{"id":252,"date":"2017-10-01T17:22:51","date_gmt":"2017-10-01T21:22:51","guid":{"rendered":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/6-2-the-rock-cycle\/"},"modified":"2021-08-23T14:36:17","modified_gmt":"2021-08-23T18:36:17","slug":"6-2-the-rock-cycle","status":"publish","type":"chapter","link":"https:\/\/pressbooks.bccampus.ca\/physicalgeologyh5p\/chapter\/6-2-the-rock-cycle\/","title":{"raw":"6.2 The Rock Cycle","rendered":"6.2 The Rock Cycle"},"content":{"raw":"The rock components of the crust are slowly but constantly being changed from one form to another. The processes involved are summarized in the rock cycle<\/strong> (Figure 6.3). The rock cycle is driven by two forces:\r\n
    \r\n \t
  1. Earth\u2019s internal heat, which causes material to move around in the core and mantle, driving plate tectonics.<\/li>\r\n \t
  2. The hydrological cycle<\/strong>-movement of water, ice, and air at the surface. The hydrological cycle is powered by the sun.<\/li>\r\n<\/ol>\r\n[caption id=\"attachment_245\" align=\"aligncenter\" width=\"864\"]\"\"<\/a> Figure 6.3<\/strong> The rock cycle describes processes that form the three types of rock: igneous, sedimentary, and metamorphic. These same processes can turn one type of rock into another. Source: Karla Panchuk (2017) CC BY-SA 4.0. Click for more attributions<\/a>.[\/caption]\r\n\r\nThe rock cycle is still active on Earth because our core is hot enough to keep the mantle moving, the atmosphere is relatively thick, and there is liquid water. On some other planets or their satellites (e.g., Mercury), the rock cycle is virtually dead because the core is no longer hot enough to drive mantle convection, and there is no atmosphere or liquid water.\r\n\r\n \r\n
    \r\n\r\nCommon Misconception Warning!\r\n<\/strong>\r\n\r\nThe rock cycle is not<\/strong><\/em> like the life cycle of an organism where a rock must pass through all of the processes or stages, and in a particular order. The rock cycle is more like a choose-your-own-adventure. A rock's history can branch off along any pathway, or just stop altogether at a particular point.\r\n\r\n<\/div>\r\n \r\n\r\nWe can start anywhere we like to describe the rock cycle, but it\u2019s convenient to start with magma. Magma<\/strong> is melted rock located within the Earth.\u00a0 Rock can melt at between about 800 \u00b0C and 1300 \u00b0C, depending on the minerals in the rock, and the pressure the rock is under.\u00a0 If it cools slowly within the Earth (over centuries to millions of years), magma forms intrusive igneous rocks<\/strong>.\u00a0 If magma erupts onto the surface, we refer to it as\u00a0lava<\/strong>.\u00a0 Lava cools rapidly on Earth's surface (within seconds to years) and forms extrusive igneous rocks <\/strong>(Figure 6.4).[footnote]Remember the difference between intrusive and extrusive igneous rocks by recalling that IN<\/strong><\/span>trusive rocks form withIN<\/strong><\/span> the Earth, and EX<\/span><\/strong>trusive rocks form when lava EX<\/strong><\/span>its the Earth's crust.[\/footnote]\r\n\r\n \r\n\r\n[caption id=\"attachment_246\" align=\"aligncenter\" width=\"500\"]\"\"<\/a> Figure 6.4<\/strong> Lava flowing from K\u012blauea Volcano, Hawai`i. Source: J. D. Griggs, U. S. Geological Survey (1985), Public Domain. View source.<\/a>[\/caption]\r\n\r\nMountain building lifts rocks upward where they are acted upon by weathering. Weathering<\/strong> includes chemical processes that break rocks apart, as well as physical processes. Figure 6.5 shows the result of rocks in mountains being broken apart when water gets into cracks, freezes, and forces the cracks wider. Uplift through mountain building is how rocks once buried deep within Earth can be exposed at Earth's surface.\r\n\r\n \r\n\r\n[caption id=\"attachment_247\" align=\"aligncenter\" width=\"500\"]\"\"<\/a> Figure 6.5<\/strong> Mountains being broken apart by the wedging action of ice near La Madaleta Glacier, Spain. Source: Luis Paquito (2006), CC BY-SA 2.0. View source.<\/a>[\/caption]\r\n\r\nThe weathering products\u2014mostly small rock and mineral fragments\u2014are eroded, transported, and then deposited as sediments<\/strong>. Transportation and deposition occur through the action of glaciers, streams, waves, wind, and other agents. Figure 6.6 shows transportation of fine-grained sediment particles by wind during the Great Depression in the 1930s.\r\n\r\n \r\n\r\n[caption id=\"attachment_248\" align=\"aligncenter\" width=\"500\"]\"\"<\/a> Figure 6.6<\/strong> Wind transports sediment in a dust storm near Okotoks, Alberta, Canada in July of 1933. Source: Glenbow Museum Archives, File Number NA-2199-1 (1933), Public Domain. View source.<\/a>[\/caption]\r\n\r\nSediments are deposited in stream channels, lakes, deserts, and the ocean. Some depositional settings result in characteristic sedimentary structures, such as the ripples that formed when flowing water moved sand along the bottom of the South Saskatchewan River (Figure 6.7).\r\n\r\n \r\n\r\n[caption id=\"attachment_249\" align=\"aligncenter\" width=\"500\"]\"\"<\/a> Figure 6.7<\/strong> Sand ripples along the South Saskatchewan River, near Saskatoon SK. Ruby for scale. Source: Karla Panchuk (2008), CC BY-SA 4.0. View source.<\/a>[\/caption]\r\n\r\nUnless sediments are re-eroded and moved along, they'll eventually be buried by more sediments. At depths of hundreds of metres or more, sediments become compressed, forcing particles closer together. Mineral crystals grow around and between the particles, binding them together (cementing them). The hardened cemented sediments are sedimentary rock<\/strong>. Figure 6.8 shows an example of an ancient sedimentary rock in which ripple structures are preserved, and visible in cross-section as wavy lines.\r\n\r\n \r\n\r\n[caption id=\"attachment_250\" align=\"aligncenter\" width=\"500\"]\"\"<\/a> Figure 6.8<\/strong> Ripples preserved in 1.2 Ga old sandstone. Notice the wavy lines above the coin. This is a side view of the ripples. Source: Anne Burgess (2008), CC BY-SA 2.0. View source.<\/a>[\/caption]\r\n\r\nRocks that are buried very deeply within the crust can reach pressures and temperatures much higher than those at which sedimentary rocks form. Existing rocks that are heated up and squeezed under those extreme conditions are transformed into metamorphic rocks<\/strong> (Figure 6.9). The transformation to a metamorphic rock can happen through physical changes, such as when the minerals making up an existing rock re-form into larger crystals of the same mineral. It can also happen through chemical changes, when minerals within the rock react to form new minerals.\r\n\r\n \r\n\r\n[caption id=\"attachment_251\" align=\"aligncenter\" width=\"500\"]\"\"<\/a> Figure 6.9<\/strong> Limestone, a sedimentary rock formed in marine waters, has been altered by metamorphism into this marble visible on Quadra Island, BC. Source: Steven Earle (2015), CC BY 4.0. View source.<\/a>[\/caption]\r\n\r\n
    \r\n\r\n<\/a>Practice with the Rock Cycle<\/strong>\r\n\r\n[h5p id=\"32\"]\r\n\r\n<\/div>","rendered":"

    The rock components of the crust are slowly but constantly being changed from one form to another. The processes involved are summarized in the rock cycle<\/strong> (Figure 6.3). The rock cycle is driven by two forces:<\/p>\n

      \n
    1. Earth\u2019s internal heat, which causes material to move around in the core and mantle, driving plate tectonics.<\/li>\n
    2. The hydrological cycle<\/strong>-movement of water, ice, and air at the surface. The hydrological cycle is powered by the sun.<\/li>\n<\/ol>\n
      \"\"<\/a>
      Figure 6.3<\/strong> The rock cycle describes processes that form the three types of rock: igneous, sedimentary, and metamorphic. These same processes can turn one type of rock into another. Source: Karla Panchuk (2017) CC BY-SA 4.0. Click for more attributions<\/a>.<\/figcaption><\/figure>\n

      The rock cycle is still active on Earth because our core is hot enough to keep the mantle moving, the atmosphere is relatively thick, and there is liquid water. On some other planets or their satellites (e.g., Mercury), the rock cycle is virtually dead because the core is no longer hot enough to drive mantle convection, and there is no atmosphere or liquid water.<\/p>\n

       <\/p>\n

      \n

      Common Misconception Warning!
      \n<\/strong><\/p>\n

      The rock cycle is not<\/strong><\/em> like the life cycle of an organism where a rock must pass through all of the processes or stages, and in a particular order. The rock cycle is more like a choose-your-own-adventure. A rock’s history can branch off along any pathway, or just stop altogether at a particular point.<\/p>\n<\/div>\n

       <\/p>\n

      We can start anywhere we like to describe the rock cycle, but it\u2019s convenient to start with magma. Magma<\/strong> is melted rock located within the Earth.\u00a0 Rock can melt at between about 800 \u00b0C and 1300 \u00b0C, depending on the minerals in the rock, and the pressure the rock is under.\u00a0 If it cools slowly within the Earth (over centuries to millions of years), magma forms intrusive igneous rocks<\/strong>.\u00a0 If magma erupts onto the surface, we refer to it as\u00a0lava<\/strong>.\u00a0 Lava cools rapidly on Earth’s surface (within seconds to years) and forms extrusive igneous rocks <\/strong>(Figure 6.4).[1]<\/sup><\/a><\/p>\n

       <\/p>\n

      \"\"<\/a>
      Figure 6.4<\/strong> Lava flowing from K\u012blauea Volcano, Hawai`i. Source: J. D. Griggs, U. S. Geological Survey (1985), Public Domain. View source.<\/a><\/figcaption><\/figure>\n

      Mountain building lifts rocks upward where they are acted upon by weathering. Weathering<\/strong> includes chemical processes that break rocks apart, as well as physical processes. Figure 6.5 shows the result of rocks in mountains being broken apart when water gets into cracks, freezes, and forces the cracks wider. Uplift through mountain building is how rocks once buried deep within Earth can be exposed at Earth’s surface.<\/p>\n

       <\/p>\n

      \"\"<\/a>
      Figure 6.5<\/strong> Mountains being broken apart by the wedging action of ice near La Madaleta Glacier, Spain. Source: Luis Paquito (2006), CC BY-SA 2.0. View source.<\/a><\/figcaption><\/figure>\n

      The weathering products\u2014mostly small rock and mineral fragments\u2014are eroded, transported, and then deposited as sediments<\/strong>. Transportation and deposition occur through the action of glaciers, streams, waves, wind, and other agents. Figure 6.6 shows transportation of fine-grained sediment particles by wind during the Great Depression in the 1930s.<\/p>\n

       <\/p>\n

      \"\"<\/a>
      Figure 6.6<\/strong> Wind transports sediment in a dust storm near Okotoks, Alberta, Canada in July of 1933. Source: Glenbow Museum Archives, File Number NA-2199-1 (1933), Public Domain. View source.<\/a><\/figcaption><\/figure>\n

      Sediments are deposited in stream channels, lakes, deserts, and the ocean. Some depositional settings result in characteristic sedimentary structures, such as the ripples that formed when flowing water moved sand along the bottom of the South Saskatchewan River (Figure 6.7).<\/p>\n

       <\/p>\n

      \"\"<\/a>
      Figure 6.7<\/strong> Sand ripples along the South Saskatchewan River, near Saskatoon SK. Ruby for scale. Source: Karla Panchuk (2008), CC BY-SA 4.0. View source.<\/a><\/figcaption><\/figure>\n

      Unless sediments are re-eroded and moved along, they’ll eventually be buried by more sediments. At depths of hundreds of metres or more, sediments become compressed, forcing particles closer together. Mineral crystals grow around and between the particles, binding them together (cementing them). The hardened cemented sediments are sedimentary rock<\/strong>. Figure 6.8 shows an example of an ancient sedimentary rock in which ripple structures are preserved, and visible in cross-section as wavy lines.<\/p>\n

       <\/p>\n

      \"\"<\/a>
      Figure 6.8<\/strong> Ripples preserved in 1.2 Ga old sandstone. Notice the wavy lines above the coin. This is a side view of the ripples. Source: Anne Burgess (2008), CC BY-SA 2.0. View source.<\/a><\/figcaption><\/figure>\n

      Rocks that are buried very deeply within the crust can reach pressures and temperatures much higher than those at which sedimentary rocks form. Existing rocks that are heated up and squeezed under those extreme conditions are transformed into metamorphic rocks<\/strong> (Figure 6.9). The transformation to a metamorphic rock can happen through physical changes, such as when the minerals making up an existing rock re-form into larger crystals of the same mineral. It can also happen through chemical changes, when minerals within the rock react to form new minerals.<\/p>\n

       <\/p>\n

      \"\"<\/a>
      Figure 6.9<\/strong> Limestone, a sedimentary rock formed in marine waters, has been altered by metamorphism into this marble visible on Quadra Island, BC. Source: Steven Earle (2015), CC BY 4.0. View source.<\/a><\/figcaption><\/figure>\n
      \n

      <\/a>Practice with the Rock Cycle<\/strong><\/p>\n

      \n