, 437
- Despretz, tables by, of temperature of maximum density of sea-water, 117
- Desor, M., on tropical fauna of the Eocene formation in Switzerland, 306
- Derbyshire, breaks in limestone of, marks of cold periods, 434
- Derbyshire limestone a product of inter-glacial periods, 434
- Devonshire, boulder clay discovered in, 463
- Diagram illustrating descent of water from equator to poles, 155
- 〃 showing variations of eccentricity, 313
- 〃 illustrative of fluidity of interior of the earth, 396
- 〃 showing formation of coal beds, 426
- Dick, Mr., chalk flints in boulder clay, 454
- Dick, Mr. R., on buried channel, 491
- Difference of level essential to gravitation theory, 176
- Dilatation of sea-water by increase of temperature calculated by Sir John Herschel, 116
- Disco district, Dr. R. Brown cited on Miocene beds of, 310
- Disco Island, Upper Miocene period of, 307−308
- Distribution, how effected by ocean-currents, 231
- Dove, Professor, method of constructing normal temperature tables by, 40
- 〃 on mean annual temperature, 401
- Dover, mass of coal imbedded in chalk found at, 303
- Drayson, Lieutenant-Colonel, on obliquity of ecliptic, 410
- Drayson, Lieutenant-Colonel, theory of the cause of the glacial epoch, 410
- Drift, examination by borings, 467
- Drumry, deep surface deposits at, 482
- Dubuat’s, M., experiments, 182
- 〃 experiments by, on water flowing down an incline, 120
- Duncan, Captain, on under current in Davis’ Strait, 134
- Dürnten lignite beds, 240
- Dürnten beds an example of inter-glacial coal formation, 433
- Durham, buried river channel at, 488
- Earth’s axis of rotation permanent, 7
- Earth, mean temperature of, increased by water at equator, 30
- 〃 not habitable without ocean-currents, 54
- 〃 mean temperature of, greatest in aphelion, 77, 78
- 〃 centre of gravity of, effects of ice-cap on, 370, 371
- Eccentricity of the earth’s orbit, Mr. Stockwell’s researches regarding, 54
- 〃 primary cause of change of climate, 54
- 〃 primary cause of glacial epochs, 77
- 〃 how it affects the winds, 228
- 〃 tables of, 314−321
- 〃 its influence on temperature, 323
- 〃 explanation of tables of, 324
- 〃 De Marian, on influence of, on climate, 528
- 〃 Sir J. F. Herschel, on influence of, on climate, 529
- 〃 Œpinus, on influence of, on climate, 529
- 〃 R. Kirwan, on influence of, on climate, 529
- 〃 of planetary orbits, superior limits as determined by Lagrange, Leverrier, and Mr. Stockwell, 531
- 〃 Sir Charles Lyell, on influence of, on climate, 529, 535
- 〃 M. Arago, on influence of, on climate, 536
- 〃 Baron Humboldt, on influence of, on climate, 538
- 〃 Sir H. T. de la Beche, on influence of, on climate, 539
- 〃 Professor Phillips, on influence of, on climate, 539
- 〃 Mrs. Somerville, on influence of, on climate, 540
- 〃 L. W. Meech, on influence of, on climate, 540
- 〃 Mr. R. Bakewell, on influence of, on climate, 540
- 〃 M. Jean Reynaud, on influence of, on climate, 541
- 〃 M. Adhémar, on influence of, on climate, 542
- Equator, reduction of level by denudation, 336
- Ecliptic, supposed effect of a change of obliquity of, 8
- 〃 changes of, effects on climate, 398−417
- 〃 obliquity of, Lieutenant-Colonel Drayson on, 410
- Emergence, physical cause of, 368
- England, inter-glacial beds of, 249
- 〃 glacial origin of Old Red Sandstone of, 294
- 〃 ice-action during Permian period in, 298
- 〃 North of, ice-sheet of, 456
- 〃 ice-sheet of South of, 463
- Eocene period, total absence of fossils in flysch, 286
- 〃 glacial epoch of, 305
- Eocene and Miocene periods, date of, 357
- Equator, heat received per square mile at, 26
- 〃 temperature of earth increased by water at, 30
- 〃 and poles, effects of stoppage of currents on temperature of, 42
- 〃 surface-currents warmer than the under currents, 92
- 〃 heat transferred by currents from southern hemisphere compared with that received by land at, 93
- 〃 temperature soundings at, 119
- 〃 temperature of sea at, decreases most rapidly at the surface, 119
- 〃 heat received by the three zones compared with that received by the, 194
- 〃 migration across, 234
- 〃 glaciation of, 234
- Equatorial current, displacement of, 229
- Erratic blocks in stratified rocks, evidence of former land-ice, 269
- 〃 in chalk, 304
- 〃 why not found in coal strata, 432
- Erratics extend further south in America than in Europe, 72
- Etheridge, R., jun., on glacial conglomerate in Australia of Old Red Sandstone age, 295
- Europe, influence of Gulf-stream on climate of, 31
- 〃 effect of deflection of Gulf-stream on condition of, 68
- 〃 glacial condition of, if Gulf-stream was stopped, 71
- 〃 river systems of, unaltered since glacial period, 393
- Faraday, Professor, on cause of regelation, 554
- Faroe Islands glaciated by land-ice from Scandinavia, 450
- Ferrel, Mr., on Dr. Carpenter’s theory, 126
- 〃 argument from the tides, 184
- Findlay, Mr. A. G., objection by, considered, 31, 203
- 〃 estimate of heat conveyed by Gulf-stream, 206
- Fisher, Rev. O., on the 〃trail〃 of Norwich, 251
- 〃 on glacial submergence, 387
- Fitzroy, Admiral, on temperature of Atlantic, 36
- Fluid molecules crystallize in interstices, 523
- Fluvio-marine beds of Norwich, 250
- “Flysch” of Eocene period, absence of fossils in, 286
- 〃 of Switzerland of glacial origin, 306
- Fogs prevent the sun’s heat from melting ice and snow in arctic regions, 60
- Forbes, Professor J. D., method adopted by, of ascertaining temperatures, 48
- 〃 on temperature of equator and poles, 48
- 〃 on the conductivity of different kinds of rock, 86
- 〃 on underground temperature, 86
- 〃 experiments by, on the power of different rocks to store up heat, 86
- Forest bed of Cromer, 250
- Former glacial periods, 266−310
- 〃 why so little known of, 266
- 〃 geological evidence of, 292
- France, evidence of ice-action during Carboniferous period in, 296
- Fraserburgh, glaciation of, 450
- 〃 crossed by North Sea ice, 454
- Fundamental problem of geology, 1
- Ganges, amount of sediment conveyed by, 331
- Gases, radiation of, 38
- Gastaldi, M., on the Miocene glacial epoch of Italy, 306
- Geikie, Professor, on geological agencies, 1
- 〃 on inter-glacial beds of Scotland, 243
- 〃 remarks on inter-glacial beds, 245
- 〃 on striated pavements, 256
- 〃 on ice-markings on Scandinavian coast, 281
- 〃 striated stones found in carboniferous conglomerate by, 296
- 〃 on sediment of European rivers, 332
- 〃 on modern denudation, 332
- 〃 suggestion regarding the loess, 452
- 〃 on striation of Caithness, 453
- 〃 on buried channel at Chapelhall, 491
- 〃 and Mr. James, on glacial conglomerate of Lower Carboniferous age, 296
- Geikie, Mr. James, on Crofthead inter-glacial bed, 248
- 〃 on the gravels of Switzerland, 268
- 〃 on difficulty of recognising former glacial periods, 289
- 〃 on Cambrian conglomerate of north-west of Scotland, 293
- 〃 on ice-action in Ayrshire during Silurian period, 293
- 〃 on boulder conglomerate of Sutherland, 301
- 〃 on buried channels, 492
- Geogr. Mittheilungen, list of papers in, relating to arctic regions, 556
- Geological agencies climatic, 2
- Geological principle, nature of, 4
- Geological climates, theories of, 6
- Geological time, 311−359
- 〃 measurable from astronomical data, 311
- 〃 why it has been over-estimated, 325
- 〃 method of measuring, 328, 329
- 〃 Professor Ramsay on, 343
- Geology, fundamental problem of, 1
- 〃 a dynamical science, 5
- 〃 and astronomy, supposed analogy between, 355
- German Polar Expedition on density of polar water, 151
- 〃 list of papers relating to, 556
- German Ocean once dry land, 479
- Germany, Professor Ramsay on Permian breccia of, 300
- Gibraltar current, Dr. Carpenter’s theory of, 167
- 〃 cause of, 215
- Glacial conditions increased by reaction of various physical causes, 75
- 〃 reach maximum when winter solstice arrives at aphelion, 77
- Glacial epoch, date of, 327
- 〃 circumstances which show recent date of, 341
- 〃 Mr. Belt’s theory of cause of, 415
- Glacial epochs dependent upon deflection of ocean-currents, 68
- 〃 caused primarily by eccentricity, 77
- 〃 why so little known of, formerly, 266
- 〃 boulder clays of former, why so rare, 269
- 〃 geological evidence of former, 292
- Glacial period in America more severe than in Western Europe, 73
- 〃 mean temperature of the earth greatest at aphelion during, 78
- 〃 records of, fast disappearing, 270
- 〃 of the Eocene formation, 305
- Glacial periods, indirect evidence of, in Eocene and Miocene formations, 287
- 〃 difficulty of determining, from fossil remains, 289
- Glacial submergence resulting from displacement of the earth’s centre of gravity, 389
- Glaciation a cause of submergence, 390
- 〃 remains of, found chiefly on land surfaces, 267
- 〃 of Scandinavia inexplicable by theory of local glaciers, 448
- Glacier des Bois, 497
- Glacier-motion, Canon Moseley’s theory of, 507
- 〃 Professor James Thomson’s theory of, 512
- 〃 M. Charpentier’s theory of, 513
- 〃 molecular, 516
- Glacier-motion, present state of the question, 514
- 〃 molecular theory of, 514−527
- 〃 heat necessary to, 515
- 〃 due to force of crystallization, 523
- 〃 due chiefly to internal molecular pressure, 523
- Glaciers, pressure exerted by, 274
- 〃 physical cause of the motion of, 495−527
- 〃 difficulties in accounting for motion of, 495
- Glasgow, actual January temperature of, 28° above normal, 72
- Godwin-Austen, Mr., on ice-action during the Carboniferous period in France, 296
- 〃 on evidence of ice-action during Cretaceous period, 303
- 〃 on mass of coal found in chalk at Dover, 304
- 〃 on the flatness of the land during Coal period, 430
- Gothland, glaciation of, 446
- Grangemouth, buried river channel at, 468
- 〃 surface-drift of, 484
- Gravitation, the whole work of, performed by descent of water down the slope, 154
- 〃 of sun’s mass, 348
- 〃 insufficient to account for sun’s heat, 349, 350
- Gravitation theory, its relation to the theory of Secular changes of climate, 97
- 〃 three modes of determining it, 115
- 〃 mechanics of, 145
- 〃 of the Gibraltar current, 167
- 〃 inadequacy of, 191
- 〃 crucial test of, 220
- 〃 of the sun’s heat, 346−355
- Gravity, force of, impelling water from equator to poles, 119, 120
- 〃 force of, insensible at a short distance below the surface, 120
- 〃 work performed by, 150
- 〃 diagram illustrating the action of, in producing currents, 155
- 〃 amount of work performed by, due solely to difference of temperature between equatorial and polar waters, 164
- 〃 specific difference in, between water of Atlantic and Mediterranean insufficient to produce currents, 169
- 〃 centre of, displacement, by polar ice-cap, 368
- Greenland, summer warm if free from ice, 59
- 〃 receives as much heat in summer as England, 66
- 〃 continental ice free from clay or mud, 284
- 〃 North, warm climate during Oolitic period in, 302
- 〃 Cretaceous formation of, 305
- Greenland, evidence of warm conditions during Miocene period in, 307
- 〃 Professor Heer cited on Miocene flora of, 308, 309
- 〃 state of, during glacial period, 259
- 〃 effect of removal of ice from, 260
- Greenland ice-sheet, probable thickness of, 378
- 〃 invaded the American continent, 445
- Greenland inland ice, 379
- Gulf-stream, estimate of its volume, 24
- 〃 United States’ coast survey of, 24
- 〃 absolute amount of heat conveyed by, 25, 26
- 〃 heat conveyed by, compared with that carried by aërial currents, 27
- 〃 heat conveyed by, compared with that received by the frigid zone from the sun, 27
- 〃 influence on climate of Europe, 31
- 〃 efficiency of, due to the slowness of its motion, 32
- 〃 climate of Britain influenced by south-eastern portion of, 33
- 〃 heat conveyed by, compared with that derived by temperate regions from the sun, 34
- 〃 heat of, expressed in foot-pounds of energy, 35
- 〃 mean temperature of Atlantic increased one-fourth by, 36
- 〃 the only current that can heat arctic regions, 45
- 〃 influence of, on climate of arctic regions, 45
- 〃 the compensating warm current, 46
- 〃 palæontological objections to influence of, 53
- 〃 agencies which deflect the, in glacial periods, 69
- 〃 result, if stopped, 71
- 〃 large portion of the heat derived from southern hemisphere, 94
- 〃 Lieut. Maury on propulsion of, by specific gravity, 102
- 〃 contradictory nature of, the causes supposed by Lieut. Maury for the, 110
- 〃 higher temperature of, considered by Lieut. Maury as the real cause of its motion, 111
- 〃 amount of heat conveyed by, not over-estimated, 197
- 〃 amount of heat conveyed by, 192
- 〃 amount of heat conveyed by, compared with that by general oceanic circulation, 194
- 〃 heat conveyed by, compared with that received by torrid zone from the sun, 194
- 〃 heat conveyed by, into Arctic Ocean compared with that received by it from the sun, 195
- 〃 Capt. Nares’s observations of, 198
- 〃 Dr. Carpenter’s estimate of the thermal work of, 199
- Gulf-stream, volume and temperature of, according to Mr. A. G. Findlay, 203, 206
- 〃 erroneous notion regarding depth of, 207
- 〃 list of papers relating to, 556
- Haughton, Professor, on recent trees in arctic regions, 263
- 〃 on fragments of granite in carboniferous limestone, 296
- 〃 on coal beds of arctic regions, 298
- 〃 on Ammonites of Oolitic period in arctic regions, 303
- Hayes, Dr., on Greenland ice-sheet, 379
- Heat received from the sun per day, 26
- 〃 received by temperate regions from the sun, 34
- 〃 radiant, absorbed by ice remains insensible, 60
- 〃 sun’s, amount of, stored up in ground, 87
- 〃 transferred from southern to northern hemisphere, 93
- 〃 internal, supposed influence of, 176
- 〃 received by the three zones compared with that received by the equator, 194
- 〃 amount radiated from the sun, 346
- 〃 received by polar regions 11,700 years ago, 403
- 〃 necessary to glacier-motion, 515
- 〃 how transmitted through ice, 517
- Heat-vibrations, nature of, 544
- Heath, Mr. D. D., on glacial submergence, 387
- Heer, Professor, on Dürnten lignite beds, 241
- 〃 on Miocene flora of Greenland, 308−310
- 〃 on Miocene flora of Spitzbergen, 309
- Hills, ice-markings on summits of, as evidence of continental ice, 458
- Helmholtz’s gravitation theory of sun’s heat, 348
- Henderson, Mr. John, on inter-glacial bed at Redhall quarry, 247
- Herschel, Sir John, on influence of eccentricity, 11
- 〃 estimate of the Gulf-stream by, 25
- 〃 on the amount of the sun’s heat, 26
- 〃 on inadequacy of specific gravity to produce ocean-currents, 116
- 〃 his objections to specific gravity not accepted, 117
- 〃 on influence of eccentricity on climate, 529
- Home, Mr. Milne, on buried river channels, 478
- Hooker, Sir W., on tree dug up by Capt. Belcher, 264
- Hooker, Dr., on preponderance of ferns among coal plants, 421
- Horne, Mr. J., on conglomerates of Isle of Man, 295
- Hoxne, inter-glacial bed of, 241
- Hudson’s Bay, low mean temperature of, in June, 62
- Hull, Professor, on ice-action during Permian age in Ireland, 299
- 〃 on equable temperature of Coal period, 421
- 〃 on estuarine origin of coal measures, 424
- Hull, buried channel at, 489
- Humboldt, Baron, on loss of heat from radiation, 82
- 〃 on rate of growth of coal, 429
- 〃 on influence of eccentricity on climate, 538
- Humphreys and Abbot on sediment of Mississippi, 330
- Ice, latent heat of, 60
- Ice, effects of removal of, from polar regions, 64
- 〃 heat absorbed by, employed wholly in mechanical work, 60
- 〃 slope necessary for motion of continental, 375
- 〃 does not shear in the solid state, 516
- 〃 how heat is transmitted through, 517
- 〃 how it can ascend a slope, 525
- 〃 how it can excavate a rock basin, 525
- Icebergs do not striate sea-bottom, 272
- 〃 markings made by, are soon effaced, 273
- 〃 exerting little pressure perform little work, 273
- 〃 behaviour of, when stranded, 274
- 〃 action of, on sea-bottoms, 274
- 〃 rocks ground smooth, but not striated by, 276
- 〃 stones seldom seen on, 281
- 〃 evidence of, in Miocene formation of Italy, 307
- 〃 comparative thickness of arctic and antarctic, 381
- 〃 great thickness of antarctic, 382
- Ice-cap, effects of, on the earth’s centre of gravity, 369
- 〃 probable thickness of antarctic, 375
- 〃 evidence from icebergs as to thickness of antarctic, 383−385
- Ice-markings, modern, observed by Sir Charles Lyell, 280
- Ice-sheet, probable thickness of in Greenland, 380
- 〃 of north of England, 456
- Ice-worn pebbles found on summit of Allermuir, 441
- Iceland, lignite of Miocene age in, 308
- 〃 probably glaciated by land-ice from North Greenland, 451
- India, evidences of glacial action of Carboniferous age in, 297
- Indian Ocean, low temperature at bottom, 123
- Internal heat, no influence on climate, 6
- 〃 supposed influence of, 176
- Inter-tropical regions, greater portion of moisture falls as rain, 29
- Inter-glacial bed at Slitrig, 243
- 〃 at Chapelhall, 244
- 〃 of Craiglockhart hill, 245
- 〃 at Kilmaurs, 248
- Inter-glacial beds, Professor Geikie on, 243
- 〃 of Dürnten, 240
- 〃 of Scotland, 243
- 〃 of England, 249
- 〃 at Norwich, 250
- 〃 evidence of, from borings, 254
- Inter-glacial character of cave and river deposits, 251
- Inter-glacial climate during Old Red Sandstone period in arctic regions, 295
- Inter-glacial periods, 236
- 〃 reason why overlooked, 237
- 〃 of Switzerland, 239
- 〃 evidence of, from shell-beds, 252
- 〃 evidence from striated pavements of, 255
- 〃 reasons why so few vestiges remain of, 257
- 〃 in arctic regions, 258−265
- 〃 of Silurian age in arctic regions, 293
- 〃 of Carboniferous age in arctic regions, 297
- 〃 of Eocene formation in Switzerland, 306
- 〃 formation of coal during, 420
- 〃 length of, indicated by thickness of coal-seams, 428
- Inglefield, Captain, erect trees found in Greenland by, 309
- Ireland, on ice-action during Permian age in, 299
- Isbister, Mr., on carboniferous limestone of arctic regions, 297
- Islay, Cambrian conglomerate of, 292
- Italy, glacial epoch of Miocene period in, 306
- Jack, Mr. R. L., on deflection of ice across England, 461
- Jamieson, Mr. T. F., on boulder clay of Caithness, 435
- 〃 opinion that Caithness was glaciated by floating ice, 437
- 〃 on thickness of ice in the north Highlands, 439
- 〃 glaciation of headland of Fraserburgh, 450, 455
- January temperature of Glasgow and Cumberland, difference between, 72
- Jeffreys, Mr. Gwyn, on Swedish glacial shell beds, 253
- Johnston, Dr. A. Keith, on coast-line of the globe, 337
- Joule’s, Dr., experiments on the thermal effect of tension, 552
- Judd, Mr., on boulders of Jurassic age in the Highlands, 302
- Jukes, Mr., on warm climate of North Greenland during Oolitic period, 302
- July, why hotter than June, 89
- Kane, Dr., on mean temperature of Von Rensselaer Harbour, 62
- Karoo beds, glacial character of, 301
- 〃 evidence of subtropical during deposition of, 301
- Kelvin, ancient bed of, 481
- Kielsen, Mr., excursion upon Greenland ice-sheet, by, 378
- Kilmours, inter-glacial bed at, 248
- Kirwan, Richard, on influence of eccentricity on climate, 529
- Kyles of Bute, southern shell bed in, 253
- Labrador, mean temperature of, for January, 72
- 〃 Mr. Packard on glacial phenomena of, 282
- Lagrange, M., on eccentricity of the earth’s orbit, 54
- 〃 table of superior limits of eccentricity, 531
- Land at equator would retain the heat at equator, 30
- 〃 radiates heat faster than water, 91
- 〃 elevation of, will not explain glacial epoch, 391
- 〃 submergence and emergence during glacial epoch, 368−397
- 〃 successive upheavals and depressions of, 391
- Land-ice necessarily exerts enormous pressure, 274
- 〃 evidence of former, from erratic blocks on stratified deposits, 269
- Land-surfaces, remains of glaciation found chiefly on, 267
- 〃 (ancient) scarcity of, 268
- Laplace, M., on obliquity of ecliptic, 398
- Laughton, Mr., on cause of Gibraltar current, 215
- Leith Walk, inter-glacial bed at, 246
- Leverrier, M., on superior limit of eccentricity, 54
- 〃 on obliquity of ecliptic, 398
- 〃 table, by, of superior limits of eccentricity, 531
- 〃 formulæ, of, 312
- Lignite beds of Dürnten, 240
- Loess, origin of, 452
- London, temperature of, raised 40° degrees by Gulf-stream, 43
- Lomonds, ice-worn pebbles found on, 439
- Lubbock, Sir J., on cave and river deposits, 252
- Lucy, Mr. W. C., on glaciation of West Somerset, 463
- 〃 on northern derivation of drift on Cotteswold hills, 460
- Lyell’s, Sir C., theory of the effect of distribution of land and water, 8
- 〃 on action of river-ice, 280
- 〃 on tropical character of the fauna of the Cretaceous formation, 305
- 〃 on warm conditions during Miocene period in Greenland, 307
- 〃 on influence of eccentricity, 324
- 〃 on sediment of Mississippi, 331
- 〃 on comparison of existing rocks with those removed, 362
- 〃 on submerged areas during Tertiary period, 392
- 〃 on change of obliquity of ecliptic, 418
- 〃 on climate best adapted for coal plants, 420
- 〃 on influence of eccentricity on climate, 529, 535
- Mackintosh, Mr., observations on the glaciation of Wastdale Crag, 457
- Magellan, Straits of, temperature at midsummer, 61
- Mahony, Mr. J. A., on Crofthead inter-glacial bed, 248
- Mälar Lake crossed by ice, 447
- Man, Isle of, Mr. Cumming on glacial origin of Old Red Sandstone of, 294
- Mars, uncertainty as to its climatic condition, 80
- 〃 objection from present condition of, 79
- Marine denudation trifling, 337
- Markham, Clements, on density of Gulf-stream water, 129
- 〃 on motion of icebergs in Davis’ Straits, 133
- Martins’s, Professor Charles, objections, 79
- Mathews, Mr., on Canon Moseley’s experiment, 499
- Maury, Lieutenant, his estimate of the Gulf-stream, 25
- 〃 his theory examined, 95
- 〃 on temperature as a cause of difference of specific gravity, 102
- 〃 on difference of saltness as a cause of ocean-currents, 103
- 〃 discussion of his views of the causes of ocean-currents, 104
- 〃 his objection to wind theory of ocean-currents, 211
- McClure, Captain, discovery of ancient forest in Banks’s Land, 261
- Mecham, Lieutenant, discovery of recent trees in Prince Patrick’s Island, 261
- Mechanics of gravitation theory, 145
- Mediterranean shells in glacial shell bed of Udevalla, 253
- 〃 shells in glacial beds at Greenock, 254
- Meech, Mr., on amount of sun’s rays cut off by the atmosphere, 26
- 〃 on influence of eccentricity on climate, 540
- Melville Island, summer temperature of, 65
- 〃 discovery of recent trees in, 262
- 〃 plants found in coal of, 298
- Mer de Glace, Professor Tyndall’s observations on, 498
- Meteoric theory of sun’s heat, 347
- Method of measuring rate of denudation, 329
- Miller, Hugh, on absence of hills in the land of the Coal period, 431
- Migration of plants and animals, how influenced by ocean-currents, 231
- 〃 across equator, 234
- Millichen, remarkable section of drift at, 483
- Miocene glacial period, 286
- Miocene period, glacial epoch of, in Italy, 306
- Miocene, warm period of, in Greenland, 307
- Miocene and Eocene periods, date of, 357
- Mississippi, amount of sediment in, 330
- 〃 volume of, 330
- Mitchell, Mr., on cause of Gulf-stream, 131
- Molecular theory of origin of 〃Crevasses,” 521
- 〃 modification of, 523
- Moore, Mr. J. Carrick, on ice-action of Silurian age in Wigtownshire, 293
- Moore, Mr. Charles, on grooved rocks in Bath district, 464
- Morlot, M., on inter-glacial periods of Switzerland, 240
- Moseley, Canon, experiment to determine unit of shear, 498
- 〃 on motion of glaciers, 498
- 〃 unit of shear uncertain, 504
- 〃 his theory examined, 507
- Motion of the sea, how communicated to a great depth, 136
- Motion in space, origin of sun’s heat, 353
- Mühry, M., on circumpolar basin, 133, 556
- Mundsley, freshwater beds of, 250
- Muncke on the expansion of sea-water, 118
- Murchison, Sir R., on southern shells at Worcester, 253
- 〃 on trees in arctic regions, 262
- 〃 on striation of islands in the Baltic, 448
- Murphy’s, Mr., theory, 66
- Musselburgh, section of contorted drift near, 465
- Nares, Captain, on low temperature of antarctic regions, 64
- 〃 discovery of great depth of warm water in North Atlantic, 198
- 〃 estimate of volume and temperature of Gulf-stream, 198
- 〃 temperature soundings by, 119, 222
- 〃 thermal condition of Southern Ocean, 225
- Natal, boulder clay of, 300
- Newberry, Professor, on inter-glacial peat-bed of Ohio, 249
- 〃 on boulder of quartzite found in seam of coal, 296
- Nicholson, Dr., on Wastdale Crag, 457
- Nicol, Professor, on inter-glacial buried channel, 244
- Nordenskjöld, Professor, on inland ice of Greenland, 379
- North Sea rendered shallow by drift deposits, 443
- Northern seas probably filled with land-ice during glacial period, 438
- Northern hemisphere, condition of, when deprived of heat from ocean-current, 68
- Norway, southern species in glacial shell beds, 253
- Norwich Crag, its glacial character, 249
- Norwich fluvio-marine beds, 250
- Norwich inter-glacial beds, 250
- Obliquity of ecliptic, its effects on climate, 398−419
- 〃 change of, influence on sea-level, 403
- 〃 Lieutenant-Colonel Drayson on, 410
- 〃 Mr. Belt on change of, 415
- 〃 Sir Charles Lyell on change of, 418
- Ocean, imperfect conception of its area, 135
- 〃 condition of, inconsistent with the gravitation theory, 136
- 〃 low temperature at bottom a result of under currents, 142
- 〃 circulation, pressure as a cause of, 187
- 〃 antiquity of, 367
- Ocean-currents, absolute heating power of, 23
- 〃 influence of, on normal temperatures overlooked, 40
- 〃 maximum effects of, reached at equator and poles, 49
- 〃 compensatory at only one point, 49
- 〃 heating effects of, greatest at the poles, 50
- 〃 cooling effects of, greatest at equator, 50
- 〃 earth not habitable without, 51
- 〃 result of deflection into Southern Ocean, 68
- 〃 palæontological objections against influence of, 53
- 〃 deflection of, the chief cause of changes of climate, 68
- 〃 how deflected by eccentricity, 69
- 〃 deflected by trade-winds, 70
- 〃 temperature of southern hemisphere lowered by transference of heat to northern hemisphere by, 92
- 〃 take their rise in the Southern Ocean, 92
- 〃 cause of, never specially examined by physicists, 95
- 〃 if due to specific gravity, strongest on cold hemisphere, 97
- 〃 if due to eccentricity, strongest on warm hemisphere, 97
- 〃 if due to specific gravity, act only by descent, 99
- 〃 mode by which specific gravity causes, 100, 101
- 〃 the true method of estimating the amount of heat conveyed by, 207
- 〃 due to system of winds, 212
- 〃 system of, agrees with the system of the winds, 213
- 〃 how they mutually intersect, 219
- 〃 in relation to climate, 226
- 〃 direction of, depends on direction of winds, 227
- 〃 causes which deflect, affect climate, 228
- 〃 in relation to distribution of plants and animals, 231
- 〃 effects of, on Greenland during glacial period, 260
- Œpinus on influence of eccentricity on climate, 529
- Ohio inter-glacial beds, 249
- Old Red Sandstone, evidence of ice-action in conglomerate of, 294, 295
- Oolite of Sutherlandshire, 454
- Oolitic period, evidence of ice-action during, 301−303
- 〃 warm climate in North Greenland during, 302
- Organic remains, absence of, in glacial conglomerate of Upper Miocene period, 286
- Organic life, paucity of, a characteristic of glacial periods, 287
- Orkney Islands, glaciated by land-ice, 444
- Osborne, Captain, remarks on recent forest trees in arctic regions, 262, 263
- Oudemans, Dr., on planet Mars, 80
- Overton Quarry, inter-glacial bed in, 247
- Pacific Ocean, depth of, 147
- Packard, Mr., on glacial phenomena of Labrador, 282
- Page, Professor, on temperate climate of Coal period, 422
- 〃 on character of coal plants, 421
- 〃 on old watercourse at Hailes quarry, 490
- Palæontological objections against influence of ocean-currents, 53
- Palæontological evidence of last glacial period, 285
- Parry, Captain, discovery of recent trees in Melville Island by, 262
- Peach, Mr. C. W., on inter-glacial bed at Leith Walk, 246
- 〃 on boulder clay of Caithness, 436
- 〃 on striated rock surfaces in Cornwall, 464
- Peach, Mr. B. N., on striation of Caithness, 453
- Pengelly, Mr. W., on raised beaches, 407
- Perigee, nearness of sun in, cause of snow and ice, 74
- Perihelion, warm conditions at maximum when winter solstice is at, 77
- Permian period, evidence of ice-action in, 298−303
- Perthshire hills, ice-worn surfaces at elevations of 2,200 feet on the, 440
- Petermann, Dr. A., on Dr. Carpenter’s theory, 138
- 〃 on thermal condition of the sea, 138
- 〃 chart of Gulf-stream and Polar current, 219
- 〃 Geogr. Mittheilungen of, list of papers in relation to arctic regions, 556
- Phillips, Professor, on influence of eccentricity on climate, 539
- Poisson’s theory of hot and cold parts of space, 7
- Polar regions, effect of removal of ice from, 64
- 〃 influence of ice on climate, 64
- 〃 low summer temperature of, 66
- Polar cold considered by Dr. Carpenter the primum mobile of ocean-currents, 173
- 〃 confusion of ideas regarding its influence, 180
- 〃 influence of, according to Dr. Carpenter, 180
- Polar ice-cap, displacement of the earth’s centre of gravity by, 368
- Port Bowen, mean temperature of, 63
- Portobello, striated pavements near, 255, 256
- Post-tertiary formations, hypothetical thickness of, 366
- Pouillet, M., on the amount of the sun’s heat, 26
- 〃 on amount of sun’s rays cut off by the atmosphere, 26
- Pratt, Archdeacon, on glacial submergence, 387
- Prestwich, Professor, on Hoxne inter-glacial bed, 241
- Pressure as a cause of circulation, 187
- Principles of geology, nature of, 4
- Prince Patrick’s Island, discovery of recent tree in, 261
- Radiation, rate of, increases with increase of temperature, 37
- 〃 of gases, 38
- 〃 the way by which the earth loses heat, 39
- 〃 how affected by snow covering the ground, 58
- 〃 how affected by humid air, 59
- 〃 accelerated by increased formation of snow and ice, 75
- Raised beaches, date of, 407
- 〃 Mr. Pengelly on, 407
- Ramsay, Professor, on glacial origin of Old Red Sandstone of North of England, 294
- 〃 on Old Red Sandstone, 367
- 〃 on geological time, 343
- 〃 on ice-action during Permian period, 298
- 〃 on boulders of Permian age in Natal, 301
- 〃 on thickness of stratified rocks of Britain, 267, 361
- Redhall Quarry, inter-glacial bed in, 247
- Red Sea, why almost rainless, 30
- Regelation, rationale of, 520, 554
- 〃 Professor James Thomson on cause of, 554
- 〃 Professor Faraday on cause of, 554
- Regnault, M., on specific heat of sandstone, 86
- Reynaud, Jean, on influence of eccentricity on climate, 541
- Rhine, ancient, bed in German Ocean, 480
- Ridge between Capes Trafalgar and Spartel, influence of, 167
- Rink, Dr., on inland ice of Greenland, 380
- River-ice, effect of, 279
- River-ice does not produce striations, 279
- River systems, carrying-power measure of denudation, 336
- River valleys, how striated across, 525
- Robertson, Mr. David, on Crofthead and Hillhead inter-glacial beds, 247, 248
- 〃 on foraminifera in red clay, 485
- Rock-basins, how excavated by ice, 525
- Rocks removed by denudation, 361
- Ross, Capt. Sir James, on South Shetland, 61
- 〃 on temperature of antarctic regions in summer, 63
- Sandwich Land, description by Capt. Cook, 60
- 〃 cold summers of, not due to latitude, 64
- Salter, Mr., on carboniferous fossils of arctic regions, 298
- 〃 on warm climate of North Greenland during Oolitic period, 302
- Saltness of the ocean, difference of, as a cause of motion, 103
- 〃 in direct opposition to temperature in producing ocean-currents, 104
- Scandinavian ice, track of, 447
- Scandinavian ice-sheet in the North Sea, 444
- Scoresby, Dr., on condition of arctic regions in summer, 58, 62
- 〃 on density of Gulf-stream water, 129
- Scotland, inter-glacial beds of, 243−249
- 〃 evidence of ice-action in carboniferous conglomerate of, 296
- 〃 buried under ice, 439
- 〃 ice-sheet of, in North Sea, 442
- 〃 why ice-sheet was so thick, 452
- Sea, height of, at equator above poles, 119
- 〃 rise of, due to combined effect of eccentricity and obliquity, 403
- 〃 bottoms not striated by icebergs, 272
- Sea and land, present arrangement indispensable to life, 52
- Sea-level, oscillations of, in relation to distribution, 394
- 〃 oscillations of, during formation of coal measures, 424
- 〃 raised, by melting of antarctic ice-cap, 388
- 〃 influence of obliquity of ecliptic on, 403
- Section of Mid-Atlantic, 222
- Section across antarctic ice-cap, 377
- Sedimentary rocks existing fragmentary, 361
- 〃 of the globe, mean thickness of, hitherto unknown, 361
- 〃 how mean thickness might be determined, 362
- 〃 mean thickness of, over-estimated, 364
- Shearing-force of ice, 496
- 〃 momentary loss of, 518
- Shetland islands glaciated by land-ice from Scandinavia, 450
- Shetland, South, glacial condition of, 61
- Shell-beds, evidence of warm inter-glacial periods from, 252
- Shells of the boulder clay of Caithness, 450
- Shore-ice, striations produced by, in Bay of Fundy, 280
- Silurian period, ice-action in Ayrshire during, 293
- 〃 evidence in Wigtownshire of ice-action during, 293
- Slitrig, inter-glacial bed of, 243
- Slope of surface of maximum density has no power to produce motion, 120
- 〃 from equator to pole, erroneous view regarding, 120
- Smith, Mr. Leigh, temperature soundings, 129
- Smith, Mr., of Jordanhill, on striated pavements, 256
- Snow, how radiation is affected by, 58
- 〃 common in summer in arctic regions, 62
- 〃 rate of accumulation of, increased by sun’s rays being cut off by fogs, 75
- 〃 formation increased by radiation, 75
- Somerset, West, glaciation of, 463
- Somerville, Mrs., on influence of eccentricity on climate, 540
- South Africa, glaciation of, 242
- 〃 boulder clay of Permian age in, 300
- South of England ice-sheet, 463
- South Shetland, glacial condition of, at mid summer, 61
- South-west winds, heat conveyed by, not derived from equatorial regions, 28
- 〃 heat conveyed by, derived from Gulf-stream, 28
- Southern hemisphere, present extension of ice on, due partly to eccentricity, 78
- 〃 why colder than northern, 81−92
- 〃 absorbs more heat than the northern, 90
- 〃 lower temperature of, due to ocean-currents, 92
- 〃 surface currents from, warmer than under currents to, 92
- 〃 glacial and inter-glacial periods of, 242
- Southern Ocean, thermal condition of, 225
- Specific gravity can act only by causing water to descend a slope, 99
- 〃 mode of action in causing ocean-currents, 100
- 〃 inadequacy of, to produce ocean-currents demonstrated by Sir John Herschel, 116
- Spitzbergen, Gulf-stream and under current at, 134
- 〃 Miocene flora of, 309
- Stellar space, temperature of, 35
- 〃 received temperature of, probably too high, 39
- Stewart, Professor Balfour, experiment on radiation, 37
- 〃 on cause of glacial cold, 79
- Stirling, Mr., on old watercourse near Grangemouth, 481
- St. John’s River, action of ice on banks of, 279
- St. Lawrence, action of ice on bank of river, 279
- Stockwell, Mr., on eccentricity of earth’s orbit, 54
- 〃 on obliquity of ecliptic, 399
- 〃 table of superior limits of eccentricity, 531
- Stone, Mr., on eccentricity of the earth’s orbit, 322
- Stow, G. W., on glacial beds of South Africa, 242
- 〃 on Karoo beds, 301
- Striæ, direction of, show the clay of Caithness came from the sea, 436
- Striations obliterated rather than produced by icebergs, 274
- Striated pavements why so seldom observed, 256
- 〃 evidence of inter-glacial periods from, 255
- Striated stones found in conglomerate of Lower Carboniferous age by Professor Geikie, 296
- 〃 in Permian breccias, 299
- 〃 in the glacial conglomerate of the Superga, Turin, 306
- Stratified rocks may be formed at all possible rates, 360
- 〃 rate of formation of, as estimated by Professor Huxley, 363
- Struve, M., formula of obliquity of ecliptic, 404
- Subaërial denudation, rate of, 331
- Submarine forests, 409
- 〃 (ancient), coal seams the remains of, 428
- Submergence, physical causes of, 368
- 〃 coincident with glaciation, 389
- 〃 of land resulting from melting of antarctic ice-cap, 389
- 〃 how affected by fluidity of interior of the earth, 395
- 〃 necessary for preservation of coal plants, 423
- 〃 frequent during formation of coal beds, 426
- Subsidence insufficient to account for general submergence, 390
- 〃 necessary to accumulation of coal seams, 427
- Sun supposed by some to be a variable star, 8
- 〃 maximum and minimum distance of, 55
- 〃 rays of, cut off by fogs in ice-covered regions, 60
- 〃 nearness in perigee a cause of snow and ice, 74
- 〃 total amount of heat radiated from, 346
- 〃 age and origin of, 346
- 〃 source of its energy, 347
- 〃 heat of, origin and chief source of, 349
- 〃 originally an incandescent mass, 350
- 〃 energy of, may have originally been derived from motion in space, 355
- Surface currents which cross the equator warmer than the compensatory under currents, 92
- Surface currents from poles to equator, according to Maury, produced by saltness, 108
- Sutherland, Dr., observations by, on stranding of icebergs, 275
- 〃 testimony, that icebergs do not striate rocks, 278
- 〃 on the boulder clay of Natal, 300
- Sutherland, boulder conglomerate of Oolitic period of, 302
- Sweden, Southern, shells in glacial shell beds of, 253
- Switzerland, inter-glacial period of, 239
- 〃 M. Morlat on inter-glacial periods of, 240
- 〃 gravels of, by Mr. James Geikie, 268
- 〃 Eocene glacial epoch in, 305
- Table of June temperatures in different latitudes, 65
- 〃 soundings in temperate regions, 222
- Tables of eccentricity, 314−321
- 〃 of eccentricity, explanation of, 322
- Tay, valley of, striated across, 526
- 〃 ancient buried channel of, 490
- Temperate regions, cold periods best marked in, 258
- Temperature of space, 532
- 〃 reasons why it should be reconsidered, 39
- Temperature (mean) of equator and poles compared, 41
- 〃 why so low in polar regions during summer, 66
- 〃 how difference of specific gravity is caused by, 102
- 〃 higher, of the waters of Gulf-stream considered by Lieutenant Maury as the real causes of its motion, 111
- 〃 of sea at equator decreases most rapidly at the surface, 119
- 〃 of Greenland in Miocene period, 310
- 〃 of poles when obliquity was at its superior limit, 402
- Tension, effect of, on ice, 522
- 〃 the cause of the cooling effect produced by, 552
- Tertiary period, climate of, error in regard to, 288
- Thermal condition of Southern Ocean, 225
- Thibet, table-land of, 418
- Thomson, Professor James, on cause of regelation, 554
- 〃 theory of glacier-motion, 512
- Thomson, Mr. James, on glacial conglomerate in Arran, 299
- 〃 on ice-action in Cambrian conglomerate of Islay, 292
- Thomson, Professor Wyville, on Dr. Carpenter’s theory, 129
- 〃 cited, 130
- 〃 thermal condition of the sea, 138
- Thomson, Sir W., amount of internal heat passing through earth’s crust, 142
- 〃 on limit to age of the globe, 343
- 〃 on influence of ice-cap on sea-level, 372
- 〃 climate not affected by internal heat, 6
- 〃 earth’s axis of rotation permanent, 7
- 〃 on volume and mass of the sun, 347
- Tidal wave, effect of friction, 336
- Tides, supposed argument from, 184
- Time, geological, 311−359
- 〃 as represented by geological phenomena, 326
- 〃 represented by existing rocks, 361
- Torrid zone, annual quantity of heat received by, per unit of surface, 194
- Towncroft farm, section of channel at, 474
- Towson, Mr., on icebergs of Southern Ocean, 383
- Trade-winds (anti), heat conveyed by, over-estimated, 28
- 〃 (anti) derive their heat from the Gulf-stream, 32
- 〃 of warm hemisphere overborne by those of cold hemisphere, 70
- 〃 causes which determine the strength of, 70
- 〃 strongest on glaciated hemisphere, 70
- 〃 reaction upon trade-winds by formation of snow and ice, 76
- 〃 influence of, in turning ocean-currents on warm hemisphere, 97
- 〃 do not explain the antarctic current, 211
- Tiddeman on North of England ice-sheet, 458
- 〃 displacement of, 230
- Transport of boulders and rubbish the proper function of icebergs, 281
- Trafalgar, effect of ridge between Capes Spartel and on Gibraltar current, 167
- Turner, Professor, on arctic seal found at Grangemouth, 485
- Tylor, Alfred, on denudation of Mississippi basin, 333
- Tyndall, Professor, on heat in aqueous vapour, 29
- 〃 on sifted rays, 47
- 〃 on diathermancy of air, 59
- 〃 on glacial epoch, 78
- Udevalla, Mediterranean shell in glacial shells, bed of, 253
- Under currents to southern hemisphere colder than surface currents from, 92
- 〃 produced by saltness, flow from equator to poles, 106
- 〃 account for cold water at equator, 124, 142
- 〃 in Davis’ Strait, 134
- 〃 take path of least resistance, 130
- 〃 why considered improbable, 135
- 〃 difficulty regarding, obviated, 217
- 〃 theory of, 217
- Underground temperature, Professor J. D. Forbes on, 86
- Underground temperature exerts no influence on the climate, 88
- 〃 absolute amount of heat derived from, 142
- 〃 supposed influence of, 176
- Uniformity, modern doctrine of, 325
- United States’ coast survey of Gulf-stream, 24
- 〃 hydrographic department, papers published by, 556
- Unstratified boulder clay must be the product of land-ice, 437
- Upsala and Stockholm striated by Baltic glacier, 447
- Vertical circulation, Lieutenant Maury’s theory of, 108
- 〃 according to Dr. Carpenter, 153
- Vertical descent of polar column caused by extra pressure of water upon it, 154
- 〃 effects of, and slope, the same, whether performed simultaneously or alternately, 159
- 〃 of polar column illustrated by diagram, 160
- Vertical distribution of heat in the ocean, Mr. Buchanan’s theory, 550
- Vogt, Professor, on Dürnten lignite bed, 241
- Warm hemisphere made warmer by increased reaction of physical causes, 76
- Warm periods best marked in arctic regions, 258
- 〃 in arctic regions, evidence of, 261
- 〃 better represented by fossils than cold periods, 288
- 〃 evidence of, during Cretaceous age, 304
- Warm inter-glacial periods in arctic regions, 258−265
- Water at equator the best means of distributing heat derived from the sun, 30
- Water, a worse radiator than land, 91
- Wastdale granite boulders, difficulty of accounting for transport of, 456
- Wastdale Crag glaciated by continental ice, 457
- Weibye, M., striation observed by, 280
- Wilkes, Lieutenant, on cold experienced in antarctic regions in summer, 63
- Wellington Sound, ancient trees found at, 265
- Winter-drift of ice on coast of Labrador, 276
- West winds, moisture of, derived from Gulf-stream, 29
- Wind, work in impelling currents, 219
- Winds, ocean-currents produced by, 212
- 〃 system of, agrees with the system of ocean-currents, 213
- Wind theory of oceanic circulation, 210
- 〃 crucial test of, 220
- Wigtownshire, ice-action during Silurian age, 293
- Work performed by descent of polar column, 157
- Wood, Mr. Nicholas, on buried channel, 488
- Wood, Jun., Mr. Searles, middle drift, 250
- 〃 on occurrence of chalk débris in south-west of England, 460
- Woodward, Mr. H. B., on boulder clay in Devonshire, 463
- Wunsch, Mr. E. A., on glacial conglomerate in Arran, 299
- Yare, ancient buried channel of, 489
- Young, Mr. J., objection considered, 482
- Yorkshire drift common in south of England, 460
- Zenger, Professor, on the moon’s influence on climate, 324