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* * * A HIDROSFERA Dr. Francisco Sergio Bernardes Ladeira * * * O CICLO HIDROLÓGICO * * * * * * * * * * * * * * * * * * Figure 14.20 e.g. flat-laying or homogeneous rocks Dendritic Drainage Pattern * * * Figure 14.20 Rectangular Drainage Pattern e.g. jointed or faulted rocks * * * Figure 14.20 e.g. folded layered rocks Trellis Drainage Pattern * * * Figure 14.20 e.g. volcano or dome Radial Drainage Pattern * * * Figure 14.6 Waterfall formed by headward erosion * * * Figure 14.9 Meandering River in Alaska Point Bar Meandering channel * * * Figure 14.9b Braided River in Alaska Braided channels * * * Figure 14.9 Meandering Streams * * * Figure 14.9 …eventually results in meander cutoffs and the formation of oxbow lakes. Oxbow Lake Point Bars Meander Cutoff * * * Figure 14.9 Meanders in the Mississippi River delta * * * Porosity The percent void space in a rock or sediment. It is a measure of the potential volume of water that can be stored in a rock. * * * Permeability The ability of a material to transmit a fluid. It is a measure of how fast the fluid can travel through the rock or sediment * * * Figure 13.7 Porosity varies with % Cement Sorting Fracturing * * * Figure 13.7 Porosity Varies with % Cement * * * Figure 13.7 Porosity Varies with Sorting * * * * * * Figure 13.7 MORE POROUS LESS POROUS Fractured Shale Unfractured Shale Porosity Varies with Fracturing * * * Figure 13.8 Unsaturated Zone: Pores include both air and water Saturated Zone: Pores filled with water Groundwater Table Unconfined Aquifer * * * Figure 13.12 Formation of a Cone of Depression * * * Figure 13.13 Fissures and depressions caused by ground subsidence due to overpumping of groundwater * * * Figure 13.19 Some Major Features of a Karst Landscape * * * Figure 13.18 The Winter Park Sinkhole, Florida * * * Figure 13.14 Dynamics of the Saltwater - Fresh Water Interface * * * Figure 13.20 Some Human Activities that Can Contaminate Groundwater * * * * * * Figure 14.10 Low Natural Levee Building a Floodplain, One Flood at a Time * * * Figure 14.10 Overbank flow results in the flooding of the floodplain Decreased flow velocity results in deposition of suspended sediment Building a Floodplain, One Flood at a Time * * * Figure 14.10 Building a Floodplain, One Flood at a Time * * * Box 14.1 Life on the Floodplain!