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Surco Intrabético

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33: 105: 234:, as the Baetic ranges were being formed. It is believed that at that time the entire Baetic system was surrounded by water, and the basin formed a single, continuous valley, sometimes referred to as the Baetic Depression. Later, the spurs crossing the basin were raised up, turning it into a series of separate valleys. 241:. The Depression of Ronda, the westernmost of the valleys, falls fully within the Cordillera Penibética. The Hoya of Antequera is intimately related to the original Baetic Depression: it was a great 249:
from the Andalusian ranges. The Depression of Granada is intermediate between the Penibético and Subbético. Finally the Hoyas of Guadix, Baza and Huéscar are more related to the Subbético.
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The valleys of the Intrabaetic Basin stand in contrast to the adjacent mountain ridges that define their collective border and the rocky spurs—formed of
211:, and yielding a dry, nearly treeless landscape—that separate them from one another in that they are formed of soft materials such as 346: 84: 319: 399: 333: 45: 55: 49: 41: 223:. Soils are deep and suitable for agriculture, but the limiting factor to human activity is the scarcity of water. 404: 66: 394: 220: 185: 197: 201: 177: 314: 153: 342: 238: 181: 165: 157: 98: 289: 277: 161: 117: 176:, the eastern Mediterranean coastal region of Spain. From west to east, the basins of the 168:. Together, these valleys constitute a route from western Andalusia and the valley of the 253: 293: 189: 173: 104: 388: 309: 285: 246: 133: 193: 169: 17: 237:
The valleys of the Intrabaetic Basin are quite heterogeneous, although all are
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to the north. These basins run more or less parallel to the
108:The valleys that constitute the Intrabaetic Basin. 54:but its sources remain unclear because it lacks 252:The Intrabaetic Basin provides a route for the 97:For the lower valley of the Guadalquivir, see 8: 85:Learn how and when to remove this message 334:Geografía túristica: general y de España 226:The Intrabaetic Basin formed at the end 337:, Ed. Centro de Estudios Ramón Areces, 152:The Intrabaetic Basin is a series of 7: 25: 320:Geology of the Iberian Peninsula 31: 128:) is a discontinuous series of 296:, which, in turn continues to 245:of the sea that separated the 1: 421: 96: 300:and the Spanish Levante. 40:This article includes a 69:more precise citations. 400:Landforms of Andalusia 160:to its south from the 121: 109: 230:and beginning of the 186:Depression of Granada 126:Depresión Intrabética 107: 367: /  178:Depression of Ronda 166:Mediterranean coast 154:intermontane basins 315:Geography of Spain 264:, passing through 239:sedimentary basins 156:that separate the 110: 42:list of references 292:, where it meets 182:Hoya of Antequera 158:Penibaetic System 122:Surco Intrabético 114:Intrabaetic Basin 99:Baetic Depression 95: 94: 87: 18:Intrabaetic Basin 16:(Redirected from 412: 405:Valleys of Spain 382: 381: 379: 378: 377: 372: 371:37.300°N 3.183°W 368: 365: 364: 363: 360: 290:Puerto Lumbreras 162:Subbaetic System 90: 83: 79: 76: 70: 65:this article by 56:inline citations 35: 34: 27: 21: 420: 419: 415: 414: 413: 411: 410: 409: 385: 384: 375: 373: 369: 366: 361: 358: 356: 354: 353: 331:Julián Alonso: 328: 306: 280:passes through 198:Hoya of Huéscar 172:to the Spanish 150: 102: 91: 80: 74: 71: 60: 46:related reading 36: 32: 23: 22: 15: 12: 11: 5: 418: 416: 408: 407: 402: 397: 387: 386: 376:37.300; -3.183 351: 350: 327: 324: 323: 322: 317: 312: 305: 302: 256:that connects 190:Hoya of Guadix 149: 146: 93: 92: 50:external links 39: 37: 30: 24: 14: 13: 10: 9: 6: 4: 3: 2: 417: 406: 403: 401: 398: 396: 395:Baetic System 393: 392: 390: 383: 380: 348: 347:84-8004-637-6 344: 340: 336: 335: 330: 329: 325: 321: 318: 316: 313: 311: 310:Baetic System 308: 307: 303: 301: 299: 295: 291: 287: 283: 279: 278:Autovía A-92N 276:. Its branch 275: 271: 267: 263: 259: 255: 250: 248: 247:Sierra Morena 244: 240: 235: 233: 229: 224: 222: 221:conglomerates 218: 214: 210: 205: 203: 202:Hoya of Lorca 199: 195: 191: 187: 183: 179: 175: 171: 167: 163: 159: 155: 147: 145: 143: 139: 135: 134:Baetic System 131: 127: 123: 119: 115: 106: 100: 89: 86: 78: 68: 64: 58: 57: 51: 47: 43: 38: 29: 28: 19: 352: 332: 254:Autovía A-92 251: 236: 225: 206: 194:Hoya of Baza 170:Guadalquivir 151: 125: 113: 111: 81: 72: 61:Please help 53: 374: / 294:Autovía A-7 148:Description 67:introducing 389:Categories 326:References 200:, and the 266:Antequera 228:Oligocene 209:limestone 138:Andalusia 304:See also 75:May 2014 359:37°18′N 270:Granada 262:Almería 258:Seville 232:Miocene 174:Levante 132:in the 130:valleys 118:Spanish 63:improve 362:3°11′W 345:  341:2006. 339:Madrid 298:Murcia 282:Cúllar 274:Guadix 272:, and 196:, the 192:, the 188:, the 184:, the 180:, the 217:silts 213:clays 142:Spain 48:, or 343:ISBN 286:Baza 284:and 243:gulf 219:and 112:The 288:to 260:to 136:of 124:or 391:: 268:, 215:, 204:. 144:. 140:, 120:: 52:, 44:, 349:. 116:( 101:. 88:) 82:( 77:) 73:( 59:. 20:)

Index

Intrabaetic Basin
list of references
related reading
external links
inline citations
improve
introducing
Learn how and when to remove this message
Baetic Depression

Spanish
valleys
Baetic System
Andalusia
Spain
intermontane basins
Penibaetic System
Subbaetic System
Mediterranean coast
Guadalquivir
Levante
Depression of Ronda
Hoya of Antequera
Depression of Granada
Hoya of Guadix
Hoya of Baza
Hoya of Huéscar
Hoya of Lorca
limestone
clays

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