JSJ  in  the  Field

 

Mt. Lassen volcanic lava (Devastated Area, Lassen Volcano National Park, northeastern California, USA) (above & below) - porphyritic black dacite from the 1915 eruption of Mt. Lassen, a large volcanic dome in the Cascade Range of America's Pacific Northwest.  The block shown below has moderately-developed columnar jointing.

 


 

Aa lava flow of vesicular basalt, basalt, and scoriaceous basalt (erupted about 5075 B.C.), Lava Butte Cinder Cone, Newberry Volcano National Monument, Oregon, USA.

 


 

Glaciated knob of Ellsworth Schist (Cambrian-Ordovician), Agassiz outcrop, Ellsworth Falls, southern Maine, USA.

 


 

Anakeesta Phyllite (Neoproterozoic) with iron oxide staining from chemical weathering of pyrite in the phyllite.  Newfound Gap, Great Smoky Mountains, Appalachian Mountains, ~Tennessee-North Carolina border, USA.

 


 

Anthracite coal (probably from the Mammoth Coal) from the Llewellyn Formation, upper Middle Pennsylvanian at the Pioneer Valley Coal Mine, Ashland, Pennsylvania, USA.

 


 

Anticline, folded Llewellyn Formation (upper Middle Pennsylvanian), Bear Valley Coal Mine, near Shamokin, Pennsylvania, USA.

 


 

Archaeocyathan limestone, Ajax Limestone, Lower Cambrian; Ajax Mine, South Australia.

 


 

View of the Pahranagat Valley from Bactrian Mountain, Mt. Irish Range, southern Nevada, USA.  The rocks in the foreground are limestone of the Guilmette Formation, Upper Devonian.

 


 

Scoriaceous basalt spatter agglomerate (~10,000 years old), Bandera Crater Volcano, Cibola County, northwestern New Mexico, USA.

 


 

Cryogenian-Ediacaran GSSP (global stratotype section and point), Neoproterozoic.  The dark reddish rock below the boundary is a Snowball Earth tillite - the Elatina Formation.  The light brown rock above the boundary is a supergreenhouse climate cap carbonate unit - the Nuccaleena Formation.  Enorama Creek, Brachina Gorge, Flinders Ranges, South Australia.

 


 

Twin Lakes area, Beartooth Mountains, ~Montana-Wyoming border, USA.  The rocks in these mountains are principally Archean-aged metamorphics.

 


 

Long Lake Granite, Neoarchean, 2.74 billion years.  Long Lake area, Beartooth Mountains, ~Montana-Wyoming border, USA.

 


 

Rock Creek Vista Point, Beartooth Mountains, ~Montana-Wyoming border, USA.  The rocks are principally Archean-aged metamorphics.

 


 

Fossiliferous limestones & shales, Bellevue Limestone, Upper Ordovician.  Maysville West roadcut, northeastern Kentucky, USA.

 


 

Beryl Hot Spring, Yellowstone Hotspot, northwestern Wyoming, USA.

 


 

Mastodon skull (fossil elephant), Pleistocene, Big Bone Lick, northern Kentucky, USA.

 


 

Scoriaceous basalt spatter agglomerate, 3300 years old, Black Crater Spatter Cone, Lava Beds National Park, northern California, USA.

 


 

Halite from modern lacustrine evaporite deposit.  Bonneville Salt Flats, Utah, USA.

 


 

Chert nodules in limestone, Casey Member of the Boyle Formation, Middle Devonian.  Drowning Creek West roadcut, eastern Kentucky, USA.

 


 

Bulguksa Granite, formed along a Cretaceous to early Paleogene subduction zone.  Lake Chungju, South Korea.

 


 

Planed-off/eroded stromatolites (layered structures built up by cyanobacterial mats in a shallow marine environment) in the Hoyt Limestone (Upper Cambrian) at Lester Park, New York State, USA.

 


 

Cannonball concretions, Sentinel Butte Formation, Upper Paleocene.  Little Missouri Badlands, North Unit of Roosevelt National Park, western North Dakota, USA.

 


 

Cross-bedded quartzose sandstones with hematite staining & desert varnish, De Chelly Sandstone, Lower Permian.  Canyon de Chelly, northeastern Arizona, USA.

 


 

Canyon Diablo Octahedrite, an iron-nickel meteorite principally composed of the Fe-Ni alloy minerals kamacite & taenite.  This is a core fragment from a now-disrupted differentiated asteroid in the Asteroid Belt (between Mars & Jupiter), 4.55 billion years.  Barringer Crater area, Arizona, USA (on display at Chicago's Field Museum of Natural History).

 


 

Carbonatite ("igneous limestone"), Magnet Cove Complex, mid-Cretaceous, 96-102 million years.  Cove Creek roadcut, Hot Spring County, central Arkansas, USA.

 


 

Travertine speleothem, Carlsbad Caverns, New Mexico, USA.

 


 

Castellate weathering, Sentinel Butte Formation, Upper Paleocene.  Little Missouri Badlands, North Unit of Roosevelt National Park, western North Dakota, USA.

 


 

Banded gypsum-calcite rock, Castile Formation, uppermost Upper Permian, 251 million years.  State Line outcrop, Rt. 180/Rt. 62 at the New Mexico-Texas border, USA.

 


 

Sulfur-bearing "minerals" near vent in the interception trench of the Centralia coal fire, Pennsylvania, USA.

 


 

Clinch Quartzite (Lower Silurian) along Rt. 460 roadcut at the Narrows of the New River, Appalachian Mountains, Giles County, Virginia, USA.

 


 

Clinker bed from naturally-burned lignite coal, Sentinel Butte Formation, Upper Paleocene.  Coal Vein Trail, South Unit of Roosevelt National Park, western North Dakota, USA.

 


 

Collecting fossil fish in the Split Fish Layer, Fossil Butte Member, Green River Formation, Lower Eocene.  Commercial quarry near Kemmerer, southwestern Wyoming, USA.

 


 

Snorkeling over a Thalassia-Syringodium seagrass bed on the western side of North Point Peninsula, San Salvador Island, eastern Bahamas.

 


 

Pegmatitic granite (K-feldspar, quartz, muscovite mica) & graphic granite, Eight Mile Park Pegmatite District (Mesoproterozoic, ~1.430-1.474 b.y.), outcrop along 3A Road, north of Royal Gorge Bridge, west of Canon City, south-central Colorado, USA.

 


 

Collecting biotite & muscovite mica from pegmatitic granite, Ruggles Pegmatite, Devonian.  Ruggles Pegmatite Mine, southern New Hampshire, USA.

 


 

Huge K-feldspar crystal in the Ruggles Pegmatite, Devonian.  Ruggles Pegmatite Mine, southern New Hampshire, USA.

 


 

Collecting trilobites and other fossils in black shales of the lower Jigunsan Formation (Ordovician) in the Seokgaejae section, southern Gangwon South Province, South Korea.

 


 

Native copper with greenish malachite coating recovered from the floor of Lake Superior, derived from the Portage Lake Volcanic Series, Upper Peninsula of Michigan, USA.  The copper mineralization age is 1.05 to 1.06 billion years (late Mesoproterozoic).  Displayed at the Quincy Mine in Michigan, USA.

 


 

Copper Creek Thrust Fault with folded Rome Formation limestones (Middle Cambrian) in the hanging wall (upper right) and tilted Moccasin Formation limestones (Middle Ordovician) in the footwall (lower left).  Thorn Hill section, northeastern Tennessee, USA.

 


 

Diabase dike intruding the Ruggles Pegmatite at Ruggles Pegmatite Mine, southern New Hampshire, USA.

 


 

Femur from a Diplodocus sauropod dinosaur, Upper Jurassic, western USA.  On display at Carnegie Museum of Natural History in Pittsburgh, Pennsylvania, USA.

 


 

Drake Well (Earth's first deliberately-drilled oil well, 1859) along Oil Creek near Titusville, northwestern Pennsylvania, USA.  Crude oil came from a shale-encased sandstone body in the lower Riceville Formation, Upper Devonian.

 


 

Lake Tahoe, Sierra Nevada Mountains, ~Nevada-California border, USA.  The rocks all around Lake Tahoe are part of the Sierra Nevada Batholith, a Cretaceous-aged granite formed underneath an ancient volcanic arc along a subduction zone.

 


 

Tidalites (finely-laminated sediments deposited in a very shallow water, tidally-influenced marine environment) in the Elatina Formation (upper Cryogenian, middle Neoproterozoic).  Pichi Richi Pass, South Flinders Ranges, South Australia.

 


 

Emu Bay Lagerstätte (soft-bodied fossil deposit), Emu Bay Shale, Lower Cambrian.  Big Gully, Kangaroo Island, offshore South Australia.

 


 

Fault in cupriferous felsite conglomerate, Allouez Conglomerate, Portage Lake Volcanic Series, upper Mesoproterozoic, 1.094 billion years.  1st level, Delaware Copper Mine, Keweenaw Peninsula, Upper Peninsula of Michigan, USA.

 


 

Fossiliferous limestone slabs derived from the upper Richmondian Stage, Upper Ordovician.  Flat Fork, Caesar Creek Lake State Park, southwestern Ohio, USA.

 


 

Folded Middle Ordovician limestones just south of the St. Clair Thrust Fault.  Rt. 460 roadcut, Narrows of the New River, Appalachian Mountains, Giles County, Virginia, USA.

 


 

Permineralized fossil tree trunk, probably from the Paleocene of western North Dakota, USA.

 


 

Shale-filled fossil tree stump, Kanawha Formation, Middle Pennsylvanian.  Interstate-64 roadcut at milepost 83 tollbooth, Kanawha County, West Virginia, USA.

 


 

Large glacial erratic deposited by Pleistocene glaciation, near summit of Cadillac Mountain, Acadia National Park, southern coastal Maine, USA.

 


 

Goosenecks of the San Juan River - the classic example of entrenched meanders, southern Utah, USA.  The rocks walls are Honaker Trail Formation and Paradox Formation (both Pennsylvanian).

 


 

Grand Canyon, northern Arizona, USA.  The lower gray slope consists of three Cambrian-aged units - Tapeats Sandstone, Bright Angel Shale, and the Muav Limestone.  The reddish cliff above that is the Redwall Limestone (Mississippian).  The reddish cliffy-slopes above that represent the Supai Group (Pennsylvanian).  The whitish cliff above that is the Coconino Sandstone (Permian).

 


 

Small-scale fold in reddish argillites of the Grinnell Formation, Mesoproterozoic, ~1.45 billion years, Glacier National Park, Montana, USA.

 


 

Argillite conglomerate & mud-chip breccia in the Grinnell Formation, Mesoproterozoic, ~1.45 billion years, Glacier National Park, Montana, USA.

 


 

Horizontal fault (at hand level) in Middle Ordovician limestones.  Rt. 100 roadcut in Pearisburg, Giles County, Virginia, USA.

 


 

Undercut cliffs of Corbin Sandstone (Middle Pennsylvanian) near Indian Staircase, Red River Gorge, eastern Kentucky, USA.

 


 

Jaspilite (banded iron formation), Negaunee Iron-Formation, Mesoproterozoic, 2.11 billion years (or 1.874 billion years).  Jasper Knob, Ishpeming, Upper Peninsula of Michigan, USA.

 


 

Diamondiferous lamproite rocks, Prairie Creek Lamproite, Early Cretaceous, 106 million years.  Crater of Diamonds, Pike County, Arkansas, USA.

 


 

Iguanodontid dinosaur tracks on tilted sandstone bedding plane, Dakota Sandstone, Cretaceous; Dinosaur Ridge, near Denver, Colorado, USA.

 


 

Weathered magnesiocarbonatites, Iron Hill Carbonatite Complex, late Neoproterozoic, ~570 million years.  Iron Hill, southeast of Powderhorn, southwestern Colorado, USA.  Magnesiocarbonatites are dolomitic intrusive igneous rocks.

 


 

Cretaceous-Tertiary ("K-T") boundary clay (65 million years) in a coal bed.  The K-T boundary clay represents fallout from the impact event that caused a mass extinction of dinosaurs and many other organisms.  Long Canyon Road, south of Trinidad Lake, southern Colorado, USA.

 


 

Fossil palm fronds in sandstone, Laramie Formation, upper Upper Cretaceous; Parfet Prehistoric Preserve, Golden, Colorado, USA.

 


 

Precambrian-Pennsylvanian nonconformity at Red Rocks Amphitheater, near Denver, Colorado, USA.  Rocks below right hand are granitic gneisses and migmatites of the Idaho Springs Formation (late Paleoproterozoic, 1.7 billion years).  Rocks above are tilted, hematite-rich conglomerates, arkoses, and sandstones of the Fountain Formation (Pennsylvanian).  1.4 billion years of missing time are repesented by this unconformity.

 


 

Summit of Pikes Peak, Colorado, USA.  Rocks in the foreground at bottom are granites of the Pikes Peak Batholith, late Mesoproterozoic, 1.08 billion years.

 


 

Radioactive dinosaur bone (dark structure in the rock), fluvial sandstone in the Westwater Member of the Morrison Formation, middle Upper Jurassic.  Dinosaur Ridge, near Denver, Colorado, USA.  Dinosaur bones are common in this sandstone unit - they have been partially permineralized/replaced by the radioactive, uranium-bearing mineral carnotite.  Scintillometer reading on a bone here: 422 counts per minute (cf. background reading of 140 cpm).

 


 

Sauropod dinosaur footprint bulge in sandstone, upper Morrison Formation, Upper Jurassic.  Dinosaur Ridge, near Denver, Colorado, USA.

 


 

Uranium roll front in Dakota Sandstone, Cretaceous; Turkey Creek Road, near Denver, Colorado, USA.  Uranium compounds are relatively mobile and move through permeable rocks while dissolved in fluids.  The black stuff is uraninite (UO2).  There's other uranium minerals here, too.  The U is ultimately coming from nearby pegmatitic granites.  A reading on this roll front shows it can emit 33,000 counts per minute radiation.

 


  

Lena Pillars in Siberia.  The rocks are fossiliferous limestones of the upper Perekhod Formation, upper Lower Cambrian.  Ulakhan-Kyyry-Taas section, southern side of the Lena River, across from At-Daban, eastern Siberia.

 


 

Pumice/pumiceous rhyolite, Big Obsidian Flow, erupted 700 A.D., Newberry Volcano National Monument, Oregon, USA.

 


 

Obsidian, Big Obsidian Flow, erupted 700 A.D., Newberry Volcano National Monument, Oregon, USA.

 


 

Paleocene-aged sedimentary rocks, Little Missouri Badlands, western North Dakota, USA.  The reddish-brown areas in the valley are clinker beds (naturally burned-out lignite coal horizons).

 


 

Metanorthosite, Marcy Anorthosite, late Mesoproterozoic, 1.155 billion years.  Jay Dome, Adirondack Mountains, New York State, USA.

 


 

Barringer Crater (aka Meteor Crater) in northern Arizona, USA.  This hole formed ~49,000 years ago by the impact of the Canyon Diablo Octahedrite, a 4.55 billion year old, iron-nickel meteorite derived from the Asteroid Belt between Mars and Jupiter.

 


 

Fossiliferous limestones of the lower Bird Spring Formation.  The geology hammer handle is pointing to the Mississippian-Pennsylvanian boundary.  This site is the GSSP (global stratotype section and point) for the Miss.-Penn. boundary.  Arrow Canyon, southern Nevada, USA.

 


 

Ordovician fossiliferous limestones nonconformably resting atop Proterozoic-aged gneiss.  Montmorency Promontory, north of Montmorency Falls, Quebec City, Quebec, Canada.  The fossiliferous limestones are relatively rich in a fossil traditionally called Solenopora, which is traditionally interpreted as a fossil rhodophyte (red alga).  This unit is the Solenopora Gravels, Trenton Group, upper Middle Ordovician.

 


 

Large-scale mudcracks in vertical beds of the ABC Range Quartzite (lower Ediacaran, upper Neoproterozoic).  Pichi Richi Pass railroad cut, South Flinders Ranges, South Australia.

 


 

Muir Beach (eastern coast of the North Pacific Basin), north of San Francisco, central California, USA.

 


 

NASA Ames Base, Moffet Field, central California, USA.  This equipment runs MARSWIT, the world's only wind tunnel that can be operated at Martian surface atmospheric conditions.  It was formerly a test chamber for the Saturn V rocket.

 


 

Vanport Flint ("Flint Ridge Flint"), upper Middle Pennsylvanian.  Nethers Flint Quarries, eastern Flint Ridge, east-central Ohio, USA.

 


 

Niagara Falls & Niagara Escarpment, New York State-Ontario border.

 


 

Novaculite (variably microporous metachert), Arkansas Novaculite, Devonian-Mississippian.  Hot Springs Mountain Anticline, ZigZag Mountains, Arkansas, USA.

 


 

Crude oil derived from Upper Cambrian porous dolostones (sandy?) at & just below the Knox Unconformity at ~2404-2410 feet below the surface.  Oil well a little southwest of Westfall, southern Pickaway County, central Ohio, USA.

 


 

Cadillac Mountain Granite, Devonian.  Otter Cliff, Mt. Desert Island, Acadia National Park, southern coastal Maine, USA.

 


 

Variably colored shales of the Petrified Forest Member of the Chinle Formation (Upper Triassic).  Painted Desert, Petrified Forest National Park, Arizona, USA.

 


 

Precambrian-Cambrian boundary, Mernmerna section, eastern side of the Three Sisters Range, South Australia.  The blackened bedding plane represents the Precambrian-Cambrian boundary, which at this locality is a minor disconformity (missing time).  The rocks to the right are part of the Rawnsley Quartzite (upper Ediacaran, uppermost Neoproterozoic).  The rocks to the left are part of the Parachilna Formation (lower Lower Cambrian).  The first complex trace fossils appear in the basal Parachilna beds here.

 


 

Permineralized fossil log of Araucarioxylon arizonicum in the Chinle Formation (Upper Triassic) at Crystal Forest, Petrified Forest National Park, Arizona, USA.

 


 

Saprolite (extremely friable, extremely weathered Proterozoic-aged gneiss) from Pine Ridge West quarry, Appalachian Mountains, Surry County, northwestern North Carolina, USA.

 


 

Pseudocolumnar jointing (in interval at ~hip level) in Paleocene sedimentary rocks produced by an ancient lignite coal fire.  South Unit of Roosevelt National Park, western North Dakota, USA.

 


 

U-shaped glacial valley incised in Mesoproterozoic Belt Supergroup rocks (1.40 to 1.47 billion years).  Reynolds Creek overlook, Glacier National Park, northwestern Montana, USA.

 


 

Shatter Zone tectonic breccia, Devonian.  Sand Beach, Mt. Desert Island, Acadia National Park, southern coastal Maine, USA.

 


 

Sky Bridge, a natural arch developed in the Corbin Sandstone, a Middle Pennsylvanian fluvial deposit.  Red River Gorge, eastern Kentucky, USA.

 


 

Specularite (micaceous hematite schist) from the Negaunee Iron-Formation, Paleoproterozoic, 2.11 billion years (or 1.874 billion years). Champion Mine, Upper Peninsula of Michigan, USA.

 


 

Large columnar thrombolites in bioherm at the top of the Wirrealpa Limestone (upper Lower Cambrian), ~200 meters north of the Blinman-Wirrealpa road near Old Wirrealpa Mine, Flinders Ranges, South Australia.  Thrombolites are similar to stromatolites, in that they are bacterial buildups.  Internally, stromatolites are thinly laminated.  Thrombolites have a clotted internal texture.

 


 

Spattering mudpot, Sulfur Works Hydrothermal Area, Mt. Lassen National Park, Cascade Range, northern California, USA.

 


 

Swiftcurrent Falls, Many Glacier area, Glacier National Park, Montana, USA.  The rocks are sandy dolostones of the Altyn Formation, Belt Supergroup, Mesoproterozoic, 1.40 to 1.47 billion years.

 


 

 

Tree molds of ponderosa pines surrounded by vesicular basalts & scoriaceous basalts of the Lava Cast Forest Flow (erupted ~5260 B.C.).  Lava Cast Forest, Newberry Volcano National Monument, Oregon, USA.

 


 

White River Badlands, western South Dakota, USA.  Rocks are differentially eroded siliciclastic sedimentary rocks of the White River Group (Oligocene).

 


 

Xiaxia Limestone (Permian) at Yangshan, near Nanjing, eastern China.

 


 

Bandelier Tuff (lower to middle Lower Pleistocene, 1.25-1.61 m.y.) exposed to the southwest of the town of White Rock, northern New Mexico, USA.  ~Neck-level & downward - ash-flow volcanic tuffs of the Otowi Member (1.61 m.y.); thin, gray bed at head-level - Tsankawi Pumice Bed, basal Tshirege Member (1.25 m.y.); thick, whitish interval above head-level - ash-flow volcanic tuffs of the Tshirege Member (1.25 m.y.).

 


 

Wall of rose quartz, derived from Colorado pegmatitic granite, at Royal Gorge Bridge, west of Canon City, south-central Colorado, USA.

 


 

Triceratops dinosaur footprint (Animalia, Vertebrata, Dinosauria, Ceratopsia) on underside of sandstone bed, Laramie Formation, upper Upper Cretaceous; Parfet Prehistoric Preserve, Golden, Colorado, USA.

 


 

Molybdenum ore - porphyritic alkalic granite (Climax Stock, Oligocene, 24-33 m.y.) having vein of silvery-gray colored molybdenite (MoS2); Climax Mine, Lake County, central Colorado, USA.

 


 

Cold Shivers Point along Columbus Canyon, Colorado National Monument, western Colorado, USA.  The ~vertical sandstone cliffs in the foreground & background are eolian, quartzose sandstones of the Wingate Sandstone (Lower Jurassic).  The maroon shales below that (see lower left & above my head) are part of the Chinle Formation (Upper Triassic), representing floodplain mud deposition.  Thin-bedded, light-colored, fluvial, quartzose sandstones of the Kayenta Sandstone (Lower Jurassic) make up the partly vegetated areas at top, above the cliff-forming Wingate Ss.  The dark gray rocks below the Chinle Fm. (see just above my shoulder) are Precambrian basement rocks of the Black Canyon Formation (late Paleoproterozoic, 1.7 b.y.) consisting of gneisses, schists, migmatites, and granite dikes.

 


 

Injection gneisses of the Black Canyon Formation (1.74 b.y., intruded by 1.36 b.y. pegmatitic granite dikes); Gunnison Point overlook, Black Canyon of the Gunnison, western Colorado, USA.

 


 

Large talus block (left) & in-situ vertical beds (right) of the Dakota Sandstone (Albian Stage, upper Lower Cretaceous), Dakota Sandstone Hogback at Stonewall, southern Colorado, USA.

 


 

Injection gneisses of the Black Canyon Formation (1.74 b.y., intruded by 1.36 b.y. pegmatitic granite dikes); Pulpit Rock overlook, Black Canyon of the Gunnison, western Colorado, USA.

 


 

1.74 billion year old gneiss (~triangular-shaped block of foliated material at lower left) in 1.48 billion year old Vernal Mesa Quartz Monzonite (Mesoproterozoic).  Outcrop at Chasm View overlook, Black Canyon of the Gunnison, western Colorado, USA.

 


 

Soda Dam (above & below - be sure to scroll to the right to see the entire photo below) - this large, ~7 k.y., hot springs travertine mound formed along the Jemez River, eastern side of Rt. 4, southwest of the Valles Caldera, north of San Ysidro, northern New Mexico, USA.  This travertine mound formed by calcite precipitation (CaCO3) from waters emerging at various hot springs.  Fluids are discharging from a Jemez Fault splay.  Over a dozen individual hot springs are still active here, but the underground plumbing at this site was wrecked by the New Mexico Highway Department while "improving" the nearby road.  As a result, Soda Dam is no longer constructional; it is slowly eroding.  (Most info. from Goff et al., 1996, The Jemez Mountain region, New Mexico Geological Society Forty-Seventh Annual Field Conference, September 25-28, 1996.)

 


 

Soda Dam (just to the west of the above location) - western side of Rt. 4, southwest of the Valles Caldera, north of San Ysidro, northern New Mexico, USA.  Here, a hot spring emerges from the rock.  Dissolved Ca+2 and CO3-2 ions precipitate out as calcite (CaCO3), forming travertine (the wet mound below knee level).  Thermophilic algae are providing the green coloration.

 


 

Royal Gorge along the Arkansas River, Royal Gorge Arch, west of Canon City, south-central Colorado, USA.  The rocks are Precambrian basement rocks dating to 1.70-1.72 billion years.  They are principally injection gneisses, consisting of high-grade, foliated metamorphic rocks multiply intruded by pegmatitic granite dikes.

 


 

Pinkish quartzites of the Sioux Quartzite (upper Paleoproterozoic, 1.65-1.70 Ga) along the Big Sioux River at Falls Park, city of Sioux Falls, southeastern South Dakota, USA.

 


 

Alice Mine (Alice Pit) - this former mine in Walkerville, southwestern Montana (just north of the town of Butte) targeted silver, manganese, and zinc minerals in hydrothermal veins (62-66 Ma) intruding the Butte Quartz Monzonite (76 Ma, Late Cretaceous).  The pit and adjacent park (grassy area in the background) are part of a completed Superfund cleanup site.

 


 

Continental Mine (Continental Pit) - this large, copper-molybdenum mine in Butte, southwestern Montana targets the minerals chalcopyrite and molybdenite.  The ore minerals are in hydrothermal veins (62-66 Ma) intruding the Butte Quartz Monzonite (76 Ma, Late Cretaceous), or are disseminated in the host rock.  I'm standing on an ore pile in the middle of the working floor of the mine.  The light brown-colored rocks in the upper walls of the mine in the background represent the oxidized zone.  The grayish rocks below that are unoxidized.  Minerals observed in the ore rock pile include pyrite, chalcopyrite, molybdenite, azurite, malachite, tenorite, and hematite.

 


 

Syndicate Pit (Butte, southwestern Montana, USA) - exposure of jointed Butte Quartz Monzonite (76 Ma, Late Cretaceous) with an intruding aplite dike (lower right of photo to under my knees).  Aplite is a finely-crystalline intrusive igneous rock having a granitic composition.

 


 

Jefferson Canyon (near Lewis & Clark Caverns, southern Montana, USA) - outcrop of the LaHood Formation (1.47 Ga, lower Mesoproterozoic), which here consists of arkoses and conglomeratic arkoses.  The LaHood Formation is in the lower Belt Supergroup, a famous and extremely thick succession of sedimentary rocks in western USA that fills a large, ancient rift valley.

 


 

Orphan Girl Mine (World Museum of Mining, town of Butte, southwestern Montana, USA) - this publicly-accessible adit leads down to the 65' level of the mine.  This zinc-lead-silver mine operated from the 1870s to the 1950s.  Target minerals occur in hydrothermal veins (62-66 Ma) that intrude the Butte Quartz Monzonite (76 Ma, Late Cretaceous).

 


 

Emma Vein (town of Butte, southwestern Montana, USA) - this 17'-wide hydrothermal composite vein intrudes the Butte Quartz Monzonite (76 Ma, Late Cretaceous).  The vein includes the dark rocks immediately surrounding me, the blackish area, and the brownish material in the right portions of the photo.  The host rock is the light brown material in the upper left portions of the outcrop.  At the surface, the Emma Vein is siliceous (quartz-dominated) and rich in manganese oxide (blackish) & iron oxide.  In the subsurface & to the east of this outcrop, the Emma Vein had economic concentrations of copper, manganese, and zinc minerals.  These have been mined out.  The subsurface Emma Vein included a 100' wide section of rhodochrosite.

 


 

Death Valley (Badwater Spring along Badwater Road, Death Valley, California, USA) - one of the harshest surface environments anywhere on Earth.  This is the valley floor of Death Valley at Badwater Spring (= behind the photographer).  This portion of the valley is well below sea level - the elevation here is -279'.  Air temperatures during boreal summers in Death Valley are extremely hot.  The temperature this day (July 2010) was 118° Fahrenheit (= ~48° Celsius).  A strong gust of wind swept through a few minutes after this photo was taken - a stereotypical "blast furnace wind".  The deposits in the valley are intermontane playa evaporites mixed with some siliciclastic material.  A playa is an ephemeral lake, or dry lake.  Playas only occasionally have standing water, but it quickly evaporates.

Death Valley & the adjacent mountain ranges are classic examples of horsts and grabens - upthrown and downthrown fault blocks resulting from crustal extension.  The mountain ranges (upthrown fault blocks) are horsts.  The valleys (downthrown fault blocks) are grabens.  Large-scale normal faults occur at the boundaries between the mountain ranges and the valleys in this area, and throughout the Basin & Range Province of western America (= Nevada, western Utah, parts of southern California & Arizona & northern Mexico, etc.).

 


 

Devil's Postpile (above & below) (Devil's Postpile National Monument, west of town of Mammoth Lakes, eastern California, USA) - the best localities on Earth for seeing excellent columnar jointing are: Giant's Causeway (Ireland), Devils' Tower (Wyoming, USA), and Devil's Postpile (California, USA).  Columnar jointing forms as a lava flow cools and contracts, resulting in the development of shrinkage cracks.  As shrinkage cracks grow, they branch at ~120º angles (as seen in map view).  Crack networks merge with other networks to form columns having a polygonal cross-section shape.  Most columns are hexagonal or pentagonal in shape.  A few are 3-sided, 4-sided, or 7-sided.

Devil's Postpile is a trachybasalt (or basaltic trachyandesite) lava flow with extremely well-developed columnar jointing.  Erosion has toppled many of the columns into a large pile at the base of the flow.  The flow represents part of the activity of the Long Valley Volcano, which is now a large caldera in the eastern Sierra Nevada Mountains of California.  The Devil's Postpile lava flow erupted outside the southwestern margin of the Long Valley Caldera.

Stratigraphy & age: Postpile Flow, Upper Pleistocene, 82 k.y.

Info. synthesized from Huber et al. (2001 - The Story of Devils Postpile, a Land of Volcanic Fire, Glacial Ice and an Ancient River, Updated from the Original Edition) and Mahood et al. (2010 - Geological Society of America Bulletin 122: 396-407) and Bailey (2004 - United States Geological Survey Professional Paper 1692).

 


 

Gypsum, Colorado (alongside 51 Road just north of the town of Gypsum, western Eagle County, northwest-central Colorado, USA) - large blocks of chickenwire rock gypsum of the Eagle Valley Evaporite, a Pennsylvanian unit dominated by rock salt (halite, NaCl), rock gypsum (CaSO4·2H2O), and rock anhydrite (CaSO4).  These three rock types formed by evaporation of seawater and the precipitation of dissolved minerals.  With deep burial, evaporites tend to engage in upward, solid-state flow.  A large area around Gypsum, Colorado is extensively deformed by dissolution and upward movement of various evaporite rocks - this is the Eagle Collapse Center, which covers about 2,500 square kilometers.  Evaporite rock movement and deformation occurred principally in the late Cenozoic.  Info. synthesized from Chronic & Williams (2002 - Roadside Geology of Colorado) and Lidke et al. (2002 - Geological Society of America Abstracts with Programs 34(6): 288).

 


 

Glacial erratic (Bumpass Hell Trailhead, just south of Mt. Lassen, Lassen Volcano National Park, northeastern California, USA) - glacial erratics are large boulders left behind by melting glaciers.  They have a somewhat rounded shape due to glacial and post-glacial meltwater abrasion.

 


 

Hailstone deposit (motel grounds in town of Limon, Colorado, USA) - a severe storm cell went over the town of Limon, Colorado on the evening of the 4th of July 2010, resulting in the development of a significant hailstone deposit.  The hailstones here have a ~bimodal size distribution and individual specimens range up to 3 cm in diameter.  Much larger aggregate hailstones also fell in places during this storm event.  More info. on hailstones.

 


 

Horseshoe Lake volcanic CO2 tree kill (northern shores of Horseshoe Lake, just south-southeast of Mammoth Mountain, southwest of the town of Mammoth Lakes, eastern Sierra Nevada Mountains, eastern California, USA) - several patches of dead lodgepole pine trees occur in the vicinity of Horseshoe Lake, California.  They were killed during the early 1990s by lethal levels of carbon dioxide gas in the soil.  The gas appears to be derived from rising magma in the Mammoth Mountain area.  This area is just to the southwest of the Long Valley Caldera, a still-active volcanic center.

 


 

Point Bonita pillow basalts (Point Bonita, southwestern tip of the Marin Peninsula, Golden Gate National Recreation Area, north of San Francisco, western coast of California, USA) - These rounded masses of volcanic rock are pillow basalts.  The pillow basalt morphology is diagnostic of an underwater lava eruption.  These basaltic lavas are part of the Franciscan Complex, and represent the top portion of Jurassic-aged oceanic crust.  This basaltic crust originally formed at an ancient mid-ocean ridge and got plastered onto the edge of the North American continent along a now-inactive subduction zone.  The upper portions of the subducting oceanic slab (the Farallon Plate) got scraped off to form an accretionary wedge.

 


 

Radiolarian ribbon chert (southern Marin Peninsula, Golden Gate National Recreation Area, north of San Francisco, western coast of California, USA) - these spectacular rocks are tilted layers of chert.  Their dark brick-red color is due to the presence of hematite (Fe2O3).  Weathering of these chert beds results in a ribbon-like appearance, hence the term ribbon chertChert is a siliceous sedimentary rock, composed of cryptocrystalline quartz (SiO2).  These particular cherts have abundant microfossils of radiolarians, a group of marine, unicellular, non-photosynthetic protists that make tiny skeletons of opal (SiO2·nH2O).  Burial and diagenesis of radiolarian-rich sediments results in the formation of radiolarian cherts.  These rocks are part of the Franciscan Complex (Jurassic) and were deposited on an ancient deep seafloor.  The rocks got scraped off from the top of a subducting slab of oceanic crust (the Farallon Plate) along coastal California.

 


 

Mono Lake tufa towers (above & below) (southern shore of Mono Lake, Mono Valley, eastern California, USA) - Mono Lake is a hyperalkaline, hypersaline lake.  It's chemistry and size have been strongly influenced by 1940s-onward human activity (diversion of Owens River water to Los Angeles).  The rocky structures seen here (above & below) are tufa towers.  They formed underwater at a time when lake levels were much higher than at present.  Tufa is a friable precursor to travertine.  Tufa rocks are composed of calcium carbonate (CaCO3).  They formed at the sites of former lake-bottom springs, where calcium-rich groundwater emerged and mixed with carbonate-rich lake water, resulting in the precipitation of CaCO3.  An unnamed, extremophile γ-proteobacterium that apparently(?) incorporates arsenic (As) in its cell structure was recently discovered at Mono Lake (more info.).

 


 

California gray whale skull (Point Reyes, westernmost Point Reyes Peninsula, western coastal California, USA) - the California gray whale (Eschrichtius robustus) is a very large marine mammal that attains an adult body length of about 50 feet.  The rocks in the cliff are quartzose sandstones and polymict conglomerates of the Point Reyes Conglomerate (Paleocene-Eocene), deposited in a continental slope environment.

 


 

San Andreas Fault Zone (Earthquake Trail, Point Reyes Peninsula, western coastal California, USA) (above & below) - the San Andreas Fault Zone is the classic example of a transform plate boundary, where two tectonic plates are sliding past each other.  In this case, it's the Pacific Plate and the North American Plate.  Despite the term "slide", fault movement is rarely slow & smooth & gradual - it tends to be sudden jolts of movement, resulting in earthquakes.  The above photo shows a fence offset along the 1906 San Francisco Earthquake fault scarp.  The San Andreas Fault Zone in the Point Reyes area is actually a broad valley (see photo below).  The Pacific Plate is to the right (west) and the North American Plate is to the left (east).

 


 

Marble (outcrop at parking lot for Crystal Cave, western end of Crystal Cave Road, northwestern part of Sequoia National Park, Sierra Nevada Mountains, eastern California, USA) - the only time I've seen marble in the field was here, in the Crystal Cave area of California's Sequoia National Park.  Marble is a crystalline, ~monomineralic, calcitic metamorphic rock.  It is composed of calcite (CaCO3) and forms by intermediate- to high-grade metamorphism of limestone.  In certain places in the Sierra Nevada Mountains, marble bedrock has been partially dissolved away by slightly acidic groundwater, resulting in the development of caves.  Crystal Cave is a short hike downhill from this outcrop.

 


 

Giant sequoia trees (above & below) (Sequoia National Park, Sierra Nevada Mountains, eastern California, USA) - California's famous giant redwoods and giant sequoias are the largest trees in the world.  Sequoia National Park has several groves of giant sequoia trees (Sequoiadendron giganteum).  The largest tree in the world is the General Sherman tree (see photo below), as defined by volume.  It is ~52,500 cubic feet in volume (a little less than 1500 cubic meters).

 


  

Yosemite Valley (view from the Wawona Tunnel overlook, Yosemite National Park, Sierra Nevada Mountains, eastern California, USA) - Bridalveil Falls is at right-center, El Capitan is the ~vertical cliff on the left, and Half-Dome is in the far-distance at center.  The broad U-shaped valley shape is the result of glacial erosion during the Pleistocene (= the last Ice Age).  The actual bedrock valley floor is well below the present surface.  The valley has partially filled with glacial and fluvial sediments.

 


 

Yosemite Valley (above & below) (view from Glacier Point, Yosemite National Park, Sierra Nevada Mountains, eastern California, USA) - Half Dome is the distinctively-shaped mountain above my head.  The rocks in the Yosemite Valley area are principally Cretaceous-aged, felsic to intermediate, intrusive igneous rocks.  Many discrete intrusions are present, ranging in composition from granite to granodiorite to diorite to quartz monzonite.  Most of these intrusive rocks have a strongly porphyritic texture (= a mix of large and small crystals).  The rocks in this area are part of the Sierra Nevada Batholith, a series of old, cooled magma chambers that were originally beneath a chain of volcanoes developed along an ancient subduction zone.

 


 

Miner's Castle (Pictured Rocks National Lakeshore, northeast of Munising, southern shore of Lake Superior, northern shore of Michigan's Upper Peninsula, USA) - the rocky cliffs along Lake Superior northeast of the town of Munising, Michigan are famous for their spectacular multicolored stains.  The projection of rock to the left in this photo is Miner's Castle, a differentially eroded succession of quartzose sandstones.  Just above lake level is the uppermost Jacobsville Sandstone, a cross-bedded quartzose and arkosic fluvial sandstone of Proterozoic age (~1.04-1.08 Ga).  Disconformably overlying the Jacobsville is the Munising Formation, which makes up most of the cliff at Miner's Castle.  A quartz-pebble conglomerate occurs in the basal Munising Fm., but much of the formation consists of planar-bedded, cross-bedded, and herringbone cross-bedded quartzose sandstones.  Body fossils are scarce in the Munising Fm., but do include polymeroid trilobites.  The trilobites indicate a late Middle Cambrian to Late Cambrian age.  Sediments of the Munising Formation were deposited in a shallow-water, nearshore marine environment that experienced tidal pumping.  The Jacobsville-Munising contact is located approximately at the color change near the base of the cliff (orange to very light brown).  This contact is the local Precambrian-Cambrian unconformity, and represents about a half-billion years worth of missing time.

 


 

Eagle Harbor (northern Keweenaw Peninsula, southern shore of Lake Superior, northern shore of Michigan's Upper Peninsula, USA) - lakeward-dipping basalts of the Lake Shore Traps Member of the Copper Harbor Conglomerate are exposed along the rocky shore at Eagle Harbor, Michigan.  These 1.087 billion-year old lava flows are flood basalts that filled an ancient rift valley.  A much thicker succession of rift valley-filling flood basalts is in the underlying stratigraphic unit, the Portage Lake Volcanic Series.

 


 

Valley of Fire (near Elephant Rock, near the eastern boundary of Valley of Fire State Park, southern Nevada, USA) - these beautiful rocks are part of the Lower Jurassic Aztec Sandstone (equivalent to the Navajo Sandstone of Zion National Park, Utah, USA), a quartzose sandstone succession deposited in an ancient sand dune facies.  Sandstones deposited in ancient sand dunes are called eolianites.  The red coloration is due to a significant hematite cement component.  Detrital zircon age analysis of the Aztec Sandstone and its equivalents elsewhere in southwestern America has shown that the principal sediment source for these ancient sand dunes was the Appalachian Mountains (!).  The sands were delivered from the east by westward-flowing paleorivers and paleowind currents (see Brenneman et al., 2006, Geological Society of America Abstracts with Programs 38(5): 10).

 


 

Mount Rushmore (central Black Hills, southwest of Keystone, western South Dakota, USA) - I have mixed feelings about this locality.  It's an historic site and memorializes four of the greatest people in the history of the planet (George Washington, Thomas Jefferson, Theodore Roosevelt, Abraham Lincoln), but it's also just large-scale defacement of nature.  I'd rather have the natural mountainside.  Destroying mountainsides in the Black Hills seems to be fad that is spreading.  American Indians are defacing another Black Hills mountain nearby - the Crazy Horse Memorial.  I wish people would leave nature alone.

Anyway - the rocks at and around the carved faces are part of the Harney Peak Granite (1.695 to 1.715 billion years).  The dark-colored, subhorizontal streak of rocks below Washington's chest is the host rock for the Harney Peak Granite.  The granite intruded through metamorphic rocks, principally quartz-mica schists.  Metamorphism of the schist host rocks occurred not long before intrusion of the granite.  The schists date to 1.715 to 1.750 billion years.  Both rock types (granite and schist) can be closely examined along the walkway between the public parking area and Mount Rushmore itself.

 


 

Goblin Valley (above & below) (Goblin Valley State Park, southeast-central Utah, USA) - differential erosion of interbedded hard quartzose sandstones and relatively soft siltstones and mudrocks has produced an abundance of oddly-shaped features at Goblin Valley, Utah (also known as Mushroom Valley).  The reddish-brown color of the rocks is from the presence of hematite (Fe2O3).  This is the Entrada Sandstone, an Upper Jurassic unit consisting of very shallow marine and nonmarine coastal sand dune deposits.  The same rocks make up the main scenery at Arches National Park, Utah.

 


 

McGee Creek glacial moraine (along McGee Creek Road, eastern slopes of McGee Mountain, eastern margin of the Sierra Nevada Mountains, eastern California, USA) - the boulder field around me is a moraine deposit consisting of glacial till (an unsorted, coarse-grained, non-stratified glacial deposit).  Behind the photographer is McGee Creek Canyon.  During the Pleistocene (= the last Ice Age), an alpine glacier eroded and carved that canyon.  The till here is rock debris left behind after the glacier melted away.  Published research indicates that this till is 10,000 to 20,000 years old (Tioga Glaciation).

The lake in the distant valley is Lake Crowley, an artificial reservoir formed by construction of the Long Valley Dam.  The mountain range in the background is the White Mountains, here consisting of Mesozoic-aged intrusive igneous rocks and metamorphic rocks.

Info. synthesized from Milliken (1992) - Guidebook, Mono/Owens Valleys Geology Field Trip, October 10-11, 1992.  Bakersfield, California, USA.  U.S. Bureau of Land Management, Bakersfield District Office.  35 pp.

 


 

Devils' Tower (northeastern Wyoming, USA) (above & below) - the principal scenery at America's first national monument is a distinctive igneous feature called Devils' Tower.  It has been variously interpreted as a volcanic neck (probable), an eroded laccolith (unlikely), or an eroded stock (possible).  The vertical to subvertical striations along the sides of Devils' Tower (see below) represent columnar jointing, formed as the original molten rock cooled and shrank slightly.  Devils' Tower is one of three classic localities on Earth that have excellent columnar jointing (along with Devil's Postpile in California and Giant's Causeway in Ireland).  The rocks of Devils' Tower formed 49 million years ago, during the latest Early Eocene.

Above: view from Rt. 24, western side of Campstool Draw (Canyon), south-southeast of Devil's Tower.

Below: view from Tower Trail, Devils' Tower National Monument.

 

Devils' Tower (Tower Trail, Devils' Tower National Monument, northeastern Wyoming, USA) - the 49 million year old rock making up Devils' Tower is porphyritic phonolite, a scarce, alkaline, intermediate igneous rock having large, whitish plagioclase feldspar crystals in a finely-crystalline groundmass.

 


 

Lehigh-Hanson Harding Street Quarry (southern Indianapolis, Indiana, USA) - looking for pyrite nodules in a waste rock pile of black shale (Blocher Member, lower New Albany Shale, upper Middle Devonian-lower Upper Devonian).  Black shale is one of two overburden units at this quarry, which targets the Middle Devonian North Vernon Limestone for use as aggregate, gravel, etc.  The black shale unit is somewhat pyritic in certain horizons.  The pyrite occurs in disseminated form, as well as in discrete small-to-large nodules, pyrite-rich laminations, and pyrite-rich thin beds.

 


 

Calistoga Petrified Forest (above & below) (northern side of Petrified Forest Road, WSW of Calistoga, eastern Sonoma County, Coast Ranges of northwest-central California, USA) - permineralized coast redwood tree trunks, Sequoia sempervirens.  The Calistoga Petrified Forest has been called the best-anywhere petrified forest of Pliocene age.  The fossil wood here is preserved with the most common permineralization mineral - quartz.  The preservation of these trees was the result of burial by a rhyolitic volcanic ash-flow tuff (Sonoma Volcanics, 3.2-3.4 m.y., Upper Pliocene).  The volcanic tuff was erupted from a vent near modern-day Mt. St. Helena (north of this locality).

 


 

Point Reyes Lighthouse (westernmost Point Reyes Peninsula, western coastal California, USA) - these polymict conglomerates are part of the Point Reyes Conglomerate (Paleocene-Eocene), a continental slope deposit.  The sands and large clasts were deposited in a underwater debris fan at the base of an ancient submarine canyon incised into the seaward margin of the continental shelf.

 


 

Resting Spring Range (Rt. 178 roadcut along western slopes of the southern Resting Spring Range, east of Shoshone, Inyo County, southeastern California, USA) - beautifully-exposed fault cutting through the Resting Spring Pass Tuff (lower Upper Miocene, 9.6 Ma).

 


 

Resting Spring Range (Rt. 178 roadcut along western slopes of the southern Resting Spring Range, east of Shoshone, Inyo County, southeastern California, USA) - an often-visited outcrop of obsidian and volcanic tuffs, part of the Resting Spring Pass Tuff (lower Upper Miocene, 9.6 Ma).  The black obsidian unit is actually the result of remelting of an extremely hot volcanic tuff unit.

 


 

San Rafael Monocline (along Interstate 70, west of the town of Green River, west-central Grand County, east-central Utah, USA) - monoclines are kinks, or bends, in rock layers.  Utah's San Rafael Monocline (aka "San Rafael Reef", meaning a barrier to travel)  is a well-exposed, world-class example of this type of structure.  The rocks are Jurassic-aged sedimentary units.  The light pinkish-brown rocks making up most of the "reef" is the Navajo Sandstone, a widespread Upper Triassic to Lower Jurassic sand dune deposit in southwestern America.  It's the same Navajo Sandstone that makes the principal scenery in Utah’s Zion National Park.

 


 

Tyrannosaurus rex (FMNH PR 2081, Field Museum of Natural History, Chicago, Illinois, USA) - this large, complete Tyrannosaurus rex skeleton (Hell Creek Formation, upper Upper Cretaceous; northwestern South Dakota, USA) is the "Sue" specimen, an old adult of 28 years.  Several deformities are present on the skeleton, representing bone lesions or healed breaks.

 


 

Firehole Falls (Firehole Canyon, Yellowstone Hotspot, northwestern Wyoming, USA) (looking ~SSW) - Yellowstone is a gigantic hotspot volcano.  So, naturally, most of the rocks at Yellowstone National Park are young volcanics.  Here in Firehole Canyon, the Firehole River flows between the margins of two rhyolite lava flows.  The rocks to the left of the river and the waterfall (to the east of the river) are rhyolites, rhyolite breccias, and some mahogany obsidian of the Nez Perce Creek Flow (Central Plateau Member, Plateau Rhyolite, Pleistocene, 160 k.y.).  The rocks on the other side of the river (to the west) are rhyolites of the West Yellowstone Flow (Central Plateau Member, Plateau Rhyolite, Pleistocene, 111 k.y.).

 


 

Arthropleura model, approximately life-sized (public display, Field Museum of Natural History, Chicago, Illinois, USA).  Arthropleura is the largest known terrestrial arthropod in Earth history (the modern coconut crab is also a giant).  The arthropleurids were giant, centipede-like organisms having a nonmineralized exoskeleton.  Fossil remains allow an estimation of a six-foot long body length.  Arthropleura fossils are only found in nonmarine, coal-bearing successions of Pennsylvanian age, indicating a coal swamp forest habitat.

The Pennsylvanian was a time of gigantism in other terrestrial invertebrates as well, including dragonflies and cockroaches.  Arthropod gigantism during the Pennsylvanian is usually explained as an evolutionary result of long-term atmospheric hyperoxia (high levels of oxygen gas compared with today).

Classification: Animalia, Arthropoda, Myriapoda, Arthropleurida

 


 

Cedar Breaks (above & below; above: Point Supreme overlook, Cedar Breaks National Monument, southwestern Utah, USA; below: North View overlook, Cedar Breaks National Monument, southwestern Utah, USA) - the spectacular scenery at this park is the result of weathering and erosion of the Claron Formation (Paleocene-Eocene), a succession of lacustrine siliciclastics and carbonates.  These colorful sedimentary rocks were originally deposited in Lake Claron, an ancient intermontane basin.  This landscape of steep, soil-free and largely vegetation-free slopes at Cedar Breaks (& at nearby Bryce Canyon) is called badlands topography.  Note the two faults at the far-left and left-center in the above photo (the best way to find the faults is to look at how the whitish, cliffy-weathering unit is offset).

 


 

Eclogite (outcrop above the eastern side of Rt. 1, just north of Jenner, coastal California, USA) - eclogite is a rare, very high-grade metamorphic rock, formed when basaltic-gabbroic rocks are subducted down to mantle depths.  Primary eclogite consists principally of greenish omphacite pyroxene and reddish pyrope garnet.  With uplift to the surface, many eclogites are retrograde metamorphosed, resulting in the appearance of other minerals.  In the Jenner area, the rocks include retrograde eclogite, some of which have distinctively bluish-gray patches of glaucophane while still having greenish pyroxene and reddish garnet.

 


 

Badwater Spring (Death Valley, California, USA) - water does emerge at the surface in the Death Valley area.  A famous example is the interestingly-named "Badwater Spring", in reference to its very salty taste.  Water constantly reaches the surface along a major normal fault plane (= at the base of the Amargosa Range mountains in the background) - the Black Mountains Frontal Fault Zone.  Due to the hot, arid climate of Death Valley, water quickly evaporates, leaving behind salt crusts rich in halite (NaCl).  Life exists in the pool, including the Badwater snail (Assiminea infima), insect larvae, and halophilic algae.

 


 

San Salvador Island (eastern Bahamas) - the Bahamas are a world-class place for studying subtropical marine communities and carbonate platform geology & paleontology.  Significant insights can result after comparing modern reefs in the water and fossil reefs on the adjacent island.  Many of the species alive now are the same species seen in the Late Pleistocene fossil record here.

 


 

Kelp (Plantae, Phaeophyta, Laminariales) at Agate Beach, southern Pt. Reyes Peninsula, western coastal California, USA.

 


 

Moro Rock exfoliation dome (western Sequoia National Park, Sierra Nevada Mountains, eastern California, USA) - the rocks are part of the Giant Forest Granodiorite (Sequoia Intrusive Suite, 97-102 million years, mid-Cretaceous).

 


 

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