Results 21 to 30 of about 64,792 (321)

Bullet impacts in building stone excavate approximately conical craters, with dimensions that are controlled by target material

open access: yesScientific Reports, 2022
Bullet impacts are a ubiquitous form of damage to the built environment resulting from armed conflicts. Bullet impacts into stone buildings result in surficial cratering, fracturing, and changes to material properties, such as permeability and surface ...
Oliver Campbell   +3 more
doaj   +1 more source

Locating the LCROSS Impact Craters [PDF]

open access: yesSpace Science Reviews, 2011
The Lunar CRater Observations and Sensing Satellite (LCROSS) mission impacted a spent Centaur rocket stage into a permanently shadowed region near the lunar south pole. The Sheperding Spacecraft (SSC) separated \sim9 hours before impact and performed a small braking maneuver in order to observe the Centaur impact plume, looking for evidence of water ...
Zachary Moratto   +11 more
openaire   +4 more sources

Automatic Mapping of Small Lunar Impact Craters Using LRO‐NAC Images

open access: yesEarth and Space Science, 2022
Impact craters are the most common feature on the Moon’s surface. Crater size–frequency distributions provide critical insight into the timing of geological events, surface erosion rates, and impact fluxes.
J. H. Fairweather   +5 more
doaj   +1 more source

Depth of Cracking beneath Impact Craters: New Constraint for Impact Velocity [PDF]

open access: yes, 2002
Both small-scale impact craters in the laboratory and less than 5 km in diameter bowl-shaped craters on the Earth are strength (of rock) controlled. In the strength regime, crater volumes are nearly proportional to impactor kinetic energy.
Ahrens, Thomas J.   +2 more
core   +1 more source

On the importance of self-secondaries

open access: yesGeoscience Letters, 2018
Self-secondaries are secondary craters that are formed on both the continuous ejecta deposits and interior of the parent crater. The possible existence of self-secondaries was proposed in the late 1960s, but their identity, formation mechanism, and ...
Zhiyong Xiao
doaj   +1 more source

Hypervelocity Impact Cratering on Semi-Infinite Concrete Targets of Projectiles with Different Length to Diameter Ratios

open access: yesApplied Sciences, 2020
Impact cratering experiments were performed on semi-infinite concrete targets with 7 mm-diameter 40CrNiMo steel long-rod projectiles at impact velocities ranging from 2117 m/s to 3086 m/s by using a two-stage combustion light-gas gun.
Yangyu Lu   +6 more
doaj   +1 more source

Expectations for the Deep Impact collision from cometary nuclei modelling [PDF]

open access: yes, 2005
Using the cometary nucleus model developed by Espinasse et al. (1991), we calculate the thermodynamical evolution of Comet 9P/Tempel 1 over a period of 360 years.
Klinger, Jurgen   +3 more
core   +4 more sources

The self‐secondary crater population of the Hokusai crater on Mercury

open access: yesGeophysical Research Letters, 2016
Whether or not self‐secondaries dominate small crater populations on continuous ejecta deposits and floors of fresh impact craters has long been a controversy. This issue potentially affects the age determination technique using crater statistics.
Zhiyong Xiao   +2 more
doaj   +1 more source

A comparative analysis of two Early Palaeozoic marine impact structures in Estonia, Baltic Sea: Neugrund and Kärdla [PDF]

open access: yesBulletin of the Geological Society of Finland, 2013
Kärdla and Neugrund are two Early Palaeozoic offshore impact structures located some 50 km apart along the Estonian coast of the Baltic Sea. They share many similarities but differing features are also found. The Kärdla impact structure is located at the
S. Suuroja, K. Suuroja, T. Flodén
doaj   +1 more source

Recognition of landslides in lunar impact craters [PDF]

open access: yesEuropean Journal of Remote Sensing, 2017
Landslides have been observed on several planets and minor bodies of the solar System, including the Moon. Notwithstanding different types of slope failures have been studied on the Moon, a detailed lunar landslide inventory is still pending. Undoubtedly, such will be in a benefit for future geological and morphological studies, as well in hazard, risk
Marco Scaioni   +6 more
openaire   +5 more sources

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