Statements (55)
| Predicate | Object |
|---|---|
| gptkbp:instance_of |
gptkb:Scientist
|
| gptkbp:affiliation |
gptkb:Siberian_Branch_of_the_Russian_Academy_of_Sciences
|
| gptkbp:awards |
gptkb:Order_of_the_Red_Banner_of_Labour
|
| gptkbp:birth_date |
1900-01-20
|
| gptkbp:collaborator |
gptkb:Mikhail_Lomonosov
gptkb:Vladimir_Obruchev |
| gptkbp:contribution |
advancements in planetary geology
Tunguska event hypothesis Tunguska event theories collaborative research in geosciences development of impact crater studies education in geology and meteorology field expeditions to Tunguska fieldwork methodologies in geology increased awareness of cosmic impacts influence on environmental science. publications on cosmic phenomena scientific expeditions in remote areas scientific literature on meteorites |
| gptkbp:death_date |
1942-12-12
|
| gptkbp:field |
geology
meteorology geophysics |
| https://www.w3.org/2000/01/rdf-schema#label |
Leonid Kulik
|
| gptkbp:impact |
understanding of meteorite impacts
public interest in meteorites geological surveys in Siberia Tunguska event studies |
| gptkbp:influence |
future meteorite researchers
geologists in Russia geophysicists globally scientific methodology in impact studies |
| gptkbp:influenced |
meteorite science
|
| gptkbp:influenced_by |
Vladimir Vernadsky
|
| gptkbp:involvement |
scientific community in Russia
Siberian meteorite expeditions international meteorite research |
| gptkbp:known_for |
studying the Tunguska event
|
| gptkbp:legacy |
influence on planetary science
Kulik crater on Mars Kulik's expeditions |
| gptkbp:nationality |
gptkb:Russian
|
| gptkbp:notable_work |
Tunguska meteorite research
|
| gptkbp:place_of_birth |
gptkb:Saint_Petersburg,_Russia
|
| gptkbp:place_of_death |
Moscow, Russia
|
| gptkbp:published_work |
The Tunguska Mystery
|
| gptkbp:research |
data analysis
sample collection geophysical surveys field geology |
| gptkbp:research_focus |
impact events
cosmic impacts |
| gptkbp:bfsParent |
gptkb:Tunguska_event
gptkb:Tunguska |
| gptkbp:bfsLayer |
7
|