Question: Mangalyaan of the country having Goa was sent to the planet containing Outflow channels by launching what?

<P0-S0> mangala valles is a complex system of criss-crossing channels on mars, located in the tharsis region and in the memnonia quadrangle. <P0-S1> it originates in the hesperian and amazonian epochs. <P0-S2> it is thought to be an outflow channel, carved by catastrophic floods, and the release of vast quantities of water across the martian surface. <P0-S3> this flooding was probably initiated by tectonic stretching and the formation of a graben, mangala fossa, at the channels' head, perhaps breaching a pressurized aquifer trapped beneath a thick "cryosphere" (layer of frozen ground) beneath the surface. <SEP> <P1-S0> Outflow channels are extremely long, wide swathes of scoured ground on Mars, commonly containing the streamlined remnants of pre-existing topography and other linear erosive features indicating sculpting by fluids moving downslope. <P1-S1> Channels extend many hundreds of kilometers in length and are typically greater than one kilometer in width; the largest valley (Kasei Vallis) is around long, greater than wide and exceeds in depth cut into the surrounding plains. <P1-S2> These features tend to appear fully sized at fractures in the Martian surface, either from chaos terrains or from canyon systems or other tectonically controlled, deep graben, though there are exceptions. <P1-S3> Besides their exceptional size, the channels are also characterized by low sinuosities and high width:depth ratios compared both to other Martian valley features and to terrestrial river channels. <P1-S4> Crater counts indicate that most of the channels were cut since the early Hesperian, though the age of the features is variable between different regions of Mars. <P1-S5> Some outflow channels in the Amazonis and Elysium Planitiae regions have yielded ages of only tens of million years, extremely young by the standards of Martian topographic features. <SEP> <P2-S0> ma'adim vallis is one of the largest outflow channels on mars, about 700 km long and significantly larger than earth's grand canyon. <P2-S1> it is over 20 km wide and 2 km deep in some places. <P2-S2> it runs from a region of southern lowlands thought to have once contained a large group of lakes (see eridania lake) north to gusev crater near the equator. <P2-S3> it looks as if water may have collected in gusev crater, forming a giant lake; the spirit rover was sent there to investigate that possibility, but found only volcanic rocks on the floor of gusev. <P2-S4> any lake deposits were probably covered over by a later deposit of volcanic materials from apollinaris mons, a nearby volcano. <SEP> <P3-S0> The Mars Orbiter Mission probe lifted - off from the First Launch Pad at Satish Dhawan Space Centre (Sriharikota Range SHAR), Andhra Pradesh, using a Polar Satellite Launch Vehicle (PSLV) rocket C25 at 09: 08 UTC on 5 November 2013. <P3-S1> The launch window was approximately 20 days long and started on 28 October 2013. <P3-S2> The MOM probe spent about a month in Earth orbit, where it made a series of seven apogee - raising orbital manoeuvres before trans - Mars injection on 30 November 2013 (UTC). <P3-S3> After a 298 - day transit to Mars, it was successfully inserted into Mars orbit on 24 September 2014. <SEP> <P4-S0> In December 1547, Francis was in Malacca (Malaysia) waiting to return to Goa (India) when he met a low-ranked samurai named Anjiro (possibly spelled "Yajiro"). <P4-S1> Anjiro was not an intellectual, but he impressed Xavier because he took careful notes of everything he said in church. <P4-S2> Xavier made the decision to go to Japan in part because this low-ranking samurai convinced him in Portuguese that the Japanese people were highly educated and eager to learn. <P4-S3> They were hard workers and respectful of authority. <P4-S4> In their laws and customs they were led by reason, and, should the Christian faith convince them of its truth, they would accept it en masse.