{"id":506,"date":"2010-09-07T11:16:28","date_gmt":"2010-09-07T01:16:28","guid":{"rendered":"https:\/\/scienceillustrated.com.au\/blog\/gallery\/mouths-of-the-earth\/"},"modified":"2010-09-07T11:16:28","modified_gmt":"2010-09-07T01:16:28","slug":"mouths-of-the-earth","status":"publish","type":"post","link":"https:\/\/scienceillustrated.com.au\/blog\/galleries\/mouths-of-the-earth\/","title":{"rendered":"Mouths of the Earth"},"content":{"rendered":"<p><div\n\tclass=\"ngg-galleryoverview ngg-ajax-pagination-none\"\n\tid=\"ngg-gallery-9e165d481ce8c29e66c7035e5a3793c4-1\">\n\n    \t\t<!-- Thumbnails -->\n\t\t\t\t<div id=\"ngg-image-0\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol6.jpg\"\n               title=\"When nearby Parinacota erupted 8,000 years ago, a six-cubic-kilometre avalanche of debris was shot into the air, littering the surrounding area. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol6.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol6.jpg\"\n               data-image-id=\"21\"\n               data-title=\"Lake Chungara, Chile\"\n               data-description=\"When nearby Parinacota erupted 8,000 years ago, a six-cubic-kilometre avalanche of debris was shot into the air, littering the surrounding area. Image: Olivier Grunewald.\"\n               data-image-slug=\"lake-chungara-chile\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Lake Chungara, Chile\"\n                    alt=\"Lake Chungara, Chile\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol6.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-1\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol5.jpg\"\n               title=\"This beautiful snow-capped peak is one of the most scenic in the Kamchatka Peninsula. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol5.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol5.jpg\"\n               data-image-id=\"20\"\n               data-title=\"Mount Kronotsky, Russia\"\n               data-description=\"This beautiful snow-capped peak is one of the most scenic in the Kamchatka Peninsula. Image: Olivier Grunewald.\"\n               data-image-slug=\"mount-kronotsky-russia\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Mount Kronotsky, Russia\"\n                    alt=\"Mount Kronotsky, Russia\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol5.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-2\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol10.jpg\"\n               title=\"A crater lake that has formed by magma rising and encountering shallow water, causing steam explosions. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol10.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol10.jpg\"\n               data-image-id=\"15\"\n               data-title=\"Lake Dal\\&#039;ny, Russia\"\n               data-description=\"A crater lake that has formed by magma rising and encountering shallow water, causing steam explosions. Image: Olivier Grunewald.\"\n               data-image-slug=\"lake-dalny-russia\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Lake Dal\\&#039;ny, Russia\"\n                    alt=\"Lake Dal\\&#039;ny, Russia\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol10.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-3\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol2.jpg\"\n               title=\"This series of dark hexagonal columns is formed in a lava flow, and surrounds the area of the popular tourist attraction Svartifoss waterfall. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol2.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol2.jpg\"\n               data-image-id=\"17\"\n               data-title=\"Svartifoss waterfall, Iceland\"\n               data-description=\"This series of dark hexagonal columns is formed in a lava flow, and surrounds the area of the popular tourist attraction Svartifoss waterfall. Image: Olivier Grunewald.\"\n               data-image-slug=\"svartifoss-waterfall-iceland\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Svartifoss waterfall, Iceland\"\n                    alt=\"Svartifoss waterfall, Iceland\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol2.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-4\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/volcano1.jpg\"\n               title=\"This towering 3,676 metre volcano has been erupting almost continuously since 1967. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/volcano1.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_volcano1.jpg\"\n               data-image-id=\"25\"\n               data-title=\"Mount Semeru, Indonesia\"\n               data-description=\"This towering 3,676 metre volcano has been erupting almost continuously since 1967. Image: Olivier Grunewald.\"\n               data-image-slug=\"mount-semeru-indonesia\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Mount Semeru, Indonesia\"\n                    alt=\"Mount Semeru, Indonesia\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_volcano1.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-5\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol3.jpg\"\n               title=\"The only known active volcano in the world that emits natrocarbonatite lava, which is more than 500 degrees cooler than typical basaltic lavas. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol3.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol3.jpg\"\n               data-image-id=\"18\"\n               data-title=\"Ol Doinyo Lengai, Tanzania\"\n               data-description=\"The only known active volcano in the world that emits natrocarbonatite lava, which is more than 500 degrees cooler than typical basaltic lavas. Image: Olivier Grunewald.\"\n               data-image-slug=\"ol-doinyo-lengai-tanzania-2\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Ol Doinyo Lengai, Tanzania\"\n                    alt=\"Ol Doinyo Lengai, Tanzania\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol3.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-6\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol11.jpg\"\n               title=\"Close-up of natrocarnonatite lava formation. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol11.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol11.jpg\"\n               data-image-id=\"16\"\n               data-title=\"Ol Doinyo Lengai, Tanzania\"\n               data-description=\"Close-up of natrocarnonatite lava formation. Image: Olivier Grunewald.\"\n               data-image-slug=\"ol-doinyo-lengai-tanzania\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Ol Doinyo Lengai, Tanzania\"\n                    alt=\"Ol Doinyo Lengai, Tanzania\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol11.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-7\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol4.jpg\"\n               title=\"One of Asia\\&#039;s deadliest mountains, the Indonesian government has partially drained the summit crater lake several times. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol4.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol4.jpg\"\n               data-image-id=\"19\"\n               data-title=\"Mount Kelud, Indonesia\"\n               data-description=\"One of Asia&#039;s deadliest mountains, the Indonesian government has partially drained the summit crater lake several times. Image: Olivier Grunewald.\"\n               data-image-slug=\"mount-kelud-indonesia\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Mount Kelud, Indonesia\"\n                    alt=\"Mount Kelud, Indonesia\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol4.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-8\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol7.jpg\"\n               title=\"Two craters top the summit of this gently smoking volcano. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol7.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol7.jpg\"\n               data-image-id=\"22\"\n               data-title=\"Manam, Papua New Guinea\"\n               data-description=\"Two craters top the summit of this gently smoking volcano. Image: Olivier Grunewald.\"\n               data-image-slug=\"manam-papua-new-guinea\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Manam, Papua New Guinea\"\n                    alt=\"Manam, Papua New Guinea\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol7.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-9\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol8.jpg\"\n               title=\"Two plumes of superheated steam escape from a crack in a lava lake on the summit. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol8.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol8.jpg\"\n               data-image-id=\"23\"\n               data-title=\"Mount Avachinsky, Russia\"\n               data-description=\"Two plumes of superheated steam escape from a crack in a lava lake on the summit. Image: Olivier Grunewald.\"\n               data-image-slug=\"mount-avachinsky-russia\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Mount Avachinsky, Russia\"\n                    alt=\"Mount Avachinsky, Russia\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol8.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\t\t<div id=\"ngg-image-10\" class=\"ngg-gallery-thumbnail-box\" >\n\t\t\t\t        <div class=\"ngg-gallery-thumbnail\">\n            <a href=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol9.jpg\"\n               title=\"Pahoehoe lava, as shown in this image, is formed from the movement of molten liquid congealing beneath a pliable surface crust. Image: Olivier Grunewald.\"\n               data-src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/vol9.jpg\"\n               data-thumbnail=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol9.jpg\"\n               data-image-id=\"24\"\n               data-title=\"Molton waves, Hawaii\"\n               data-description=\"Pahoehoe lava, as shown in this image, is formed from the movement of molten liquid congealing beneath a pliable surface crust. Image: Olivier Grunewald.\"\n               data-image-slug=\"molton-waves-hawaii\"\n               class=\"shutterset_9e165d481ce8c29e66c7035e5a3793c4\">\n                <img\n                    title=\"Molton waves, Hawaii\"\n                    alt=\"Molton waves, Hawaii\"\n                    src=\"https:\/\/scienceillustrated.com.au\/blog\/wp-content\/gallery\/mouths-of-the-earth\/thumbs\/thumbs_vol9.jpg\"\n                    width=\"100\"\n                    height=\"75\"\n                    style=\"max-width:100%;\"\n                \/>\n            <\/a>\n        <\/div>\n\t\t\t\t\t\t\t<\/div> \n\t\t\t\n        \n\t\t\n\t\t<!-- Pagination -->\n\t<div class='ngg-clear'><\/div>\t<\/div>\n<\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":13,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[113],"tags":[],"class_list":["post-506","post","type-post","status-publish","format-standard","hentry","category-galleries"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts\/506"}],"collection":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/users\/13"}],"replies":[{"embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/comments?post=506"}],"version-history":[{"count":0,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/posts\/506\/revisions"}],"wp:attachment":[{"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/media?parent=506"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/categories?post=506"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/scienceillustrated.com.au\/blog\/wp-json\/wp\/v2\/tags?post=506"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}