From b08be5d830627f52e88fe3667561e27bf5fa0372 Mon Sep 17 00:00:00 2001
From: Peter Powers <pmpowers@usgs.gov>
Date: Thu, 2 Sep 2021 12:02:18 -0600
Subject: [PATCH] doc edits
---
docs/pages/Model-Files.md | 2 +-
docs/pages/Source-Types.md | 3 +--
2 files changed, 2 insertions(+), 3 deletions(-)
diff --git a/docs/pages/Model-Files.md b/docs/pages/Model-Files.md
index 03a0c5203..1e573cb77 100644
--- a/docs/pages/Model-Files.md
+++ b/docs/pages/Model-Files.md
@@ -140,7 +140,7 @@ source-tree branches.
How MFDs are intialized (or realized) depends on the presence and contents of `mfd-config.json` and
`rate-tree.json` files. See the
[magnitude frequency distributions](./Magnitude-Frequency-Distributions.md) page for details on
-these files and the types of MFDs supported in _nshmp-haz_. Note also the
+these files and the types of MFDs supported in _nshmp-haz_.
## Rupture Sets
diff --git a/docs/pages/Source-Types.md b/docs/pages/Source-Types.md
index 67244fe9d..fc6d2042c 100644
--- a/docs/pages/Source-Types.md
+++ b/docs/pages/Source-Types.md
@@ -50,7 +50,6 @@ defines the bounds of the gridded seismicity source. A grid rupture set `mfd-tre
defined inline and always points to a tree in a
[`mfd-map`](./Magnitude-Frequency-Distributions.md#mfd-construction).
-
```json
[
{
@@ -106,7 +105,7 @@ some may contain depth values (intraslab sources), maximum magnitude caps, or ot
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
-`2018 CONUS NSHM > active-crust > grid-sources` for examples of both approaches.
+`2018 CONUS NSHM > active-crust > grid-sources` for examples of both approaches.
## Zone Sources
--
GitLab