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White Chuck Mountain

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danger. During winter months, weather is usually cloudy, but due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade
382:), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of 407:. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. These climate differences lead to vegetation variety defining the 457:
period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross section of the river valleys is a result of recent glaciation.
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Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C). The months July through September offer the most favorable weather for viewing or climbing this peak.
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in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the North Cascades area.
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that is 15.5 mi (24.9 km) east-southeast of White Chuck, began forming in the mid-Pleistocene. In addition, small fragments of the
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Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
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The history of the formation of the Cascade Mountains dates back millions of years ago to the late
378:. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range ( 375: 367: 339: 534: 288: 463: 383: 379: 247: 447: 404: 351: 307: 233: 692: 431: 423: 400: 371: 331: 240: 327: 281: 267: 487: 454: 574: 683: 524: 355: 335: 69: 109: 96: 408: 387: 291: 306:, is a 6,989 ft (2,130 m) summit near the western edge of the 459: 443: 427: 399:
The North Cascades features some of the most rugged topography in the
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originating in the Pacific Ocean travel northeast toward the
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University of Washington Press. 639:Dictionary of the Chinook Jargon 543:Geology of the Pacific Northwest 527: 514:White Chuck seen from Mount Pugh 507: 495: 477: 177: 170: 144: 137: 27: 709:Mountains of Washington (state) 548:Geography of the North Cascades 676:White Chuck Mountain weather: 161:Show map of Washington (state) 1: 719:North American 2000 m summits 194:Show map of the United States 191:Location in the United States 450:about 50 million years ago. 346:on land administered by the 330:which is one of the Cascade 59:3,789 ft (1,155 m) 49:6,989 ft (2,130 m) 658:Kruckeberg, Arthur (1991). 430:persisted. Glacier Peak, a 276:, Thomas Gerdine, Sam Strom 82:4.92 mi (7.92 km) 735: 484:White Chuck from Mt. Pugh 428:volcanic igneous activity 130: 26: 334:. It is situated at the 440:continental lithosphere 110:48.208495°N 121.41696°W 682:Climbing White Chuck: 320:Darrington, Washington 158:Location in Washington 324:Mountain Loop Highway 274:Albert Hale Sylvester 115:48.208495; -121.41696 637:George Gibbs, 1863, 420:North American Plate 300:White Chuck Mountain 256:White Chuck Mountain 185:White Chuck Mountain 152:White Chuck Mountain 22:White Chuck Mountain 326:, and northwest of 106: /  384:maritime influence 39:Highest point 678:Mountain Forecast 376:Cascade Mountains 368:marine west coast 340:White Chuck River 302:, or native name 297: 296: 726: 664: 663: 655: 642: 641:, Cramoisy Press 635: 629: 626: 607: 606: 604: 603: 589: 583: 582: 571: 537: 535:Mountains portal 532: 531: 530: 511: 499: 481: 418:Epoch. With the 312:Snohomish County 284: 236: 195: 181: 180: 174: 162: 148: 147: 141: 121: 120: 118: 117: 116: 111: 107: 104: 103: 102: 99: 31: 19: 734: 733: 729: 728: 727: 725: 724: 723: 689: 688: 673: 668: 667: 657: 656: 645: 636: 632: 627: 610: 601: 599: 597:listsofjohn.com 591: 590: 586: 573: 572: 561: 556: 533: 528: 526: 523: 518: 515: 512: 503: 500: 491: 485: 482: 472: 422:overriding the 405:glacial valleys 397: 380:orographic lift 364: 332:stratovolcanoes 282: 234: 200: 199: 198: 197: 196: 193: 192: 189: 188: 187: 186: 182: 165: 164: 163: 160: 159: 156: 155: 154: 153: 149: 114: 112: 108: 105: 100: 97: 95: 93: 92: 34: 17: 12: 11: 5: 732: 730: 722: 721: 716: 711: 706: 701: 699:North Cascades 691: 690: 687: 686: 680: 672: 671:External links 669: 666: 665: 643: 630: 608: 584: 579:Peakbagger.com 558: 557: 555: 552: 551: 550: 545: 539: 538: 522: 519: 517: 516: 513: 506: 504: 501: 494: 492: 483: 476: 473: 471: 468: 448:North Cascades 426:, episodes of 411:in this area. 396: 393: 372:weather fronts 363: 360: 352:Chinook Jargon 322:, east of the 308:North Cascades 295: 294: 286: 278: 277: 272:July 28, 1897 270: 264: 263: 259: 258: 250: 244: 243: 238: 230: 229: 224: 220: 219: 214: 210: 209: 206: 202: 201: 190: 184: 183: 176: 175: 169: 168: 167: 166: 157: 151: 150: 143: 142: 136: 135: 134: 133: 132: 131: 128: 127: 123: 122: 90: 84: 83: 80: 74: 73: 67: 61: 60: 57: 51: 50: 47: 41: 40: 36: 35: 32: 24: 23: 15: 13: 10: 9: 6: 4: 3: 2: 731: 720: 717: 715: 712: 710: 707: 705: 704:Cascade Range 702: 700: 697: 696: 694: 685: 681: 679: 675: 674: 670: 661: 654: 652: 650: 648: 644: 640: 634: 631: 625: 623: 621: 619: 617: 615: 613: 609: 598: 594: 588: 585: 580: 576: 570: 568: 566: 564: 560: 553: 549: 546: 544: 541: 540: 536: 525: 520: 510: 505: 498: 493: 489: 480: 475: 469: 467: 465: 461: 456: 451: 449: 445: 441: 437: 433: 432:stratovolcano 429: 425: 424:Pacific Plate 421: 417: 412: 410: 406: 402: 401:Cascade Range 394: 392: 389: 385: 381: 377: 373: 369: 361: 359: 357: 353: 349: 345: 341: 337: 333: 329: 325: 321: 317: 313: 309: 305: 301: 293: 290: 287: 285: 283:Easiest route 279: 275: 271: 269: 265: 260: 257: 254: 251: 249: 245: 242: 241:Cascade Range 239: 237: 231: 228: 225: 221: 218: 215: 211: 208:United States 207: 203: 173: 140: 129: 124: 119: 91: 89: 85: 81: 79: 75: 71: 68: 66: 62: 58: 56: 52: 48: 46: 42: 37: 30: 25: 20: 659: 638: 633: 600:. Retrieved 596: 587: 578: 452: 446:created the 413: 398: 365: 328:Glacier Peak 303: 299: 298: 268:First ascent 255: 235:Parent range 488:Mount Baker 455:Pleistocene 453:During the 113: / 101:121°25′01″W 88:Coordinates 65:Parent peak 693:Categories 602:2024-04-07 554:References 409:ecoregions 356:Mount Pugh 344:Sauk River 336:confluence 316:Washington 217:Washington 98:48°12′31″N 72:(7,201 ft) 70:Mount Pugh 55:Prominence 388:avalanche 227:Snohomish 126:Geography 78:Isolation 45:Elevation 521:See also 490:to left) 464:faulting 444:terranes 342:and the 304:Hi Khaed 292:climbing 262:Climbing 248:Topo map 684:YouTube 470:Gallery 442:called 436:oceanic 395:Geology 362:Climate 338:of the 289:class 5 205:Country 460:Uplift 416:Eocene 223:County 310:, in 213:State 462:and 438:and 253:USGS 314:of 695:: 646:^ 611:^ 595:. 577:. 562:^ 605:. 581:. 486:(

Index


Elevation
Prominence
Parent peak
Mount Pugh
Isolation
Coordinates
48°12′31″N 121°25′01″W / 48.208495°N 121.41696°W / 48.208495; -121.41696
White Chuck Mountain is located in Washington (state)
White Chuck Mountain is located in the United States
Washington
Snohomish
Parent range
Cascade Range
Topo map
USGS
First ascent
Albert Hale Sylvester
Easiest route
class 5
climbing
North Cascades
Snohomish County
Washington
Darrington, Washington
Mountain Loop Highway
Glacier Peak
stratovolcanoes
confluence
White Chuck River

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