Earth Science — The Rock Cycle
Magma through igneous, sedimentary and metamorphic rock and back, with the short-cuts across the ring, the texture evidence for cooling rate, and typical time-scales.
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{
"nodes": [
{
"id": "rc-magma",
"type": "gas-flame",
"label": "Magma — silicate melt at 700–1300 °C",
"x": 620,
"y": 60,
"width": 240,
"height": 117,
"fill": "#fee2e2",
"stroke": "#b91c1c"
},
{
"id": "rc-extrusive",
"type": "volcano",
"label": "Extrusive igneous — lava quenched at the surface: basalt, rhyolite, obsidian",
"x": 1180,
"y": 60,
"width": 240,
"height": 117,
"fill": "#fef3c7",
"stroke": "#b45309"
},
{
"id": "rc-subduction",
"type": "arrow-right",
"label": "Subduction & crustal thickening — the tectonic driver of melting",
"x": 60,
"y": 235,
"width": 240,
"height": 117,
"fill": "#ede9fe",
"stroke": "#6d28d9"
},
{
"id": "rc-intrusive",
"type": "iso-cube",
"label": "Intrusive igneous — magma crystallising at depth: granite, gabbro",
"x": 1180,
"y": 235,
"width": 240,
"height": 117,
"fill": "#fef3c7",
"stroke": "#b45309"
},
{
"id": "rc-texture",
"type": "note",
"label": "Texture records the cooling rate: coarse interlocking crystals mean slow cooling kilometres down; glass means the melt was quenched in minutes.",
"x": 620,
"y": 235,
"width": 240,
"height": 117,
"fill": "#fef9c3",
"stroke": "#ca8a04"
},
{
"id": "rc-melting",
"type": "gas-flame",
"label": "Partial melting — above roughly 650 °C, and lower still with water present",
"x": 60,
"y": 410,
"width": 240,
"height": 117,
"fill": "#fef3c7",
"stroke": "#b45309"
},
{
"id": "rc-shortcuts",
"type": "note",
"label": "Any rock can become any other. The short-cuts across the ring — igneous straight to metamorphic, sedimentary straight back to magma — are as common as the full circuit.",
"x": 620,
"y": 410,
"width": 240,
"height": 117,
"fill": "#fef9c3",
"stroke": "#ca8a04"
},
{
"id": "rc-uplift",
"type": "mountain",
"label": "Uplift & unroofing — brings deep rock to the surface to be attacked",
"x": 1180,
"y": 410,
"width": 240,
"height": 117,
"fill": "#ede9fe",
"stroke": "#6d28d9"
},
{
"id": "rc-metamorphic",
"type": "layers",
"label": "Metamorphic rock — slate → schist → gneiss; limestone → marble",
"x": 60,
"y": 585,
"width": 240,
"height": 117,
"fill": "#dbeafe",
"stroke": "#1d4ed8"
},
{
"id": "rc-time",
"type": "note",
"label": "Time-scales: lithification 10³–10⁶ years, regional metamorphism 10⁶–10⁷ years, a full circuit of the cycle 10⁸ years or more.",
"x": 620,
"y": 585,
"width": 240,
"height": 117,
"fill": "#fef9c3",
"stroke": "#ca8a04"
},
{
"id": "rc-weathering",
"type": "rain-cloud",
"label": "Weathering & erosion — frost, rain, acids, roots",
"x": 1180,
"y": 585,
"width": 240,
"height": 117,
"fill": "#fef3c7",
"stroke": "#b45309"
},
{
"id": "rc-metamorphism",
"type": "rect",
"label": "Heat & pressure — burial below ~5 km, or contact with an intrusion",
"x": 60,
"y": 760,
"width": 240,
"height": 117,
"fill": "#ede9fe",
"stroke": "#6d28d9"
},
{
"id": "rc-sedimentary",
"type": "stacked-cylinder",
"label": "Sedimentary rock — sandstone, shale, limestone; the only rocks with fossils",
"x": 620,
"y": 760,
"width": 240,
"height": 117,
"fill": "#dbeafe",
"stroke": "#1d4ed8"
},
{
"id": "rc-sediment",
"type": "layers",
"label": "Sediment — gravel, sand, silt, clay, plus shells and dissolved salts",
"x": 1180,
"y": 760,
"width": 240,
"height": 117,
"fill": "#dbeafe",
"stroke": "#1d4ed8"
}
],
"edges": [
{
"id": "rc-e1",
"source": "rc-magma",
"target": "rc-extrusive",
"label": "erupts as lava, quenched"
},
{
"id": "rc-e2",
"source": "rc-magma",
"target": "rc-intrusive",
"label": "cools slowly at depth"
},
{
"id": "rc-e3",
"source": "rc-intrusive",
"target": "rc-uplift",
"label": "must be uplifted and unroofed first"
},
{
"id": "rc-e4",
"source": "rc-uplift",
"target": "rc-weathering"
},
{
"id": "rc-e5",
"source": "rc-extrusive",
"target": "rc-weathering",
"label": "already exposed"
},
{
"id": "rc-e6",
"source": "rc-weathering",
"target": "rc-sediment",
"label": "transport by rivers, wind and ice"
},
{
"id": "rc-e7",
"source": "rc-sediment",
"target": "rc-sedimentary",
"label": "burial, compaction & cementation"
},
{
"id": "rc-e8",
"source": "rc-sedimentary",
"target": "rc-metamorphism"
},
{
"id": "rc-e9",
"source": "rc-metamorphism",
"target": "rc-metamorphic",
"label": "recrystallises in the solid state"
},
{
"id": "rc-e10",
"source": "rc-metamorphic",
"target": "rc-melting"
},
{
"id": "rc-e11",
"source": "rc-melting",
"target": "rc-magma"
},
{
"id": "rc-e12",
"source": "rc-subduction",
"target": "rc-melting",
"label": "water lowers the solidus"
},
{
"id": "rc-e13",
"source": "rc-intrusive",
"target": "rc-metamorphism",
"label": "short-cut: igneous rock metamorphoses too"
},
{
"id": "rc-e14",
"source": "rc-metamorphic",
"target": "rc-weathering",
"label": "short-cut: uplifted gneiss weathers like anything else"
},
{
"id": "rc-e15",
"source": "rc-sedimentary",
"target": "rc-melting",
"label": "short-cut: subducted sediment melts"
}
]
}