Which process limits the height of topographic features along a transform fault boundary?

💡 Explanation

When tectonic plates slide past each other along a transform fault, topographic features may form due to localized compression or transpression; however, erosion continuously acts to lower these features because erosion rates are related to slope angle, steepness, and material properties. Therefore, uplift must equal erosion for mountain building to stall rather than rebound, phase change, or aftershocks resulting.

• Which risk markedly increases above limestone caverns when seasonal water tables surpass a critical saturation point?
• Which geological feature primarily results from mantle upwelling during oceanic plate subduction?
• Which mechanism limits lake formation when downcutting rate exceeds sediment deposition in a fluvial valley?
• Which mechanism causes regional metamorphism during oceanic plate subduction beneath a continental plate?
• Which landform change rapidly accelerates when surface permafrost degradation forms in cirques?
• Which mechanism explains the development of columnar basalt when lava cools?