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Published byAbner Stokes Modified over 9 years ago
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Major geologic terranes and belts of Massachusetts 1
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The Boston Basin is in the Precambrian Avalon terrane. 2
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Geologic Section for the Boston Basin. Note the boundary fault at the left of the section. 4
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Stop 1 – Chestnut Hill Mall Roxbury Formation (Brookline Member) Outcrop sequence (from west to east) 5
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Types of Rocks found in the Chestnut Hill Mall Outcrops 15
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Conglomerate – large pebbles in sand-sized matrix 16
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The types of pebbles in the conglomerate tell us what rock(s) were being eroded. These rock fragments were deposited in the basin of deposition. 17
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Basalt clast Rhyolite clast 18
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Quartzite clast 19
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20 Sandstone – sand sized grains cemented together
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21 Siltstone – silt-sized pinkish color in center of picture
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22 Basalt – fine-grained mafic igneous rock
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23 Contact between conglomerate and sandstone
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24 Asymmetric ripple marks show current direction. Pencil points in direction of current. N
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25 Sill – a tabular intrusion injected parallel to existing layering. We can tell this is a sill, not a lava flow, because it has chilled margins. Close-up view of contact between sill and country rock. Note the fine- grained margin indicating rapid cooling.
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26 Direction of movement Slickenslides show sense and direction of movement on a fault plane.
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27 Glacial grooves and striations. Pencil shows sense of motion. N
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28 Physical weathering – growing tree wedging rock apart
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34 Stop 2- Beacon Street
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35 Along Beacon Street – conglomerate overlies siltstone
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36 Corner of Beacon Street and Bishopgate Road – Siltstone
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37 Soft sediment deformation
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38 Soft sediment deformation
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39 Soft sediment deformation
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40 Soft sediment deformation
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29 Stop 3 – Newton Conservation Area
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30 Roxbury Formation – conglomerate and sandstone Lava flow
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31 Roxbury conglomerate Note change in pebble (clast) size and density
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32 Channel fill in conglomerate Cross-bedding in channel fill Current direction
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33 Lava flow Vesicular basalt at top of lava flow
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