1162:
29:
922:) is also present. In the haĆ¼yne structure the tetrahedra are linked to form six-membered rings that are stacked up in an ..ABCABC.. sequence along one direction, and rings of four tetrahedra are stacked up parallel to another direction. The resulting arrangement forms continuous channels that can accommodate a large variety of
878:(framework silicates) each oxygen ion is shared between two tetrahedra, linking all the tetrahedra together to form a framework. Since each O is shared between two tetrahedra only half of it "belongs" to the Si ion in either tetrahedron, and if no other components are present then the formula is SiO
903:(positive ions) are Si then the positive charges on the Si's exactly balance the negative charges on the O's. When Al replaces Si there is a deficiency of positive charge, and this is made up by extra positively charged ions (cations) entering the structure, somewhere in between the tetrahedra.
760:
with nosean and with sodalite. Complete solid solution exists between synthetic nosean and haĆ¼yne at 600 Ā°C, but only limited solid solution occurs in the sodalite-nosean and sodalite-haĆ¼yne systems.
986:
is 1.50; although this is quite low, similar to that of ordinary window glass, it is the largest value for minerals of the sodalite group. It may show reddish orange to purplish pink
896:) tetrahedra. If the substitution is random the ions are said to be disordered, but in haĆ¼yne the Al and Si in the tetrahedral framework are fully ordered.
950:
crystals that may reach 3 cm across; it also occurs as rounded grains. The crystals are transparent to translucent, with a vitreous to greasy
1848:
1169:
of haĆ¼yne (diameter about 1 mm) surrounded by a fine-grained groundmass in a foidite (volcanic rock) from Melfi (Italy), as seen in
459:
113:
1575:
1277:
Italy: Millimetric transparent blue crystals in ejecta consisting mainly of K-feldspar and plagioclase from Albano
Laziale, Roma
1018:
281:
1853:
1678:
Chukanov, Nikita V.; Sapozhnikov, Anatoly N.; Shendrik, Roman Yu.; Vigasina, Marina F.; Steudel, Ralf (23 November 2020).
1316:
314:
792:
1838:
1006:
127:
1833:
1343:
1055:
504:
1828:
796:
1843:
1823:
1362:
1181:
1174:
103:
939:
1791:
1818:
1251:
271:
261:
1668:
in minerals of the haĆ¼yne-sodalite group: an FTIR spectroscopy study. Mineralogical
Magazine 73:399-413
703:
660:
1691:
1434:
539:
142:
38:
1733:
Deer Howie and
Zussman (1963) Rock-forming minerals, Volume 4, Framework Silicates, pages 289 to 302
1772:
1680:"Spectroscopic and Crystal-Chemical Features of Sodalite-Group Minerals from Gem Lazurite Deposits"
979:
959:
951:
304:
294:
1858:
1452:
1002:
954:. The color is usually bright blue, but it can also be white, grey, yellow, green and pink. In
251:
1305:
1107:
852:
188:
1384: ā Alumino-silicate mineral whose blue colour is due to a sulfide species and not copper
1773:"L'Olotipo della HaĆ¼yna. Il Cercapietre, Notiziario del Gruppo Mineralogico Romano, NĀ° 1ā2/"
1699:
1442:
1312:
1043:
983:
430:
342:
324:
241:
67:
1765:
1695:
1438:
1611:
1067:
1009:
is common, as contact, penetration and polysynthetic twins. The fracture is uneven to
875:
757:
534:
group. Hauyne was first described in 1807 from samples discovered in
Vesuvian lavas in
137:
1582:
1812:
1456:
1271:
1099:
1038:. All the members of the sodalite group have quite low densities, less than that of
975:
469:
352:
225:
149:
55:
1633:
Farndon and Parker (2009). Minerals, Rocks and
Fossils of the World. Lorenz Books
1375:
1170:
1161:
987:
955:
943:
753:
527:
230:
207:
1606:
764:
The characteristic blue color of sodalite-group minerals arises mainly from caged
538:, Italy, and was named in 1807 by Brunn-Neergard for the French crystallographer
1358:
1350:
1285:
1255:
1244:
1189:
1071:
1047:
1014:
991:
856:
804:
535:
396:
362:
172:
1378: ā Metamorphic rock containing lazurite, prized for its intense blue color
1544:
1331:
1289:
1236:
1166:
1146:
1010:
947:
382:
372:
234:
160:
1046:
is only 2.44 to 2.50. If haĆ¼yne is placed on a glass slide and treated with
1354:
1240:
1210:
1185:
1126:
1115:
1103:
1091:
1083:
971:
889:
812:
683:
476:
28:
1479:
1381:
1327:
1301:
1281:
1263:
1221:
1214:
1200:
1138:
1130:
1123:
1063:
1035:
820:
636:
580:
531:
523:
194:
59:
1704:
1679:
1447:
1422:
1642:
Tables of
Gemstone Identification By Roger Dedeyne, Ivo Quintens, p.109
1339:
1335:
1293:
1259:
1229:
1150:
1142:
1119:
1087:
923:
915:
911:
867:
472:
1540:
1297:
1225:
1207:
1204:
1134:
1111:
1095:
1059:
1039:
927:
907:
883:
860:
604:
1660:
Bellatreccia, Della
Ventura, Piccinini, Cavallo and Brilli (2009): H
1199:
Canary
Islands: A pale blue mineral intermediate between haĆ¼yne and
1323:
1160:
892:
ions Al, can substitute for some of the silicon ions, forming (AlO
34:
899:
Si has a charge 4+, but the charge on Al is only 3+. If all the
1267:
816:
1515:
Gaines et al (1997) Danaās New
Mineralogy Eighth Edition. Wiley
1742:
Wulff-Pedersen et al (2000) American
Mineralogist 85:1397-1405
900:
863:
442:
433:
448:
1407:
1220:
Ecuador: Phenocrysts found in alkaline extrusive rocks (
1054:, and then the solution is allowed to evaporate slowly,
1792:"La riscoperta del minerale di Nemi Lazialite ā HaĆ¼yna"
1751:
Carnein and Bartos (2005) Mineralogical Record 36-2:173
1766:
http://rruff.geo.arizona.edu/AMS/viewJmol.php?id=05334
1408:"IMA Mineral List with Database of Mineral Properties"
978:, but haĆ¼yne is weakly birefringent when it contains
460:
445:
439:
451:
1042:; haĆ¼yne is the densest of them all, but still its
436:
403:
391:
381:
371:
361:
351:
341:
333:
323:
313:
303:
293:
280:
270:
260:
250:
240:
224:
216:
206:
201:
187:
171:
148:
136:
126:
112:
102:
66:
51:
46:
21:
958:the crystals are colorless or pale blue, and the
542:(1743ā1822). It is sometimes used as a gemstone.
1070:under the same conditions. The mineral is not
1247:volcanic complex, Eifel, Rhineland-Palatinate
823:. More accurate measurements are as follows:
8:
1349:US: HaĆ¼yne is common in small quantities as
395:May fluoresce orange to pink under longwave
914:Ca, and in addition the negatively charged
1703:
1446:
1535:
1533:
1531:
1529:
1527:
1525:
1523:
1521:
1474:
1472:
1470:
1468:
1466:
1224:), product of effusive volcanism of the
779:
740:
736:
732:
728:
724:
720:
716:
712:
708:
696:
692:
688:
677:
673:
669:
665:
653:
649:
645:
641:
625:
621:
617:
613:
609:
597:
593:
589:
585:
573:
569:
565:
561:
557:
517:
509:
498:
494:
490:
486:
482:
94:
90:
86:
82:
78:
1511:
1509:
1394:
1288:, Rome Province, Latium, contain white
855:have a basic structural unit that is a
1729:
1727:
1725:
1723:
1721:
1719:
1717:
1715:
1507:
1505:
1503:
1501:
1499:
1497:
1495:
1493:
1491:
1489:
1062:form. This distinguishes haĆ¼yne from
791:HaĆ¼yne belongs to the hexatetrahedral
220:Blue, white, gray, yellow, green, pink
18:
1656:
1654:
1652:
1650:
1648:
1570:
1568:
1566:
1564:
1562:
1560:
1558:
1556:
1554:
1402:
1400:
1398:
7:
1423:"IMAāCNMNC approved mineral symbols"
1078:Geological setting and associations
974:. Truly isotropic minerals have no
1102:; less commonly in nepheline-free
906:In haĆ¼yne these extra cations are
870:ion Si in the middle, forming (SiO
14:
811:3n. It has one formula unit per
1192:, Rome Province, Latium, Italy.
1114:). Associated minerals include
1066:, which forms cubic crystals of
429:
27:
1322:US: HaĆ¼yne occurs in nepheline
1365:Mining District, Colorado, US.
1:
1790:Nasti, Vincenzo (2019ā2020).
1317:St. Lawrence County, New York
1280:Italy: Ejected blocks in the
1235:Germany: In ejected rocks of
1315:occurs at the Edwards Mine,
1274:, Melfi, Basilicata, Potenza
1005:is distinct to perfect, and
962:is very pale blue to white.
1849:Minerals in space group 218
938:HaĆ¼yne crystallizes in the
1875:
319:Transparent to translucent
1612:Dictionary.com Unabridged
1344:Petroleum County, Montana
514:may be present, and also
26:
1771:Nasti, Vincenzo (2009).
1576:"Handbook of Mineralogy"
1034:to 6, almost as hard as
1363:Cripple Creek, Colorado
1292:haĆ¼yne associated with
1175:petrographic microscope
752:All these minerals are
309:Very pale blue to white
1427:Mineralogical Magazine
1228:volcano, of northeast
1177:
866:O at each apex, and a
819:with side length of 9
1195:Occurrences include:
1164:
392:Other characteristics
193:a = 9.08 ā 9.13
114:Strunz classification
1854:Luminescent minerals
942:system forming rare
815:(Z = 1), which is a
530:and a member of the
387:Gelatinises in acids
266:Uneven to conchoidal
39:Rhineland-Palatinate
1705:10.3390/min10111042
1696:2020Mine...10.1042C
1448:10.1180/mgm.2021.43
1439:2021MinM...85..291W
1421:Warr, L.N. (2021).
998:Physical properties
128:Dana classification
1839:Aluminium minerals
1313:metamorphic origin
1254:blue to dark grey
1203:has been found in
1178:
966:Optical properties
833:a = 9.10 to 9.13 Ć
830:a = 9.08 to 9.13 Ć
347:n = 1.494 to 1.509
334:Optical properties
299:Vitreous to greasy
1482:. Webmineral.com.
1217:, Canary Islands.
1108:metamorphic rocks
1082:HaĆ¼yne occurs in
1013:, the mineral is
756:. HaĆ¼yne forms a
704:vladimirivanovite
661:tsaregorodtsevite
410:
409:
256:Distinct on {110}
197:; Z = 2
122:
1866:
1834:Calcium minerals
1805:
1803:
1802:
1796:
1786:
1784:
1783:
1778:. pp. 16ā43
1777:
1752:
1749:
1743:
1740:
1734:
1731:
1710:
1709:
1707:
1675:
1669:
1658:
1643:
1640:
1634:
1631:
1625:
1624:
1622:
1620:
1603:
1597:
1596:
1594:
1593:
1587:
1581:. Archived from
1580:
1572:
1549:
1548:
1537:
1516:
1513:
1484:
1483:
1476:
1461:
1460:
1450:
1418:
1412:
1411:
1404:
1044:specific gravity
1033:
1032:
1028:
1025:
984:refractive index
810:
802:
797:isometric system
782:
775:
774:
773:
770:
748:
700:
680:
657:
633:
601:
577:
521:
513:
503:. As much as 5
502:
464:
458:
457:
454:
453:
450:
447:
444:
441:
438:
435:
343:Refractive index
325:Specific gravity
286:
182:
166:
157:
154:Hextetrahedral (
121:8/J.11-30 (8 ed)
120:
118:9.FB.10 (10 ed)
98:
73:
72:(repeating unit)
31:
19:
16:Silicate mineral
1874:
1873:
1869:
1868:
1867:
1865:
1864:
1863:
1829:Sodium minerals
1809:
1808:
1800:
1798:
1794:
1789:
1781:
1779:
1775:
1770:
1761:
1756:
1755:
1750:
1746:
1741:
1737:
1732:
1713:
1677:
1676:
1672:
1667:
1663:
1659:
1646:
1641:
1637:
1632:
1628:
1618:
1616:
1605:
1604:
1600:
1591:
1589:
1585:
1578:
1574:
1573:
1552:
1539:
1538:
1519:
1514:
1487:
1478:
1477:
1464:
1420:
1419:
1415:
1406:
1405:
1396:
1391:
1372:
1159:
1080:
1053:
1030:
1026:
1023:
1021:
1000:
990:under longwave
968:
936:
921:
895:
881:
873:
849:
808:
800:
789:
781:
777:
771:
768:
767:
765:
746:
742:
738:
734:
730:
726:
722:
718:
714:
710:
706:
698:
694:
690:
686:
679:
675:
671:
667:
663:
655:
651:
647:
643:
639:
631:
627:
623:
619:
615:
611:
607:
599:
595:
591:
587:
583:
575:
571:
567:
563:
559:
555:
548:
519:
515:
511:
507:
500:
496:
492:
488:
484:
480:
462:
432:
428:
367:None, isotropic
357:None, isotropic
284:
246:Common on {111}
180:
164:
159:
155:
119:
96:
92:
88:
84:
80:
76:
71:
70:
42:
17:
12:
11:
5:
1872:
1870:
1862:
1861:
1856:
1851:
1846:
1844:Cubic minerals
1841:
1836:
1831:
1826:
1824:Sodalite group
1821:
1811:
1810:
1807:
1806:
1787:
1768:
1760:
1759:External links
1757:
1754:
1753:
1744:
1735:
1711:
1670:
1665:
1661:
1644:
1635:
1626:
1598:
1550:
1517:
1485:
1462:
1433:(3): 291ā320.
1413:
1393:
1392:
1390:
1387:
1386:
1385:
1379:
1371:
1368:
1367:
1366:
1347:
1320:
1311:US: HaĆ¼yne of
1309:
1278:
1275:
1248:
1243:rock from the
1233:
1218:
1158:
1155:
1079:
1076:
1051:
999:
996:
967:
964:
935:
932:
919:
893:
879:
876:tectosilicates
871:
848:
845:
844:
843:
840:
837:
834:
831:
828:
788:
785:
758:solid solution
750:
749:
744:
701:
681:
658:
634:
629:
602:
578:
547:
546:Sodalite group
544:
540:RenĆ© Just HaĆ¼y
468:), is a rare
419:, also called
408:
407:
405:
401:
400:
393:
389:
388:
385:
379:
378:
375:
369:
368:
365:
359:
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355:
349:
348:
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327:
321:
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264:
258:
257:
254:
248:
247:
244:
238:
237:
228:
222:
221:
218:
214:
213:
212:1,032.43 g/mol
210:
204:
203:
202:Identification
199:
198:
191:
185:
184:
175:
169:
168:
152:
146:
145:
140:
138:Crystal system
134:
133:
130:
124:
123:
116:
110:
109:
106:
100:
99:
74:
64:
63:
53:
49:
48:
44:
43:
32:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
1871:
1860:
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1835:
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1830:
1827:
1825:
1822:
1820:
1817:
1816:
1814:
1793:
1788:
1774:
1769:
1767:
1763:
1762:
1758:
1748:
1745:
1739:
1736:
1730:
1728:
1726:
1724:
1722:
1720:
1718:
1716:
1712:
1706:
1701:
1697:
1693:
1689:
1685:
1681:
1674:
1671:
1657:
1655:
1653:
1651:
1649:
1645:
1639:
1636:
1630:
1627:
1615:(Online). n.d
1614:
1613:
1608:
1602:
1599:
1588:on 2020-04-10
1584:
1577:
1571:
1569:
1567:
1565:
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1504:
1502:
1500:
1498:
1496:
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1492:
1490:
1486:
1481:
1475:
1473:
1471:
1469:
1467:
1463:
1458:
1454:
1449:
1444:
1440:
1436:
1432:
1428:
1424:
1417:
1414:
1409:
1403:
1401:
1399:
1395:
1388:
1383:
1380:
1377:
1374:
1373:
1369:
1364:
1360:
1356:
1352:
1348:
1345:
1341:
1337:
1333:
1329:
1325:
1321:
1318:
1314:
1310:
1307:
1303:
1299:
1295:
1291:
1287:
1283:
1279:
1276:
1273:
1272:Monte Vulture
1269:
1265:
1261:
1257:
1253:
1249:
1246:
1242:
1238:
1234:
1231:
1227:
1223:
1219:
1216:
1212:
1209:
1206:
1202:
1198:
1197:
1196:
1193:
1191:
1187:
1183:
1182:type locality
1176:
1172:
1168:
1163:
1156:
1154:
1152:
1148:
1144:
1140:
1136:
1132:
1128:
1125:
1121:
1117:
1113:
1109:
1105:
1101:
1100:igneous rocks
1097:
1093:
1089:
1085:
1077:
1075:
1073:
1069:
1065:
1061:
1057:
1049:
1045:
1041:
1037:
1020:
1017:, and it has
1016:
1012:
1008:
1004:
997:
995:
993:
989:
985:
981:
977:
976:birefringence
973:
965:
963:
961:
957:
953:
949:
945:
941:
933:
931:
929:
925:
917:
913:
909:
904:
902:
897:
891:
887:
885:
877:
869:
865:
862:
858:
854:
846:
841:
838:
836:a = 9.11(2) Ć
835:
832:
829:
826:
825:
824:
822:
818:
814:
806:
798:
794:
786:
784:
762:
759:
755:
754:feldspathoids
705:
702:
685:
682:
662:
659:
638:
635:
606:
603:
582:
579:
553:
552:
551:
545:
543:
541:
537:
533:
529:
525:
506:
478:
475:mineral with
474:
471:
470:tectosilicate
467:
466:
456:
426:
422:
418:
414:
406:
402:
398:
394:
390:
386:
384:
380:
376:
374:
370:
366:
364:
360:
356:
354:
353:Birefringence
350:
346:
344:
340:
336:
332:
328:
326:
322:
318:
316:
312:
308:
306:
302:
298:
296:
292:
288:
283:
279:
275:
273:
269:
265:
263:
259:
255:
253:
249:
245:
243:
239:
236:
232:
229:
227:
226:Crystal habit
223:
219:
215:
211:
209:
205:
200:
196:
192:
190:
186:
179:
176:
174:
170:
162:
153:
151:
150:Crystal class
147:
144:
141:
139:
135:
131:
129:
125:
117:
115:
111:
107:
105:
101:
75:
69:
65:
61:
57:
56:Tectosilicate
54:
50:
45:
40:
37:, Eifel Mts,
36:
30:
25:
20:
1819:Feldspathoid
1799:. Retrieved
1797:. p. 40
1780:. Retrieved
1747:
1738:
1690:(11): 1042.
1687:
1683:
1673:
1638:
1629:
1617:. Retrieved
1610:
1601:
1590:. Retrieved
1583:the original
1430:
1426:
1416:
1376:Lapis lazuli
1194:
1179:
1171:thin section
1165:A six-sided
1086:and related
1081:
1001:
988:fluorescence
969:
956:thin section
944:dodecahedral
937:
905:
898:
888:
850:
790:
763:
751:
549:
528:feldspathoid
424:
420:
416:
412:
411:
231:Dodecahedral
208:Formula mass
177:
33:Hauyne from
1359:lamprophyre
1351:phenocrysts
1286:Alban Hills
1256:phenocrysts
1190:Alban Hills
1072:radioactive
1058:needles of
1048:nitric acid
992:ultraviolet
857:tetrahedron
839:a = 9.116 Ć
805:space group
536:Monte Somma
397:ultraviolet
363:Pleochroism
315:Diaphaneity
173:Space group
1813:Categories
1801:2023-10-09
1782:2023-10-09
1607:"haĆ¼ynite"
1592:2011-11-19
1545:Mindat.org
1389:References
1332:phlogopite
1290:octahedral
1245:Laach lake
1237:hornblende
1167:phenocryst
1157:Localities
1147:phlogopite
1104:extrusives
1084:phonolites
1056:monoclinic
1011:conchoidal
980:inclusions
970:HaĆ¼yne is
948:octahedral
946:or pseudo-
934:Appearance
842:a = 9.13 Ć
783:clusters.
550:Formulae:
526:. It is a
404:References
383:Solubility
373:Fusibility
329:2.4 to 2.5
282:Mohs scale
235:octahedral
233:or pseudo-
161:H-M symbol
104:IMA symbol
1859:Gemstones
1457:235729616
1355:phonolite
1306:latiumite
1266:-bearing
1241:scapolite
1211:xenoliths
1186:Lake Nemi
1127:andradite
1116:nepheline
1092:nepheline
972:isotropic
940:isometric
918:group (SO
890:Aluminium
853:silicates
847:Structure
827:a = 8.9 Ć
813:unit cell
787:Unit cell
684:tugtupite
505:wt %
477:endmember
337:Isotropic
189:Unit cell
143:Isometric
41:, Germany
1684:Minerals
1664:O and CO
1541:"Hauyne"
1480:"Hauyne"
1382:Lazurite
1370:See also
1328:melilite
1302:melilite
1282:peperino
1264:melilite
1252:Anhedral
1239:-haĆ¼yne-
1222:tephrite
1215:La Palma
1201:lazurite
1173:under a
1139:sanidine
1131:melilite
1124:titanian
1068:chlorite
1064:sodalite
1036:feldspar
1019:hardness
1007:twinning
1003:Cleavage
882:, as in
859:with an
637:lazurite
628:)·H
581:sodalite
532:sodalite
479:formula
425:haĆ¼ynite
421:hauynite
285:hardness
272:Tenacity
262:Fracture
252:Cleavage
242:Twinning
132:76.2.3.3
60:sodalite
52:Category
1692:Bibcode
1435:Bibcode
1361:at the
1340:Winnett
1336:apatite
1324:alnoite
1294:leucite
1284:of the
1260:leucite
1250:Italy:
1230:Ecuador
1151:apatite
1143:biotite
1120:leucite
1098:-poor,
1094:-rich,
1088:leucite
1029:⁄
1015:brittle
994:light.
924:cations
916:sulfate
912:calcium
910:Na and
901:cations
874:). In
868:silicon
795:of the
743:·H
715:[Al
676:(SiAl)O
554:haĆ¼yne
473:sulfate
276:Brittle
68:Formula
47:General
1764:JMol:
1619:4 June
1455:
1298:garnet
1226:Sumaco
1208:dunite
1205:spinel
1135:augite
1112:marble
1096:silica
1060:gypsum
1040:quartz
982:. The
960:streak
952:luster
928:anions
908:sodium
884:quartz
861:oxygen
691:BeAlSi
605:nosean
417:haĆ¼yne
413:Hauyne
305:Streak
295:Luster
289:5 to 6
22:HaĆ¼yne
1795:(PDF)
1776:(PDF)
1586:(PDF)
1579:(PDF)
1453:S2CID
1346:, US.
1326:with
1213:from
1090:- or
793:class
707:Na Na
644:Ca(Si
560:Ca(Si
485:Ca(Si
465:-nyte
399:light
217:Color
81:Ca(Si
62:group
35:Mayen
1621:2016
1357:and
1334:and
1304:and
1268:lava
1180:The
1149:and
1106:and
926:and
851:All
817:cube
803:3m,
776:and
739:,Cl)
727:](SO
664:N(CH
522:and
158:3m)
1700:doi
1443:doi
1353:in
1338:at
1270:at
1258:in
1184:is
1050:HNO
864:ion
624:(SO
612:(Al
588:(Al
572:(SO
497:(SO
463:WEE
461:ah-
423:or
415:or
377:4.5
167:3m)
108:Hyn
93:(SO
1815::
1714:^
1698:.
1688:10
1686:.
1682:.
1647:^
1609:.
1553:^
1543:.
1520:^
1488:^
1465:^
1451:.
1441:.
1431:85
1429:.
1425:.
1397:^
1342:,
1330:,
1300:,
1296:,
1188:,
1153:.
1145:,
1141:,
1137:,
1133:,
1129:,
1122:,
1118:,
1074:.
930:.
886:.
799:,
735:,S
731:,S
725:24
719:Si
711:Ca
699:Cl
697:12
687:Na
678:12
672:Si
654:12
652:)O
648:Al
640:Na
622:24
620:)O
616:Si
608:Na
600:Cl
598:12
596:)O
592:Si
584:Na
570:12
568:)O
564:Al
556:Na
524:Cl
495:12
493:)O
489:Al
481:Na
449:aÉŖ
443:iĖ
434:ÉĖ
183:3n
91:12
89:)O
85:Al
77:Na
58:,
1804:.
1785:.
1708:.
1702::
1694::
1666:2
1662:2
1623:.
1595:.
1547:.
1459:.
1445::
1437::
1410:.
1319:.
1308:.
1262:-
1232:.
1110:(
1052:3
1031:2
1027:1
1024:+
1022:5
920:4
894:4
880:2
872:4
821:Ć
809:4
807:P
801:4
780:4
778:S
772:3
769:ā
766:S
747:O
745:2
741:2
737:2
733:3
729:4
723:O
721:6
717:6
713:2
709:6
695:O
693:4
689:4
674:4
670:4
668:)
666:3
656:S
650:3
646:3
642:3
632:O
630:2
626:4
618:6
614:6
610:8
594:3
590:3
586:4
576:)
574:4
566:3
562:3
558:3
520:O
518:2
516:H
512:O
510:2
508:K
501:)
499:4
491:3
487:3
483:3
455:/
452:t
446:n
440:w
437:Ė
431:/
427:(
195:Ć
181:4
178:P
165:4
163:(
156:4
97:)
95:4
87:3
83:3
79:3
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