369:
167:
201:
249:
22:
241:
284:
about eight metres above the ground, leads to a first room that leads to two lanes of forty metres in length, at different levels, leading to a large room in which there are two columns of stalagmites. A conduit leads to a third room containing concretions and eccentrics. At this level, progress is blocked by a narrow conduit.
283:
The cavity, with a total length of 310 metres and a height of 60 metres, contains a tectonic accident: its cross section shows a general shape of a triangle with a straight wall western wall and a shaped
Eastern staircase reversed. A gallery of thirty metres, covered in concentric circles and ovals,
178:. The two main caves are on the mountain ridges Jebel Serj and Jebel Bargou. They culminate respectively 1,309 and (m) 1,268 m and are oriented southwest and northeast. The first of these is composed of two parallel ridges separated by deep notch. All of the backbone is formed by
304:. Access to the cave of El Blida is difficult: it is entered through a narrow conduit that leads to a very small room leading into the main room; the passage between these two rooms is made through a slope of approximately 20°.
227:
It then goes to the second room that looks much like the previous one with the presence of concretions and basins . This last room is closed on a crack up to two metres above the ground. There is a colony of
358:
The cave itself has a narrow entrance allowing access to a room with cracks along the length of the walls and showing cavities. The room is followed by a narrow corridor formed by the wall and giant
328:
209:
362:
concretions, which ends with a stack of 32 metres. On the sides of the second room there are draperies, small stalactites and young stalagmites.
307:
Access to the cave of Bou Touil is the entrance is from a fairly broad which leads to narrow corridors on the left side. It leads to a room with
208:
There are caves, the most important step is the cave of El Kef Biadh whose access is via a series of wells or galleries, most of which come from
332:
260:
is an extension of the mine
Ghanguet Kef at Jebel El Damous which peaked at about 202 metres. The latter is formed by land dating from the
221:
224:
which opens on a well. It measures about 150 metres long and 50 metres wide. The vault is located some thirty metres above the ground.
293:
232:. The second room is over 200 meters long and 75 metres wide and has a vault located about forty metres above the ground in places.
315:
and columns. A large, steep (about 45 ° to 50 °) corridor in the back is ended by a narrow passage that stops the progression.
94:
66:
73:
43:
113:
51:
80:
175:
47:
62:
390:
395:
166:
323:
The
Ichkeul cave is located in the Jebel Ichkeul, located about twenty kilometres from the city of
32:
36:
87:
197:
There are sources emerging in wild vegetation and Roman ruins such as the bridge Sidi Amara.
8:
149:
began in 1979, in the youth house in the city. In 1981, a second club was opened in
130:
340:
384:
374:
248:
200:
137:
emerged in the late 1970s and includes a limited number of practitioners.
312:
308:
301:
261:
229:
217:
213:
336:
269:
183:
212:. The first large room of 1,608 m long and 267 metres deep shelters
21:
352:
348:
297:
150:
359:
324:
240:
187:
146:
344:
265:
191:
179:
134:
257:
277:
273:
364:
216:and boulders; its walls are covered with bushes of
382:
331:covering an area of 12,600 hectares including a
194:are pronounced, forming a safe fold structure.
50:. Unsourced material may be challenged and
355:and are located above a collapsed ditch.
114:Learn how and when to remove this message
247:
239:
199:
165:
383:
48:adding citations to reliable sources
15:
13:
14:
407:
272:. At these sites are deposits of
186:'s reef summit are almost all of
170:Caver descending in the Mine Cave
367:
287:
20:
318:
1:
235:
161:
7:
140:
10:
412:
174:It is believed to be the
204:Roman bridge Sidi Amara.
156:
296:has land dating to the
220:. The hall ends with a
176:longest cave in Tunisia
253:
245:
205:
171:
329:National Park Ichkeul
251:
243:
203:
169:
129:is a relatively rare
44:improve this article
335:of 8,500 hectares.
190:. The sides of the
145:The caving club of
63:"Caving in Tunisia"
254:
246:
206:
172:
391:Caving by country
127:Caving in Tunisia
124:
123:
116:
98:
403:
396:Sport in Tunisia
377:
372:
371:
370:
347:rocks date from
133:in the country.
119:
112:
108:
105:
99:
97:
56:
24:
16:
411:
410:
406:
405:
404:
402:
401:
400:
381:
380:
373:
368:
366:
321:
290:
238:
164:
159:
143:
120:
109:
103:
100:
57:
55:
41:
25:
12:
11:
5:
409:
399:
398:
393:
379:
378:
320:
317:
292:The region of
289:
286:
237:
234:
163:
160:
158:
155:
142:
139:
122:
121:
28:
26:
19:
9:
6:
4:
3:
2:
408:
397:
394:
392:
389:
388:
386:
376:
375:Africa portal
365:
363:
361:
356:
354:
350:
346:
342:
338:
334:
330:
326:
319:Cave Ichkeul
316:
314:
310:
305:
303:
299:
295:
288:Caves Joumine
285:
281:
279:
275:
271:
267:
263:
259:
250:
242:
233:
231:
225:
223:
219:
215:
211:
202:
198:
195:
193:
189:
185:
181:
177:
168:
154:
152:
148:
138:
136:
132:
128:
118:
115:
107:
96:
93:
89:
86:
82:
79:
75:
72:
68:
65: –
64:
60:
59:Find sources:
53:
49:
45:
39:
38:
34:
29:This article
27:
23:
18:
17:
357:
322:
306:
291:
282:
255:
226:
207:
196:
173:
144:
126:
125:
110:
101:
91:
84:
77:
70:
58:
42:Please help
30:
313:stalagmites
309:stalactites
214:concretions
182:land whose
385:Categories
302:Cretaceous
268:, and the
262:Cretaceous
252:Stalactite
236:Cave Nefza
74:newspapers
337:Limestone
270:Oligocene
256:The cave
244:Draprerie
222:diaclases
218:Eccentric
184:limestone
162:Mine Cave
104:June 2019
31:does not
360:calcitic
353:Jurassic
349:Triassic
341:dolomite
298:Triassic
188:outcrops
151:Zaghouan
141:Practice
327:in the
325:Bizerte
294:Joumine
147:Bizerte
88:scholar
52:removed
37:sources
345:marble
343:, and
266:Eocene
264:, the
210:mining
192:djebel
180:Aptian
135:Caving
90:
83:
76:
69:
61:
258:Nefza
157:Sites
131:sport
95:JSTOR
81:books
351:and
333:lake
311:and
300:and
278:lead
276:and
274:zinc
230:bats
67:news
35:any
33:cite
46:by
387::
339:,
280:.
153:.
117:)
111:(
106:)
102:(
92:·
85:·
78:·
71:·
54:.
40:.
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.