Knowledge (XXG)

Joint valley landscape

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17: 116: 132: 51:
which leaves out small plateaus or ridges in between. When the block summits in joint valley landscape are of different height it may indicate the past movement of a vertical
115: 131: 101:(lit. square plateau land). Joint valley landscapes are among the few places in southern Sweden where there are steep slopes in excess of 25°. 16: 184: 58: 238:. Statens offentliga utreningar (in Swedish). Vol. 39. Stockholm: Jordbruksdepartamentet. 1943. p. 21. 233: 235:
Utredning angående Norrlands näringsliv. Förberendade undersökning verkställd av 1940 års norrlandsutredning
189: 86: 21: 281: 213: 261: 286: 253: 32: 89:. In addition to this there is a large-scale joint valley landscape that extends from the 52: 44: 142: 122: 275: 254: 249: 208: 94: 40: 74: 70: 66: 90: 85:. In the last three areas the flat summits of the landscapes are parts of the 82: 78: 62: 48: 138: 187:(1995). "Relief and saprolites through time on the Baltic Shield". 252:(1997). "Sweden". In Embleton, C.; Embleton-Hamann, C. (eds.). 221:. Swedish Society for Anthropology and Geography: 125–136. 173:(in Swedish). Nordiska ministerrådet. 1984. p. 9. 61:
identified joint valley landscape areas centered on
93:inland. The landscape type was first identified by 137:Model of the joint valley landscape around lake 43:. The landscape originates from the erosion of 211:(1926). "Norra Sveriges landforms-regioner". 8: 165: 163: 20:Joint valley terrain seen in wintertime 15: 159: 111: 121:Large scale joint valley landscape at 37:sprickdalslandskap, sprickdalsterräng 7: 256:Geomorphological Hazards of Europe 14: 130: 114: 39:) is a type of relief common in 1: 31:or fissure valley terrain ( 303: 185:Lidmar-Bergströrm, Karna 171:Terrängformer i Norden 97:who in 1926 called it 87:Sub-Cambrian peneplain 59:Karna Lidmar-Bergström 36: 29:Joint valley landscape 25: 22:Stockholm archipelago 19: 260:. Elsevier. p.  232:"Regionindelning". 214:Geografiska Annaler 197:. Elsevier: 45–61. 26: 294: 266: 265: 259: 246: 240: 239: 229: 223: 222: 205: 199: 198: 181: 175: 174: 167: 134: 118: 53:geological fault 302: 301: 297: 296: 295: 293: 292: 291: 272: 271: 270: 269: 248: 247: 243: 231: 230: 226: 207: 206: 202: 183: 182: 178: 169: 168: 161: 156: 151: 150: 149: 146: 135: 126: 125:, Ångermanland. 119: 107: 12: 11: 5: 300: 298: 290: 289: 284: 274: 273: 268: 267: 241: 224: 217:(in Swedish). 200: 176: 158: 157: 155: 152: 148: 147: 143:naturum Sommen 136: 129: 127: 123:The High Coast 120: 113: 110: 109: 108: 106: 103: 13: 10: 9: 6: 4: 3: 2: 299: 288: 285: 283: 280: 279: 277: 263: 258: 257: 251: 250:Rudberg, Sten 245: 242: 237: 236: 228: 225: 220: 216: 215: 210: 209:De Geer, Sten 204: 201: 196: 192: 191: 190:Geomorphology 186: 180: 177: 172: 166: 164: 160: 153: 144: 140: 133: 128: 124: 117: 112: 104: 102: 100: 96: 92: 88: 84: 80: 76: 72: 68: 64: 60: 56: 54: 50: 46: 42: 38: 34: 30: 23: 18: 255: 244: 234: 227: 218: 212: 203: 194: 188: 179: 170: 99:rutplatåland 98: 95:Sten De Geer 57: 41:Fennoscandia 28: 27: 282:Scandinavia 276:Categories 154:References 91:High Coast 83:Hudiksvall 79:Stockholm 75:Västervik 71:Linköping 67:Bohuslän 63:Blekinge 287:Geology 105:Gallery 49:bedrock 47:in the 33:Swedish 139:Sommen 45:joints 81:and 262:457 141:in 55:. 278:: 195:12 193:. 162:^ 77:, 69:, 65:, 35:: 264:. 219:8 145:. 73:/ 24:.

Index


Stockholm archipelago
Swedish
Fennoscandia
joints
bedrock
geological fault
Karna Lidmar-Bergström
Blekinge
Bohuslän
Linköping
Västervik
Stockholm
Hudiksvall
Sub-Cambrian peneplain
High Coast
Sten De Geer
Large scale joint valley landscape at The High Coast, Ångermanland.
The High Coast
Model of the joint valley landscape around lake Sommen in naturum Sommen.
Sommen
naturum Sommen


Lidmar-Bergströrm, Karna
Geomorphology
De Geer, Sten
Geografiska Annaler
Utredning angående Norrlands näringsliv. Förberendade undersökning verkställd av 1940 års norrlandsutredning
Rudberg, Sten

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