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on martian volcanoes in the Hesperian: Evidence for melting of summit snowpack, caldera lake formation, drainage and erosion on Ceraunius Tholus (PDF)
on Martian Volcanoes in the Hesperian: Evidence for Melting of Summit Snowpack, Caldera Lake Formation, Drainage and Erosion on Ceraunis Tholus, Mars
來，產生原因通常是積雪處於一種「危險」的平衡狀態下，如果稍微有外力作用，就會失去平衡，造成雪塊滑動，進而引起更多積雪運動，使大量的積雪（英语：Snowpack）瞬間傾盆而下；附近的人及村莊往往不能倖免。 雪崩一般而言是由某一區域的積雪重量超過其強度所成（板状雪崩，slab
1987. Generation of liquid water on Mars through the melting of a dusty snowpack. Icarus: 72. 93–127. Barlow, N. 2008. Mars: An Introduction to its Interior
1987. Generation of liquid water on Mars through the melting of a dusty snowpack. Icarus: 72. 93-127. Barlow, N. 2008. Mars: An Introduction to its Interior