Knowledge (XXG)

Middelzee

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141:). After 5500 years ago, sea level rise slowed down to a rate of 0.15 meters per century. This allowed sedimentation to catch up and fill in the estuary. Tidal inlets further to the west were blocked by sediment by 3300 years ago. However the Boorne remained open and gradually eroded further and further south and then branched west south of what is now Westergo. People started living adjacent to the channels about 600 BC. The tidal channel moved to the east to what would become the Middelzee. Before the year 900, the new tidal channel scoured deeper and deeper and flooding extended even further inland. After 900 the flooding reached its maximum extent, and it became known as the Middelzee. The southwestern extremity joined up with the 17: 149: 164:
At the beginning of the 10th century people became more organised and worked to prevent the further encroachment of the Middelzee. Levees and natural marsh bars were raised along the shore north of Steins on the western coast of Oostergo. This also happened on the north west facing coast of Westergo
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time period, and the mouth of the river was forced more and more easterly, until it was heading in a north-northwest direction from Akkrum. In the Holocene, the sea rose flooding the valley to form an estuary. Before 7000 years ago, the sea was rising at a rate of 0.75 meters per century, and the
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The southwestern arm of the Middelzee was progressively sectioned off by building dykes across the arm, in four stages. Around 1200 AD a dyke near Rauwerd finished the closure of the arm. This turned what was a mud flat into a salt marsh, and silt gradually collected to fill the areas in.
206:. It can still be recognized as new land since there are only a small number of villages lying in the area of the former Middelzee. The fertile sea clay bottom is mostly used as meadow land but also 229:
By the fifteenth century the Middelzee was reduced to a funnel shape along Frisia's north coast and further silting of the remaining part rendered it unusable. From the early sixteenth century the
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in Friesland, Drenthe, and Groningen. It flowed from Saalien glacial till plateau in a southwest direction, and met the sea west of Het Bildt. The Boorne passed the current location of
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Leeuwarden and the trading terp villages along the coast of Middelzee lost their ability to trade with watercraft when they became isolated from the route to the Wadden Zee.
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van der Spek, A. J. F. (11 August 1995). "Reconstruction of Tidal Inlet and Channel Dimensions in the Frisian Middelzee, a Former Tidal Basin in the Dutch Wadden Sea".
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along the Reid. During the 10th century a dyke was established along the east coast of Westergo along the coast of the Middelzee. The mother
188:. The 12th century also saw land reclamation along the north west shore of Oostergo, shrinking the funnel shaped part of the Middelzee. 133:
rising sea was faster than the sedimentation There are still estuary sediments west of Jorwerd, that were deposited during 6400-5300
367: 418: 202:, literally meaning "new land", and also there are several villages where the lands formerly of the Middelzee are still called 240:
The name Middelzee is still used as a name for an administrative coalition between the so-called Middelzee municipalities of
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is situated on the new lands. The border between Eastergoa and Westergoa in the former Middelzee is now drained by the River
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was formed in that funnel, and is now a Frisian municipality that fills the mouth of what once was the Middelzee.
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was dyked off in the first half of the 13th century, and by 1300 it was reclaimed up to
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This text is based on an article on the West Frisian Knowledge (XXG):
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were established as regions of land completely encircled by dykes.
147: 65: 15: 84:(Oostergo). Other historical names for the Middelzee include 152:
Map of the former Middelzee in West Frisian showing dates of
351:Tidal Signatures in Modern and Ancient Sediments 194:Gradually the Middelzee silted up, forming the 176:The northern section of the Middelzee, passing 384:"Cultural Entities (The Netherlands) Westergo" 222:, but which once reached the southern edge of 8: 270: 268: 100:. The names like Bordine, mean "border". 343: 341: 339: 337: 335: 264: 198:("new lands"). One village is called 313:. CultGIS. 3 May 2015. Archived from 308:"Aandachtsgebied 87: Middelzee-Marne" 276:"Aandachtsgebied 87: Middelzee-Marne" 7: 128:became blocked by sand dunes in the 72:and marked the border between main 20:An 1834 map of the former Middelzee 112:the Boorne was a river that had a 14: 64:. It ran from as far south as 1: 218:), that runs from Sneek to 435: 360:10.1002/9781444304138.ch16 281:. CultGIS. Archived from 124:. The connection to the 419:Geography of Friesland 156: 37: 21: 151: 19: 354:. pp. 239–258. 320:on 15 February 2017 288:on 15 February 2017 208:Leeuwarden Air Base 48:mouth of the River 157: 32:for "middle sea"; 22: 68:northward to the 426: 395: 394: 392: 390: 380: 374: 373: 345: 330: 329: 327: 325: 319: 312: 304: 298: 297: 295: 293: 287: 280: 272: 154:land reclamation 434: 433: 429: 428: 427: 425: 424: 423: 409: 408: 398: 388: 386: 382: 381: 377: 370: 347: 346: 333: 323: 321: 317: 310: 306: 305: 301: 291: 289: 285: 278: 274: 273: 266: 262: 250:Leeuwarderadeel 214:(West Frisian: 162: 145:near Bolsward. 106: 80:(Westergo) and 52:(West Frisian: 40:), also called 12: 11: 5: 432: 430: 422: 421: 411: 410: 407: 406: 397: 396: 375: 368: 331: 299: 263: 261: 258: 246:Ferwerderadiel 161: 158: 135:before present 114:drainage basin 105: 102: 13: 10: 9: 6: 4: 3: 2: 431: 420: 417: 416: 414: 404: 400: 399: 385: 379: 376: 371: 369:9781444304138 365: 361: 357: 353: 352: 344: 342: 340: 338: 336: 332: 316: 309: 303: 300: 284: 277: 271: 269: 265: 259: 257: 255: 251: 247: 243: 238: 236: 232: 227: 225: 221: 217: 213: 209: 205: 201: 197: 192: 189: 187: 183: 179: 174: 170: 168: 159: 155: 150: 146: 144: 143:Marne Estuary 140: 136: 131: 127: 123: 119: 115: 111: 103: 101: 99: 95: 91: 87: 83: 79: 75: 71: 67: 63: 59: 56:) now in the 55: 51: 47: 43: 39: 35: 31: 27: 18: 403:fy:Middelsee 387:. Retrieved 378: 350: 322:. Retrieved 315:the original 302: 290:. Retrieved 283:the original 254:Menameradiel 239: 228: 215: 203: 195: 193: 190: 175: 171: 163: 139:Mid-Atlantic 108:Back in the 107: 97: 93: 89: 85: 60:province of 53: 41: 34:West Frisian 25: 23: 292:15 February 196:nije lannen 160:Reclamation 130:Weichselian 110:Pleistocene 104:Pre-history 76:regions of 260:References 220:Leeuwarden 178:Leeuwarden 126:Wadden Sea 70:Wadden Sea 44:, was the 242:Het Bildt 235:Het Bildt 224:Het Bildt 204:it Nijlân 82:Eastergoa 78:Westergoa 62:Friesland 38:Middelsee 26:Middelzee 413:Category 389:23 March 324:24 March 94:Boerdiep 90:Borndiep 186:Beetgum 167:polders 122:Rauwerd 98:Bordena 74:Frisian 46:estuary 42:Bordine 366:  252:, and 231:polder 216:Swette 212:Zwette 200:Nijlân 182:Stiens 118:Akkrum 96:, and 86:Bordaa 50:Boorne 318:(PDF) 311:(PDF) 286:(PDF) 279:(PDF) 66:Sneek 58:Dutch 54:Boarn 30:Dutch 391:2018 364:ISBN 326:2018 294:2017 184:and 120:and 24:The 356:doi 233:of 415:: 362:. 334:^ 267:^ 256:. 248:, 244:, 226:. 92:, 88:, 36:: 405:. 393:. 372:. 358:: 328:. 296:. 137:( 28:(

Index


Dutch
West Frisian
estuary
Boorne
Dutch
Friesland
Sneek
Wadden Sea
Frisian
Westergoa
Eastergoa
Pleistocene
drainage basin
Akkrum
Rauwerd
Wadden Sea
Weichselian
before present
Mid-Atlantic
Marne Estuary

land reclamation
polders
Leeuwarden
Stiens
Beetgum
Nijlân
Leeuwarden Air Base
Zwette

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