leg site hole core coretype section top interval bottom interval piece subpiece unit number sub unit observer rockname texture where sampled grain size phenocrysts observed phenocrysts mineral name (1) phenocrysts present persent (1) phenocrysts original percent (1) phenocrysts size (1) phenocrysts composition (1) phenocrysts morphology (1) phenocrysts comments (1) phenocrysts mineral name (2) phenocrysts present persent (2) phenocrysts original percent (2) phenocrysts size (2) phenocrysts composition (2) phenocrysts morphology (2) phenocrysts comments (2) phenocrysts mineral name (3) phenocrysts present persent (3) phenocrysts original percent (3) phenocrysts size (3) phenocrysts composition (3) phenocrysts morphology (3) phenocrysts comments (3) phenocrysts mineral name (4) phenocrysts present persent (4) phenocrysts original percent (4) phenocrysts size (4) phenocrysts composition (4) phenocrysts morphology (4) phenocrysts comments (4) phenocrysts mineral name (5) phenocrysts present persent (5) phenocrysts original percent (5) phenocrysts size (5) phenocrysts composition (5) phenocrysts morphology (5) phenocrysts comments (5) groundmass observed groundmass mineral name (1) groundmass present percent (1) groundmass original percent (1) groundmass size (1) groundmass composition (1) groundmass morphology (1) groundmass comments (1) groundmass mineral name (2) groundmass present percent (2) groundmass original percent (2) groundmass size (2) groundmass composition (2) groundmass morphology (2) groundmass comments (2) groundmass mineral name (3) groundmass present percent (3) groundmass original percent (3) groundmass size (3) groundmass composition (3) groundmass morphology (3) groundmass comments (3) groundmass mineral name (4) groundmass present percent (4) groundmass original percent (4) groundmass size (4) groundmass composition (4) groundmass morphology (4) groundmass comments (4) groundmass mineral name (5) groundmass present percent (5) groundmass original percent (5) groundmass size (5) groundmass composition (5) groundmass morphology (5) groundmass comments (5) vesicles oberserved vesicles type code (1) vesicles percent (1) vesicles size (1) vesicles location (1) vesicles filling (1) vesicles shape (1) vesicles comments (1) vesicles type code (2) vesicles percent (2) vesicles size (2) vesicles location (2) vesicles filling (2) vesicles shape (2) vesicles comments (2) vesicles type code (3) vesicles percent (3) vesicles size (3) vesicles location (3) vesicles filling (3) vesicles shape (3) vesicles comments (3) secondary mineraliztion observed secondary mineral name (1) secondary percent (1) secondary replacement (1) secondary comment (1) secondary mineral name (2) secondary percent (2) secondary replacement (2) secondary comment (2) secondary mineral name (3) secondary percent (3) secondary replacement (3) secondary comment (3) secondary mineral name (4) secondary percent (4) secondary replacement (4) secondary comment (4) secondary mineral name (5) secondary percent (5) secondary replacement (5) secondary comment (5) secondary mineral name (6) secondary percent (6) secondary replacement (6) secondary comment (6) secondary mineral name (7) secondary percent (7) secondary replacement (7) secondary comment (7) secondary mineral name (8) secondary percent (8) secondary replacement (8) secondary comment (8) main comments more data latitude longitude depth top interval depth bottom interval depth 104 642 E 005 Rotary 03 061 063 008 0001 LEH Sparsely olivine plagioclase phyric basalt Flow unit 1 Olivine 3-5 3-5 .1-.4 Euhedral Completely altered to iddingsite. Opaques 2-3 2-3 <0.1 Fe3O4 Skeletal Plagioclase/Cpx 85-90 85-90 N/A N/A Completely altered to clays and carbonate. Vesicles ~5 Round Sometimes difficult to discriminate from altered groundmass. Clays/carbonate 85-90 Plagioclase, clinopyroxene Groundmass virtually completely altered. Altered. no 67.22000 2.93000 0337.45 33806 104 642 E 007 Rotary 01 036 038 008 0002 LEH Sparsley plagioclase phyric basalt Intersertal Flow 2 Plagioclase <1 <1 1.5 Prismatic Altered to clays. Plagioclase 30 30 0.05-<0.5 Laths Altered to clays. Olivine 3 3 0.1-0.2 Euhedral Altered to iddingsite. Oxides N/A N/A 0.05-0.5 Subhedral Vesicles 0 1-2 Clays 40-45 Plagioclase, vesicle rims Interstitial, slightly pleoch., relatively high birefringence. Smectite-illmenite <1 Inner vesicles Slightly greenish. Clay 45-50 Matrix Brown to opaque, slightly greenish. Radial, fibrous (quenched textures?) in matrix. no 67.22000 2.93000 0354.30 35465 104 642 E 011 Rotary 02 055 057 002 A 0004 LEH Sparsely clinopyroxene plagioclase phyric basalt Intersertal Flow 4 Plagiocalse <1 <1 0.4 Prismatic Clinopyroxene ~1 ~1 0.4-0.5 Subhedral Wavy extinction. Plagioclase 35-40 35-40 0.3 Laths Clinopyroxene 20-25 20-25 <0.05 N/A Olivine <1 <1 0.05-0.1 Euhedral Completely iddingsitized. Opaques 2-3 2-3 0.05-0.07 Fe3O4 Skeletal vesicles 0 Clays 20 Interstices Brownish green no 67.22000 2.93000 0384.65 38519 104 642 E 013 Rotary 01 091 095 013 B 0007 LEH Moderately plagioclase phyric basalt Intersertal Flow 7 Plagioclase ~10 ~10 0.5-2.0 Prismatic Agglomerated, fractured and filled with smectite. Plagioclase ~50 ~50 <0.1 Laths Clinopyroxene ~20 ~20 0.05-0.1 N/A Hourglass extinction. Olivine(?) <1 <1 N/A Euhedral Altered to iddingsite. Opaques ~5 ~5 <0.05 Subhedral Some alteration to iron oxyhydroxides. Vesicles 1-2 0.5-1.0 Smectite Round to subrounded Clays 10-12 Yellowish green in interstices and possibly small percent replacing olivine. Fe-Ti hydroxides? ~1 In smectite lined vesicles Also around opaques. no 67.22000 2.93000 0394.80 39570 104 642 E 014 Rotary 01 038 043 007 0007 LEH Highly plagioclase phyric basalt Intersertal Flow 7 Plagioclase 12-15 12-15 0.5-2.0 Prismatic Glomerophyric; some cored with previous plagioclase generation and clinopyroxene. Plagioclase 35 35 0.05-0.13 Laths Clinopyroxene 20 20 <0.1 Subhedral Very pale colors, partially altered. Opaques 2-3 2-3 N/A Fe3O4 Subhedral Vesicles <1 Clays 20-25 Interstices Replaces groundmass, cracks in phenocrysts. Several radial aggregates of plagioclase laths, at least one with olivine (iddingsite) at center. no 67.22000 2.93000 0399.80 40017 104 642 E 014 Rotary 01 128 130 019 0008 LEH Highly plagioclase phyric basalt Intersertal, aphanitic Flow 8 Plagioclase 10-12 10-12 0.5-2.0 Prismatic, skeletal Partially altered, zoned, glomerophyric; some with clinopyroxene cores. Plagioclase 25 25 0.1-0.2 Laths Clinopyroxene 20 20 0.1-0.15 N/A Olivine <1 <1 0.1-0.2 Euhedral to subhedral Completely iddingsitized. Opaques 3-5 3-5 N/A Magnetite Subhedral Vesicles N/A 0.2-5.0 Calcite/smectite Round Clays 25-30 Interstices, all minerals Medium green smectite. no 67.22000 2.93000 0399.80 40107 104 642 E 015 Rotary 02 073 076 009 0010 LEH Aphyric basalt Subophitic, aphyric Flow 10 Plagioclase 35 35 0.4-0.5 Lathes Size measured along length. Clinopyroxene 35 35 0.1-0.3 Euhedral, subhedral Two varities: 1) pale green, incipient alteration. 2) Very pale green;2V ~40 degrees. Olivine 10-12 10-12 0.1-0.3 Euhedral to subhedral Rims iddingsitized, remainder altered to clays. Opaques 5 5 N/A Embayed Rims coated with altered Fe-Ti OH. Vesicles 4-5 Rimmed with smectite Ovoid Precent of rock estimated separate from rims. Clays 15 Interstitial Olivine tholeiite. Thin section nearly completely destroyed during polisihing; olivine "crystals" (relict) especially affected. no 67.22000 2.93000 0406.80 40752 104 642 E 015 Rotary 04 103 106 007 0011 LUV Sparsely plagioclase phyric basalt Subophitic to intergranular Flow 11 Plagioclase 1-2 1-2 1.5 An60 Short laths, stubby Euhedral, embayed zoned, multiple zones up to An80. Olivine 5 5 0.15 Equant, subhedral Completely altered to iddinsite. Plagioclase 30 30 0.3 Subhedral, laths Clinopyroxene 20 20 0.15 Anhedral Magnetite 2 2 0.1 Subhedral to skeletal Vesicles 0 Clays 10 Intergranular Green-brown radiating fibers. Clays 30 Intergranular Amorphous, green-brown. 30% of the slide is plucked. Probably piece number 7. no 67.22000 2.93000 0409.59 41061 104 642 E 015 Rotary 05 009 012 001 0013 LUV Sparsely plagioclase phyric basalt Subophitic, intergranular Flow 13 Plagioclase 1-2 1-2 1-1.5 An54 N/A Plagioclase 45 45 0.2-0.4 An50 Thin laths Clinopyroxene 30 30 0.15-0.6 N/A Olivine 10 10 ~0.2 Equant Altered to iddingsite to smectite. Magnetite 4 4 N/A N/A Intergranular to plagioclase. Vesicles 0 Clays 10 Intergranular Fibrous, green-brown. no 67.22000 2.93000 0410.99 41107 104 642 E 015 Rotary 05 105 112 009 B 0012 LUV Sparsely plagioclase phyric basalt Subophitic to intergranular Flow 12 Plagioclase 4 4 1.5 An60 Subhedral Laths, glomerophyric. Plagioclase 50 50 0.3 An50 Laths Clinopyroxene 20 20 0.3 Augite N/A Olivine 7 7 0.15-0.3 Subhedral, equant Altered to iddingsite then smectite. Magnetite 5 5 0.1-0.2 Subhedral Intergranular, anhedral also. Vesicles 10 3-6 Subround Carbonate centers, smectite rims. Clays 10 Intergranular Also altering olivine. Carbonate in vesicles radiates from a single point. Probably piece number 9B. yes 67.22000 2.93000 0410.99 41203 104 642 E 016 Rotary 01 022 024 003 0015 LUV Medium grained mixed basalt Flow 15, mixed flow top Plagioclase 40 40 0.2 An52 Laths Intergranular and intersertal. Clinopyroxene 45 45 0.15-0.3 N/A Magnetite 6 6 0.1-0.2 N/A Clay 9 9 N/A N/A Replacing clinopyroxene. Plagioclase 35 35 0.3 N/A Very thin laths or columns. Clinopyroxene 5 5 0.1-0.3 Euhedral to subhedral Better developed than plagioclase. Magnetite 5 5 0.05-0.1 N/A Clays? 55 55 N/A N/A Vesicles 0 Domains of medium grained separated by fine grained or quenched material. Sharp boundary between fine and medium grained material. Probably piece number 3. no 67.22000 2.93000 0414.80 41501 104 642 E 016 Rotary 01 032 034 004 0015 LUV Medium grained basalt Flow 15, mixed flow top Olivine 5 5 0.3 N/A Iddingsitized. Plagioclase 35 35 0.5-1.0 An52 Stubby laths Clinopyroxene 20 20 0.3 N/A Magnetite 10 10 N/A N/A Clay 30 30 N/A N/A Intergranular, replacing clinopyroxene. Plagioclase 45 45 0.1-0.4 Laths to columns Clinopyroxene 2 2 0.07-0.25 Subhedral Magnetite 8 8 0.035-0.090 N/A Clay 45 45 N/A N/A Altered groundmass. Vesicles 15 0.1 Fine grained portion Dark green clay Irregular Intergranular. Domain of medium grained separated by fine grained material, sharp boundaries between them. no 67.22000 2.93000 0414.80 41511 104 642 E 017 Rotary 01 104 106 019 0017 PAR Red-weathered aphyric basalt Weak pilotaxitic Flow 17, weathered top, 1m below top. Olivine 20 20 0.05-0.2 Euhedral-subhedral Iddingsitized throughout-red-brown, completely iddingsitized cores of olivine may hold calcite. Plagioclase 40 40 0.05-0.2 An56 Subhedral, laths Clinopyroxene 35 35 0.05-0.1 Anhedral Very weakly zoned, locally weakly pilotax. Opaques 5 5 0.025-0.1 Interstitial Vesicles 0 Clays ~5 Plagioclase Green smectite: first phase vein fill smectite. Clays Vein margins Green-brown smectite growth, late celadonite. Carbonate Veins 0.5-1.5 mm Sparry, with relict dog tooth and colloform growth rings. Oxide? Vein fill Local earliest pre-smectite vein margin growth. Fe-oxide Intergranular Weathering. Probably piece number 19. no 67.22000 2.93000 0424.30 42533 104 642 E 017 Rotary 02 104 107 015 0017 PAR Weakly reddened basalt Weak trachytic Flow 17, 2.6 m below recovered flow top. Plagioclase 1-2 1-2 .8-.4 An65 N/A Zoned (An55 on outer rim). Olivine 15 15 0.1-0.5 Subhedral Some euhedral and anhedral. Iddingsite pseudomorphs. Plagioclase 45 45 0.1-0.4 An53 Subhedral, lath Weak trachytic/pilotaxitic. Clinopyroxene 37 37 0.05-0.1 Anhedral Opaque 3 3 <0.05 Magnetite Subhedral and interstitial Vesicles 7 2.5-5.0 Unfilled Round Narrow, oxide staining around vesicle. Cavities <1 <1.0 Smectite/carbonate/calcite Cavities and vein fill-carbonate 95%. Clays 7-10 Plagioclase and margins To olivine/green smectite. Clays Yellow/brown smectite vein fill second phase. Fe-oxode? Vein margin first phase, localized. Celadonite Vein margin third phase, pre-calcite. 3-5mm xenolith of basalt identified within thin section. Black, dusty margin to finer grained groundmass with moderate to strong pilotaxitic texture. no 67.22000 2.93000 0425.75 42679 104 642 E 017 Rotary 03 070 072 006 0017 PAR Aphyric tholeiitic basalt Flow 17, 3.7m below recovered flow top. Plagioclase <1 <1 2-5 An60 Euhedral tabules Center margin normally zoned, locally glomerophyric. Olivine 15 15 0.1-0.3 Subhedral-anhedral All smectite or iddingsite in alteration zones. Plagioclase 45 45 0.1-0.3 An58-60 Subhedral-laths Weak/sporadic pilotaxitic. Clinopyroxene 33 33 0.05-0.15 Anhedral Oopaque 7 7 0.05-0.15 Magnetite Subhedral-interstitial Some rhombics. Vesicles 0 Clays <3 (?) Cavities and margins Yellow brown smectite, radiofibrous. Clays 10 Interstices or plagioclase Patchy, in alteration fabric. Patchy, smectite-rich alteration zones, plagioclase (locally replaced 80% by green smectite), altered olivines are iddingsite-rich, c.f. to smectite-rich outside zones. Plagioclase is relatively fresh. Open fracture cutting section has altered margins. no 67.22000 2.93000 0427.05 42774 104 642 E 018 Rotary 02 027 029 011 B 0017 PAR Streaky aphyric basalt Locally trachytic Flow 17, 5.4 m below recovered flow top. Olivine 12 12 0.1-0.6 Subhedral to euhedral Iddingsite margins, smectite cores. Cleanest alteration textures in olivines in alteration zones. Plagioclase 45 45 0.1-0.3 Subhedral, laths Local moderate pilotaxitic. Clinopyroxene 35 35 0.05-0.1 Anhedral Opaques 8 8 <0.15 Magnetite Subhedral, few rhombics Vesicles 0 Clays N/A Plagioclase (+ cpx?) Green smectite to maximum of 65% of discrete alteration zones (streaky laminations(?)). Zones make up 10% of rock, about 1mm wide, discontinuous, approximately parallel or patchy. Clearest alteration textures in olivines in alteration zones. Preferred orientation of plagioclase groundmass only locally subparallel to alteration streaking. no 67.22000 2.93000 0434.12 43438 104 642 E 018 Rotary 02 027 028 011 B 0017 PAR Streaky tholeiitic basalt Subophitic/trachytic Flow 17, 6.7 m below recovered flow top. Plagioclase 50 50 0.2-0.65 An60 Subhedral laths Moderate trachytic/pilotaxitic, deflection into alteration fabric. Olivine 12 12 0.1-0.5 Anhedral to subhedral Olivines are dirty green smectite replacements outside of alteration streaks, clearly defined within streaks as part iddingsite, part smectite. Clinopyroxene 33 33 0.05-0.15 (?) Pigeonite Anhedral, granular Sub-ophitic with plagioclase. Opaques 5 5 0.075-0.15 Magnetite Needles/rhombic, euhedral Vesicles 0 Clays N/A Interstices and locally plagioclase In alteration streaks/bands. Within alteration bands rock is up to 45% smectite, 1.0+ mm wide discontinuous, locally diffuse. no 67.22000 2.93000 0434.12 43438 104 642 E 018 Rotary 03 072 075 001 B 0017 PAR Aphyric tholeiitic basalt Trachytic/pilotaxitic glomerophyric Flow 17, 8.5 m below recovered flow top. Palgioclase <2 <2 0.1 An65 Subhedral Locally glomerophyric. Olivine 12 12 0.1-0.35 Anhedral Iddingsite within alteration fabric and smectite replaces olivine outside alteration fabric, little iddingsite. Plagioclase 42 42 0.1-0.4 An60 Subhedral, anhedral, laths Smectite in alteration zones, moderate pilotaxitic. Clinopyroxene 37 37 0.025-0.2 Anhedral, granular Fresh. Opaques 8 8 0.05-0.1 Anhedral-subhedral Fresh. Vesicles 0 Clays N/A Plagioclase Strongly altered in alteration "streak" zones. Poor alteration fabric, patches and single streak. no 67.22000 2.93000 0435.28 43599 104 642 E 018 Rotary 04 037 039 002 0017 PAR Aphyric tholeiitic basalt Trachytic/pilotaxitic Flow 17, flow interior Olivine 12 12 0.1-1.0 Anhedral Smectite and iddingsite replacement. Iddingsite only within alteration zones. Plagioclase 42 42 0.1-0.5 An65 Lath, subhedral Good pilotaxitic text, domainal. Clinopyroxene 38 38 0.05-0.15 Anhedral, granular Opaque 8 8 0.05-0.2 Magnetite Anhedral Vesicles 0 Clays N/A Interstitial and plagioclase In alteration zones, green smectite. Carbonate <1 Cavity fills Alteration zones are well developed, about 1 mm wide, green smectite rich, with good alignment of feldspar laths within zones. Probalbly piece number 2. no 67.22000 2.93000 0436.72 43709 104 642 E 019 Rotary 01 042 044 004 C 0018 LEH Sparsely phyric tholeiitic basalt Glomerophyric Flow 18, 0.6 m below recovered flow top. Plagioclase 2 2 1-2 An65 Tabular and laths Normally zoned, locally glomerophyric Clinopyroxene N/A N/A <1 Pigeonite? Laths Olivine 12 12 0.1-0.4 Subhedral-anhedral Iddingsitized, rims mostly smectite psuedomorphs. Plagioclase 40 40 <0.1-0.5 Subhedral, laths Clinopyroxene 38 38 0.05-0.15 N/A Opaques 5 5 <0.1 Magnetite Interstitial Vesicles 7 4 Smectite calcite cores Irregular Radio-fibrous green smectite fill, yellow smectite rims. Clays 3 Interstitial and plagioclase Smectite patches. no 67.22000 2.93000 0442.10 44252 104 642 E 019 Rotary 02 099 102 003 0018 LEH Tholeiite basalt Intersertal to subophitic Flow 18 Plagioclase 1 1 0.5-1.0 Prismatic Glomerophyric, zoned. Plagioclase ~40 ~40 0.2-0.6 Laths Width is <0.05 mm. Clinopyroxene ~40 ~40 0.1-0.3 2 Pyroxene? Subhedral to anhedral High 2V, > 40 degrees, purplish color, second cpx(?) has a very pale color, lower 2V (~30 degrees). Olivine 5-7 5-7 0.05-0.5 N/A Altered to iddingsite and clays. Opaques 2-3 2-3 <0.15 Euhedral Some altered around edges (Fe stain). Vesicles N/A <10 Ovoid Filled with smectite and isotropic mineral. Clays 10 Interstices and vesicles Maybe two clinopyroxenes: 1) Augite with ~Ti (purplish color). 2) Pigeonite (very pale to colorless; 2V; lower extinction angle). no 67.22000 2.93000 0443.51 44450 104 642 E 019 Rotary 04 009 010 001 A 0018 PAR Sparsely phyric tholeiitic basalt Subophitic Flow 18, 5.2 m below recovered flow top. Plagioclase >1 >1 0.1-1.2 AN60 Tabular and laths Fresh, most normally zoned, few oscillatory. Olivine 10 10 0.1-0.5 Subhedral or anhedral Iddingsitized and smectite replaced. Plagioclase 41 41 0.1-0.9 An60 N/A Clinopyroxene (x2) 39 39 0.05-0.1 Pigeonite + ? N/A 2V ~0 degrees/+2V ~45 degrees, some subophitic. Opaques 4 4 0.05-0.2 Magnetite N/A Vesicles 0 Clays 5 Green smectite rich alteration patches. Probably piece number 1A. no 67.22000 2.93000 0446.13 44622 104 642 E 027 Rotary 03 015 019 014 0029 LEH Plagioclase-phyric tholeiitic basalt Hyalocrystalline or trachylitic Flow 29 Plagioclase 1 1 0.5-2.5 Prismatic Glomerophyric, fractured, partially altered. Tachylite 40 40 N/A Interstitial Opaque, "isotropic", cryptocrystalline. Plagioclase 40 40 N/A N/A Clino-orthopyroxene 3-5 3-5 0.15-0.35 Pigeonite Euhedral Inverted pigeonite, i.e. opx with augite lamellae. Vesicles Lots 1-3 Smectite, zeolite Irregular Some with center voids. Clays 12-15 Fractures in plagioclase phenocrysts Also altering large plagioclase, interstitial. no 67.22000 2.93000 0514.07 51422 104 642 E 027 Rotary 04 066 068 008 A 0029 DIV Lehgioclase-phyric basalt Intersertal Flow 29 Plagioclase 10-12 10-12 1.0-2.5 Prismatic Tend to be fractured and/or embayed. Plagioclase 35 35 0.05-0.2 Laths Occasional laths up to 0.7 mm. Clinpyroxene 5 5 N/A Augite N/A Mostly altered, percentage is for partially altered. Olivine 2-3 2-3 <0.05 Euhedral to subhedral Replaced by brown smectite (counted as olivine). Opaques 5 5 0.1-0.2 Fe3O4 Skeletal Some oxidation, tend to cluster near vesicles. Vesicles 5 >0.5 Smectite Round Not counted in mineral totals. Clays 15 Interstitial Uniform brown. Clays 30 Pyroxene (and plagioclase?) Splotchy appearance. Plagioclase laths radiate from (altered) olivine. Opaques and (altered) olivine are often concentrated in linear bands and around vesicle rims. no 67.22000 2.93000 0515.57 51623 104 642 E 027 Rotary 05 011 015 001 0029 LEH Plagioclase-clinopyroxene phyric basalt Intersertal to subophitic Flow 29 Plagioclase 12 12 1-2 Prismatic Glomerophyric, subophitic. Clinopyroxene 2 2 0.7-1.0 Pigeonite, augite Subhedral 2V <2.5 degrees, + very pale pigeonite to low Ca Augite, slight brown tinge. Plagioclase 45 45 0.05-0.6 Laths Size: 0.05-0.6 length, ~0.5 width. Clinopyroxene 35 35 <0.05 Subhedral to anhedral Opaques 3-5 3-5 N/A Euhedral to skeletal Vesicles 15 1-20 Smectite and zeolite Elongate, irregular Clays 3-5 Interstices Medium brown. Minerals are quite fresh. no 67.22000 2.93000 0516.98 51708 104 642 E 067 Rotary 01 121 123 026 0074 LEH Altered aphyric basalt (?) hyalocrystalline to intersertal Flow 74 Medium Plagioclase 20 20 0.2-2.0 Laths, prisms Prismatic crystalls tend to be more altered. Clinopyroxene 15 15 0.05-0.2 Augite Subhedral to anhedral Nearly colorless, hourglass extinction. Olivine 3-5 3-5 0.1-1.0 Euhedral to subhedral Completely altered to iddingsite. Opaques 20 20 N/A N/A Fe-Ti oxides (altered) plus tachylite(?) in interstices. Vesicles 15 0.1-3.0 Smectite and zeolite Rounded to irregular Clays 10 Interstices Light green smectite, well crystallized. Clays 30 Feldspar, cpx, "groundmass" Dark green smectite, micro- or cryptocrystalline. no 67.22000 2.93000 0844.20 84541 104 642 E 067 Rotary 02 052 054 012 0074 LEH Aphyric tholeiitic basalt Intersertal Flow 74 Medium Plagioclase 40 40 0.05-1.5 Laths and prismatic Clinopyroxene 25 25 0.1-0.6 Pigeonite and augite Subhedral to anhedral Very pale green, low 2V, positive, hourglass extinction. Olivine 2 2 ~0.1 Euhedral to subhedral Altered to smectite, some iddingsitization. Opaques 3 3 N/A Interstial, skeletal, subhedral Vesicles 15 0.2-1.5 Smectite Round Clays 30 Interstices Light greenish brown. Magnetite, nice skeletal structures, polishing scratches observable in reflected light under XP, also hematite. no 67.22000 2.93000 0845.70 84622 104 642 E 097 Rotary 01 054 056 017 0106 LEH Throughly altered flow Quenched Flow 106 Plagioclase 2 2 <0.1 Prismatic Plagioclase 7 7 N/A Swallowtail Quenched. Skeletons of incipient crystals, quenched, altered. Vesicles 0 Clays 90 All Cryptocrystalline. Thin section has been almost completely wiped during processing, possible relict perlitic structures. no 67.22000 2.93000 1108.90 110944 104 642 E 098 Rotary 01 106 108 014 0109 LEH Altered quenched flow Quenched, altered Flow 109 Plagioclase 1 1 0.1-1.2 Prismatic Mildly to severely altered. Plagioclase 10 10 N/A Swallowtail Quenched, altered percentage is for distinguishable plagioclase. Vesicles 20 Smectite-analcite-mordenite-adularia, in from rims. Clays 90 All Quenched textures preserved. Alteration assemblage typical of 100 - 150 degree C fluid. no 67.22000 2.93000 1115.80 111686 104 642 E 098 Rotary 02 062 064 013 0109 LEH Perlite (glassy flow) Perlitic Flow 109 Plagioclase 2 2 0.2-1.3 Prismatic Tends toward glomerophyric. Glass 98 98 N/A N/A Altered to perlite, light purplish brown. Vesicles 5 Smectite and zeolite Round Also includes fractures. no 67.22000 2.93000 1117.27 111789 104 642 E 099 Rotary 03 013 015 001 0112 LEH Altered quenched flow Quenched Flow 112 Plagioclase 15 15 N/A Swallowtail to skeletal Quenched. Clinopyroxene(?) 15 15 N/A Acicular Incipient crystal growth. Vesicles 0 Clays 70 All Light greenish brown and brown smectites(?). Carbonate >1 Feldspars Biaxial, negative, very high birefringence, colorless, rhombic cleavage. no 67.22000 2.93000 1128.20 112832 104 642 E 102 Rotary 02 026 028 007 0115 LEH Hydrothermally leached glassy flow Bleached Flow 115 Plagioclase 3-5 3-5 0.1-1.5 Prismatic Glomerophyric. Pyrite <<1 <<1 N/A Skeletal Replaced (reflected light). Vesicles N/A None Round Clays 95 All minerals Cryptocrystalline. Rock has been leached white. no 67.22000 2.93000 1155.00 115526 104 642 E 107 Rotary 02 124 126 011 0006 LEH Shallow level basalt dike Hyalocrystalline Dike 6 Opaques 40 40 N/A N/A Tachylite? and pyrite. Plagioclase <1 <1 0.05-0.7 Laths Clinopyroxene 40 40 N/A N/A Glass 10 10 N/A N/A Dark brown. Vesicles 0 Clays(?) 10 Interstices May be incipient crystallization structures? Grain size of plagioclase increases, amount of glass increases, pyrite increases near vein-like structure; no apparent increase in alteration. no 67.22000 2.93000 1192.79 119403