Subject ASC0000izh

The Quarterly journal of the Geological Society of London.
v.51 (1895), Page 569 (1895)
Smithsonian Libraries
BHL Page 39016564

Keywords

sandy slate section Sulby River Snaefell geology slate river bank banding Sulby river Snaefell Lamplugh strain-slip close faulting slates 1895 rock formation fault fracture

Contributors

Species

Metadata

contributor

"Smithsonian Libraries"

has_illustrations_count

item_id

"120480"

original_size

{"width":1929,"height":3238}

page_id

"39016564"

page_no

"Page 569"

page_seq

"675"

sponsor

"Biodiversity Heritage Library"

volume

"v.51 (1895)"

year

"1895"

Drawn marks

drawing

{"keywords":["sandy slate","section","Sulby River","Snaefell","geology","slate","river bank","banding","Sulby river Snaefell","rock formation","fault","fracture"]}

inscription

{"text":["Sketch-section of strongly-banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards N. of 'Leadmine.' (Length = about 5 feet.)","y","Fig. 3 - Sketch-session of strongly-banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards N. of 'Lead-mine.' (Length=about 5 feet.)","z","B","N.W.","A","Fig. 3--Sketch section of strongly-banded sandy slate in eastern bank of Sulby River, Below Snaefell, 450 yards N. of 'Lead-mine.' (Length=about 5 feet.)","Sketch-section of strongly banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards north of 'lead mine'.","AA. Band of grit about half inch thick among puckered slates.\nBBB. Isolated pebble-like fragments of grit, presumably detached from band A.\ny-y-y-y. Planes of strain-slip or close faulting.\nz-z-z. Planes of the later shear-cleavage, striking N.40°W with the bedding, but crossing the folds with a dip of about 30°.","AA. Band of grit about 1/2 inch thick among puckered slates, chumpled and partially broken.\nBBB. Isolated pebble-like fragments of grit, presumably detached or squeezed out from the band A.\ny-y y-y. Planes of strain-slip or close-faulting.\nz-z-z. Planes of the later shear-cleavage, striking N.40°W. with the bedding, but crossing the folds with a dip of about 30°.","A A. Band of grit about 1/2 inch thick among puckered slates, crumpled and partially broken","B B B. Isolated pebble-like fragments of grit, presumably detached or squeezed out from the band A.","y-y-y-y. Planes of strain-slip or close-faulting.","z-z-z. Planes of the later sheer-cleavage, striking N.40[degrees] W. with the bedding, but crossing the folds with a dip of about 30[degrees]."]}

inscription

{"text":[" Sketch-section of strongly-banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards N. of 'Leadmine.' (Length = about 5 feet.)","S.E.","A"]}

Raw result

classification_count

group_id

"GSC000000a"

"5dc445fc7716a10004001ab8"

keywords

["sandy slate","section","Sulby River","Snaefell","geology","slate","river bank","banding","Sulby river Snaefell","Lamplugh","strain-slip","close faulting","slates","1895","rock formation","fault","fracture"]

page

"Page 569"

page_id

"39016564"

reduced

[{"type":"drawing","coords":[0,0,105,556,689,484],"value":{"keywords":["sandy slate","section","Sulby River","Snaefell","geology","slate","river bank","banding","Sulby river Snaefell","rock formation","fault","fracture"]}},{"type":"inscription","coords":[304,780,0,0,0,0],"value":{"text":["Sketch-section of strongly-banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards N. of 'Leadmine.' (Length = about 5 feet.)","y","Fig. 3 - Sketch-session of strongly-banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards N. of 'Lead-mine.' (Length=about 5 feet.)","z","B","N.W.","A","Fig. 3--Sketch section of strongly-banded sandy slate in eastern bank of Sulby River, Below Snaefell, 450 yards N. of 'Lead-mine.' (Length=about 5 feet.)","Sketch-section of strongly banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards north of 'lead mine'.","AA. Band of grit about half inch thick among puckered slates.\nBBB. Isolated pebble-like fragments of grit, presumably detached from band A.\ny-y-y-y. Planes of strain-slip or close faulting.\nz-z-z. Planes of the later shear-cleavage, striking N.40°W with the bedding, but crossing the folds with a dip of about 30°.","AA. Band of grit about 1/2 inch thick among puckered slates, chumpled and partially broken.\nBBB. Isolated pebble-like fragments of grit, presumably detached or squeezed out from the band A.\ny-y y-y. Planes of strain-slip or close-faulting.\nz-z-z. Planes of the later shear-cleavage, striking N.40°W. with the bedding, but crossing the folds with a dip of about 30°.","A A. Band of grit about 1/2 inch thick among puckered slates, crumpled and partially broken","B B B. Isolated pebble-like fragments of grit, presumably detached or squeezed out from the band A.","y-y-y-y. Planes of strain-slip or close-faulting.","z-z-z. Planes of the later sheer-cleavage, striking N.40[degrees] W. with the bedding, but crossing the folds with a dip of about 30[degrees]."]}},{"type":"inscription","coords":[717,743,0,0,0,0],"value":{"text":[" Sketch-section of strongly-banded sandy slate in eastern bank of Sulby River, below Snaefell, 450 yards N. of 'Leadmine.' (Length = about 5 feet.)","S.E.","A"]}}]

scale

0.4323656578134651

subject_id

"ASC0000izh"

volume

"v.51 (1895)"

year

"1895"