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3. The mobility of lava is strongly influenced by temperature.
                    4. A magma’s viscosity is directly related to its silica content.
                    5. The amount of volatiles contained in magma never affects its mobility.
                    6. As the magma body cools, minerals having high melting temperatures crystallize
                       first.
                    7. Only some magmas contain some water and other volatiles.
                    8. Lava  fountains  are  always  spectacular  and  mostly  harmless  and  not  generally
                       associated with major explosive events that cause great loss of life and property.
                    9. Volcanic explosions can continue until the entire magma chamber is emptied.
                    10.  The vast majority of lava on Earth is basaltic in composition.
                    11.  AA flows exhibit smooth surfaces that often resemble the twisted braids of ropes.
                    12.  Aa and pahoehoe lavas can erupt from the same vent.
                    13.  Pillow lavas are useful in the reconstruction of geologic history.

                         Task 2. Choose the correct variant in the summary below:
                      The  primary  factors  that  determine  the  nature  of  volcanic  eruptions  include  the
                  magma’s composition/chaines, its pressure/temperature, and the amount of dissolved
                  gases/fat  it  contains.  As  lava  cools,  it  begins  to  congeal  and,  as  freezing/viscosity
                  increases, its mobility decreases. The viscosity of magma is also directly related to its
                  silica/  halide  content.  Basaltic/Rhyolitic  lava,  with  its  high  silica  content  (over  70
                  percent), is very viscous and forms short, thick flows. Basaltic/ Rhyolitic lava, with a
                  lower silica content (about 50%), is more fluid and may travel a long distance before
                  congealing. Dissolved gases tend to make magma less/more fluid and, as they expand,
                  provide the force that propels molten rock from the volcano.

                                                        UNIT 7
                          VOLCANIC STRUCTURES AND ERUPTIVE STYLES
                                                         Part 1

                         Task 1.  Read and memorize the following words:
                   gradual – поступовий, послідовний         accumulation – скупчення, маса
                   erode – розмивати, піддаватися ерозії     collapse – рушитись, розвалитись
                   rim – край кратера                        depression    -   улоговина,     низина,
                                                             западина,
                   in rare cases – у рідких випадках         exceed – перевищувати, бути більшим
                   flank – бік, сторона                      fumarole – випаровування, суфляр
                   eventually – врешті-решт, у кінцевому  funnel-shaped - воронкоподібний
                   підсумку
                   discharge – виверження                    mature – дозріти, цілком розвинутись
                   terminate - завершувати                   path - шлях
                   circular    conduit     –      круговий  pipe      –     труба,     трубкоподібна
                   трубопровід                               порожнина


                         Task 2. Read the following text, translate it into Ukrainian.

                                                  Anatomy of a Volcano
                         Volcanic activity begins when a fissure (crack) develops in the crust as magma
                  moves  forcefully  toward  the  surface.  As  the  gas-rich  magma  moves  up  through  a
                  fissure, its path is usually localized into a circular conduit, or pipe, that terminates at a
                  surface opening called a vent. Successive eruptions of lava, pyroclastic material, or a


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