• No results found

GIPSDALEN, Svalbard ��I ternary Geology and Geomorphology

N/A
N/A
Protected

Academic year: 2022

Share "GIPSDALEN, Svalbard ��I ternary Geology and Geomorphology "

Copied!
1
0
0

Laster.... (Se fulltekst nå)

Fulltekst

(1)

Part of Environmental Alias Gipsdalen, Svalbard Norsk Polarinstitutt

GIPSDALEN, Svalbard ��I ternary Geology and Geomorphology

/

'j

�Fi{ . '<\

i-

r, o

}

,

"

V (: ..

.' <

<

t '

!� "'" ! !

"

�. ,

f

}

) \

\ /

\ I

�: 1,r,

"

.i'" � ..

.

, '-" ,,/

t;

, .

, ""'-

.

ID

ri

�jt

.

,

,

'\

o

q�

*-

Department of Physical Geography, University of Oslo

AVdel,ng lor nalU'geOQ'erl, Un,vers/telel l O�lo

v

o o

lo

T ill

Mo,enem.,er/.le

Glaciofluvial material

Gla$III".ial/ møler/aJe

, ' , ,

Fluvial material, pre-recent

FkJv/all meleri.le, pre"UIfII

Fluvial material, recen!

F/"vl.1I møler/ele, ,esen'

Marine beach material

Mørml Slrendmeter�/e

Marine material, line-grained

Marml mIlIetlele, II(1�o'nlQ

Eolian material

Eo/isk meIetlaIe

Weathering material

For.llringsmalerløle

Scala 1:40,000

MllestoH 1 '.0000

Colluvium

Rum.,erl.1e

Gelifluction material

Ge!lfhJkl/on,melerlllle

Organic material

Orgenis� mele,/a/a

Exposed bedrock

Betl liell

Glaeier I snow patch (1961)

Bre f sn"fonn (196 l )

Icing (1989)

Icing (l989)

Glaeial strlae

SkurongBSlnpar

Terminal and medial moraine mainly Iee-cored

Rand- og midtmorene, "esent/ig ISk/e",e

�' / ø

. .

%

, , ' ,

! ,

q \ ,

" .....

-",

--1

,--'­

, I

, '-I .;.,,-

i \. � ,

�-

� (j(:), = ...

�: � �

�&,

1'1" \

-.. " \ -r -; -+

-e

\

r-, i'.,'"

-. .. .-; l' " : ,

�- �' � , , : . � �:\.

. ,

Æ' ,

\' \

, \ �. ·,

,

\ 7

/

r

De Geer moraines

�f;f;

Beaeh ridges distinct,less dis tinet Srram1voller De Geer morener

Canyon , , Strandline

Canyon '.' ./ Sirand!onie

Meltwater channels

/

Aråte

Spylerermer '"

Washed surface

.;::;

Erosjon scarps in bedrOCk large

Spy/e/all

Etos/on,hnter IIJ{I", $Iore

Gullies . Erosjon scarps in bedrock

--</

small

R.vm'"

Erosjondenter ; fjell. sm.

Channels on alluvial fans and river fiats

Erosion scarps in sediments E,o'Jon,k.nter I le",,,,'e,,ala Rentle, p. vifler og e/veskme, .'

Atluvial fan

0

Terrace edge

Ville Terr.ueken,

Eolian forms Depression, thermokarst

Eol/ske former C> Forsenknlng,lermokllrsr

o o o

o o

"'"

-, . " '

I I ' "

" , , ,

, , . '

--:-

,

:

"

ii

,

,

,

Tundra polygons

Tundr.polYQoner

Earth hummocks JordlOJ<Jr

Nonsorted polygons and circles

USOIlette poIYf1OIIIIt og P1<Jer

Sorted polygons

Sortarie polygoner

Sorted circles

Sorle"e �Ir�let

Stripes

Srrlper

Gelifluction lobes

GelilluksjonsvalhN

Rock glaeier

SI""o'e

, , ,

" " I I

" I / ,

/ I I

d6:JO

.'

<

, '

,<

",=<��=<,"oxo',=============,=============

=l

'==============',==============l,=============

'==============

±

'=============='

l=

============

" l=

' ============

'==============Jl0.km

- I I I ! I I I I I I

Avalanche tracks

Sbalilep

Talus cones

Rask/egler

Debris slide, small

Jordsk,ed, /ile

Large boulders

Sla'. blokkar

Mounds and ridges

Hauget og rYf1Qer

Crevasses (1961)

Sre,pteUer (r 91J I )

Vehicular track

K;ørespor

CootOlJ' ilterval 50 metres Elrvii:irfanse 50 ..-

,

l: 40,000

" :

.-4.

!

. '

� .J

.. ,' /

-! ;,'

,' "

.;.

'''

/';. , ' , ''''

��d.JJ..

Reference:

I

Tolgensbakk, J. 1990: GIPSDALEN, Svalbard, Quaternary Geology and Geomorphology 1:40,000 Department of Physical Geography, University of OslO

Fieldwork:

Fe/lll,oeide;

K. Høgvard, L Sørbel and J. Tolgensbakk 1988-1989 Reprography:

RePfOfP·1i

Departm8flt of PhysiCal Geography University of OSlo

Printing:

rrvkklng=

Harald lyche & Co. A.S 3 -1990 Commissioned by:

(}pprkttgsfJIVfJF=

Northern Resources Ltd.

Base map:

Gru,mlllgskllrl;

Topographic map ol Svalbard 1:tOO,ooo, C8 Billefjorden enlarged to scala 1:40,000

...-IliD_�

U�\\

"o� � J

Published by

Utg'" e.

Norsk Polarinstitutt, Oslo 1990 .j' ...

... OlAltl�'>-<'

Referanser

RELATERTE DOKUMENTER

The presented study of ternary MNiSn and pseudo-ternary M 0.5 M′ 0.5 NiSn/M 0.5 M′ 0.25 M″ 0.25 NiSn HH compounds, performed with high-resolution SR-PXD, reveal the separation of

Bøe, R.: Marine geology at the Geological Survey of Norway.. EuroGeoSurveys Marine Geology Expert Group,

The Iddefjord granite forms part of the Swedish Bohus batholith and ranges in composition from diorite to granite.. The gran ite consists of 13 individual plutons, and the mechanism

The process of creating terrain and landscape models is important in a variety of computer graphics and visual- ization applications, from films and computer games, via

specialized insight in one of the following fields; marine geology and geophysics, petrology/structural geology, sedimentology and Quaternary geology, or petroleum geoscience.. 

fartøyet &#34;Lance&#34;, fly og helikoptre. I felt samarbeidet instituttet med mer enn 50 forskere fra andre institusjoner. Ytterligere 40 forskere fikk anledning til å

Towards the end of the Permian, Svalbard and the Barents Sea became a land surface for some million years, and were still part of a continuous continent which included,

In this work we use seismic reflection data to examine the evolution of a normal fault network in the Oseberg Fault Block in the northern North Sea Rift System e a rift system