Fix markdown

docs/pages/Calculation-Configuration.md

@@ -106,7 +106,7 @@ T ≤ 10 s   | 0.000333, 0.000499, 0.000749, 0.00112, 0.00169, 0.00253, <br>0.00
   * [Site Specification](./Site-Specification.md#site-specification)
   * [Examples](../../etc/examples) (or
     [on GitLab](https://code.usgs.gov/ghsc/nshmp/nshmp-haz/-/tree/main/etc/examples))
-* [**Documentation Index**](../README.md)
+* [__Documentation Index__](../README.md)
 
 ---
 ![USGS logo](./images/usgs-icon.png) &nbsp;[U.S. Geological Survey](https://www.usgs.gov)

docs/pages/Functional-PSHA.md

@@ -119,10 +119,10 @@ foreach IMT {
 Break the traditional PSHA formulation down into discrete steps and preserve the data associated
 with each step:
 
-* **[1]** Source & Site parameterization
-* **[2]** Ground motion calculation (mean and standard deviation only)
-* **[3]** Exceedance curve calculation (per source)
-* **[4]** Recombine
+* __[1]__ Source & Site parameterization
+* __[2]__ Ground motion calculation (mean and standard deviation only)
+* __[3]__ Exceedance curve calculation (per source)
+* __[4]__ Recombine
 
 Whereas the traditional pipeline looks something like this:
 
@@ -132,9 +132,9 @@ The functional pipeline can be processed stepwise:
 
 ![image](images/psha-functional.png "PSHA functional pipeline")
 
-**Need a disaggregation?** Revisit and parse the results of steps 1 and 2
+__Need a disaggregation?__ Revisit and parse the results of steps 1 and 2
 
-**Need a response spectra?** Spawn more calculations, one for each IMT, at step 2.
+__Need a response spectra?__ Spawn more calculations, one for each IMT, at step 2.
 
 ## Benefits
 
@@ -161,7 +161,7 @@ The functional pipeline can be processed stepwise:
 
 ---
 
-[**Documentation Index**](../README.md)
+[__Documentation Index__](../README.md)
 
 ---
 ![USGS logo](./images/usgs-icon.png)  [U.S. Geological Survey](https://www.usgs.gov)

docs/pages/Ground-Motion-Models.md

@@ -44,7 +44,7 @@ The following sample `gmm-config.json` file applies the NGA-West 2 epistemic unc
 
 ## GMM Uncertainty Models
 
-*nshmp-haz* supports additional epistemic uncertainty models derived from the PEER NGA-West 1
+_nshmp-haz_ supports additional epistemic uncertainty models derived from the PEER NGA-West 1
 and PEER NGA-West 2 projects. These models both have factors for distance (`Rrup`) bins
 Rrup < 10 km, 10 km <= Rrup, < 30 km, and 30 km <= Rrup, and for magnitude bins M < 6.0, 6.0 <=
 M < 7.0, and 7.0 <= M. These models can be applied within the `gmm-config.json` file as shown in
@@ -52,7 +52,7 @@ the [GMM Uncertainty](#gmm-uncertainty) section above.
 
 ## GMMs By Tectonic Setting
 
-GMMs available in *nshmp-haz* are tabulated by tectonic setting below. See the javadocs for the
+GMMs available in _nshmp-haz_ are tabulated by tectonic setting below. See the javadocs for the
 [GMM Package](https://earthquake.usgs.gov/nshmp/docs/nshmp-lib/gov/usgs/earthquake/nshmp/gmm/package-summary.html)
 for implementation details of each GMM and comprehensive lists of GMM IDs.
 
@@ -93,7 +93,7 @@ NGA-East<br>[Goulet et al., 2017](https://peer.berkeley.edu/sites/default/files/
 [Shahjouei and Pezeshk, 2016](http://dx.doi.org/10.1785/0120140367) | NGA_EAST_SEED_SP16 | RotD50 | 3
 **Other**
 [Atkinson, 2008](http://dx.doi.org/10.1785/0120070199)<br>[Atkinson & Boore, 2011](http://dx.doi.org/10.1785/0120100270) | ATKINSON_08_PRIME | horizontal | 4
-[Atkinson & Boore, 2006](http://dx.doi.org/10.1785/0120050245) | *AB_06_\*<br>140BAR\|200BAR<br>none\|_AB\|_J* | horizontal | 4
+[Atkinson & Boore, 2006](http://dx.doi.org/10.1785/0120050245) | _AB\_06\_\*<br>140BAR\|200BAR<br>none\|\_AB\|\_J_ | horizontal | 4
 [Atkinson & Boore, 2006](http://dx.doi.org/10.1785/0120050245)<br>[Atkinson & Boore, 2011](http://dx.doi.org/10.1785/0120100270) | AB_06_PRIME | horizontal | 4
 [Campbell, 2003](http://dx.doi.org/10.1785/0120020002) | CAMPBELL_03<br>CAMPBELL_03_AB<br>CAMPBELL_03_J | Geometric mean | 4
 [Frankel et al., 1996](https://pubs.usgs.gov/of/1996/532/) | FRANKEL_96<br>FRANKEL_96_AB<br>FRANKEL_96_J | not specified | 4
@@ -112,24 +112,24 @@ for individual NGA-East component model IDs
 
 ### Subduction GMMs
 
-*Note: See the [GMM javadocs](https://earthquake.usgs.gov/nshmp/docs/nshmp-lib/gov/usgs/earthquake/nshmp/gmm/Gmm.html)
-for a comprehensive list of GMM IDs.*
+_Note: See the [GMM javadocs](https://earthquake.usgs.gov/nshmp/docs/nshmp-lib/gov/usgs/earthquake/nshmp/gmm/Gmm.html)
+for a comprehensive list of GMM IDs._
 
 Reference | ID | Component | Notes
 :---------|:---|:----------|:------:
 **NGA-Subduction**
-[Abrahamson & Gülerce, 2020](https://peer.berkeley.edu/sites/default/files/2020_25.pdf) | *AG_20_\*<br>GLOBAL\|CASCADIA\|ALASKA<br>INTERFACE\|SLAB<br>no basin\|_BASIN* | RotD50
-[Kuehn et al., 2020](https://peer.berkeley.edu/sites/default/files/2020_04_kuehn_final.pdf) | *KBCG_20_\*<br>GLOBAL\|CASCADIA\|ALASKA<br>INTERFACE\|SLAB<br>no basin\|_BASIN* | RotD50
-[Parker et al., 2020](https://peer.berkeley.edu/sites/default/files/2020_03_parker_final.pdf) | *PSHAB_20_\*<br>GLOBAL\|CASCADIA\|ALASKA<br>INTERFACE\|SLAB<br>no basin\|_BASIN* | RotD50
+[Abrahamson & Gülerce, 2020](https://peer.berkeley.edu/sites/default/files/2020_25.pdf) | _AG\_20\_\*<br>GLOBAL\|CASCADIA\|ALASKA<br>INTERFACE\|SLAB<br>no basin\|\_BASIN_ | RotD50
+[Kuehn et al., 2020](https://peer.berkeley.edu/sites/default/files/2020_04_kuehn_final.pdf) | _KBCG\_20\_\*<br>GLOBAL\|CASCADIA\|ALASKA<br>INTERFACE\|SLAB<br>no basin\|\_BASIN_ | RotD50
+[Parker et al., 2020](https://peer.berkeley.edu/sites/default/files/2020_03_parker_final.pdf) | _PSHAB\_20\_\*<br>GLOBAL\|CASCADIA\|ALASKA<br>INTERFACE\|SLAB<br>no basin\|\_BASIN_ | RotD50
 **Other**
-[Atkinson & Boore, 2003](http://dx.doi.org/10.1785/0120020156) | *AB_03\*<br>GLOBAL\|CASCADIA<br>INTERFACE\|SLAB<br>none\|_LOW_SAT*| horizontal |
+[Atkinson & Boore, 2003](http://dx.doi.org/10.1785/0120020156) | _AB\_03\*<br>GLOBAL\|CASCADIA<br>INTERFACE\|SLAB<br>none\|\_LOW_SAT_| horizontal |
 [Atkinson & Macias, 2009](http://dx.doi.org/10.1785/0120080147) | AM_09_INTERFACE<br>AM_09_INTERFACE_BASIN | Geometric mean | 1
-BC Hydro<br>[Abrahamson et al., 2016](http://dx.doi.org/10.1193/051712EQS188MR) | *BCHYDRO_12_\*<br>INTERFACE\|SLAB<br>none\|_BASIN<br>none\|_BACKARC* | Geometric mean |
-BC Hydro NGA<br>[Abrahamson et al., 2018](https://peer.berkeley.edu/sites/default/files/2018_02_abrahamson_9.10.18.pdf)² | *BCHYDRO_18_NGA_\*<br>INTERFACE\|SLAB<br>none\|_NO_EPI* | Geometric mean | 3
+BC Hydro<br>[Abrahamson et al., 2016](http://dx.doi.org/10.1193/051712EQS188MR) | _BCHYDRO\_12\_\*<br>INTERFACE\|SLAB<br>none\|\_BASIN<br>none\|\_BACKARC_ | Geometric mean |
+BC Hydro NGA<br>[Abrahamson et al., 2018](https://peer.berkeley.edu/sites/default/files/2018_02_abrahamson_9.10.18.pdf)² | _BCHYDRO\_18\_NGA\_\*<br>INTERFACE\|SLAB<br>none\|\_NO_EPI_ | Geometric mean | 3
 [McVerry et al., 2000](http://doi.org/10.5459/BNZSEE.39.1.1-58) | MCVERRY_00_INTERFACE<br>MCVERRY_00_SLAB<br>MCVERRY_00_VOLCANIC | Max-horizontal,<br>also supports geometric mean | 4
 [Youngs et al., 1997](http://dx.doi.org/10.1785/gssrl.68.1.58) | YOUNGS_97_INTERFACE<br>YOUNGS_97_SLAB | Geometric mean |
-[Zhao et al., 2006](http://dx.doi.org/10.1785/0120050122) | *ZHAO_06_\*<br>INTERFACE\|SLAB<br>none\|_BASIN* | Geometric mean |
-[Zhao et al., 2016](http://dx.doi.org/10.1785/0120150034)<br>[Zhao et al., 2016](http://dx.doi.org/10.1785/0120150056) | ZHAO_16_INTERFACE<br>ZHAO_16_SLAB<br>*ZHAO_16_UPPER_MANTLE* | Geometric mean<br>(random orientation) | 5
+[Zhao et al., 2006](http://dx.doi.org/10.1785/0120050122) | _ZHAO\_06\_\*<br>INTERFACE\|SLAB<br>none\|\_BASIN_ | Geometric mean |
+[Zhao et al., 2016](http://dx.doi.org/10.1785/0120150034)<br>[Zhao et al., 2016](http://dx.doi.org/10.1785/0120150056) | ZHAO_16_INTERFACE<br>ZHAO_16_SLAB<br>_ZHAO_16_UPPER_MANTLE_ | Geometric mean<br>(random orientation) | 5
 
 ¹ Interface only  
 ² Likely to be superseded by the final EQ Spectra paper  

docs/pages/Logic-Trees-&-Uncertainty.md

@@ -3,7 +3,7 @@
 The following page details the logic trees of epistemic uncertainty considered in NSHMs supported
 by *nshmp-haz*. Logic trees are represented in a NSHM using files ending in `-tree.json`.
 
-[[_TOC_]]
+[[*TOC*]]
 
 ## Terminology
 
@@ -15,34 +15,34 @@ alternative models.
 
 | Description | 2008  | 2014 | 2018 |
 |:----------- |:----- |:---- |:---- |
-| CEUS   | __0.1__ : AB_06 (140 bar)<br>__0.1__ : AB_06 (200 bar)<br>__0.1__ : CAMPBELL_03<br>__0.1__ : FRANKEL_96<br>__0.1__ : SILVA_02<br>__0.2__ : SOMERVILLE_01<br>__0.2__ : TORO_97<br>__0.1__ : TP_05 | __0.22__ : AB_06'<br>__0.08__ : ATKINSON_08'<br>__0.11__ : CAMPBELL_03<br>__0.06__ : FRANKEL_96<br>__0.15__ : PEZESHK_11<br>__0.06__ : SILVA_02<br>__0.10__ : SOMERVILLE_01<br>__0.11__ : TORO_97<br>__0.11__ : TP_05 | __0.667__ : NGA_EAST_USGS (17)<br>__0.333__ : NGA_EAST_SEEDS (14)<br>(common aleatory variability) |
-| Sigma Epistemic | _(none)_ | _(no change)_ | __0.2__ : USGS Panel<br>__0.8__ : EPRI |
-| Site Aleatory | _(none)_ | _(no change)_ | __0.185, 0.63, 0.185__ : Site ± σ |
+| CEUS   | **0.1** : AB_06 (140 bar)<br>**0.1** : AB_06 (200 bar)<br>**0.1** : CAMPBELL_03<br>**0.1** : FRANKEL_96<br>**0.1** : SILVA_02<br>**0.2** : SOMERVILLE_01<br>**0.2** : TORO_97<br>**0.1** : TP_05 | **0.22** : AB_06'<br>**0.08** : ATKINSON_08'<br>**0.11** : CAMPBELL_03<br>**0.06** : FRANKEL_96<br>**0.15** : PEZESHK_11<br>**0.06** : SILVA_02<br>**0.10** : SOMERVILLE_01<br>**0.11** : TORO_97<br>**0.11** : TP_05 | **0.667** : NGA_EAST_USGS (17)<br>**0.333** : NGA_EAST_SEEDS (14)<br>(common aleatory variability) |
+| Sigma Epistemic | *(none)* | *(no change)* | **0.2** : USGS Panel<br>**0.8** : EPRI |
+| Site Aleatory | *(none)* | *(no change)* | **0.185, 0.63, 0.185** : Site ± σ |
 
 ## Active Crustal Ground Motion Models
 
 | Description | 2008  | 2014 | 2018 |
 |:----------- |:----- |:---- |:---- |
-| WUS | __0.3333__ : BA_08<br>__0.3333__ : CB_08<br>__0.3334__ : CY_08 | __0.22__ : ASK_14<br>__0.22__ : BSSA_14<br>__0.22__ : CB_14<br>__0.22__ : CY_14<br>__0.22__ : IDRISS_14 | __0.25__ : ASK_14<br>__0.25__ : BSSA_14<br>__0.25__ : CB_14<br>__0.25__ : CY_14 |
-| Mean Epistemic | NGA-West1 (M,R)<br>__0.185__ : epi+<br>__0.630__ : off<br>__0.185__ : epi- | NGA-West2 (M,R)<br>__0.185__ : epi+<br>__0.630__ : off<br>__0.185__ : epi- | _(no change)_  |
+| WUS | **0.3333** : BA_08<br>**0.3333** : CB_08<br>**0.3334** : CY_08 | **0.22** : ASK_14<br>**0.22** : BSSA_14<br>**0.22** : CB_14<br>**0.22** : CY_14<br>**0.22** : IDRISS_14 | **0.25** : ASK_14<br>**0.25** : BSSA_14<br>**0.25** : CB_14<br>**0.25** : CY_14 |
+| Mean Epistemic | NGA-West1 (M,R)<br>**0.185** : epi+<br>**0.630** : off<br>**0.185** : epi- | NGA-West2 (M,R)<br>**0.185** : epi+<br>**0.630** : off<br>**0.185** : epi- | *(no change)*  |
 
 ## Subduction Ground Motion Models
 
 | Description | 2008  | 2014 | 2018 |
 |:----------- |:----- |:---- |:---- |
-| Cascadia<br>(interface) | __0.25__ : AB_03 (global)<br>__0.25__ : YOUNGS_97<br>__0.50__ : ZHAO_06 | __0.1__ : AB_03 (global)<br>__0.3__ : AM_09<br>__0.3__ : BCHYDRO_12<br>__0.3__ : ZHAO_06 | __0.3333__ : AM_09<br>__0.3334__ : BCHYDRO_12<br>__0.3333__ : ZHAO_06 |
-| Cascadia<br>(slab) | __0.25__ : AB_03 (global)<br>__0.25__ : AB_03 (cascadia)<br>__0.50__ : YOUNGS_97 | __0.1665__ : AB_03 (global, mod)<br>__0.1665__ : AB_03 (cascadia, mod)<br>__0.3330__ : BCHYDRO_12<br>__0.3340__ : ZHAO_06 | __0.5__ : BCHYDRO_12<br>__0.5__ : ZHAO_06 |
+| Cascadia<br>(interface) | **0.25** : AB_03 (global)<br>**0.25** : YOUNGS_97<br>**0.50** : ZHAO_06 | **0.1** : AB_03 (global)<br>**0.3** : AM_09<br>**0.3** : BCHYDRO_12<br>**0.3** : ZHAO_06 | **0.3333** : AM_09<br>**0.3334** : BCHYDRO_12<br>**0.3333** : ZHAO_06 |
+| Cascadia<br>(slab) | **0.25** : AB_03 (global)<br>**0.25** : AB_03 (cascadia)<br>**0.50** : YOUNGS_97 | **0.1665** : AB_03 (global, mod)<br>**0.1665** : AB_03 (cascadia, mod)<br>**0.3330** : BCHYDRO_12<br>**0.3340** : ZHAO_06 | **0.5** : BCHYDRO_12<br>**0.5** : ZHAO_06 |
 
 ## Fault Source Model (CEUS)
 
 | Model | Description | 2008 | 2014 | 2018 |
 |:----- |:----------- |:---- |:---- |:---- |
-| Deformation |  | __1.0__ : GEO | __0.1__ : BIRD<br>__0.8__ : GEO<br>__0.1__ : ZENG | _(no change)_  |
-| Rupture |  | __0.5__ : Full<br> __0.5__ : Partial | _(no change)_ | _(no change)_ |
-| Magnitude Scaling |  | __1.0__ : Somerville-01 (area) | _(no change)_  | _(no change)_  |
-| Maximum M¹ | Partial: epistemic | __0.2, 0.6, 0.2__ : M ± 0.2 | _(no change)_  | _(no change)_  |
-|           | Full : epistemic   | __0.2, 0.6, 0.2__ : M ± 0.2 | _(no change)_  | _(no change)_  |
-|           | Full : aleatory    |  M ± 0.24 (±2σ normal PDF)  | _(no change)_  | _(no change)_  |
+| Deformation |  | **1.0** : GEO | **0.1** : BIRD<br>**0.8** : GEO<br>**0.1** : ZENG | *(no change)*  |
+| Rupture |  | **0.5** : Full<br> **0.5** : Partial | *(no change)* | *(no change)* |
+| Magnitude Scaling |  | **1.0** : Somerville-01 (area) | *(no change)*  | *(no change)*  |
+| Maximum M¹ | Partial: epistemic | **0.2, 0.6, 0.2** : M ± 0.2 | *(no change)*  | *(no change)*  |
+|           | Full : epistemic   | **0.2, 0.6, 0.2** : M ± 0.2 | *(no change)*  | *(no change)*  |
+|           | Full : aleatory    |  M ± 0.24 (±2σ normal PDF)  | *(no change)*  | *(no change)*  |
 
 ¹ There are a very limited number of fault sources in CEUS  
 
@@ -50,59 +50,59 @@ alternative models.
 
 | Model | Description | 2008 | 2014 | 2018 |
 |:----- |:----------- |:---- |:---- |:---- |
-| Deformation |  | __1.0__ : GEO | __0.1__ : BIRD<br>__0.8__ : GEO<br>__0.1__ : ZENG | _(no change)_  |
-| Rupture | Partial | __0.333__ : IMW, __0.5__ : PNW | _(no change)_ | _(no change)_ |
-|         | Full    | __0.667__ : IMW, __0.5__ : PNW | _(no change)_ | _(no change)_ |
-| Magnitude Scaling |  | __1.0__ : WC_94 (length) | _(no change)_  | _(no change)_  |
-| Maximum M | Partial: epistemic | __0.2, 0.6, 0.2__ : M ± 0.2 | _(no change)_  | _(no change)_  |
-|           | Full : epistemic   | __0.2, 0.6, 0.2__ : M ± 0.2 | _(no change)_  | _(no change)_  |
-|           | Full : aleatory    |  M ± 0.24 (±2σ normal PDF)  | _(no change)_  | _(no change)_  |
-| Dip | Reverse & Strike-Slip | __1.0__ : assigned | _(no change)_ | _(no change)_ |
-|     | Normal | __0.2, 0.6, 0.2__ : 50 ± 10° | __0.2, 0.6, 0.2__ : 50±15° | _(no change)_ |
+| Deformation |  | **1.0** : GEO | **0.1** : BIRD<br>**0.8** : GEO<br>**0.1** : ZENG | *(no change)*  |
+| Rupture | Partial | **0.333** : IMW, **0.5** : PNW | *(no change)* | *(no change)* |
+|         | Full    | **0.667** : IMW, **0.5** : PNW | *(no change)* | *(no change)* |
+| Magnitude Scaling |  | **1.0** : WC_94 (length) | *(no change)*  | *(no change)*  |
+| Maximum M | Partial: epistemic | **0.2, 0.6, 0.2** : M ± 0.2 | *(no change)*  | *(no change)*  |
+|           | Full : epistemic   | **0.2, 0.6, 0.2** : M ± 0.2 | *(no change)*  | *(no change)*  |
+|           | Full : aleatory    |  M ± 0.24 (±2σ normal PDF)  | *(no change)*  | *(no change)*  |
+| Dip | Reverse & Strike-Slip | **1.0** : assigned | *(no change)* | *(no change)* |
+|     | Normal | **0.2, 0.6, 0.2** : 50 ± 10° | **0.2, 0.6, 0.2** : 50±15° | *(no change)* |
 
 ## Grid Source Model
 
 | Model | Description | 2008 | 2014 | 2018 |
 |:----- |:----------- |:---- |:---- |:---- |
-| Maximum M | WUS (exceptions) | __1.0__ : 7.0 | __0.9__ : 7.5 (truncated)<br>__0.1__ : 8.0 (tapered) | _(no change)_  |
-|           | CEUS (craton) | __0.1__ : 6.6<br>__0.2__ : 6.8<br>__0.5__ : 7.0<br>__0.2__ : 7.2 | __0.2__ : 6.5<br>__0.5__ : 7.0<br>__0.2__ : 7.5<br>__0.1__ : 8.0 | _(no change)_  |
-| Smoothing |  | __1.0__ : Fixed |__0.4__ : Adaptive<br>__0.6__ : Fixed | _(no change)_  |
-| Magnitude Scaling | CEUS & WUS | __1.0__ : WC_94 (length) | _(no change)_  | _(no change)_  |
-| Focal Mechanisms | Spatially Varying | __1.0__ : assigned | _(no change)_  | _(no change)_  |
-| Depth (zTor) | WUS, M < 6.5 | __1.0__ : 5.0 km | _(no change)_  | _(no change)_  |
-|              | WUS, M ≥ 6.5 | __1.0__ : 1.0 km | _(no change)_  | _(no change)_  |
-|              | CEUS, All M  | __1.0__ : 5.0 km | _(no change)_  | _(no change)_  |
+| Maximum M | WUS (exceptions) | **1.0** : 7.0 | **0.9** : 7.5 (truncated)<br>**0.1** : 8.0 (tapered) | *(no change)*  |
+|           | CEUS (craton) | **0.1** : 6.6<br>**0.2** : 6.8<br>**0.5** : 7.0<br>**0.2** : 7.2 | **0.2** : 6.5<br>**0.5** : 7.0<br>**0.2** : 7.5<br>**0.1** : 8.0 | *(no change)*  |
+| Smoothing |  | **1.0** : Fixed |**0.4** : Adaptive<br>**0.6** : Fixed | *(no change)*  |
+| Magnitude Scaling | CEUS & WUS | **1.0** : WC_94 (length) | *(no change)*  | *(no change)*  |
+| Focal Mechanisms | Spatially Varying | **1.0** : assigned | *(no change)*  | *(no change)*  |
+| Depth (zTor) | WUS, M < 6.5 | **1.0** : 5.0 km | *(no change)*  | *(no change)*  |
+|              | WUS, M ≥ 6.5 | **1.0** : 1.0 km | *(no change)*  | *(no change)*  |
+|              | CEUS, All M  | **1.0** : 5.0 km | *(no change)*  | *(no change)*  |
 
 ## Fault Source Model (CA, UCERF3)
 
 | Model | 2014 | 2018 |
 |:----- |:---- |:---- |
-| Fault | __0.5__ : FM3.1<br> __0.5__ : FM3.2 | _(no change)_ |
-| Deformation | __0.1__ : ABM<br>__0.3__ : BIRD<br>__0.3__ : GEO<br>__0.3__ : ZENG | _(no change)_  |
-| Scaling Relationship<br>(mag-area & slip-length)| __0.2__ : ELLS_B<br>__0.2__ : ELLS_B (sqrt-L)<br>__0.2__ : HB_08<br>__0.2__ : SHAW_09<br>__0.2__ : SHAW_09 (csd) | _(no change)_  |
-| Slip Distribution | __0.5__ : Tapered<br>__0.5__ : Boxcar | _(no change)_ |
-| M ≥ 5 rate (yr⁻¹) | __0.1__ : 6.5<br>__0.6__ : 7.9<br>__0.3__ : 9.6 | _(no change)_  |
-| Inversion Constraint | __1.0__ : UCERF2 (CH) | _(no change)_  |
-| Fault Mo Rate | __1.0__ : off |  _(no change)_  |
+| Fault | **0.5** : FM3.1<br> **0.5** : FM3.2 | *(no change)* |
+| Deformation | **0.1** : ABM<br>**0.3** : BIRD<br>**0.3** : GEO<br>**0.3** : ZENG | *(no change)*  |
+| Scaling Relationship<br>(mag-area & slip-length)| **0.2** : ELLS_B<br>**0.2** : ELLS_B (sqrt-L)<br>**0.2** : HB_08<br>**0.2** : SHAW_09<br>**0.2** : SHAW_09 (csd) | *(no change)*  |
+| Slip Distribution | **0.5** : Tapered<br>**0.5** : Boxcar | *(no change)* |
+| M ≥ 5 rate (yr⁻¹) | **0.1** : 6.5<br>**0.6** : 7.9<br>**0.3** : 9.6 | *(no change)*  |
+| Inversion Constraint | **1.0** : UCERF2 (CH) | *(no change)*  |
+| Fault Mo Rate | **1.0** : off |  *(no change)*  |
 
 ## Grid Source Model (CA, UCERF3)
 
 | Model | 2014 | 2018 |
 |:----- |:---- |:---- |
-| Grid: Maximum M | __0.1__ : 7.3<br>__0.8__ : 7.6<br>__0.1__ : 7.9 | _(no change)_  |
-| Grid: Smoothing | __0.5__ : Adaptive<br>__0.5__ : Fixed | _(no change)_  |
-| Grid: Focal Mechanisms | __1.0__ : assigned | _(no change)_  |
-| Magnitude Scaling | __1.0__ : WC_94 (length) | _(no change)_  |
+| Grid: Maximum M | **0.1** : 7.3<br>**0.8** : 7.6<br>**0.1** : 7.9 | *(no change)*  |
+| Grid: Smoothing | **0.5** : Adaptive<br>**0.5** : Fixed | *(no change)*  |
+| Grid: Focal Mechanisms | **1.0** : assigned | *(no change)*  |
+| Magnitude Scaling | **1.0** : WC_94 (length) | *(no change)*  |
 
 ## Subduction seismic source model
 
 | Model | 2008 | 2014 | 2018 |
 |:----- |:---- |:---- |:---- |
-| Rupture | __0.67__ : Full<br>__0.33__ : Partial | __1.0__ : Full<br>__0.5__ : Partial (segmented)<br>__0.5__ : Partial (unsegmented) | _(no change)_ |
-| Magnitude Scaling | __1.0__ : Youngs et al. (length) | __0.334__ : Strasser et al. (2010)<br>__0.333__ : Murotani et al. (2008)<br>__0.333__ : Papazachos et al. (2004)  | _(no change)_  |
-| Magnitude Uncertainty | __0.2, 0.6, 0.2__ : M±0.2 | _(none)_  | _(no change)_  |
-| Depth | __0.5__ : Base<br>__0.2__ : Bottom<br>__0.2__ : Middle<br>__0.1__ : Top | __0.3__ : Bottom<br>__0.5__ : Middle<br>__0.2__ : Top | _(no change)_ |
-| Slab: Maximum M | __1.0__ : 7.2 | __0.9__ : 7.5<br>__0.1__ : 8.0 | _(no change)_ |
+| Rupture | **0.67** : Full<br>**0.33** : Partial | **1.0** : Full<br>**0.5** : Partial (segmented)<br>**0.5** : Partial (unsegmented) | *(no change)* |
+| Magnitude Scaling | **1.0** : Youngs et al. (length) | **0.334** : Strasser et al. (2010)<br>**0.333** : Murotani et al. (2008)<br>**0.333** : Papazachos et al. (2004)  | *(no change)*  |
+| Magnitude Uncertainty | **0.2, 0.6, 0.2** : M±0.2 | *(none)*  | *(no change)*  |
+| Depth | **0.5** : Base<br>**0.2** : Bottom<br>**0.2** : Middle<br>**0.1** : Top | **0.3** : Bottom<br>**0.5** : Middle<br>**0.2** : Top | *(no change)* |
+| Slab: Maximum M | **1.0** : 7.2 | **0.9** : 7.5<br>**0.1** : 8.0 | *(no change)* |
 
 * Full: a.k.a. 'characteristic'
 * Partial: a.k.a. 'Gutenberg-Richter' or 'floating'

docs/pages/Model-Editions.md

@@ -99,7 +99,7 @@ one of the dynamic editions is likely better.
   * [Model Editions](./Model-Editions.md#model-editions)
   * [Logic Trees & Uncertainty](./Logic-Trees-&-Uncertainty.md#logic-trees-&-uncertainty)
   * [Code Versions](./Code-Versions.md#code-versions)
-* [**Documentation Index**](../README.md)
+* [__Documentation Index__](../README.md)
 
 ---
 ![USGS logo](./images/usgs-icon.png)  [U.S. Geological Survey](https://www.usgs.gov)

docs/pages/Model-Structure.md

@@ -139,9 +139,9 @@ See also: [Grid Source Type](./Source-Types.md#grid-sources)
 
 Zone sources specify a single rate that is distributed over a GeoJSON `Polygon` using point source
 rupture models. Presently, there is a 1:1 mapping of source zones to their associated rate files.
-*__Note:__ The rate file approach will be discouraged and/or deprecated in the near future in favor
+_**Note:** The rate file approach will be discouraged and/or deprecated in the near future in favor
 of dynamically computing rates over a zone from a single value or `rate-tree.json` when the loading
-a model.*
+a model._
 
 ```text
 zone/

docs/pages/Site-Specification.md

@@ -107,7 +107,7 @@ outside the 'calculation' polygon are set to zero. For an example, see the
   * [Site Specification](./Site-Specification.md#site-specification)
   * [Examples](../../etc/examples) (or
     [on GitLab](https://code.usgs.gov/ghsc/nshmp/nshmp-haz/-/tree/main/etc/examples))
-* [**Documentation Index**](../README.md)
+* [__Documentation Index__](../README.md)
 
 ---
 ![USGS logo](./images/usgs-icon.png)  [U.S. Geological Survey](https://www.usgs.gov)

docs/pages/Source-Types.md

@@ -12,15 +12,15 @@ geometry itself is unknown or very poorly defined.
 
 [[_TOC_]]
 
-Source models for use with *nshmp-haz* are defined using [JSON](https://www.json.org) and
-[GeoJSON](https://geojson.org). *nshmp-haz* makes determinations about how to represent a source
+Source models for use with _nshmp-haz_ are defined using [JSON](https://www.json.org) and
+[GeoJSON](https://geojson.org). _nshmp-haz_ makes determinations about how to represent a source
 based on a GeoJSON geometry type in conjunction with supporting JSON configuration files. Example
 source configuration files, `*-config.json`, are provided with each source type description.
 Configuration files must be fully specified with `null` JSON member values used to specify 'do
 nothing' where appropriate. Any configuration member value in ALL_CAPS indicates the value is one
 of a fixed number of options commonly referred to as an enum.
 
-__Note on Coordinates:__ *nshmp-haz* supports longitude and latitude values in the closed ranges
+__Note on Coordinates:__ _nshmp-haz_ supports longitude and latitude values in the closed ranges
 `[-360°‥360°]` and `[-90°‥90°]`. Note, however, that mixing site and/or source coordinates across
 the antimeridian (the -180° to 180° transition) will yield unexpected results. For Pacific models
 and calculations, always use positive or negative longitudes exclusively.
@@ -43,7 +43,7 @@ Grid sources are represented in a model using a logic tree with a `rupture-sets.
 ruptures on each branch.  Because gridded seismicity models may be governed by regionally
 varying MFD properties (e.g. `mMax`), rupture sets for grids are defined in a JSON array.
 
-**rupture-sets.json**: Defines an array of one or more rupture sets. Multiple rupture sets are
+__rupture-sets.json__: Defines an array of one or more rupture sets. Multiple rupture sets are
 used to model regional differences in MFD properties such as maximum magnitude. The `feature`
 member points to the ID of a geojson feature (in the `grid-sources/features` directory) that
 defines the bounds of the gridded seismicity source. A grid rupture set `mfd-tree` is never
@@ -62,7 +62,7 @@ defined inline and always points to a tree in a
 ]
 ```
 
-**grid-config.json**: A `grid-depth-map` defines a mapping of magnitude ranges to logic trees of
+__grid-config.json__: A `grid-depth-map` defines a mapping of magnitude ranges to logic trees of
 depth distributions. The map can use arbitrary names as keys, but the magnitude ranges defined by
 each member must be non-overlapping. The magnitude ranges are interpreted as closed (inclusive) –
 open (exclusive), e.g. [mMin..mMax). `maxDepth` constrains the maximum depth of any pseudo fault
@@ -104,7 +104,7 @@ to upper-right). While most gridded rate files contain columns of longitude, lat
 some may contain depth values (intraslab sources), maximum magnitude caps, or other values. Scaled
 spatial PDFs are the preferred approach to modeling regional rate variations, however it is also
 possible to define explicit MFDs at each grid node. To do so, the `spatial-pdf` member
-of a **rupture-sets.json** is replaced with `grid-mfds`. See
+of a __rupture-sets.json__ is replaced with `grid-mfds`. See
 `2018 CONUS NSHM > active-crust > grid-sources` for examples of both approaches.
 
 ## Zone Sources
@@ -146,7 +146,7 @@ directly.
 }
 ```
 
-**zone-config.json:** Zone source model configuration is identical to a grid source configuration.
+__zone-config.json:__ Zone source model configuration is identical to a grid source configuration.
 
 ```json
 {
@@ -182,7 +182,7 @@ they occur in multiple locations on the fault surface with appropriately scaled
 associated with finite fault models may be explicitly defined or derived from slip rates.
 Fault rupture rates may be modeled using explicitly defined MFDs or logic trees of slip rate.
 
-**fault-source.geojson**: Defines the geometry and properties of a single source. In the example
+__fault-source.geojson__: Defines the geometry and properties of a single source. In the example
 below the presence of a `rate-map` property indicates MFDs should be constructed from the supplied
 slip rates and using the weights defined in a `rate-tree.json`.
 
@@ -229,7 +229,7 @@ slip rates and using the weights defined in a `rate-tree.json`.
 }
 ```
 
-**fault-config.json**: Controls the point spacing on a gridded surface used to realize the fault
+__fault-config.json__: Controls the point spacing on a gridded surface used to realize the fault
 geometry as well as define the models to use for magnitude scaling and rupture floating. Dip
 variations and an associated slip-rate scaling model are also supported for normal faults.
 
@@ -243,7 +243,7 @@ variations and an associated slip-rate scaling model are also supported for norm
 }
 ```
 
-**rupture-set.json**: When a fault source is represented with a logic tree a
+__rupture-set.json__: When a fault source is represented with a logic tree a
 `rupture-set.json` defines the ruptures for each branch. A rupture set _may_ also define custom
 properties and _may_ also contain a `sections` member that defines the fault sections for the
 rupture set (see note on fault section stitching, [below](#fault-section-stitching)).
@@ -281,7 +281,7 @@ as the joint probability of exceeding ground motions from each independent event
 a cluster may only have an mfd-tree composed of `Mfd.Type.SINGLE` MFDs and the mfd-trees must
 match across all sources in a cluster (i.e. each mfd-tree has the same IDs and weights).
 
-**cluster-set.json** A specialized type of rupture set, this file defines the array of fault
+__cluster-set.json__ A specialized type of rupture set, this file defines the array of fault
 rupture sets that make up a 'cluster'. As with fault sources, the nested rupture sets in a cluster
 set _may_ define `properties` and `sections` members.
 
@@ -317,10 +317,10 @@ U.S. Fault system source sets require three files: `rupture_set.json`, `sections
 logic tree. Note that system sources _may_ have complementary gridded seismicity source models
 with matching logic trees.
 
-**rupture-set.json**: Provides identifying information for the ruptures defined in the adjacant
+__rupture-set.json__: Provides identifying information for the ruptures defined in the adjacant
 sections and ruptures files.
 
-**sections.geojson**: defines a feature collection of the fault sections in a fault network.
+__sections.geojson__: defines a feature collection of the fault sections in a fault network.
 Because fault sections are derived by dividing larger faults into subsections, section features
 contain several properties that differ from standalone fault section source models (e.g.
 `dip-direction`).
@@ -356,7 +356,7 @@ contain several properties that differ from standalone fault section source mode
 }
 ```
 
-**ruptures.csv**: Defines the properties of every rupture. The last column in a rupture file
+__ruptures.csv__: Defines the properties of every rupture. The last column in a rupture file
 defines the ordered array of participating fault section IDs using the shorthand
 `1127:1131-2411:2412`. Colons denote continous ranges of sections and hyphens denote breaks.
 
@@ -383,7 +383,7 @@ using an `slab-config.json` file.
   * [Magnitude Frequency Distributions (MFDs)](./Magnitude-Frequency-Distributions.md#magnitude-frequency-distributions)
   * [Rupture Scaling Relations](./Rupture-Scaling-Relations.md#rupture-scaling-relations)
   * [Ground Motion Models (GMMs)](./Ground-Motion-Models.md#ground-motion-models)
-* [**Documentation Index**](../README.md)
+* [__Documentation Index__](../README.md)
 
 ---
 ![USGS logo](./images/usgs-icon.png)  [U.S. Geological Survey](https://www.usgs.gov)

docs/pages/USGS-Models.md

@@ -20,10 +20,10 @@ Each model region has a dedicated repository with version tags marking different
 
 * [Conterminous U.S.](https://code.usgs.gov/ghsc/nshmp/nshms/nshm-conus)
 * [Hawaii](https://code.usgs.gov/ghsc/nshmp/nshms/nshm-hawaii)  
-* Alaska - _update not yet published_
-* Guam & Marianas - _update not yet published_  
-* Puerto Rico & U.S. Virgin Islands - _update not yet published_  
-* Samoa & Pacific Islands - _update not yet published_  
+* Alaska - *update not yet published*
+* Guam & Marianas - *update not yet published*  
+* Puerto Rico & U.S. Virgin Islands - *update not yet published*  
+* Samoa & Pacific Islands - *update not yet published*  
 
 ---
 

docs/pages/Web-Services.md

@@ -73,7 +73,7 @@ Open browser to [http://localhost:8080/](http://localhost:8080/).
 
 #### Docker Memory on Mac
 
-By default, Docker Desktop for Mac is set to use 2 GB runtime memory. To run nshmp-haz-ws, the 
+By default, Docker Desktop for Mac is set to use 2 GB runtime memory. To run nshmp-haz-ws, the
 memory available to Docker must be [increased](https://docs.docker.com/docker-for-mac/#advanced)
 to a minimum of 4 GB.
 

etc/examples/1-hazard-curve/README.md

@@ -49,4 +49,4 @@ In the next example, we'll override the model supplied configuration with a cust
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

etc/examples/2-custom-config/README.md

@@ -47,4 +47,4 @@ __Results directory structure:__
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

etc/examples/3-sites-file/README.md

@@ -45,4 +45,4 @@ __Results directory structure:__
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

etc/examples/4-hazard-map/README.md

@@ -37,4 +37,4 @@ __Results directory structure:__
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

etc/examples/5-complex-model/README.md

@@ -76,4 +76,4 @@ __Results directory structure:__
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

etc/examples/6-enhanced-output/README.md

@@ -64,4 +64,4 @@ __Results directory structure:__
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

etc/examples/7-disaggregation/README.md

@@ -65,4 +65,4 @@ will not be saved.
 
 ---
 
-* [**Documentation Index**](../../../docs/README.md)
+* [__Documentation Index__](../../../docs/README.md)

gradle/node.gradle

@@ -10,8 +10,8 @@ task nodeInstall(type: NpmTask) {
   description "Install markdownlint-clia and yamllint with NPM"
   args = [
     "install",
-    "markdownlint-cli",
-    "yaml-lint",
+    "markdownlint-cli@0.31.1",
+    "yaml-lint@1.2.4",
     "--save-dev",
     "--loglevel",
     "error"