{ "currentVersion": 11.3, "cimVersion": "3.3.0", "id": 7, "name": "Geologic units 2m", "type": "Feature Layer", "description": "", "geometryType": "esriGeometryPolygon", "sourceSpatialReference": { "wkid": 32636, "latestWkid": 32636, "xyTolerance": 0.0012134012154638248, "zTolerance": 0.001, "mTolerance": 0.001, "falseX": -5120899.999617771, "falseY": -9998099.999678822, "xyUnits": 6593.0377339716, "falseZ": -100000, "zUnits": 10000, "falseM": -100000, "mUnits": 10000 }, "copyrightText": "", "parentLayer": { "id": 5, "name": "Geology 2 Million scale" }, "subLayers": [], "minScale": 0, "maxScale": 0, "referenceScale": 0.0, "drawingInfo": { "renderer": { "type": "uniqueValue", "field1": "descriptio", "uniqueValueGroups": [ { "heading": "descriptio", "classes": [ { "label": " ", "description": " ", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 255, 255, 255, 0 ], "outline": null }, "values": [ [ " " ] ] }, { "label": "CARBONIFEROUS-Uppermost dolomites (40 m thick ) and clastics of Umm Bogma Formation in central and western Sinai and clastics of the west coast of Gulf of Suez and the 'Uweinat area", "description": "CARBONIFEROUS-Uppermost dolomites (40 m thick ) and clastics of Umm Bogma Formation in central and western Sinai and clastics of the west coast of Gulf of Suez and the 'Uweinat area", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 63, 162, 171, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "CARBONIFEROUS-Uppermost dolomites (40 m thick ) and clastics of Umm Bogma Formation in central and western Sinai and clastics of the west coast of Gulf of Suez and the 'Uweinat area" ] ] }, { "label": "CENOMANIAN AND TURONIAN- Clastics with thin carbonates at Bahariya , Abu Rawash , El Galalas , Wadi Qena and north and central Sinai . Clastic material dominates at base and carbonate at top", "description": "CENOMANIAN AND TURONIAN- Clastics with thin carbonates at Bahariya , Abu Rawash , El Galalas , Wadi Qena and north and central Sinai . Clastic material dominates at base and carbonate at top", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 111, 73, 133, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "CENOMANIAN AND TURONIAN- Clastics with thin carbonates at Bahariya , Abu Rawash , El Galalas , Wadi Qena and north and central Sinai . Clastic material dominates at base and carbonate at top" ] ] }, { "label": "CLCARENITE BARS - Along the Mediterranean coast", "description": "CLCARENITE BARS - Along the Mediterranean coast", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 103, 54, 143, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "CLCARENITE BARS - Along the Mediterranean coast" ] ] }, { "label": "DOKHAN VOLCANICS -Slightly metamorphosed andesite, porphyrite, pyroclastics, and the purple-coloured Imperil porphyry", "description": "DOKHAN VOLCANICS -Slightly metamorphosed andesite, porphyrite, pyroclastics, and the purple-coloured Imperil porphyry", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 83, 92, 230, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "DOKHAN VOLCANICS -Slightly metamorphosed andesite, porphyrite, pyroclastics, and the purple-coloured Imperil porphyry" ] ] }, { "label": "EOCENE rocks ( Te ) and the underlying Paleocene rocks ( Tp ) along the Red sea coast are grouped together and labeled T, owing to the complexity of data", "description": "EOCENE rocks ( Te ) and the underlying Paleocene rocks ( Tp ) along the Red sea coast are grouped together and labeled T, owing to the complexity of data", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 169, 191, 109, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "EOCENE rocks ( Te ) and the underlying Paleocene rocks ( Tp ) along the Red sea coast are grouped together and labeled T, owing to the complexity of data" ] ] }, { "label": "EOCENE - Thick marine limestone with chert and minor clay beds form high cliffs and plateaux overlooking the Nile between Esna and Cairo The limestone is partly exposed along the Sin el-kaddab scarp and further west where it forms most of the plateau to", "description": "EOCENE - Thick marine limestone with chert and minor clay beds form high cliffs and plateaux overlooking the Nile between Esna and Cairo The limestone is partly exposed along the Sin el-kaddab scarp and further west where it forms most of the plateau to", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 247, 181, 161, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "EOCENE - Thick marine limestone with chert and minor clay beds form high cliffs and plateaux overlooking the Nile between Esna and Cairo The limestone is partly exposed along the Sin el-kaddab scarp and further west where it forms most of the plateau to" ] ] }, { "label": "EXTRUSIVE ROCKS-Basalt -dolerite dykes and sheets mainly of Tertiary age. Some extrusives in the Gulf of Suze area are of Mesozoic age whereas those in the Nubian Desert are of Quaternary age", "description": "EXTRUSIVE ROCKS-Basalt -dolerite dykes and sheets mainly of Tertiary age. Some extrusives in the Gulf of Suze area are of Mesozoic age whereas those in the Nubian Desert are of Quaternary age", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 143, 227, 198, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "EXTRUSIVE ROCKS-Basalt -dolerite dykes and sheets mainly of Tertiary age. Some extrusives in the Gulf of Suze area are of Mesozoic age whereas those in the Nubian Desert are of Quaternary age" ] ] }, { "label": "GABBRO Fresh oilvine gabbro, norite, and troctolite", "description": "GABBRO Fresh oilvine gabbro, norite, and troctolite", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 138, 59, 112, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "GABBRO Fresh oilvine gabbro, norite, and troctolite" ] ] }, { "label": "GEOSYNCLINAL METAVOLCANICS - Fissure eruptions of surface or submarine effusives represented by regionally metamorphosed rhyolite, dacite, andesite, basalt, and py- roclastic rocks", "description": "GEOSYNCLINAL METAVOLCANICS - Fissure eruptions of surface or submarine effusives represented by regionally metamorphosed rhyolite, dacite, andesite, basalt, and py- roclastic rocks", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 161, 84, 168, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "GEOSYNCLINAL METAVOLCANICS - Fissure eruptions of surface or submarine effusives represented by regionally metamorphosed rhyolite, dacite, andesite, basalt, and py- roclastic rocks" ] ] }, { "label": "GEOSYNCLINAL METSEDIMENTS - A wide range of lithological types including hornblende, biotite, and chlor- ite schists, metagreywacke, metamudatone, phyllite, slate, and some conglomerate", "description": "GEOSYNCLINAL METSEDIMENTS - A wide range of lithological types including hornblende, biotite, and chlor- ite schists, metagreywacke, metamudatone, phyllite, slate, and some conglomerate", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 129, 109, 209, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "GEOSYNCLINAL METSEDIMENTS - A wide range of lithological types including hornblende, biotite, and chlor- ite schists, metagreywacke, metamudatone, phyllite, slate, and some conglomerate" ] ] }, { "label": "HAMMAMAT GROUP-Slightly metamorphosed conglomer- ate ( Breccia Verde antico ) , greywacke, arenite and slitstone", "description": "HAMMAMAT GROUP-Slightly metamorphosed conglomer- ate ( Breccia Verde antico ) , greywacke, arenite and slitstone", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 138, 130, 73, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "HAMMAMAT GROUP-Slightly metamorphosed conglomer- ate ( Breccia Verde antico ) , greywacke, arenite and slitstone" ] ] }, { "label": "JURASSIC -Represented by marine and associated fluviomarine beds in northern and central Sinai, the west coast of Gulf of Suze,and the thick clastic section forming the Gilf Kebir in southwestern Egypt; the upper part of this latter section is of Creta", "description": "JURASSIC -Represented by marine and associated fluviomarine beds in northern and central Sinai, the west coast of Gulf of Suze,and the thick clastic section forming the Gilf Kebir in southwestern Egypt; the upper part of this latter section is of Creta", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 237, 163, 83, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "JURASSIC -Represented by marine and associated fluviomarine beds in northern and central Sinai, the west coast of Gulf of Suze,and the thick clastic section forming the Gilf Kebir in southwestern Egypt; the upper part of this latter section is of Creta" ] ] }, { "label": "LOWER CRETACEOUS- Marine fossiliferous beds intercalated within a continental clastic section in northern sinai , west coast of Gulf of Suez, and in Wadi Qena area", "description": "LOWER CRETACEOUS- Marine fossiliferous beds intercalated within a continental clastic section in northern sinai , west coast of Gulf of Suez, and in Wadi Qena area", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 69, 128, 105, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "LOWER CRETACEOUS- Marine fossiliferous beds intercalated within a continental clastic section in northern sinai , west coast of Gulf of Suez, and in Wadi Qena area" ] ] }, { "label": "METAGABBRO-DIORITE COMPLEX - Gabbroid and doler- itic masses, tectonised, uralitised, and affected by Older Granitoids", "description": "METAGABBRO-DIORITE COMPLEX - Gabbroid and doler- itic masses, tectonised, uralitised, and affected by Older Granitoids", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 247, 104, 101, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "METAGABBRO-DIORITE COMPLEX - Gabbroid and doler- itic masses, tectonised, uralitised, and affected by Older Granitoids" ] ] }, { "label": "MIGIF-HAFAFIT GNEISSES AND MIGMATITE - Psam- mitic hornblende and biotite geneisses and migmatite", "description": "MIGIF-HAFAFIT GNEISSES AND MIGMATITE - Psam- mitic hornblende and biotite geneisses and migmatite", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 45, 58, 128, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "MIGIF-HAFAFIT GNEISSES AND MIGMATITE - Psam- mitic hornblende and biotite geneisses and migmatite" ] ] }, { "label": "MIOCENE -Covers most of the Western Desert north of latitude 29°; consists of a basal clastic section overlain by a carbonate unit; along the Gluf of Suez and Red sea coast, clastics ,gypsum and carbonates are dominant, especially in the north", "description": "MIOCENE -Covers most of the Western Desert north of latitude 29°; consists of a basal clastic section overlain by a carbonate unit; along the Gluf of Suez and Red sea coast, clastics ,gypsum and carbonates are dominant, especially in the north", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 130, 184, 232, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "MIOCENE -Covers most of the Western Desert north of latitude 29°; consists of a basal clastic section overlain by a carbonate unit; along the Gluf of Suez and Red sea coast, clastics ,gypsum and carbonates are dominant, especially in the north" ] ] }, { "label": "NILE DEPOSITS - Cultivaled", "description": "NILE DEPOSITS - Cultivaled", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 215, 148, 242, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "NILE DEPOSITS - Cultivaled" ] ] }, { "label": "NUBIA FORMATIOM - Represented in southern and central Egypt by a magnafacies coeval with the Upper Cretaceous marine beds of northern Egypt and is defined by a suite of litho-biostratigraphic units with Duwi or Dakhala at the top and the basement rocks b", "description": "NUBIA FORMATIOM - Represented in southern and central Egypt by a magnafacies coeval with the Upper Cretaceous marine beds of northern Egypt and is defined by a suite of litho-biostratigraphic units with Duwi or Dakhala at the top and the basement rocks b", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 92, 237, 102, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "NUBIA FORMATIOM - Represented in southern and central Egypt by a magnafacies coeval with the Upper Cretaceous marine beds of northern Egypt and is defined by a suite of litho-biostratigraphic units with Duwi or Dakhala at the top and the basement rocks b" ] ] }, { "label": "OLDER GRANITOIDS-Syntetonic to late tectoonic plutonites essentially of granodioritic composition previously refer - red to as Grey Granite ,Shaitian Granite or Older Granite", "description": "OLDER GRANITOIDS-Syntetonic to late tectoonic plutonites essentially of granodioritic composition previously refer - red to as Grey Granite ,Shaitian Granite or Older Granite", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 199, 141, 99, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "OLDER GRANITOIDS-Syntetonic to late tectoonic plutonites essentially of granodioritic composition previously refer - red to as Grey Granite ,Shaitian Granite or Older Granite" ] ] }, { "label": "OLIGOCENE - Fluviatile and lacustrine clastics and gravel sheets between Cairo and Suez, around Cairo and Faiyum, and Bahariya Oasis; conglomerate of Nakheil Formation in Quseir- Safaga stretch and further north. Marl section at foot of the Sallum scar", "description": "OLIGOCENE - Fluviatile and lacustrine clastics and gravel sheets between Cairo and Suez, around Cairo and Faiyum, and Bahariya Oasis; conglomerate of Nakheil Formation in Quseir- Safaga stretch and further north. Marl section at foot of the Sallum scar", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 247, 245, 116, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "OLIGOCENE - Fluviatile and lacustrine clastics and gravel sheets between Cairo and Suez, around Cairo and Faiyum, and Bahariya Oasis; conglomerate of Nakheil Formation in Quseir- Safaga stretch and further north. Marl section at foot of the Sallum scar" ] ] }, { "label": "PALEOCENE- Consists of the lower part of Esna Shale and upper part of Sudr Chalk in northern egypt;and the upper Dakhla , Tarawan , Kurkur and lower Garra beds or their equivalent formations in the middle and southern parts of Egypt", "description": "PALEOCENE- Consists of the lower part of Esna Shale and upper part of Sudr Chalk in northern egypt;and the upper Dakhla , Tarawan , Kurkur and lower Garra beds or their equivalent formations in the middle and southern parts of Egypt", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 57, 158, 55, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "PALEOCENE- Consists of the lower part of Esna Shale and upper part of Sudr Chalk in northern egypt;and the upper Dakhla , Tarawan , Kurkur and lower Garra beds or their equivalent formations in the middle and southern parts of Egypt" ] ] }, { "label": "PLIOCENE -Marine beds of the Nile Valley , Red Sea and Mediterranean coasts; fresh water and spring deposits of the Nile Valley and Western Desert oases; and nonmarine scree deposits outside the Nile Valley", "description": "PLIOCENE -Marine beds of the Nile Valley , Red Sea and Mediterranean coasts; fresh water and spring deposits of the Nile Valley and Western Desert oases; and nonmarine scree deposits outside the Nile Valley", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 133, 194, 79, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "PLIOCENE -Marine beds of the Nile Valley , Red Sea and Mediterranean coasts; fresh water and spring deposits of the Nile Valley and Western Desert oases; and nonmarine scree deposits outside the Nile Valley" ] ] }, { "label": "POST-HAMMAMAT FELSITE Effusive felsite, felsite porphyry and quartz porphyry", "description": "POST-HAMMAMAT FELSITE Effusive felsite, felsite porphyry and quartz porphyry", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 82, 128, 52, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "POST-HAMMAMAT FELSITE Effusive felsite, felsite porphyry and quartz porphyry" ] ] }, { "label": "RING COMPLEXES - Mostly alkaline syenites", "description": "RING COMPLEXES - Mostly alkaline syenites", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 207, 118, 149, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "RING COMPLEXES - Mostly alkaline syenites" ] ] }, { "label": "SABKHA DEPOSITS", "description": "SABKHA DEPOSITS", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 83, 166, 104, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "SABKHA DEPOSITS" ] ] }, { "label": "SAND DUNES", "description": "SAND DUNES", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 93, 99, 158, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "SAND DUNES" ] ] }, { "label": "SERPENTINTE - Serpentinite, talc carbonate, and related rocks", "description": "SERPENTINTE - Serpentinite, talc carbonate, and related rocks", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 146, 159, 247, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "SERPENTINTE - Serpentinite, talc carbonate, and related rocks" ] ] }, { "label": "TRACHYTYPLUGS AND SHEETS", "description": "TRACHYTYPLUGS AND SHEETS", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 156, 62, 64, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "TRACHYTYPLUGS AND SHEETS" ] ] }, { "label": "TRIASSIC- Carbonate / clastic section at Arif el-Naga", "description": "TRIASSIC- Carbonate / clastic section at Arif el-Naga", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 151, 70, 199, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "TRIASSIC- Carbonate / clastic section at Arif el-Naga" ] ] }, { "label": "UNDIFFERENTIATED PALEOZOIC (PRE-CARBONIFEROUS) Clastics below Carboniferous rocks in Gulf of suez area including probable Cambrian beds above the basement rocks in west and central Sinai, Devonian clastics west of Gilf Kebir, and Cambrian-Ordovician cla", "description": "UNDIFFERENTIATED PALEOZOIC (PRE-CARBONIFEROUS) Clastics below Carboniferous rocks in Gulf of suez area including probable Cambrian beds above the basement rocks in west and central Sinai, Devonian clastics west of Gilf Kebir, and Cambrian-Ordovician cla", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 128, 82, 100, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "UNDIFFERENTIATED PALEOZOIC (PRE-CARBONIFEROUS) Clastics below Carboniferous rocks in Gulf of suez area including probable Cambrian beds above the basement rocks in west and central Sinai, Devonian clastics west of Gilf Kebir, and Cambrian-Ordovician cla" ] ] }, { "label": "UNDIVDED QUATERNARY- wadi and playa deposits; raised beaches and corals of the red sea coast", "description": "UNDIVDED QUATERNARY- wadi and playa deposits; raised beaches and corals of the red sea coast", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 150, 242, 85, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "UNDIVDED QUATERNARY- wadi and playa deposits; raised beaches and corals of the red sea coast" ] ] }, { "label": "UNDIVIDED CRETACEOUS - Rocks can be divided in the field , but were grouped together owing to the extreme complexity of data", "description": "UNDIVIDED CRETACEOUS - Rocks can be divided in the field , but were grouped together owing to the extreme complexity of data", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 59, 114, 138, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "UNDIVIDED CRETACEOUS - Rocks can be divided in the field , but were grouped together owing to the extreme complexity of data" ] ] }, { "label": "UPPER PALEOZIC (POST-CARBONIFEROUS )- clastic section overlying Carboniferous beds to the west of Gulf of Suze in the northern part of wadi Qena, and in south central Sinai this section may be either Permain and/or Triassic in age", "description": "UPPER PALEOZIC (POST-CARBONIFEROUS )- clastic section overlying Carboniferous beds to the west of Gulf of Suze in the northern part of wadi Qena, and in south central Sinai this section may be either Permain and/or Triassic in age", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 240, 84, 235, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "UPPER PALEOZIC (POST-CARBONIFEROUS )- clastic section overlying Carboniferous beds to the west of Gulf of Suze in the northern part of wadi Qena, and in south central Sinai this section may be either Permain and/or Triassic in age" ] ] }, { "label": "UPPER CRETACEOUS-clastics , phosphate and carbonate rocks above Nubia Sandstone in the Western Desert, Nile valley, Red sea coast, and wadi Qena ;represented mainly by Duwi Phosphate and lower part of Dakhla Formation In northern Egypt , Abu Rawash , El-", "description": "UPPER CRETACEOUS-clastics , phosphate and carbonate rocks above Nubia Sandstone in the Western Desert, Nile valley, Red sea coast, and wadi Qena ;represented mainly by Duwi Phosphate and lower part of Dakhla Formation In northern Egypt , Abu Rawash , El-", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 133, 87, 64, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "UPPER CRETACEOUS-clastics , phosphate and carbonate rocks above Nubia Sandstone in the Western Desert, Nile valley, Red sea coast, and wadi Qena ;represented mainly by Duwi Phosphate and lower part of Dakhla Formation In northern Egypt , Abu Rawash , El-" ] ] }, { "label": "WADI NATASH VOLCANICS -Dominantly alkaline basalt and andesite", "description": "WADI NATASH VOLCANICS -Dominantly alkaline basalt and andesite", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 224, 90, 168, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "WADI NATASH VOLCANICS -Dominantly alkaline basalt and andesite" ] ] }, { "label": "YOUNGER GRANITOIDS-Gattarian and all post-tectonic granite, granodiorite, and adamellite. The alkali granite masses of Gabal el-Zeit and Gabal Gharib are younger", "description": "YOUNGER GRANITOIDS-Gattarian and all post-tectonic granite, granodiorite, and adamellite. The alkali granite masses of Gabal el-Zeit and Gabal Gharib are younger", "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 108, 245, 158, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "values": [ [ "YOUNGER GRANITOIDS-Gattarian and all post-tectonic granite, granodiorite, and adamellite. The alkali granite masses of Gabal el-Zeit and Gabal Gharib are younger" ] ] } ] } ], "uniqueValueInfos": [ { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 255, 255, 255, 0 ], "outline": null }, "value": " ", "label": " " }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 63, 162, 171, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "CARBONIFEROUS-Uppermost dolomites (40 m thick ) and clastics of Umm Bogma Formation in central and western Sinai and clastics of the west coast of Gulf of Suez and the 'Uweinat area", "label": "CARBONIFEROUS-Uppermost dolomites (40 m thick ) and clastics of Umm Bogma Formation in central and western Sinai and clastics of the west coast of Gulf of Suez and the 'Uweinat area" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 111, 73, 133, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "CENOMANIAN AND TURONIAN- Clastics with thin carbonates at Bahariya , Abu Rawash , El Galalas , Wadi Qena and north and central Sinai . Clastic material dominates at base and carbonate at top", "label": "CENOMANIAN AND TURONIAN- Clastics with thin carbonates at Bahariya , Abu Rawash , El Galalas , Wadi Qena and north and central Sinai . Clastic material dominates at base and carbonate at top" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 103, 54, 143, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "CLCARENITE BARS - Along the Mediterranean coast", "label": "CLCARENITE BARS - Along the Mediterranean coast" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 83, 92, 230, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "DOKHAN VOLCANICS -Slightly metamorphosed andesite, porphyrite, pyroclastics, and the purple-coloured Imperil porphyry", "label": "DOKHAN VOLCANICS -Slightly metamorphosed andesite, porphyrite, pyroclastics, and the purple-coloured Imperil porphyry" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 169, 191, 109, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "EOCENE rocks ( Te ) and the underlying Paleocene rocks ( Tp ) along the Red sea coast are grouped together and labeled T, owing to the complexity of data", "label": "EOCENE rocks ( Te ) and the underlying Paleocene rocks ( Tp ) along the Red sea coast are grouped together and labeled T, owing to the complexity of data" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 247, 181, 161, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "EOCENE - Thick marine limestone with chert and minor clay beds form high cliffs and plateaux overlooking the Nile between Esna and Cairo The limestone is partly exposed along the Sin el-kaddab scarp and further west where it forms most of the plateau to", "label": "EOCENE - Thick marine limestone with chert and minor clay beds form high cliffs and plateaux overlooking the Nile between Esna and Cairo The limestone is partly exposed along the Sin el-kaddab scarp and further west where it forms most of the plateau to" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 143, 227, 198, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "EXTRUSIVE ROCKS-Basalt -dolerite dykes and sheets mainly of Tertiary age. Some extrusives in the Gulf of Suze area are of Mesozoic age whereas those in the Nubian Desert are of Quaternary age", "label": "EXTRUSIVE ROCKS-Basalt -dolerite dykes and sheets mainly of Tertiary age. Some extrusives in the Gulf of Suze area are of Mesozoic age whereas those in the Nubian Desert are of Quaternary age" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 138, 59, 112, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "GABBRO Fresh oilvine gabbro, norite, and troctolite", "label": "GABBRO Fresh oilvine gabbro, norite, and troctolite" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 161, 84, 168, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "GEOSYNCLINAL METAVOLCANICS - Fissure eruptions of surface or submarine effusives represented by regionally metamorphosed rhyolite, dacite, andesite, basalt, and py- roclastic rocks", "label": "GEOSYNCLINAL METAVOLCANICS - Fissure eruptions of surface or submarine effusives represented by regionally metamorphosed rhyolite, dacite, andesite, basalt, and py- roclastic rocks" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 129, 109, 209, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "GEOSYNCLINAL METSEDIMENTS - A wide range of lithological types including hornblende, biotite, and chlor- ite schists, metagreywacke, metamudatone, phyllite, slate, and some conglomerate", "label": "GEOSYNCLINAL METSEDIMENTS - A wide range of lithological types including hornblende, biotite, and chlor- ite schists, metagreywacke, metamudatone, phyllite, slate, and some conglomerate" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 138, 130, 73, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "HAMMAMAT GROUP-Slightly metamorphosed conglomer- ate ( Breccia Verde antico ) , greywacke, arenite and slitstone", "label": "HAMMAMAT GROUP-Slightly metamorphosed conglomer- ate ( Breccia Verde antico ) , greywacke, arenite and slitstone" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 237, 163, 83, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "JURASSIC -Represented by marine and associated fluviomarine beds in northern and central Sinai, the west coast of Gulf of Suze,and the thick clastic section forming the Gilf Kebir in southwestern Egypt; the upper part of this latter section is of Creta", "label": "JURASSIC -Represented by marine and associated fluviomarine beds in northern and central Sinai, the west coast of Gulf of Suze,and the thick clastic section forming the Gilf Kebir in southwestern Egypt; the upper part of this latter section is of Creta" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 69, 128, 105, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "LOWER CRETACEOUS- Marine fossiliferous beds intercalated within a continental clastic section in northern sinai , west coast of Gulf of Suez, and in Wadi Qena area", "label": "LOWER CRETACEOUS- Marine fossiliferous beds intercalated within a continental clastic section in northern sinai , west coast of Gulf of Suez, and in Wadi Qena area" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 247, 104, 101, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "METAGABBRO-DIORITE COMPLEX - Gabbroid and doler- itic masses, tectonised, uralitised, and affected by Older Granitoids", "label": "METAGABBRO-DIORITE COMPLEX - Gabbroid and doler- itic masses, tectonised, uralitised, and affected by Older Granitoids" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 45, 58, 128, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "MIGIF-HAFAFIT GNEISSES AND MIGMATITE - Psam- mitic hornblende and biotite geneisses and migmatite", "label": "MIGIF-HAFAFIT GNEISSES AND MIGMATITE - Psam- mitic hornblende and biotite geneisses and migmatite" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 130, 184, 232, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "MIOCENE -Covers most of the Western Desert north of latitude 29°; consists of a basal clastic section overlain by a carbonate unit; along the Gluf of Suez and Red sea coast, clastics ,gypsum and carbonates are dominant, especially in the north", "label": "MIOCENE -Covers most of the Western Desert north of latitude 29°; consists of a basal clastic section overlain by a carbonate unit; along the Gluf of Suez and Red sea coast, clastics ,gypsum and carbonates are dominant, especially in the north" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 215, 148, 242, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "NILE DEPOSITS - Cultivaled", "label": "NILE DEPOSITS - Cultivaled" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 92, 237, 102, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "NUBIA FORMATIOM - Represented in southern and central Egypt by a magnafacies coeval with the Upper Cretaceous marine beds of northern Egypt and is defined by a suite of litho-biostratigraphic units with Duwi or Dakhala at the top and the basement rocks b", "label": "NUBIA FORMATIOM - Represented in southern and central Egypt by a magnafacies coeval with the Upper Cretaceous marine beds of northern Egypt and is defined by a suite of litho-biostratigraphic units with Duwi or Dakhala at the top and the basement rocks b" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 199, 141, 99, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "OLDER GRANITOIDS-Syntetonic to late tectoonic plutonites essentially of granodioritic composition previously refer - red to as Grey Granite ,Shaitian Granite or Older Granite", "label": "OLDER GRANITOIDS-Syntetonic to late tectoonic plutonites essentially of granodioritic composition previously refer - red to as Grey Granite ,Shaitian Granite or Older Granite" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 247, 245, 116, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "OLIGOCENE - Fluviatile and lacustrine clastics and gravel sheets between Cairo and Suez, around Cairo and Faiyum, and Bahariya Oasis; conglomerate of Nakheil Formation in Quseir- Safaga stretch and further north. Marl section at foot of the Sallum scar", "label": "OLIGOCENE - Fluviatile and lacustrine clastics and gravel sheets between Cairo and Suez, around Cairo and Faiyum, and Bahariya Oasis; conglomerate of Nakheil Formation in Quseir- Safaga stretch and further north. Marl section at foot of the Sallum scar" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 57, 158, 55, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "PALEOCENE- Consists of the lower part of Esna Shale and upper part of Sudr Chalk in northern egypt;and the upper Dakhla , Tarawan , Kurkur and lower Garra beds or their equivalent formations in the middle and southern parts of Egypt", "label": "PALEOCENE- Consists of the lower part of Esna Shale and upper part of Sudr Chalk in northern egypt;and the upper Dakhla , Tarawan , Kurkur and lower Garra beds or their equivalent formations in the middle and southern parts of Egypt" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 133, 194, 79, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "PLIOCENE -Marine beds of the Nile Valley , Red Sea and Mediterranean coasts; fresh water and spring deposits of the Nile Valley and Western Desert oases; and nonmarine scree deposits outside the Nile Valley", "label": "PLIOCENE -Marine beds of the Nile Valley , Red Sea and Mediterranean coasts; fresh water and spring deposits of the Nile Valley and Western Desert oases; and nonmarine scree deposits outside the Nile Valley" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 82, 128, 52, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "POST-HAMMAMAT FELSITE Effusive felsite, felsite porphyry and quartz porphyry", "label": "POST-HAMMAMAT FELSITE Effusive felsite, felsite porphyry and quartz porphyry" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 207, 118, 149, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "RING COMPLEXES - Mostly alkaline syenites", "label": "RING COMPLEXES - Mostly alkaline syenites" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 83, 166, 104, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "SABKHA DEPOSITS", "label": "SABKHA DEPOSITS" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 93, 99, 158, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "SAND DUNES", "label": "SAND DUNES" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 146, 159, 247, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "SERPENTINTE - Serpentinite, talc carbonate, and related rocks", "label": "SERPENTINTE - Serpentinite, talc carbonate, and related rocks" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 156, 62, 64, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "TRACHYTYPLUGS AND SHEETS", "label": "TRACHYTYPLUGS AND SHEETS" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 151, 70, 199, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "TRIASSIC- Carbonate / clastic section at Arif el-Naga", "label": "TRIASSIC- Carbonate / clastic section at Arif el-Naga" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 128, 82, 100, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "UNDIFFERENTIATED PALEOZOIC (PRE-CARBONIFEROUS) Clastics below Carboniferous rocks in Gulf of suez area including probable Cambrian beds above the basement rocks in west and central Sinai, Devonian clastics west of Gilf Kebir, and Cambrian-Ordovician cla", "label": "UNDIFFERENTIATED PALEOZOIC (PRE-CARBONIFEROUS) Clastics below Carboniferous rocks in Gulf of suez area including probable Cambrian beds above the basement rocks in west and central Sinai, Devonian clastics west of Gilf Kebir, and Cambrian-Ordovician cla" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 150, 242, 85, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "UNDIVDED QUATERNARY- wadi and playa deposits; raised beaches and corals of the red sea coast", "label": "UNDIVDED QUATERNARY- wadi and playa deposits; raised beaches and corals of the red sea coast" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 59, 114, 138, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "UNDIVIDED CRETACEOUS - Rocks can be divided in the field , but were grouped together owing to the extreme complexity of data", "label": "UNDIVIDED CRETACEOUS - Rocks can be divided in the field , but were grouped together owing to the extreme complexity of data" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 240, 84, 235, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "UPPER PALEOZIC (POST-CARBONIFEROUS )- clastic section overlying Carboniferous beds to the west of Gulf of Suze in the northern part of wadi Qena, and in south central Sinai this section may be either Permain and/or Triassic in age", "label": "UPPER PALEOZIC (POST-CARBONIFEROUS )- clastic section overlying Carboniferous beds to the west of Gulf of Suze in the northern part of wadi Qena, and in south central Sinai this section may be either Permain and/or Triassic in age" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 133, 87, 64, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "UPPER CRETACEOUS-clastics , phosphate and carbonate rocks above Nubia Sandstone in the Western Desert, Nile valley, Red sea coast, and wadi Qena ;represented mainly by Duwi Phosphate and lower part of Dakhla Formation In northern Egypt , Abu Rawash , El-", "label": "UPPER CRETACEOUS-clastics , phosphate and carbonate rocks above Nubia Sandstone in the Western Desert, Nile valley, Red sea coast, and wadi Qena ;represented mainly by Duwi Phosphate and lower part of Dakhla Formation In northern Egypt , Abu Rawash , El-" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 224, 90, 168, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "WADI NATASH VOLCANICS -Dominantly alkaline basalt and andesite", "label": "WADI NATASH VOLCANICS -Dominantly alkaline basalt and andesite" }, { "symbol": { "type": "esriSFS", "style": "esriSFSSolid", "color": [ 108, 245, 158, 255 ], "outline": { "type": "esriSLS", "style": "esriSLSSolid", "color": [ 110, 110, 110, 255 ], "width": 0.4 } }, "value": "YOUNGER GRANITOIDS-Gattarian and all post-tectonic granite, granodiorite, and adamellite. 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