Class information for: |
Basic class information |
ID | Publications | Average number of references |
Avg. shr. active ref. in WoS |
---|---|---|---|
1340 | 2613 | 53.7 | 40% |
Classes in level above (level 2) |
ID, lev. above |
Publications | Label for level above |
---|---|---|
111 | 24282 | GEOGRAPHY, PHYSICAL//BOREAS//QUATERNARY SCIENCE REVIEWS |
Terms with highest relevance score |
Rank | Term | Type of term | Relevance score (tfidf) |
Class's shr. of term's tot. occurrences |
Shr. of publ. in class containing term |
Num. of publ. in class |
---|---|---|---|---|---|---|
1 | BOREAS | Journal | 92 | 25% | 12% | 320 |
2 | DRUMLINS | Author keyword | 32 | 65% | 1% | 31 |
3 | DRUMLIN | Author keyword | 30 | 79% | 1% | 19 |
4 | BRITISH IRISH ICE SHEET | Author keyword | 26 | 69% | 1% | 22 |
5 | RIBBED MORAINE | Author keyword | 24 | 91% | 0% | 10 |
6 | SUBGLACIAL DEFORMATION | Author keyword | 21 | 85% | 0% | 11 |
7 | TILL | Author keyword | 20 | 33% | 2% | 49 |
8 | LOCH LOMOND STADE | Author keyword | 18 | 89% | 0% | 8 |
9 | GLACIAL SEDIMENTOLOGY | Author keyword | 17 | 79% | 0% | 11 |
10 | TUNNEL VALLEY | Author keyword | 17 | 79% | 0% | 11 |
Web of Science journal categories |
Author Key Words |
Rank | Web of Science journal category | Relevance score (tfidf) |
Class's shr. of term's tot. occurrences |
Shr. of publ. in class containing term |
Num. of publ. in class |
LCSH search | Wikipedia search |
---|---|---|---|---|---|---|---|
1 | DRUMLINS | 32 | 65% | 1% | 31 | Search DRUMLINS | Search DRUMLINS |
2 | DRUMLIN | 30 | 79% | 1% | 19 | Search DRUMLIN | Search DRUMLIN |
3 | BRITISH IRISH ICE SHEET | 26 | 69% | 1% | 22 | Search BRITISH+IRISH+ICE+SHEET | Search BRITISH+IRISH+ICE+SHEET |
4 | RIBBED MORAINE | 24 | 91% | 0% | 10 | Search RIBBED+MORAINE | Search RIBBED+MORAINE |
5 | SUBGLACIAL DEFORMATION | 21 | 85% | 0% | 11 | Search SUBGLACIAL+DEFORMATION | Search SUBGLACIAL+DEFORMATION |
6 | TILL | 20 | 33% | 2% | 49 | Search TILL | Search TILL |
7 | LOCH LOMOND STADE | 18 | 89% | 0% | 8 | Search LOCH+LOMOND+STADE | Search LOCH+LOMOND+STADE |
8 | GLACIAL SEDIMENTOLOGY | 17 | 79% | 0% | 11 | Search GLACIAL+SEDIMENTOLOGY | Search GLACIAL+SEDIMENTOLOGY |
9 | TUNNEL VALLEY | 17 | 79% | 0% | 11 | Search TUNNEL+VALLEY | Search TUNNEL+VALLEY |
10 | LOCH LOMOND STADIAL | 17 | 70% | 1% | 14 | Search LOCH+LOMOND+STADIAL | Search LOCH+LOMOND+STADIAL |
Key Words Plus |
Rank | Web of Science journal category | Relevance score (tfidf) |
Class's shr. of term's tot. occurrences |
Shr. of publ. in class containing term |
Num. of publ. in class |
---|---|---|---|---|---|
1 | DRUMLIN FORMATION | 110 | 95% | 1% | 37 |
2 | SUBGLACIAL TILL | 104 | 75% | 3% | 76 |
3 | PERIGLACIAL PHENOMENA | 81 | 96% | 1% | 25 |
4 | HUMMOCKY MORAINE | 77 | 80% | 2% | 48 |
5 | LOCH LOMOND READVANCE | 73 | 89% | 1% | 33 |
6 | TILL | 69 | 37% | 6% | 151 |
7 | SEDIMENT DEFORMATION | 68 | 67% | 2% | 62 |
8 | MICROSCOPIC EVIDENCE | 64 | 72% | 2% | 50 |
9 | DEFORMATION BENEATH GLACIERS | 62 | 85% | 1% | 33 |
10 | BASAL TILL | 61 | 95% | 1% | 20 |
Journals |
Rank | Web of Science journal category | Relevance score (tfidf) |
Class's shr. of term's tot. occurrences |
Shr. of publ. in class containing term |
Num. of publ. in class |
---|---|---|---|---|---|
1 | BOREAS | 92 | 25% | 12% | 320 |
2 | SCOTTISH JOURNAL OF GEOLOGY | 8 | 11% | 3% | 73 |
Reviews |
Title | Publ. year | Cit. | Active references | % act. ref. to same field |
---|---|---|---|---|
The northern sector of the last British Ice Sheet: Maximum extent and demise | 2008 | 110 | 96 | 63% |
Subglacial till: Formation, sedimentary characteristics and classification | 2006 | 159 | 178 | 79% |
Subglacial till: the deforming glacier bed | 2003 | 111 | 69 | 90% |
Fennoscandian palaeoglaciology reconstructed using a glacial geological inversion model | 1997 | 174 | 41 | 83% |
The composition and internal structure of drumlins: Complexity, commonality, and implications for a unifying theory of their formation | 2011 | 16 | 80 | 93% |
Extent and timing of the Last Glacial Maximum (LGM) in Britain and Ireland: a review | 2010 | 33 | 83 | 76% |
Middle and Late Weichselian (Devensian) glaciation history of south-western Norway, North Sea and eastern UK | 2009 | 51 | 65 | 66% |
The interpretation and classification of subglacially-deformed materials | 1996 | 196 | 75 | 76% |
Controlled moraines: origins, characteristics and palaeoglaciological implications | 2009 | 40 | 95 | 77% |
A new 'microstructural mapping' methodology for the identification, analysis and interpretation of polyphase deformation within subglacial sediments | 2011 | 15 | 50 | 80% |
Address terms |
Rank | Address term | Relevance score (tfidf) |
Class's shr. of term's tot. occurrences |
Shr. of publ. in class containing term |
Num. of publ. in class |
---|---|---|---|---|---|
1 | GLACIOL | 11 | 17% | 2.1% | 56 |
2 | EDUC COMMUNITY STUDIES | 7 | 33% | 0.7% | 18 |
3 | MURCHISON HOUSE | 6 | 22% | 1.0% | 26 |
4 | GLACIAL GRP | 6 | 71% | 0.2% | 5 |
5 | FYS GEOG BODEMKUNDIG | 5 | 63% | 0.2% | 5 |
6 | LANDSC E LANDFORM GRP | 5 | 50% | 0.3% | 7 |
7 | GEOG TOPOG SCI | 4 | 18% | 0.8% | 22 |
8 | EARTH SCI GEOG | 4 | 11% | 1.3% | 33 |
9 | MICROMORPHOL | 3 | 43% | 0.2% | 6 |
10 | ICE SHEETS PROGRAMME | 3 | 60% | 0.1% | 3 |
Related classes at same level (level 1) |
Rank | Relatedness score | Related classes |
---|---|---|
1 | 0.0000145241 | GEOGRAPHIE PHYSIQUE ET QUATERNAIRE//REGIONAL DEGLACIATION//NEW JERSEY SHELF |
2 | 0.0000136693 | GLACIAL LAKE MISSOULA//MISSOULA FLOODS//CHANNELED SCABLAND |
3 | 0.0000132727 | ARCTIC OCEAN//REMOTE SENSING METHODS GEOL//LAPTEV SEA |
4 | 0.0000128446 | JOURNAL OF GLACIOLOGY//GLACIER HYDROLOGY//CRYOSPHERE |
5 | 0.0000111417 | ANCYLUS LAKE//LITORINA SEA//LITTORINA TRANSGRESSION |
6 | 0.0000102551 | HOXNIAN//EEMIAN INTERGLACIAL//EEMIAN |
7 | 0.0000095931 | VARVES//GLACIER FED LAKE//HUMUS LAYERS |
8 | 0.0000094995 | COSMOGENIC NUCLIDES//IN SITU C 14//SURFACE EXPOSURE DATING |
9 | 0.0000092709 | ROCK GLACIER//MOUNTAIN PERMAFROST//PERMAFROST AND PERIGLACIAL PROCESSES |
10 | 0.0000078082 | JOURNAL OF GLACIOLOGY//ANTARCTIC GLACIOLOGY//RADIO ECHO SOUNDING |