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Piotruś

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The tallest mountain in the Beskid Dukielski, Piotruś is relatively flat-structured, giving it its alternative name of Płazyna. The mountain is crescent-shaped, aligned roughly north-south. It is bounded to the west and south by the valley of the Jasiołka river, separating it from Ostra Mountain to
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Piotruś is the highest mountain of the Beskid Dukielski. A tourist trail passes through the mountain. Its most prominent characteristic is a stream and pond related to the Saint
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the Cergowa Sandstones or Shales with interbedded layers of Tylawa Limestone. Prominent ridges near the top of the mountain consist of thick-bedded layers of sandstone and
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rock is prominently displayed at the top of the mountain, which likely contributed to its name (Piotr – Polish for
269:, who is said to have rested there. There is also a "Papal stone" ("Kamień papieski), commemorating the presence of 254: – also means stone). Some of it was excavated for buildings, and several unused large blocks can be found. 257:
The mountain is the source for numerous streams, which form small ponds the largest of which is known as the
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The Beskid Dukielski Range is located within the outer part of the Carpathians, which is part of the
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age rocks, particularly the Menilite Beds, which contain the Mszanka Sandstones, the Jawornik
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Environmental, Structural and Stratigraphic Evolution of the Western Carpathians
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forest on Piotruś's western slope was mostly destroyed in a fire during the
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A short yellow tourist trail passes through Piotruś. The trail starts at
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the south. The mountain is covered in forest, primarily old
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range, Poland. Beskid Dukielski forms the middle of the
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here. A small chapel was raised in the site in 2005.
450:. Oficyna Wydawnicza "Rewasz". pp. 180–181. 543: 439: 437: 435: 433: 431: 396: 394: 392: 325: 323: 511: 477: 443: 400: 329: 505: 471: 428: 389: 320: 518:. Oficyna Wydawnicza "Rewasz". p. 191. 484:. Oficyna Wydawnicza "Rewasz". p. 192. 407:. Oficyna Wydawnicza "Rewasz". p. 193. 336:. Oficyna Wydawnicza "Rewasz". p. 131. 216: 362: 360: 213:that form part of the Mszanka Sandstones. 357: 14: 544: 367:Ruciński, P.; Cieszkowski M. (2008). 557:Mountains of the Western Carpathians 261:. Another pond (Holy Water, Polish: 201:in age. Piotruś itself is formed of 276:There are plans to extend a nearby 265:) is linked to the legend of Saint 24: 25: 573: 38: 13: 1: 314: 177:, is subdivided into several 226:trees, and near the top, in 7: 10: 578: 164: 57:727 m (2,385 ft) 283: 115: 105: 100: 61: 51: 46: 37: 32: 515:Beskid Niski: przewodnik 512:Wojciech Krukar (2007). 481:Beskid Niski: przewodnik 478:Wojciech Krukar (2007). 447:Beskid Niski: przewodnik 444:Wojciech Krukar (2007). 404:Beskid Niski: przewodnik 401:Wojciech Krukar (2007). 333:Beskid Niski: przewodnik 330:Wojciech Krukar (2007). 217:Physical characteristics 173:. The Outer Carpathians 232:European mountain-ash 85:49.47750°N 21.74972°E 175:fold and thrust belt 171:Alpine orogenic belt 152:Carpathian Mountains 552:Mountains of Poland 81: /  305:Zawadka Rymanowska 294:Cergowa (mountain) 90:49.47750; 21.74972 47:Highest point 27:Mountain in Poland 525:978-83-89188-63-2 491:978-83-89188-63-2 457:978-83-89188-63-2 414:978-83-89188-63-2 343:978-83-89188-63-2 292:and goes through 246:period. A yellow 191:sedimentary rocks 129: 128: 16:(Redirected from 569: 537: 536: 534: 532: 509: 503: 502: 500: 498: 475: 469: 468: 466: 464: 441: 426: 425: 423: 421: 398: 387: 386: 384: 382: 373: 364: 355: 354: 352: 350: 327: 302: 259:Murowana Studnia 195:Upper Cretaceous 144:Beskid Dukielski 119: 96: 95: 93: 92: 91: 86: 82: 79: 78: 77: 74: 42: 30: 29: 21: 577: 576: 572: 571: 570: 568: 567: 566: 542: 541: 540: 530: 528: 526: 510: 506: 496: 494: 492: 476: 472: 462: 460: 458: 442: 429: 419: 417: 415: 399: 390: 380: 378: 371: 365: 358: 348: 346: 344: 328: 321: 317: 307:and Piotruś to 296: 286: 219: 167: 150:in the Western 117: 89: 87: 83: 80: 75: 72: 70: 68: 67: 28: 23: 22: 15: 12: 11: 5: 575: 565: 564: 559: 554: 539: 538: 524: 504: 490: 470: 456: 427: 413: 388: 356: 342: 318: 316: 313: 285: 282: 278:nature reserve 218: 215: 166: 163: 127: 126: 121: 113: 112: 107: 103: 102: 98: 97: 65: 59: 58: 55: 49: 48: 44: 43: 35: 34: 26: 9: 6: 4: 3: 2: 574: 563: 562:Krosno County 560: 558: 555: 553: 550: 549: 547: 527: 521: 517: 516: 508: 493: 487: 483: 482: 474: 459: 453: 449: 448: 440: 438: 436: 434: 432: 416: 410: 406: 405: 397: 395: 393: 377: 370: 363: 361: 345: 339: 335: 334: 326: 324: 319: 312: 310: 306: 300: 295: 291: 281: 279: 274: 272: 271:Karol Wojtyła 268: 267:John of Dukla 264: 260: 255: 253: 249: 245: 241: 237: 233: 229: 225: 214: 212: 208: 204: 200: 196: 192: 188: 184: 183:thrust faults 180: 176: 172: 162: 160: 159:John of Dukla 155: 153: 149: 145: 141: 137: 133: 125: 122: 120: 114: 111: 108: 104: 99: 94: 66: 64: 60: 56: 54: 50: 45: 41: 36: 31: 19: 529:. Retrieved 514: 507: 495:. Retrieved 480: 473: 461:. Retrieved 446: 418:. Retrieved 403: 379:. Retrieved 375: 347:. Retrieved 332: 287: 275: 262: 258: 256: 220: 211:conglomerate 168: 156: 139: 135: 131: 130: 118:Parent range 297: [ 263:Święta Woda 181:bounded by 148:Low Beskids 124:Low Beskids 88: / 63:Coordinates 546:Categories 315:References 309:Stasnianie 76:21°44′59″E 73:49°28′39″N 248:sandstone 203:Oligocene 199:Paleogene 101:Geography 53:Elevation 244:interwar 106:Location 381:27 June 165:Geology 132:Piotruś 33:Piotruś 18:Piotrus 531:8 June 522:  497:8 June 488:  463:8 June 454:  420:8 June 411:  349:8 June 340:  284:Trails 240:spruce 187:flysch 179:nappes 140:Petros 136:Petrus 134:(also 110:Poland 372:(PDF) 301:] 290:Dukla 252:Peter 236:alder 228:birch 224:beech 207:Marls 189:type 533:2012 520:ISBN 499:2012 486:ISBN 465:2012 452:ISBN 422:2012 409:ISBN 383:2012 351:2012 338:ISBN 238:. A 234:and 197:to 193:of 548:: 430:^ 391:^ 374:. 359:^ 322:^ 311:. 303:, 299:pl 230:, 161:. 154:. 138:, 535:. 501:. 467:. 424:. 385:. 353:. 20:)

Index

Piotrus

Elevation
Coordinates
49°28′39″N 21°44′59″E / 49.47750°N 21.74972°E / 49.47750; 21.74972
Poland
Parent range
Low Beskids
Beskid Dukielski
Low Beskids
Carpathian Mountains
John of Dukla
Alpine orogenic belt
fold and thrust belt
nappes
thrust faults
flysch
sedimentary rocks
Upper Cretaceous
Paleogene
Oligocene
Marls
conglomerate
beech
birch
European mountain-ash
alder
spruce
interwar
sandstone

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