Page 294 - Ultimate Visual Dictionary (DK)
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GEOLOGY, GEOGRAPHY, AND METEOROLOGY

       Lakes and groundwater



       NATURAL LAKE OCCUR WHERE a large quantity of water collects in a hollow      EXAMPLES OF SPRINGS
       in impermeable rock, or is prevented from draining away by a barrier, such
                                                                                 Permeable   Water table
       as moraine (glacial deposits) or solidified lava. Lakes are often relatively   limestone
       short-lived landscape features, as they tend to become silted up by sediment
       from the streams and rivers that feed them. Some of the more long-lasting   Spring
                                                                               line
                                     lakes are found in deep rift valleys formed
                                     by vertical movements of the Earth’s crust
                                                                             Stream
                                     (see pp. 58-59)—for example, Lake Baikal
                                     in Russia, the world’s largest freshwater
                                     lake, and the Dead Sea in the Middle East,
                                     one of the world’s saltiest lakes. Where   Spring          Impermeable
                                     water is able to drain away, it sinks into                 shale
                                     the ground until it reaches a layer of           LIMESTONE SPRING
                                     impermeable rock, then accumulates in            Permeable    Water
                                     the permeable rock above it; this water-         gravel       table
                                     saturated permeable rock is called an
                                                                              Spring
                                     aquifer. The saturated zone varies in    line
                                     depth according to seasonal and climatic
            LAKE BAIKAL, RUSSIA
                                     changes. In wet conditions, the water
       stored underground builds up, while in dry periods it becomes depleted.
       Where the upper edge of the saturated zone—the water table—meets    Stream
       the ground surface, water emerges as springs. In an artesian basin, where the   Spring   Impermeable
       aquifer is below an aquiclude (layer of impermeable rock), the water table               clay
       throughout the basin is determined by its height at the rim. In the center    COASTAL (VALLEY) SPRING
       of such a basin, the water table is above ground level. The water in the            Fault   Water
       basin is thus trapped below the water table and can rise under its own    Permeable         table
                                                                                 sandstone
       pressure along faultlines or well shafts.
                                                                           Spring line

       STRUCTURE OF AN ARTESIAN BASIN            Recharge area          Spring

                           Water table
                                                                             Stream
        Height of  water table                                                                   Impermeable
        in recharge area                                                                         shale
                                                                                       FAULT SPRING
                                                                                               Water
                                                                                Spring         table
                                                                                line
                                                                         Jointed,
       Artesian                                                          solidified
       spring
                                                                         lava
                                                                         Spring
                                                             Aquiclude
                                                    Aquifer   (impermeable
       Aquiclude                                    (saturated   rock)   Jointed,
       (impermeable                      Artesian   rock)                solidified   Stream    Impermeable
       rock)                             well                            lava                   mudstone
                     Artesian       Fault
                     spring                                                             LAVA SPRING

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