| Discovery [1] | |
|---|---|
| Discovered by | Mount Lemmon Survey | 
| Discovery site | Summerhaven, Arizona, US | 
| Discovery date | 11 July 2005 | 
| Designations | |
| 2005 NB56 | |
| Orbital characteristics [2] | |
| Epoch 14 July 2005 (JD 2453565.5) | |
| Uncertainty parameter 7 | |
| Observation arc | 17 [1] d | 
| Aphelion | 2.41707 AU (361.589 Gm) | 
| Perihelion | 0.86585 AU (129.529 Gm) | 
| 1.64146 AU (245.559 Gm) | |
| Eccentricity | 0.47251 | 
| 2.10 yr (768.15 d) | |
| 25.175° | |
| 0° 28m 7.176s /day | |
| Inclination | 6.7563° | 
| 112.359° | |
| 114.15° | |
| Earth MOID | 0.0163799 AU (2,450,400 km) | 
| Jupiter MOID | 2.5887 AU (387.26 Gm) | 
| Physical characteristics | |
| ~170 m [3] | |
| 22.9 [2] | |
2005 NB56, also written as 2005 NB56, is a near-Earth asteroid of the Apollo group. [2] In 2009, research physicist Edward Drobyshevski and colleagues have suggested that 2005 NB56 could be a possible source of the meteoroid that caused the Tunguska event on 30 June 1908. It has been also suspected to be a dormant comet. [4]
One study "suggests that a chunk of a comet caused the 5-10 megaton fireball, bouncing off the atmosphere and back into orbit around the sun." [4]
This object made a close approach to Earth when it was discovered in 2005 and will do so again in 2045. [5] This object has a poorly known orbit and was only observed over an observation arc of 17 days, not sufficient to predict its position in 1908 with sufficient accuracy. [2]