![Transactions . Fig.37 * XXXI. VOL. xxiir.—23 udlsy ^ PouUa. E..jr3. .V. r. 354 THE GENESIS OF ORE-DEPOSITS. Description of Figures. Fig. 40.—Ideal section through Bohutin, near Przibram. a, Cam-brian sandstone; Transactions . Fig.37 * XXXI. VOL. xxiir.—23 udlsy ^ PouUa. E..jr3. .V. r. 354 THE GENESIS OF ORE-DEPOSITS. Description of Figures. Fig. 40.—Ideal section through Bohutin, near Przibram. a, Cam-brian sandstone;](https://c8.alamy.com/comp/2CE185M/transactions-fig37-xxxi-vol-xxiir23-udlsy-pouua-ejr3-v-r-354-the-genesis-of-ore-deposits-description-of-figures-fig-40ideal-section-through-bohutin-near-przibram-a-cam-brian-sandstone-b-pre-carabrian-schists-c-granite-cz-main-fault-fissure-e-e-diorite-dikes-note-at-przibram-itself-the-pre-cara-brian-schists-constitute-the-hanging-wall-of-the-main-fault-fissure-tothe-entire-depth-of-the-minesabout-1110-meters-or-3600-feet-fig-41diagrammatic-representation-of-the-structure-of-theverespatak-ore-bodies-volbura-showing-the-ore-replacing-thewashed-o-2CE185M.jpg)
Transactions . Fig.37 * XXXI. VOL. xxiir.—23 udlsy ^ PouUa. E..jr3. .V. r. 354 THE GENESIS OF ORE-DEPOSITS. Description of Figures. Fig. 40.—Ideal section through Bohutin, near Przibram. a, Cam-brian sandstone;
![Transactions . h Bohutin, near Przibram. a, Cam-brian sandstone; b, pre-Carabrian schists; c, granite; cZ, main fault-fissure ; e e, diorite dikes. (Note : At Przibram itself the pre-Cara-brian schists constitute Transactions . h Bohutin, near Przibram. a, Cam-brian sandstone; b, pre-Carabrian schists; c, granite; cZ, main fault-fissure ; e e, diorite dikes. (Note : At Przibram itself the pre-Cara-brian schists constitute](https://c8.alamy.com/comp/2CE163M/transactions-h-bohutin-near-przibram-a-cam-brian-sandstone-b-pre-carabrian-schists-c-granite-cz-main-fault-fissure-e-e-diorite-dikes-note-at-przibram-itself-the-pre-cara-brian-schists-constitute-the-hanging-wall-of-the-main-fault-fissure-tothe-entire-depth-of-the-minesabout-1110-meters-or-3600-feet-fig-41diagrammatic-representation-of-the-structure-of-theverespatak-ore-bodies-volbura-showing-the-ore-replacing-thewashed-out-cement-of-a-breccia-mostly-of-porphyritic-fragments-fig-42the-same-only-conglomerate-instead-of-breccia-fig-43vertical-s-to-n-secti-2CE163M.jpg)
Transactions . h Bohutin, near Przibram. a, Cam-brian sandstone; b, pre-Carabrian schists; c, granite; cZ, main fault-fissure ; e e, diorite dikes. (Note : At Przibram itself the pre-Cara-brian schists constitute
![The floor of a rectangular banquet hall has an area of 3,600 square meters. The length is 90m. a.) What is the width of the banquet hall? b.) A square banquet hall The floor of a rectangular banquet hall has an area of 3,600 square meters. The length is 90m. a.) What is the width of the banquet hall? b.) A square banquet hall](https://useruploads.socratic.org/wN3niO1JRU2B6UmX02F0_Solution%20a%20Image.png)