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Grønfjord-Colesbukta

Natural and human history

Map: Grønfjord-Colesbukta

Map: Grønfjord-Cole­s­buk­ta.

Gene­ral

This page is about the natu­ral and human histo­ry of the Grønfjord area and the Isfjord coast fur­ther east. The­re is a dedi­ca­ted page about Bar­ents­burg. In ear­lier times, Grønfjord was known as Green Har­bour. Both names mean the same.

Grønfjord

Grønfjord from abo­ve as a snow land­s­cape in March.
Seen from the sche­du­led flight, view to the nor­thwest.

But the area is, of cour­se, hea­vi­ly influ­en­ced by Bar­ents­burg and the aban­do­ned dou­ble sett­le­ment of Cole­s­buk­ta and Grum­ant­by­en. You will find traces of acti­vi­ties rela­ted to the­se sett­le­ments, most­ly mining, almost any­whe­re. This is some­ti­mes inte­res­ting and some­ti­mes rather annoy­ing, when it comes to indus­tri­al was­te, often harm­ful to wild­life, that is just left in the arc­tic envi­ron­ment.

Barentsburg, Grønfjord

View over Bar­ents­burg and into Grønfjord: snow land­s­cape in the ear­ly win­ter (Octo­ber).

Nevertheless, the area has one of Spitsbergen’s richest tun­dra envi­ron­ments, in Grønfjord, Cole­s­da­len and other lar­ge val­leys. The­re and near Grum­ant­by­en it is recom­men­ded to boil water tho­rough­ly befo­re drin­king it or using it to pre­pa­re food or other hygie­ni­cal­ly sen­si­ti­ve pur­po­ses, as the­re are intro­du­ced mice that can spread fox tape­worm (Echi­no­coc­cus mul­ti­lo­cu­la­ris). An infec­tion is unli­kely, but if this kind of dis­as­ter hap­pens to strike, then it is extre­me­ly dan­ge­rous.

The area has good oppor­tu­nities for sum­mer hiking and win­ter expe­di­ti­ons, from day hikes – from Bjørn­da­len to the west or star­ting in Bar­ents­burg – to lon­ger trips. Hiking from Lon­gye­ar­by­en to Bar­ents­burg (or the other way around), inclu­ding tra­vel­ling the other way by boat, is an opti­on for a first several-day hiking tour in Spits­ber­gen. But I have to admit that I pre­fer the hiking oppor­tu­nities and the sce­ne­ry in Dick­son Land, which is also rea­son­ab­ly acces­si­ble from Pyra­mi­den.

Hiking terrain, Grønfjord

Hiking in Grønfjord. The­re are ple­nty of the­se stee­ply incis­ed litt­le river val­leys in the area, which requi­re time and ener­gy espe­cial­ly when you have to nego­tia­te them
with a hea­vy bag­pack.

The coas­tal area bet­ween Grønfjord and Cole­s­buk­ta is a fre­quent­ly used win­ter rou­te as it is one of two main snow mobi­le rou­tes bet­ween Lon­gye­ar­by­en and Bar­ents­burg. The­re is ano­t­her rou­te fol­lowing some inland val­leys (the­re is a detail­ed descrip­ti­on of this rou­te and other ones in the gui­de­book Spits­ber­gen-Sval­bard). Both rou­tes may also be used on hiking tours in the sum­mer, but they will inclu­de various ter­rain chal­len­ges inclu­ding river cros­sings and wet tun­dra in Cole­s­da­len.

Snow mobile tour, Grønfjord

On snow mobi­le tour in Grønfjord, on the way to Bar­ents­burg.

But the cos­tal rou­te bet­ween Cole­s­buk­ta and Grønfjord – local­ly often refer­red to as the Kapp Lai­la rou­te – is not at all a beach walk or, in the win­ter, a dri­ve along the coast. The coast its­elf is most­ly a low cliff. And the­re is a cou­p­le of ter­rain chal­len­ges in shape of several deeply incis­ed river val­leys which can be dif­fi­cult to nego­tia­te, now mat­ter how you are tra­vel­ling. During a snow mobi­le trip, navi­ga­ting the slo­pes around the­se val­leys can be pret­ty chal­len­ging espe­cial­ly for begin­ners.

Motorschlittentour nach Barentsburg: Nordhallet

Snow mobi­le tour to Bar­ents­burg: Nord­hal­let, the slo­pes south of the Isfjord coast bet­ween Cole­s­da­len and Hol­len­darda­len. Loo­king west, towards Hol­len­darda­len.

A lot depends on the wea­ther during the days befo­re the trip: in case the ground is icy and slip­pe­ry, the stee­per slo­pes, espe­cial­ly tho­se rela­ted to the abo­ve-men­tio­ned, can be dif­fi­cult or even dan­ge­rous and impos­si­ble. This poten­ti­al­ly tri­cky slo­pe area bet­ween Cole­s­buk­ta and Hol­len­darda­len is cal­led Nord­hal­let; the area is more of an obsta­cle than anything else, the most sce­nic aspect being the wide view over Isfjord. Other than that, the­re are ple­nty of other parts of Spits­ber­gen that are more sce­ni­cal­ly attrac­ti­ve than Nord­hal­let. And con­si­de­ring the dif­fi­cul­ties and poten­ti­al dan­gers, it is cer­tain­ly recom­men­ded to join a gui­ded tour unless you have rele­vant expe­ri­ence and know­ledge, or at least pay good atten­ti­on to local advice.

For more, detail­ed infor­ma­ti­on: the Gui­de­book Spits­ber­gen-Sval­bard

Guidebook Spitsbergen-Svalbard

Pro­tec­ted are­as

The only legal­ly pro­tec­ted area in the regi­on is the Fest­nin­gen geo­to­pe, a geo­lo­gi­cal sanc­tua­ry on the Isfjord coast west of Grønfjord. But it does not inclu­de access restric­tions.

Festningen

Sand­stone cliffs at Fest­nin­gen at the ent­ran­ce to Grønfjord.

Geo­lo­gy

The bed­rock on the west side of Grønfjord con­sists most­ly of stee­ply til­ted sedi­men­ta­ry rocky, main­ly fos­sil-rich lime­stones from the upper Car­bo­ni­fe­rous and lower Permi­an. The­se lay­ers are run­ning through the moun­tains Pro­duc­tustop­pen, Braganz­at­op­pen and Var­de­borg to Kapp Sta­ros­tin, giving them a spe­cial struc­tu­re and appearan­ce. See sec­tion geo­lo­gy (Kapp Sta­ros­tin) on the page Kapp Lin­né-Fest­nin­gen.

Geology Grønfjord

Moun­tain cliffs of hard sedi­ment lay­ers (Car­bo­ni­fe­rous-Permi­an) south of Grønfjord.

East of Grønfjord, we find bed­rock con­sis­ting of most­ly hori­zon­tal lower Ter­tia­ry lay­ers. The­re are alter­na­ting lay­ers of sand-, silt- and clay­stone; the sand­stones are coal-bea­ring and part­ly rich in fos­sils (imprints of lea­ves like from hazel­nut trees etc.). The chan­ge from sand- to clay­stone is due to chan­ging rela­ti­ve sea level and thus of chan­ging depo­si­tio­nal envi­ron­ment from del­taic to deeper shelf and can nice­ly be seen in the slo­pes, espe­cial­ly when you ascend one of the few moun­tains towe­ring abo­ve the wide-ran­ging pla­teau, which is 400-500 metres high. In some of the sand­stones, you can find nice ripp­le marks and other sedi­men­ta­ry struc­tures.

Sediment layers, lower Tertiary, Finneset

Lower Ter­tia­ry sedi­ment lay­ers at Fin­nes­et.

The lay­ers are most­ly hori­zon­tal and tec­to­ni­cal­ly undis­tur­bed, but the­re are some smal­ler faults. A thrust cuts the rocks just east of Grum­ant­by­en and is nice­ly visi­ble from the Isfjord. This fault cau­sed dif­fi­cul­ties for the Rus­si­an mine in Grum­ant­by­en, which was one of the rea­sons for clo­sing the mine in 1962.

Recom­men­ded book for fur­ther, well-digesta­ble (real­ly!) info about geo­lo­gy and land­s­cape of Sval­bard.

Land­s­cape

View from Grønfjordfjellet

View from Grønfjor­dfjel­let south of Bar­ents­burg over inner Grønfjord.

The cha­rac­te­ris­tic land­s­cape in most parts of Nor­dens­kiöld Land east of Grønfjord inclu­des pla­teau-shaped moun­tains with wide pla­teaus in an ele­va­ti­on bet­ween 400 and 600 metres. Few moun­tains tower abo­ve this pla­teau and reach a good 1000 metres abo­ve sea level; other­wi­se, the rocks once covering the who­le pla­teau have been ero­ded. The area is most­ly ungla­cia­ted and has some lar­ge ice-free val­leys such as Cole­s­da­len and Grøn­da­len. The val­ley bot­toms are most­ly occup­pied by brai­ded rivers, the lar­ger bran­ches of which can be dif­fi­cult to cross. This also app­lies to some of the lagoon out­lets and meltwa­ter rivers in inner Grønfjord.

Crossing meltwater river near Grønfjordbreane

Cros­sing a meltwa­ter river near Grønfjor­dbrea­ne in inner Grønfjord.

The net-like rivers of the­se rivers form aeste­tic pat­terns, which are espe­cial­ly nice when seen from an ele­va­ted posi­ti­on. Ano­t­her spe­cial­ty of the lar­ge, ice-free val­leys are pin­gos: per­ma­frost phe­no­me­na con­sis­ting of lar­ge, ice-fil­led cones, up to 30-40 metres high. The­re are several pin­gos in Grøn­da­len.

Grøndalen

View over lower­most Grøn­da­len.

Flo­ra and fau­na

The tun­dra near the coast is amongst the richest tun­dra are­as of Spits­ber­gen, espe­cial­ly in Cole­s­da­len, but some are­as around Grønfjord are also com­pa­ra­tively lush and green. Rein­de­er are accord­in­gly abundant.

Reindeer antler, tundra

Rein­de­er ant­ler on the tun­dra at San­defj­ord­ne­set.

Salt marsh tundra Tundra

Salt mar­sh tun­dra near the coast in inner Grønfjord in evening light, late August.

A fau­nistic spe­cial­ty in Sval­bard, which is other­wi­se free of rodents, are mice which live in the sett­le­ments. Sur­pri­sin­gly, they have sur­vi­ved until today in Grum­ant­by­en, alt­hough the sett­le­ment was aban­do­ned in 1962. They do spread bey­ond the for­mer sett­le­ment area and the­re are records of them as far away as Advent­da­len, but during the win­ter, they seem to be restric­ted to Grum­ant­by­en, at least so far. They may spread para­si­tes (tape­worm), so it is stron­gly recom­men­ded to boil drin­king water tho­rough­ly in this area.

Walrus on drift ice floe

Wal­rus on drift ice floe: both are rare visi­tors in Grønfjord.

Bar­ents­burg has its own influ­ence on the vege­ta­ti­on and wild­life, for examp­le due to the intro­duc­tion of new plant spe­ci­es. The Sys­sel­man­nen is try­ing to con­trol or, whe­re pos­si­ble, era­di­ca­te them.

Cat, Barentsburg

Cat in Bar­ents­burg: not real­ly part of Spitsbergen’s natu­ral envi­ron­ment.

Histo­ry

Isfjord was one of the first parts of Spits­ber­gen to be dis­co­ve­r­ed and used exten­si­ve­ly. The name Hol­len­darda­len tells alrea­dy that Dut­ch 17th cen­tu­ry wha­lers fre­quen­ted the area, which was later also used by both Pomors and Nor­we­gi­an trap­pers. The­re are, howe­ver, not many visi­ble remains from the­se ear­ly peri­ods, which is in part due to the more recent infra­st­ruc­tu­re.

At Fin­nes­et south of Bar­ents­burg, the­re was a wha­ling sta­ti­on in the ear­ly 20th cen­tu­ry, and a radio sta­ti­on for com­mu­ni­ca­ti­on with the main­land. The radio sta­ti­on was in 1933 moved to Kapp Lin­né becau­se of the topo­gra­phy which was more sui­ta­ble for radio com­mu­ni­ca­ti­on.

As is evi­dent from the name, Bar­ents­burg was ori­gi­nal­ly foun­ded by a Dut­ch mining com­pa­ny (Neder­land­sche Spits­ber­gen Com­pa­gnie = NeSpi­Co), but after a few years it was sold to the Rus­si­ans. It is the only acti­ve Rus­si­an mining sett­le­ment in Spits­ber­gen, with a gro­wing empha­sise on tou­rism in recent years. See the page about Bar­ents­burg for fur­ther infor­ma­ti­on.

Mine entrance, Barentsburg

Old mine ent­ran­ce on the south side of Glad­da­len direct­ly abo­ve Bar­ents­burg.
The first mine in the area, from the Dut­ch years, must have been in this area.

Grum­ant­by­en was ano­t­her coal mining sett­le­ment, ori­gi­nal­ly Bri­tish-Rus­si­an an later ent­i­re­ly Rus­si­an and at some point the lar­gest sett­le­ment of Spits­ber­gen with a good 1000 inha­bi­tants, which is hard to belie­ve when you see the few houses which are left at the steep coast. The mine and con­se­quent­ly also the sett­le­ment were aban­do­ned in 1962. Becau­se of the lack of sui­ta­ble ancho­ring posi­ti­ons and har­bour faci­li­ties at Grum­ant­by­en, the coal was ship­ped from Cole­s­buk­ta. The old sett­le­ment the­re was the har­bour for Grum­ant­by­en.

The­re is a page about Cole­s­buk­ta with more infor­ma­ti­on about that place.

Gal­le­ry Grønfjord

Some impres­si­ons from the area around Grønfjord. Dif­fe­rent kinds of trips, dif­fe­rent sea­sons.

Click on thumb­nail to open an enlar­ged ver­si­on of the spe­ci­fic pho­to.

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last modification: 2020-10-26 · copyright: Rolf Stange
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