The strandflat and isostasy:
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Buch |
| Sprache: | English |
| Veröffentlicht: |
Kristiania
Dybwad
1921 [erschienen] 1922
|
| Schriftenreihe: | Skrifter / Videnskabsselskapet i Kristiania, Matematisk-Naturvidenskabelig Klasse
1921,11 |
| Schlagworte: | |
| Online-Zugang: | Inhaltsverzeichnis |
| Beschreibung: | VIII, 313 S. zahlr. Ill., Kt. |
Internformat
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| 100 | 1 | |a Nansen, Fridtjof |d 1861-1930 |e Verfasser |0 (DE-588)118586378 |4 aut | |
| 245 | 1 | 0 | |a The strandflat and isostasy |c by Fridtjof Nansen |
| 264 | 1 | |a Kristiania |b Dybwad |c 1921 [erschienen] 1922 | |
| 300 | |a VIII, 313 S. |b zahlr. Ill., Kt. | ||
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| 490 | 1 | |a Skrifter / Videnskabsselskapet i Kristiania, Matematisk-Naturvidenskabelig Klasse |v 1921,11 | |
| 650 | 4 | |a Isostasy | |
| 810 | 2 | |a Videnskabsselskapet i Kristiania, Matematisk-Naturvidenskabelig Klasse |t Skrifter |v 1921,11 |w (DE-604)BV010931525 |9 1921,11 | |
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Datensatz im Suchindex
| _version_ | 1805079386110558208 |
|---|---|
| adam_text |
Titel: The strandflat and isostasy
Autor: Nansen, Fridtjof
Jahr: 1922
CONTENTS.
I'tlljV
L Iritroductiim.i
'T. Tlit'orU-s 01' ihr: gt-noiir «ricin -il' the stnindîlut .|
71 f. The eJfi'ct of tfic sHiMa'riai 'tanudfttion in :h - coastal / i'c.16
IV. Glacial cmsion.'-*o
'11m- erosion of tin ^lairitrs of iht inland ; v .so
Tili1 wosimi of lortii ylneicr^.-5
V. .Mariiur tlemulation. Shore erosion by froM. .128
VI. The development ui tisi- Norwegian ytrund'laî .4H
When was the Nnnwjdan strandllat dewloprd.46
The height of the; Norvvesrian stnmdflal .V ?
riio partial ahsontv uf ;i .straiidflal ulonp; snmi- part* of tin¦ Niirvvi^irin i'u.K jg
Summary .5a
VII. 'I'll*.1 strandflat 01 ti't- N'oruvirinr. coa.-t from tin- region ;' Sovile Fjurtä t
ihi- lvsjion ii." llanl-msjer Fjorù.5S
'I'll,- ^r.inuilfvt of Supy Fjord.57
Tli ^¦-rtetie origin r, ' :lu ^iraiuWut in So nr Fjord.66
The htrandtlat north niKi south of the -noi;th of Sotm-: Fjord .60
The r-fjinn of Li'idu« Ps.-qis;.-Hi!u .71
The- îvdon of Kfui-i .73
[¦Lotion of [-»iTtct-n.-Q
Rftrii-n of Soin: .81
lslamln (u-tween Kurs Fionj and Hardangc.- Fjord.83
Harûaniîtr Fjo-.-d and Bommel Fjord .84
VII!. TIi - istrandt'ii! of the i-oiitfwi'^iern and «ouJicrn ron-t of N »r\va\ .9'
The region r«f Kanu«; .Qi
'3"he Slavanji^r region .93
I-Matio'i Iw-tweer the g:eolo;rie:d WLnu-ture of tin- roiet and llie ominvnee of
tlü- Ktrandfiht .
Javb.-i-'-n .ioo
The hijjli, st«¦•-[ eonst. :- f w 1. n Jagden-» nnd l.i;V.( r .102
Fron» l.i.str" to the Xjiz - 'I.inde«iKS .iO-i
The southern find ^liSi-ef^tem cuast of Norway.105
The inn-.-r fr.«i ot' Christiania -l';ord . 07
IX. The intnf|'l!U îùuns the from So^uo Fjonl t Vikien.1 rs
Thu ivifio''. 'it' Wolijo'-d, aod r-hil .113
TU." r.-^ir.i! ot' Ale-und .*.113
Tito r -pi-)o 01' lütteren, .-md Fmi».füO
fVo-)i T,-ni»üi;t ru F/t'I k \'t«c(i n.Jat
VIJ
Pl.jjr
X. The ^trandUat r.l' northern Norway.;yq
Heideland.120
Traîna .
Relation between tlin différences in the surface topography of the submerged
plateaus ami dilferein-es in tin- nature of their rocks.( j.7
Const of northern Helgoland and tin- cast coast ot' West Fjord.152
I.ofoten and Wslerafcn .i-^6
Senjen lo Ringvasni.163
Finmarfcen .163
XI. Tlie strandllat of Bear Island .165
XII. The strandflat of Spitsbergen .17Ü
Literature.1 78
Relation between thi; development of the strandflat sind the geological struc-
ture of the land .185
Prince Charles Foreland.185
West coast of Spitsbergen south of Ice Fjord .ioa
Cape C.uissez in Crass Hay.1Q3
Cape Mitre Peninsula and the north-western j art of Spitsbergen .to;-j
Reindeer Land. . 106
The peninsula betivei-n I.iefde Bay and Wijde Ray.197
East coast of Wijde Hay, and Verleegeii Hook . .200
North-west coast of North East (.and.soy
The fjords .i-'oy
The age and genesis of the strandflat of Spitsbergen .«04
Raised shore-lines .-'07
Platforms at high levels .ao8
Xm. Thf strandflat along the coast inside and outside the arctic region*.aii
The coasts of Siberia, Greenland, and Alaska.an
Shetland Islands . -.^14
XIV. Tb«: levels of the strandflat and their development .ai y
Summary of the results of our investigations of the- strandflat .u 1 ;
The emerged strainlflat.ai;
The submerged strandflat uf Norway.!.ûîH
The three levels of the strandflat.-"Q
Causes of the charges in the level of tb«; strandflüt .ano
nie nature of the rooks and the topography of the slramltlat and the conti-
nental shelf.2~5
XV. Tiie continental shelf and its formation .unj
Fluctuations in sea-level caused by the formation of ice-caps.asg
The thickness of the ice-caps.030
Shifts of sea-level and shore-line caused by changes in the volume of t(i»-
Ocean.233
Tin; lowering of sen-level during- the glacial period* and the surfac* of the
continental slielf.^37
The deposition of sediment has gradually raised the general sen-level.ayo
XVI. The strandflat and the late-glacial and postglacial submergence of Fonno-Scandia 345
The late-glacial and postglacial upheaval of Sogne Fjord.246
'Hie late-glaeial anil postglacial upheaval in the region of N'ord Fjord.u 48
Gradient of the- laty-glaeial and jiostgkeial upheaval of the- west and north
coast of Kenno-S'*:mdia .-5 *
Helfliioi: between the inclinations of the two conspicuous raise»'. shure-liiK
of Northern Norway and the Kola Peninsula .056
VIII
K--Siitii i! lii twivi1 die altitudes 'if t!u- uv" oouvpir-unu-: raised shoredims in
Iii-- l'fonisn Hamm«di-tricts. -îjs«-'1
Relation b.uvi-in Un' altitude.« of Taunrr's shore-lines n.n«I !H in Finmark üoi.1
TU- npprr limit of lair-^laoiaJ suhnn-wntv and ihr I'sijjfr. Irwl on the Köln
I'rninsnla . -Jöo
riif np]ji r limit t" -ulin- • and the Tapi s Irvrl almig ihr N'urwetrian
si'udi nt't/ii- Tj'oiiw» district. uoc)
Thr uniform rharurUr ot' ihr lat«--j;Iarial and postglacial upheaval nlnn^ the
\%t st and north eoaM of I'Vnno-i-M'andin . ^T.'l
'1'hr Iriti--jfliiriiil an l postglacial siibimTy.viuv anil emergence in central am!
ea-trrn Fni'U'-Soainiiii and in .Intlund. 275
I hr present enislal movements in the regions round ihr Baltii' Sea and ihr
»ulf of Bothnia . 276
I hr possibility f a sirandflat al« n r thr Baltic am! üothiiian roast . 1276
Thr tvasons why ihr po-Urlacial crustal movements have been retarded in
the vcjiiviii- round ihr Baltic S.-a ami thr m\f t«V Bothnia . '-280
Relation hiWccn ihr heights ot' ihr Tapes level and of ihr upper marine
limit in rentrai and suiitlieru I'Vnno-Scandia. üBg
The cans«- of tin; transgression of Ihr *ea in tin- Tuprs-I.ittoriua period. uB6
W/i.'il may have firm Ihr ranse nf n rise or' the srft-I.'vrl during the "i'jjjrs-
Litlorina period?. ljc*7
X\II. Isosiasy . joo
Thr llieniv of isowlasv . 29 t
Thr ('rust's capacity of iso-statir lviulHMmrnt. ii )4
How arc ;li: isostatic vertical mo\rmnls of thr litliosphriv elfcrtrd . 297
How lonsr a lim.' dor* thr earth's erust r "|irirr to tvru'h its nr\v isustatic
level alUT a disturbance of its rsjiiilihriunt V.
W'hal i lit'- ext.'nt ot thr small, -st an a within which i.sortatie movements
may mviu''? . M'- 4
and rrosiim. 304 |
| any_adam_object | 1 |
| author | Nansen, Fridtjof 1861-1930 |
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| indexdate | 2024-07-20T06:44:09Z |
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| language | English |
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| owner_facet | DE-12 DE-29 DE-19 DE-BY-UBM DE-11 DE-83 DE-188 |
| physical | VIII, 313 S. zahlr. Ill., Kt. |
| psigel | HUB-ZB011201010 BSBQK0092 |
| publishDate | 1921 |
| publishDateSearch | 1922 |
| publishDateSort | 1922 |
| publisher | Dybwad |
| record_format | marc |
| series2 | Skrifter / Videnskabsselskapet i Kristiania, Matematisk-Naturvidenskabelig Klasse |
| spelling | Nansen, Fridtjof 1861-1930 Verfasser (DE-588)118586378 aut The strandflat and isostasy by Fridtjof Nansen Kristiania Dybwad 1921 [erschienen] 1922 VIII, 313 S. zahlr. Ill., Kt. txt rdacontent n rdamedia nc rdacarrier Skrifter / Videnskabsselskapet i Kristiania, Matematisk-Naturvidenskabelig Klasse 1921,11 Isostasy Videnskabsselskapet i Kristiania, Matematisk-Naturvidenskabelig Klasse Skrifter 1921,11 (DE-604)BV010931525 1921,11 HBZ Datenaustausch application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=013862909&sequence=000002&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis |
| spellingShingle | Nansen, Fridtjof 1861-1930 The strandflat and isostasy Isostasy |
| title | The strandflat and isostasy |
| title_auth | The strandflat and isostasy |
| title_exact_search | The strandflat and isostasy |
| title_full | The strandflat and isostasy by Fridtjof Nansen |
| title_fullStr | The strandflat and isostasy by Fridtjof Nansen |
| title_full_unstemmed | The strandflat and isostasy by Fridtjof Nansen |
| title_short | The strandflat and isostasy |
| title_sort | the strandflat and isostasy |
| topic | Isostasy |
| topic_facet | Isostasy |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=013862909&sequence=000002&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA |
| volume_link | (DE-604)BV010931525 |
| work_keys_str_mv | AT nansenfridtjof thestrandflatandisostasy |