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Biu Plateau

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cones caused by explosions when water penetrated downward and came into contact with fresh lava. There are a number of well-preserved volcanic cones rising above the Plateau along a NNW-SSE axis in the Miringa volcanic zone.
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with thin flows of lava issuing from small cinder cones and filling the valleys. Most of the basalts date between 7 and 2 million years ago, but some are less than a million years old. The plateau includes many small
219:"The Role of Continental Crust and Lithospheric Mantle in the Genesis of Cameroon Volcanic Line Lavas: Constraints from Isotopic Variations in Lavas and Megacrysts from the Biu and Jos Plateaux" 36:. It covers about 5,200 km (2,000 sq mi) and has an average elevation of 700 m (2,300 ft). The plateau lies between the Upper Benue Basin to the south and the 201: 328: 70:
that have erupted from small vents or fissures, and then spread in a thin layer over wide areas. Activity resumed in the
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Some geologists consider that the volcanic activity in the Biu Plateau is associated with the activity in the
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to the north. High points are Wade Hill at 775 m (2,543 ft) above sea level and
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There is evidence of early volcanic activity in the area during the
15: 217:K. RANKENBURG, J. C. LASSITER and G. BREY (2004). 8: 118: 116: 20:Major geological features near Cameroon line 176:. Taylor & Francis. 1971. p. 285. 234: 193:Geology and Mineral Resources of Nigeria 112: 145: 143: 7: 28:is a highland area in Northeastern 14: 32:containing many recently extinct 63:, and the bulk of the rocks are 173:West Africa, Volume 25, Part 1 1: 190:, Nuhu George Obaje (2009). 52:plains and the Chad Basin. 345: 151:"Borno: Physical Setting" 259:Global Volcanism Program 236:10.1093/petrology/egh067 196:. Springer. p. 50. 264:Smithsonian Institution 128:Encyclopædia Britannica 21: 295:10.67833°N 12.00528°E 19: 329:Volcanoes of Nigeria 223:Journal of Petrology 291: /  319:Geology of Nigeria 300:10.67833; 12.00528 22: 203:978-3-540-92684-9 188:Obaje Nuhu George 336: 306: 305: 303: 302: 301: 296: 292: 289: 288: 287: 284: 273: 271: 270: 241: 240: 238: 214: 208: 207: 184: 178: 177: 168: 162: 161: 159: 158: 153:. Online Nigeria 147: 138: 137: 135: 134: 120: 344: 343: 339: 338: 337: 335: 334: 333: 309: 308: 299: 297: 293: 290: 285: 282: 280: 278: 277: 268: 266: 252: 249: 244: 216: 215: 211: 204: 186: 185: 181: 170: 169: 165: 156: 154: 149: 148: 141: 132: 130: 122: 121: 114: 110: 93: 12: 11: 5: 342: 340: 332: 331: 326: 321: 311: 310: 275: 274: 248: 247:External links 245: 243: 242: 229:(1): 169–190. 209: 202: 179: 163: 139: 111: 109: 106: 105: 104: 99: 92: 89: 87:to the south. 13: 10: 9: 6: 4: 3: 2: 341: 330: 327: 325: 324:Lava plateaus 322: 320: 317: 316: 314: 307: 304: 265: 261: 260: 255: 254:"Biu Plateau" 251: 250: 246: 237: 232: 228: 224: 220: 213: 210: 205: 199: 195: 194: 189: 183: 180: 175: 174: 167: 164: 152: 146: 144: 140: 129: 125: 124:"Biu Plateau" 119: 117: 113: 107: 103: 100: 98: 95: 94: 90: 88: 86: 85:Cameroon line 81: 78: 73: 69: 66: 62: 58: 53: 51: 47: 46:Gongola River 43: 39: 35: 31: 27: 18: 276: 267:. Retrieved 257: 226: 222: 212: 192: 182: 172: 166: 155:. Retrieved 131:. Retrieved 127: 97:Biu, Nigeria 82: 54: 25: 23: 298: / 102:Biu Emirate 77:pyroclastic 26:Biu Plateau 313:Categories 283:10°40′42″N 269:2021-06-24 157:2011-02-02 133:2011-02-02 108:References 72:Quaternary 57:Cretaceous 38:Chad Basin 286:12°0′19″E 42:Wiga Hill 34:volcanoes 91:See also 65:Pliocene 68:basalts 61:Miocene 30:Nigeria 200:  50:Bauchi 198:ISBN 24:The 231:doi 315:: 262:. 256:. 227:46 225:. 221:. 142:^ 126:. 115:^ 272:. 239:. 233:: 206:. 160:. 136:.

Index


Nigeria
volcanoes
Chad Basin
Wiga Hill
Gongola River
Bauchi
Cretaceous
Miocene
Pliocene
basalts
Quaternary
pyroclastic
Cameroon line
Biu, Nigeria
Biu Emirate


"Biu Plateau"


"Borno: Physical Setting"
West Africa, Volume 25, Part 1
Obaje Nuhu George
Geology and Mineral Resources of Nigeria
ISBN
978-3-540-92684-9
"The Role of Continental Crust and Lithospheric Mantle in the Genesis of Cameroon Volcanic Line Lavas: Constraints from Isotopic Variations in Lavas and Megacrysts from the Biu and Jos Plateaux"
doi
10.1093/petrology/egh067

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