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## E-Learning
### Answer
questionOption_AC8F9553_B6C5_B43D_41DE_0EC529F4F534.text = A hot spot
questionOption_8965DD89_B93A_742D_41D2_C317F8A50198.text = Calderas
questionOption_8E4D858D_BECD_9425_41E4_936F0ECA8020.text = It cooled the climate by absorbing more solar radiation
questionOption_896F004F_B93A_6C25_41E2_233E41D67091.text = All the above
questionOption_ADA7EC3B_B6CA_F46D_41D1_5AC2B302F36B.text = Andesitic explosive eruptions
questionOption_9427299D_B6DD_9C24_41E4_DDB06E6E6489.text = Andesitic lava
questionOption_9502BD69_B6C6_94ED_41E1_49F859414401.text = Basaltic lava traveling long distances and creating gentle slopes
questionOption_943B0502_B6DD_941C_41E1_B680AB9923BB.text = Basaltic lavas
questionOption_ADAE53CE_B6CA_EC27_41E0_E4C820616AB1.text = Basaltic lavas with high viscosity
questionOption_ADB76034_B6CA_EC7B_41E1_F5B76CE189A0.text = Basaltic lavas with low viscosity
questionOption_895D7AFC_B93A_7DEB_41C7_25E34B6C12D6.text = Cinder cones
questionOption_ACB70BFB_B6C5_B3ED_41D9_04DD260D257A.text = Compression associated with subduction
questionOption_958BEAFF_B6DD_9DE5_41E0_298CC7B4B93F.text = Divergent boundaries
questionOption_8EBD16EB_BEDA_F5ED_41D8_AA944EFF19E1.text = Explosive eruptions of steam from magma coming into contact with the water table
questionOption_ACB10F0D_B6C5_B425_41DB_5CCF7840D266.text = Extension associated with the Basin and Range
questionOption_ACD9A94C_B6C6_7C2B_41E5_883CC743B62B.text = Gentle slopes formed by low viscosity lava flows
questionOption_942D5C90_B6DD_943B_41D7_95384D7D5D3F.text = Granitic lava
questionOption_8E9E60B8_BEDA_EC6B_41DE_C57223304379.text = High viscosity, highly explosive rhyolitic eruptions
questionOption_949CE4F0_B6DF_B5FB_41DD_8BA7BD710AE4.text = Intraplate hot spots
questionOption_8E55B30B_BECA_6C2D_41A2_28783A15A884.text = It cooled the climate by reflecting more solar radiation
questionOption_8E5D8080_BECA_6C1B_41E5_8811CA6F18A4.text = It warmed the climate by absorbing more solar radiation
questionOption_8E6E2DA4_BECA_741B_41D7_A90439C223D1.text = It warmed the climate by reflecting more solar radiation
questionOption_8E94DD07_BEDA_F425_41BC_F8A9B585F3EC.text = Low viscosity basaltic eruptions
questionOption_8F3DDA11_BEC6_7C3D_41E0_F32137024258.text = Low viscosity basaltic flows generating gentle slopes
questionOption_ACFA92F2_B6C6_6DFC_41D6_32B557B915B0.text = Massive craters from the evacuation of explosive rhyolitic magma chambers
questionOption_950CAFED_B6C6_93E5_41CF_37F3B7A57F6E.text = Multiple eruptive styles over long period of time leading to relatively steep slopes
questionOption_95292969_B6C6_9CED_41E4_92437A096EF6.text = Rapid accumulation of cinder over a small area
questionOption_94492295_B6DD_AC25_41D5_A2C3C2E88A66.text = Rhyolitic lava
questionOption_AD977C08_B6CA_942B_41E5_C685F799F38C.text = Rhyolitic lavas with low viscosity
questionOption_ACBC498F_B6C5_BC25_41DC_E8D2BD16BDF5.text = Shearing stress due to the San Andreas Fault
questionOption_8EACAA5A_BEDA_FC2F_41D7_3FCBAD59413F.text = Small, localized eruptions of cinder
questionOption_ACC0DFB3_B6C6_747D_41E1_1C67E60603BD.text = Steep slopes formed by cinder which is piled quickly next to their craters
questionOption_ACC4BD12_B6C6_743F_41A7_58A8D278A648.text = Steep slopes formed by multiple eruptive styles and compositions
questionOption_894697DE_B93A_7427_41DC_C205913190CA.text = Stratovolcanoes
questionOption_956915B0_B6DE_747B_41AA_F337E787CD27.text = Subduction zones
questionOption_8FAF1B93_BEC7_FC3D_41E0_A80F8051C7D7.text = The collapse of a mountain following evacuation of a magma chamber
questionOption_8F41A821_BEC6_7C1D_41C5_E03C6C7D7A5D.text = The collapse of the magma chamber due to the removal magma over time though volcanic eruptions
questionOption_8F2B5FDD_BEC6_7425_41DA_80F7F875BF9B.text = The eruption of andesitic lava and the formation of steep slopes
questionOption_8FB5E8FB_BEC7_FDED_41C1_438895E9C597.text = The gradual addition of basaltic lava flows generating a large, broad feature with gentle slopes
questionOption_8FB8F644_BEC7_F41B_41E1_CED392298C7E.text = The rapid accumulation of lava blocks and bombs over relatively short periods of time that form into a small, symmetrical, steep-sided feature
questionOption_8F23CD01_BEC6_741D_41DF_F52BF0AA51DD.text = The rapid release of cinder creating a small cone
questionOption_8FF83178_BEC7_ECEB_41AD_CAF1C2D7EA7B.text = The slow extrusion of high viscosity, rhyolitic lavas into a dome
questionOption_957CAE55_B6DD_9425_41E3_72E5A997F05D.text = Transform boundaries
questionOption_94F7C316_B6C6_AC27_41D9_747A7B96AA7C.text = Volcano collapse following magma chamber evacuation
### Question
question_8F948EAC_BEC6_946B_41B3_78AE4C613D73.title = Calderas form from:
question_8E23AF3B_BEC6_946D_41DE_CF4FC9991E1D.title = Cinder cones form due to:
question_961032FE_B6DD_ADE7_41DB_BB28FFB85982.title = In what tectonic setting are strato-, also known as composite, volcanoes found?
question_AD1FA1D0_B6C6_EC3B_41E2_451E020AB46E.title = Shield volcano are characterized by:
question_AE31E66F_B6CD_94E5_41CF_378C9281DBB9.title = Shield volcanoes are formed from:
question_955B5E5B_B6C6_B42D_41E3_1F558FB58272.title = Stratovolcanoes form due to:
question_8F2D7623_BEDA_741D_41BB_4E4EFFB27541.title = The most explosive eruptions in Crater Lake/Mt Mazama’s history are associated with:
question_8EAEC720_BECA_B41C_41D7_12C14A673845.title = What impact did the ash erupted from Mt. Mazama have on climate for several years following the event?
question_ACC16A2E_B6C5_9C67_41E5_D37FEC8356F3.title = What led to the formation of this shield volcano in Utah?
question_94CF6CD7_B6DE_9425_41E4_A0D087C8FE0C.title = What type of lava is most commonly erupted from a stratovolcano?
question_8F2A4925_BEC5_9C65_41D2_1018BFEDE4BD.title = What volcanic landforms are found in the Cascades Volcanic Arc?
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