Is this rock further proof of water on Mars? Small white boulder uncovered by Curiosity rover contains evidence of water-bearing minerals Curiosity is exploring a region within Gale Crater, near the Martian equator Rock split open to reveal dazzling white interior - sign of hydrated minerals Scientists believe billions of years ago water poured down the rim of crater More signs that there was once water on Mars have been uncovered by a Nasa rover. A rock crushed under the Curiosity Mars rover's wheels split open to reveal a dazzling white interior - a sign that it contains hydrated minerals, formed when water flowed through it, scientists say. Powder drilled from a Martian rock last week revealed evidence of drinkable water and conditions favourable to life. Now instruments on the rover have found more water-bearing minerals in the area around the rock. NASA images of a rock known as 'Tintina' broken under one of the Mars rover Curiosity's wheels reveals its striking white interior. Powder drilled from Martian rocks has revealed evidence of drinkable water and conditions favourable to life Water-bearing minerals in Tintina and elsewhere have added to a list of water evidence at the area. Curiosity is exploring a region within Gale Crater, near the Martian equator, called Yellowknife Bay. Scientists believe that billions of years ago water poured down the rim of the crater and formed streams that might have been up to three feet deep. The new discoveries were made using the infrared imaging capability of Curiosity's mast camera, and an instrument that shoots neutron particles into the ground to probe for hydrogen. Differences in brightness between near-infrared wavelengths of light can indicate the presence of some hydrated minerals that have been altered by water. An image captured by the Mast Camera (Mastcam) on NASA's Mars rover Curiosity revealing interesting internal color in this rock which was broken by Curiosity when it drove over it Water-bearing minerals in Tintina and elsewhere have added to a list of water evidence at the area 'With Mastcam, we see elevated hydraion signals in the narrow veins that cut many of the rocks in this area,' said Dr Melissa Rice, from the California Institute of Technology in Pasadena. These bright veins contain hydrated minerals that are different from the clay minerals in the surrounding rock matrix. The Russian-made Dynamic Albedo of Neutrons (DAN) instrument detected hydrogen in water molecules bound into minerals in the soil beneath the rover. Yellowknife Bay contained more water than other areas previously visited by Curiosity, the results showed. 'More water is detected at Yellowknife Bay than earlier on the route,' said DAN deputy principal investigator Dr Maxim Litvak, from the Space Research Institute in Moscow. Even within Yellowknife Bay, we see significant variation. The findings were presented at the Lunar and Planetary Science Conference in The Woodlands, Texas.