35:
80:
145:
111:
may have been pushed over the crest of the initial rim from the initial impact, thereby increasing its overall height. When combined with potential weathering due to atmospheric erosion over time, determining the average height of a crater rim can be somewhat difficult. It has also been observed that
54:
is the part that extends above the height of the local surface, usually in a circular or elliptical pattern. In a more specific sense, the rim may refer to the circular or elliptical edge that represents the uppermost tip of this raised portion. If there is no raised portion, the rim simply refers
131:
between the two planetary bodies that collide. Additionally, crater depth and the volume of melt produced in the impact are directly related to the gravitational acceleration between the two bodies. It has been proposed that “reverse faulting and thrusting at the final crater rim one of the main
103:
Large craters are those with a diameter greater than 2.3 km, and are distinguished by central uplifts within the impact zone. These larger (also called “complex”) craters can form rims up to several hundred meters in height.
127:
Complex crater rims observed on Earth have anywhere between 5X – 8X greater height:diameter ratio compared to those observed on the Moon, which can likely be attributed to the greater force of
132:
contributing factors forming the elevated crater rim”. When an impact crater is formed on a sloped surface, the rim will form in an asymmetric profile. As the impacted surface's
267:
Krohn, K., Jaumann, R., Otto, K., Hoogenboom, T., Wagner, R., Buczkowski, D., Schenk, P. (2014). "Mass
Movement on Vesta at Steep Scarps and Crater Rims".
334:
Neish, C., Herrick, R., Zanetti, M., & Smith, D. (2017). "The Role of Pre-Impact
Topography in Impact Melt Emplacement on Terrestrial Planets".
369:
320:
253:
266:
206:"Structural Uplift and Ejecta Thickness of Lunar Mare Craters: New Insights Into the Formation of Complex Crater Rims"
17:
128:
63:
Smaller, simple craters retain rim geometries similar to the features of many craters found on the
432:
427:
386:
Hayashi, K.; Sumita, I. (2017). "Low-Velocity Impact
Cratering Experiments in Granular Slopes".
363:
314:
247:
55:
to the inside edge of the curve where the flat surface meets the curve of the crater bottom.
221:
34:
395:
343:
276:
217:
183:
28:
8:
399:
347:
280:
187:
174:
Pike, R.J. (1981). "Meteorite
Craters: Rim Height, Circularity, and Gravity Anomalies".
152:
The rim type classifications are full-rim craters, broken-rim craters, and depressions.
302:
235:
84:
239:
113:
96:
333:
403:
351:
306:
292:
284:
225:
68:
407:
355:
288:
133:
107:
A process to consider when determining the exact height of a crater rim is that
108:
92:
421:
203:
51:
39:
121:
297:
112:
the slope along the excavated interior of many craters can facilitate a
230:
205:
124:
events occurring due to slope instability and nearby seismic activity.
144:
79:
148:
A side view of a crater, with a raised rim, highlighted in red.
117:
88:
64:
136:
increases, the crater's profile becomes more elongate.
204:
KrĂĽger, T., Kenkmann, T., & Hergarten, S. (2017).
419:
385:
368:: CS1 maint: multiple names: authors list (
319:: CS1 maint: multiple names: authors list (
252:: CS1 maint: multiple names: authors list (
296:
229:
143:
78:
33:
381:
379:
199:
197:
14:
420:
169:
167:
165:
376:
194:
173:
210:Meteoritics & Planetary Science
162:
24:
74:
25:
444:
139:
58:
327:
260:
13:
1:
155:
27:For other uses of "Rim", see
408:10.1016/j.icarus.2017.03.027
356:10.1016/j.icarus.2017.07.004
289:10.1016/j.icarus.2014.03.013
7:
176:Lunar and Planetary Science
10:
449:
129:gravitational acceleration
26:
222:2017M&PS...52.2220K
149:
120:morphology, including
100:
43:
147:
82:
37:
29:Rim (disambiguation)
400:2017Icar..291..160H
348:2017Icar..297..240N
281:2014Icar..244..120K
188:1981LPI....12..842P
91:, as seen from the
231:10.1111/maps.12925
150:
101:
44:
216:(10): 2220–2240.
97:Opportunity rover
16:(Redirected from
440:
412:
411:
383:
374:
373:
367:
359:
331:
325:
324:
318:
310:
300:
264:
258:
257:
251:
243:
233:
201:
192:
191:
171:
85:Endurance Crater
21:
448:
447:
443:
442:
441:
439:
438:
437:
418:
417:
416:
415:
384:
377:
361:
360:
332:
328:
312:
311:
265:
261:
245:
244:
202:
195:
172:
163:
158:
142:
134:angle of repose
77:
75:Complex craters
67:and the planet
61:
32:
23:
22:
15:
12:
11:
5:
446:
436:
435:
433:Impact craters
430:
428:Impact geology
414:
413:
375:
326:
298:2286/R.I.28057
259:
193:
160:
159:
157:
154:
141:
140:Classification
138:
76:
73:
60:
59:Simple craters
57:
50:or edge of an
38:Crater rim of
9:
6:
4:
3:
2:
445:
434:
431:
429:
426:
425:
423:
409:
405:
401:
397:
393:
389:
382:
380:
371:
365:
357:
353:
349:
345:
341:
337:
330:
322:
316:
308:
304:
299:
294:
290:
286:
282:
278:
274:
270:
263:
255:
249:
241:
237:
232:
227:
223:
219:
215:
211:
207:
200:
198:
189:
185:
181:
177:
170:
168:
166:
161:
153:
146:
137:
135:
130:
125:
123:
119:
115:
110:
105:
98:
94:
90:
86:
81:
72:
70:
66:
56:
53:
52:impact crater
49:
41:
40:Meteor Crater
36:
30:
19:
18:Rim (craters)
391:
387:
364:cite journal
339:
335:
329:
315:cite journal
272:
268:
262:
248:cite journal
213:
209:
179:
175:
151:
126:
122:mass wasting
106:
102:
93:landing site
62:
47:
45:
394:: 160–175.
342:: 240–251.
275:: 120–132.
182:: 842–844.
83:The rim of
422:Categories
156:References
240:135227558
42:, Arizona
396:Bibcode
344:Bibcode
307:2313339
277:Bibcode
218:Bibcode
184:Bibcode
95:of the
69:Mercury
388:Icarus
336:Icarus
305:
269:Icarus
238:
303:S2CID
236:S2CID
118:gully
116:-and-
370:link
321:link
254:link
114:spur
109:melt
89:Mars
65:Moon
46:The
404:doi
392:291
352:doi
340:297
293:hdl
285:doi
273:244
226:doi
180:XII
87:on
48:rim
424::
402:.
390:.
378:^
366:}}
362:{{
350:.
338:.
317:}}
313:{{
301:.
291:.
283:.
271:.
250:}}
246:{{
234:.
224:.
214:52
212:.
208:.
196:^
178:.
164:^
71:.
410:.
406::
398::
372:)
358:.
354::
346::
323:)
309:.
295::
287::
279::
256:)
242:.
228::
220::
190:.
186::
99:.
31:.
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.