Mamta Chauhan

and 2 more

Central peaks of lunar complex craters of Copernican period provide best examples to study morphologies of impact melts and exposed subsurface as they are better preserved and less affected by the space weathering. Crater Tycho, present towards SW, nearside of the Moon is one such example of young and fresh complex crater. Present study is high-resolution mineralogical investigation coupled with morphological study of central peaks and floor of crater Tycho and other contemporary craters to understand the nature of occurrence and distribution of compositionally distinct lithologies identified near their central peaks that differ in colour and specific appearance. A detailed high-resolution analysis suggests that the clastic exposures associated with the melts have a mafic composition that have been observed at similar other contemporary craters. They represent the fragmental polymict breccia clasts and their stratigraphic relation with the melts alongwith with their mineralogy suggests them to be representative of subsurface anorthositic gabbro/noritic body. Their occurrence and association with structural features, such as breccias dikes and cooling cracks suggest their formation at different stages of cratering and associated crustal modification. The formation mechanism of the polymict breccia clasts causing lithological variability has been discussed. We also report here the occurrence of rejuvenated dykes peculiar to Tycho setting that are distinct from the fractures in the immediate viscinity. Their unique nature suggests different emplacement mechanism associated with dynamic cratering process till not reported at any young complex crater on the Moon.

Chandra Bhatt

and 4 more

Today with the advancement in remote sensing technology, very high resolution imaging together with the capability of stereo data acquisition has greatly enhanced the disaster management of high hazardous and inaccessible mountainous terrain. The Rishiganga valley in the Chamoli district of Uttarakhand (North India) was impacted by sudden flash floods triggered due to a massive rockslide, caused by wedge failure on 7th February, 2021. This event caused loss of more than 200 lives besides widespread damage to hydropower projects downstream. Due to the high altitude of the terrain, huge flow of mud and debris down the valley and disruption of road connectivity, made the disaster site inaccessible through conventional means. Therefore most of the preliminary and subsequent studies carried out to assess the impact and the causes of the rockslide have heavily relied on the space based observations. The Indian Space Agency (ISRO) activated (Call Id-803) the International Charter “Space and Major Disasters” (ICSMD) to image the area of the disaster in Uttarakhand. The ICSMD is a consortium of space faring members having a constellation (61 as on date) of highly agile, multi-sensor and multi-resolution of satellite resources, which can be tasked based on type of disaster and requirement, very rapidly over the disaster affected areas to collect information on being activated. These satellite datasets are provided freely by the space agencies under ICSMD platform to serve humanitarian response for the disaster affected sites, keeping aside the commercial interests. The present study is carried out with two objectives first highlighting the role of space data in quick satellite based disaster response for this particular event which assisted the Uttarakhand State Disaster Management Agency (USDMA), Govt. of Uttarakhand to take immediate steps to mitigate the problem. The second objective tries to do an assessment and review of major studies published in peer reviewed journal between February and July, 2021 on this disaster globally to have a synthesised understanding of the event. The pre and post multi-temporal and multi-sensor and multi-resolution satellite data from ICSMD over Rishiganga and Dhauliganga valleys provided first-hand information on the chronology of the events, causes and process mechanism of this unique event and identifying locations impacted downstream. The high resolution images were useful in providing in depth understanding of the damage to hydropower projects, changes in the river geomorphology and the river impoundment due to the obstruction in the flow of one of the tributaries of the Rishiganga joining from the northeast. The satellite based inputs proved to be valuable source of information during this event for the state machinery. From all the analysis it has emerged that the satellite images have unequivocally allowed researchers to determine and quantify various terrain parameters (volume, ele