29:
230:
287:
187:
Nicholas W. Hayman and W. S. F. Kidd., Reactivation of prethrusting, synconvergence normal faults as ramps within the
Ordovician Champlain-Taconic thrust system., Geological Society of America Bulletin (April 2002),
328:
197:
Rolf
Stanley, The Champlain thrust fault, Lone Rock Point, Burlington, Vermont., Geological Society of America Centennial Field Guide--Northeast Section, 1987
271:
362:
321:
314:
352:
347:
113:
rocks. The Middle
Ordovician accretion of the one or more island arcs terranes drove the initial thrusting during the
264:
357:
257:
130:
109:
passive margin shelf rocks westward by about 30–50 miles (48–80 km) and places them on top of
54:
294:
90:
215:
166:
110:
86:
82:
28:
146:
138:
118:
114:
70:
298:
241:
142:
134:
341:
94:
98:
210:
117:, though reactivation of the fault may have occurred during the middle Devonian
229:
121:. The Champlain Thrust marks the most westerly thrust of the Taconic Orogeny.
106:
286:
102:
237:
78:
44:
149:
can be seen thrust on top of the Middle
Ordovician Iberville shales.
74:
216:
Photos of the thrust from Lone Rock Point, Burlington
Vermont
33:
Champlain Thrust Fault, Lone Rock Point, Burlington
Vermont
129:
The thrust fault is exposed to the north of the city of
302:
245:
53:
43:
38:
21:
322:
265:
169:. University of Vermont Department of Geology
8:
329:
315:
272:
258:
18:
158:
16:Fault in Quebec, Vermont, and New York
211:Vermont State Geologic Survey Website
7:
283:
281:
226:
224:
167:"The Champlain Thrust…what is it?"
14:
285:
228:
27:
1:
301:. You can help Knowledge by
244:. You can help Knowledge by
379:
280:
223:
26:
363:Structural geology stubs
73:extending from southern
77:, down through western
240:-related article is a
97:. This east dipping
293:This article about
131:Burlington, Vermont
125:Prominent exposures
85:, and into eastern
69:is a 200-mile long
353:Structural geology
348:Geology of Vermont
295:structural geology
310:
309:
253:
252:
133:on the shores of
111:Middle Ordovician
63:
62:
370:
331:
324:
317:
289:
282:
274:
267:
260:
232:
225:
198:
195:
189:
185:
179:
178:
176:
174:
163:
83:Champlain Valley
67:Champlain Thrust
31:
22:Champlain Thrust
19:
378:
377:
373:
372:
371:
369:
368:
367:
338:
337:
336:
335:
279:
278:
221:
207:
202:
201:
196:
192:
186:
182:
172:
170:
165:
164:
160:
155:
139:Lone Rock Point
127:
119:Acadian Orogeny
115:Taconic Orogeny
49:Taconic Orogeny
34:
17:
12:
11:
5:
376:
374:
366:
365:
360:
355:
350:
340:
339:
334:
333:
326:
319:
311:
308:
307:
290:
277:
276:
269:
262:
254:
251:
250:
233:
219:
218:
213:
206:
205:External links
203:
200:
199:
190:
188:114(4):476-489
180:
157:
156:
154:
151:
143:Lower Cambrian
135:Lake Champlain
126:
123:
61:
60:
57:
51:
50:
47:
41:
40:
36:
35:
32:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
375:
364:
361:
359:
358:Vermont stubs
356:
354:
351:
349:
346:
345:
343:
332:
327:
325:
320:
318:
313:
312:
306:
304:
300:
296:
291:
288:
284:
275:
270:
268:
263:
261:
256:
255:
249:
247:
243:
239:
234:
231:
227:
222:
217:
214:
212:
209:
208:
204:
194:
191:
184:
181:
168:
162:
159:
152:
150:
148:
144:
140:
136:
132:
124:
122:
120:
116:
112:
108:
104:
100:
96:
95:Hudson Valley
92:
88:
84:
80:
76:
72:
68:
58:
56:
52:
48:
46:
42:
37:
30:
25:
20:
303:expanding it
292:
246:expanding it
235:
220:
193:
183:
171:. Retrieved
161:
128:
99:thrust fault
66:
64:
141:. Here the
101:transports
55:Age of rock
342:Categories
153:References
107:Ordovician
59:Ordovician
91:Catskills
173:25 April
147:Dolomite
103:Cambrian
87:New York
238:Vermont
145:Dunham
89:in the
81:in the
79:Vermont
45:Orogeny
39:Geology
75:Quebec
297:is a
236:This
71:fault
299:stub
242:stub
175:2016
65:The
137:at
344::
330:e
323:t
316:v
305:.
273:e
266:t
259:v
248:.
177:.
105:-
93:/
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
