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The main building was destroyed in a fire in 1913, and today only the foundations remain. Next to
Ljansbrukveien the two old porter's lodges today contain handicraft stores run by local craftspeople, and the gazebo at Hvervenbukta beach harbors a cafe which is open during the summer.
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debris. As the weight of the glacier lifted the land heaved. In fact, the land around the inner
Oslofjord rose 200–220 meters. But before that had taken place, a fjord went up at Ljan to Hauketo, with a narrow inlet into the Lusetjern Valley at
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soil heaped up at the Ljan fields (today
Hundejordet and Hallagerjordet) because the mountain blocked the further movement, creating deep dents in the terrain where the soil accumulated. Here arable land remained up to the 45 meter
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Overall, the soil cover in the Ljan area is thin as almost all soils were washed away from the steep hills and hillsides. In many places naked rock protrudes. In valley hollows though, such as at
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at least five times. Each time, when the ice melted, water seared into the thin fissures—weakness zones—that had originated in the three previous geological periods. At Ljan and neighboring
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The bedrock surface cracked up further still, also outside the main fault lines, exacerbated by erosion by water and ice. Looser accretions that had settled on top of the bedrock during the
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interspersed in layers. Due to the erosion that took place for hundreds of millions of years, today's rock surface was deep inside the mountains that were originally formed. During the
317:, at Skredderjordet and Åsdalsveien, nutrient-rich soil with clay minerals appear. The clay soil can be quite stiff and heavy, but it is also mixed with a considerable amount of
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flat rock layers go horizontally, and this gave rise to the steep slope of the
Ljanselva valley, Liadalen, as ice and water sheared straight down into the packed rock layers.
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Periods eroded off during the following 200 million years, causing much of the bedrock to resurface. The final "molding" of the landscape of Ljan took place during the
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88:. The borders to the north and east are less obvious and drawn between the school circuits Ljan and Nordstrand. The name originates with an
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to arise across the Oslo region. As
Bundefjorden sank, the Oslo valley sank along a northern fault line along the steep
457:
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then took over. Maren Juel and
Rosenkrantz sold off the estate to Juel's niece, Gjertrud Maren Juel and her husband,
128:) and Stubljan, however, the two former were purchased by the owners of Stubljan and with the addition of the farm
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243:, the other along Ljanselva. The Ljanselva crack can be followed further inland with one branch going to
310:. Here, at Store Ljan, the first Ljan farm was cleared, followed by another, Stubljan, at Hvervenbukta.
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bought the farm in 1765 and had built the large main building at
Hvervenbukta. Holter's widow, Madam
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Originally Ljan was an old farm first written about in 1308. After 1650 it was partitioned in three,
211:(around 250 million years ago) comprehensive volcanism marked the entire Oslo Graben and caused
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289:, about 10,000 years ago, the Ljan fissure and other dents in the terrain were filled with
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is known as one of the very few churches in Norway that was built in the 1930s in the
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slope which remained elevated. The main western fault line follows
Bundefjorden from
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212:
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502:
484:
471:
448:
Henriksen, Lise (1990). "Gård og grunn". In
Johannessen, Finn Erhard (ed.).
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385:
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Stubljan received its name from its first owner, Christopher
Nilsson Stub.
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235:. Two branches of this fault line also emerged as crack zones: one along
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44:, Norway. It is located in the eastern rolling hillsides of the fjord
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Period—the recent 1½ million years—when the land was frozen under
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64:. The number of inhabitants was about 3,500 in 2004.
415:(in Norwegian) (4 ed.). Oslo: Kunnskapsforlaget.
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at Ljan it also constitutes the border with borough
199:, i.e. 1 billion years old: mostly nutrient-poor
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301:As rivers moved the sediment back into the sea,
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36:) is a residential neighborhood in the borough
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398:(in Norwegian) (2 ed.). Oslo: Aschehoug.
450:Fint folk i bratte bakker – Ljans historie
452:(in Norwegian). Selskapet til Ljans Vel.
187:Ljan is located immediately south of the
56:has its mouth, and where it runs through
366:(in Norwegian). Oslo: Norsk nettleksikon
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100:but the meaning has been lost to time.
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409:Tvedt, Knut Are, ed. (2000) . "Ljan".
72:style. The public beaches at Ljan are
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144:, they constituted the Ljan Estate (
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191:with the ground being predominantly
20:Old copperplate engraving from Ljan.
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163:and her second and third husbands,
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358:"Ljan – boligområde i Oslo"
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1:
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434:Henriksen 1990, pp. 13–15
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392:, eds. (1966) . "Ljan".
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203:with more nutrient-rich
29:Norwegian pronunciation:
169:Marcus Gjøe Rosenkrantz
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509:Neighbourhoods of Oslo
227:, past Nordstrand and
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165:Ole Christopher Wessel
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363:Store norske leksikon
19:
331:Jens Christian Hauge
481: /
287:last glacial period
195:dating back to the
167:and First Minister
285:At the end of the
104:The old Ljan farms
70:Romanesque Revival
22:
485:59.833°N 10.783°E
354:Godal, Anne Marit
62:Søndre Nordstrand
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412:Oslo byleksikon
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395:Oslo byleksikon
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48:. To the south
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490:59.833; 10.783
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325:Notable people
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223:Sjømannsskolen
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33:[jɑːn]
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368:. Retrieved
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315:Ljan Station
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308:contour line
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284:
257:
229:Ingierstrand
186:
177:
157:Peder Holter
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107:
93:
74:Hvervenbukta
46:Bunnefjorden
24:
23:
488: /
321:particles.
241:Gjersjøelva
205:amphibolite
197:Precambrian
189:Oslo Graben
173:Lars Ingier
150:Ljansgodset
92:river name
66:Ljan Church
442:References
390:Just, Carl
370:1 February
272:Quaternary
264:Ordovician
245:Klemetsrud
231:and on to
161:Maren Juel
138:White Bear
136:(English:
132:Hvitebjørn
126:Lower Ljan
124:(English:
121:Nedre Ljan
116:Upper Ljan
114:(English:
86:Mosseveien
78:Ljansbadet
38:Nordstrand
249:Nøklevann
237:Gjersjøen
146:Norwegian
111:Øvre Ljan
90:Old Norse
50:Ljanselva
503:Category
276:glaciers
268:Silurian
260:Cambrium
142:Oppegård
58:Liadalen
476:10°47′E
473:59°50′N
356:(ed.).
296:Holmlia
291:moraine
280:Hauketo
253:Lutvann
217:Ekeberg
209:Permian
193:bedrock
183:Geology
54:Lutvann
456:
213:faults
201:gneiss
82:Katten
337:Notes
140:) in
96:Ljǫrn
454:ISBN
372:2012
319:sand
303:clay
266:and
251:and
239:and
233:Moss
80:and
42:Oslo
25:Ljan
152:).
118:),
40:in
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421:^
388:;
360:.
345:^
298:.
262:,
255:.
175:.
148::
76:,
462:.
374:.
27:(
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