Springs Monitoring at Montezuma Castle National Monument: 2024

Bryn Callie, Annika Munson, Cheryl McIntyre, Andy Hubbard

Edited by Tani Hubbard

Please cite this publication as:

Callie, B., A. Munson, C. McIntyre, and A. Hubbard. 2026. Springs Monitoring at Montezuma Castle National Monument: 2024. Science Report NPS/SR—2026/448. National Park Service, Fort Collins, Colorado. https://doi.org/10.36967/2318587

Abstract

The Sonoran Desert Inventory and Monitoring Network monitors one spring, Expansion Spring, each year at Montezuma Castle National Monument, Arizona. We assess the condition of the site, measure spring discharge and wetted extent (area that contained water), collect core water quality and water chemistry data, note the wetland plants and invasive plants and animals present, and sample for environmental DNA (eDNA) to inventory springs for rare species, invasive species, and pathogens. Each spring is somewhat unique, and Arizona has not adopted water quality standards that apply across the diversity of springs in the state. Therefore, we continue to collect water quality data at the spring to form a baseline reference of natural variance. We did not detect any of our eDNA target organisms at Expansion Spring in 2024. Expansion Spring surfaces at the base of a limestone outcrop and flows down a narrow channel to a large, shallow pool. The site is well-shaded by cottonwoods. The spring had water during our visit in 2024 but we were unable to find the temperature sensor, so there are no data on water persistence for the rest of the year. Prior data show the spring has had water throughout most years. The site is largely undisturbed, but we detected invasive crayfish for the first time in 2024, perhaps due to winter floodwater from Beaver Creek flushing these invasive animals into the spring. No invasive plants and no wetland plants were found in 2024.

A large round pool of water reflecting the steep banks surrounding it that are covered in desert shrubs, trees, and rock outcrops with rugged desert mountains in the distance.
Montezuma Castle National Monument, Arizona.

NPS

Background

Springs, seeps, and tinajas (discrete pools in a rock basin or impoundments in bedrock) are small, relatively rare biodiversity hotspots in arid lands. They are the primary connection between groundwater and surface water and are important water sources for plants and animals. At Montezuma Castle National Monument, Sonoran Desert Network scientists study how ecosystems may be changing by taking measurements of key resources, or “vital signs,” year after year—much as a doctor keeps track of a patient’s vital signs. This long-term ecological monitoring provides early warning of potential problems, allowing managers to mitigate them before they become worse. We monitor one spring at Montezuma Castle National Monument each year. The most important questions we ask are about persistence (How long was there water in the spring?) and water quantity (How much water was in the spring?).

Climate change is an emerging influence on springs in the American Southwest. Possible changes include increased air temperatures, evaporation rates, and drought intensity; more frequent and extreme rainfall and heat events; and potentially reduced precipitation in the winter and spring. These changes may cause springs to experience reduced flow or even go dry, which may disrupt ecological functions, reduce species diversity, and negatively impact visitor experience.

Springs reporting is by calendar year starting in 2024. Prior to 2024, springs data were summarized by water year (WY), which ran from October through September (e.g., WY2023 started in October 2022 and went through September 2023). In 2024, springs sampling at Montezuma Castle National Monument occurred on 13 May. Water persistence is monitored continuously throughout the year, but in this report, we only present 2024 persistence data up to the sampling visit date for Expansion Spring.

Methods

Sonoran Desert Network springs monitoring is organized into the four modules described below (see McIntyre et al. 2018 for additional details) and eDNA inventories. All data have undergone certification processes to ensure they have been verified and validated for accuracy, are complete, and are fully documented. Data used in this report are available to park staff on the NPS DataStore and can be provided upon request.

Site Characterization

This module provides context for interpreting change in the other modules. We record GPS locations, draw a site diagram, and describe the spring type (e.g., helocrene, limnocrene, rheocrene, or tinaja) and its associated vegetation in this module. Helocrene springs emerge as low-gradient wetlands, limnocrene springs emerge as pools, and rheocrene springs emerge as flowing streams. This module is completed once every five years or after significant events.

Site Condition

We estimate the level of natural and anthropogenic disturbances and the level of stress on vegetation and soils at the spring on a scale of 1–4, where 1 = undisturbed, 2 = slightly disturbed, 3 = moderately disturbed, and 4 = highly disturbed. Types of natural disturbances can include flooding, drying, fire, wildlife impacts, windthrow of trees and shrubs, beaver activity, and insect infestations. Anthropogenic disturbances can include roads, off-highway vehicle trails, hiking trails, livestock and feral-animal impacts, removal of invasive non-native plants, flow modification, and other evidence of human use of the spring site. We take repeat photographs from the same location and perspective to show the spring and its landscape context. We note the presence of certain obligate wetland plant species (plant species that almost always occur only in wetlands), facultative wetland plant species (plant species that usually occur in wetlands, but also occur in other habitats), and invasive non-native crayfish and American bullfrog (Rana catesbeiana). We also record the density of invasive non-native plants using a qualitative scale (1–5 plants, scattered patches, evenly distributed patches, or a matrix). We complete the site condition module during each springs monitoring visit.

Water Quantity

We measure the persistence of surface water, amount of spring discharge, and wetted extent (area that contained water). To estimate persistence, we analyze the variance of temperature measurements taken by two logging thermometers placed at or near the orifice (spring opening). Because water mediates variation in diurnal temperatures, data from a submerged sensor will show less daily variation than data from an exposed, open-air sensor; this tells us when the spring was wet or dry. Surface discharge is measured with a timed sample of water volume. Wetted extent is a systematic measurement of the physical length (up to 100 m), width, and depth of surface water. It is assessed using a technique for either standing water (e.g., limnocrene and helocrene springs) or flowing water (e.g., rheocrene springs). We complete discharge and wetted extent measurements during each visit when possible. Water persistence measurements are continuous throughout the year.

Water Quality

We measure core water quality and water chemistry parameters. Core water quality parameters include water temperature, pH, specific conductivity (a measure of dissolved compounds and contaminants), dissolved oxygen (how much oxygen is present in the water), and total dissolved solids (an indicator of potentially undesirable compounds). Discrete measurements of these parameters are collected with a multiparameter meter. If the meter fails calibration checks, we do not present data. Water chemistry is assessed by collecting surface water samples and estimating the concentration of major ions with a photometer in the field. These parameters are collected at one or more sampling locations within a spring, but we only present data for the primary sampling location. Each perennial spring is somewhat unique, and Arizona has not adopted applicable water quality standards for most perennial springs, including Expansion Spring. Ongoing, long-term data collection at each spring will improve our understanding of the natural range in water quality and water chemistry parameters for a given site. We complete the water quality module during each visit when possible. The total number of measurements value we present in the data tables is across all years and may reflect multiple measurements taken in a single year and missing values in other years for a variety of reasons.

eDNA Inventory of Rare Species, Invasive Species, and Pathogens

We inventory rare species, invasive species, and pathogens in perennial springs using environmental DNA (eDNA) techniques. One or more 5-liter water samples are collected and filtered (using a 5 µm self-preserving mesh filter) from Expansion Spring using a Smith Root Citizen Science Pump. Samples are preserved in ethanol prior to DNA extraction and analysis by the Goldberg Lab at Washington State University.

Target Organisms for the eDNA Project

  • The invasive non-native American bullfrog (Rana catesbeiana) that has been observed within Montezuma Castle National Monument along Beaver and Wet Beaver creeks (Schmidt et al. 2006).

  • The pathogen chytrid fungus (Batrachochytrium dendrobatidis), a major threat to amphibians globally that is currently expanding in the American Southwest but has not been previously detected in the park.

  • Ranaviruses, pathogens that can infect amphibians and produce 90–100% mortality in tadpoles and adults and can persist in affected wetlands. Ranaviruses have not been previously detected at the park.

  • The native Chiricahua leopard frog (Rana chiricahuensis), a federally designated threatened species with a range that historically included the watersheds within the monument (Holycross et al. 2022). The current known range and defined critical habitat occur south of the park (Schmidt et al. 2006), though there have been recent detections nearby (A. Owens, personal communication).

  • The native lowland leopard frog (Rana yavapaiensis), a species of conservation concern that has historically been found within the park (Schmidt et al. 2006) but may be locally extirpated.

  • The native aquatic northern Mexican garter snake (Thamnophis eques megalops), a federally designated threatened species that has historically been found within the park (Schmidt et al. 2006) and may still occur within its boundaries in suitable wetland habitats. Designated critical habitat includes the nearby Verde River.

  • The native jaguar (Panthera onca), a federally designated endangered species that historically was found within the park, although current designated critical habitat for jaguar recovery is located well south of the Verde Valley.

Results

Expansion Spring

Expansion Spring (Figures 1 and 2) is a rheocrene spring (a spring that emerges into one or more stream channels), which surfaces from the base of a limestone outcrop in a side canyon and flows into Beaver Creek. Water flows down a narrow channel to a large, shallow pool located about a meter above the river. The site is well-shaded by cottonwood trees. The 2024 visit occurred on 13 May, and the spring contained water.

Figure 1. Water flowing from the base of a rocky, root-covered bank into a small channel.
Figure 1. Expansion Spring at Montezuma Castle National Monument, May 2024.

NPS

Figure 2. A small brook entering a pool of water with small plants on the banks and large trees and branches hanging above it.
Figure 2. Expansion Spring and Beaver Creek at Montezuma Castle National Monument, May 2024.

NPS

Site Condition

Consistent with past years, we observed slight disturbance from wildlife use at Expansion Spring, with game trails, deer scat, and deer tracks around the lower pool and across the springbrook (Figure 3). Except for an invasive crayfish (discussed next), no other natural or human-caused disturbances were observed at Expansion Spring in 2024.

Figure 3. Left image shows up-turned sediment and trailing vegetation adjacent to the springbrook and right image shows a greenish–gray crayfish laying on the floor of the water pool with pincers extended in front of its head.
Figure 3. Examples of disturbance at Expansion Spring, Montezuma Castle National Monument, May 2024. Left: game trails alongside the springbrook. Right: crayfish detected in the spring.

NPS

For the first time in 2024, we detected invasive non-native crayfish (likely Cambaridae) at Expansion Spring. We did not detect invasive non-native American bullfrog (Rana catesbeiana), and as in past years, we did not observe any invasive non-native plants or any obligate or facultative wetland plants at the spring, though native wetlands plants were abundant along the nearby Beaver Creek corridor.

eDNA Inventory of Rare Species, Invasive Species, and Pathogens

Four water samples were collected and filtered at Expansion Spring during the May 2024 visit. None of our target organisms were detected.

Water Quantity

Sensors are deployed and data are downloaded during our annual visit; the dates of these visits are indicated by black diamonds in the persistence graph (Figure 4). The temperature sensor used to estimate water persistence at Expansion Spring was not found during the 2024 visit; therefore, there are no persistence data available for 2024. As the sensor’s housing and cable were also missing, it is likely they were washed away in a flooding event that past winter. In prior years, Expansion Spring was wetted (contained water) 95.3–100% of the days measured across entire years.

Figure 4. Area chart showing the spring was consistently wet through April 2022, with one period of intermittent dryness occurring March to April 2019. Data are missing from April 2022 to the 2024 visit.
Figure 4. Water persistence through 13 May 2024 in Expansion Spring, Montezuma Castle National Monument. White areas indicate dates before sensors were first deployed or after the 2024 visit. Black diamonds indicate sensor deployment dates.

NPS

In 2024, the estimated volumetric discharge was 66.5 ± 5.4 L/min (17.6 ± 1.41 gal/min), which is substantially lower than the previous mean of 151.1 L/min recorded in 2022 (Table 1). Wetted extent was evaluated using a method for flowing water. In 2024, the total springbrook length was 15.6 m (51.2 ft). Previously, lengths ranged from 11.5 to 21.6 m (37.7 to 70.9 ft). In 2024, width and depth along the springbrook averaged 78.6 cm (30.9 in) and 6.5 cm (2.6 in), respectively. In 2024, the brook was wider than in prior years, whereas brook depth was within the range of previous measurements (Table 2).

Table 1. Discharge data (L/min; mean ± SD) for Expansion Spring in 2024 and a range of means from prior years.
Sampling
Location
2024 Mean
(Range of Prior Means)
Prior Years Measured
(# of Visits with Measurements)
005 66.5 ± 5.4 (151.1) 2022 (1)

Table 2. Length and average (± SD) width and depth of Expansion Spring (measured within the first 100 m of springbrook length) in 2024 and ranges of length values and width and depth means from prior years.
Measurement 2024 Value
(Range of Prior Values/Means)
Prior Years Measured
(# of Visits with Measurements)
Width (cm) 78.6 ± 55.0 (21.3–62.8) 2017–2022 (5)
Depth (cm) 6.5 ± 3.1 (0.3–12.8) 2017–2022 (5)
Length (m) 15.6 (11.5–21.6) 2017–2022 (5)

Water Quality

Core water quality (Table 3) and water chemistry (Table 4) data for Expansion Spring were collected at the primary sampling location in 2024. Dissolved oxygen, pH, and temperature values were within the ranges in prior years. Specific conductivity and total dissolved solids levels were slightly lower than previous measurements. Alkalinity, sulphate, and potassium levels were within the ranges of previous years, with potassium being at the lower end of its respective range. Calcium and magnesium levels were lower than previously recorded, with magnesium being lower than the detectible limit in 2024. Chloride was moderately higher than in previous years.

Table 3. Core water quality data for Expansion Spring in 2024 and a range of values from prior years.
Sampling Location Parameter 2024 Value
(Range of Prior Values)
Prior Years Measured
(# of Measurements)
001 Dissolved oxygen (mg/L) 6.68 (0.85–7.75) 2017–2022 (4)
001 pH 7.31 (7.23–7.49) 2017–2022 (5)
001 Specific conductivity (µS/cm) 518.0 (580.9–883.0) 2017–2022 (5)
001 Temperature (°C) 16.5 (15.5–20.0) 2017–2022 (6)
001 Total dissolved solids (mg/L) 337.0 (377.6–572.0) 2017–2022 (5)

Table 4. Water chemistry data (mg/L) for Expansion Spring in 2024 and a range of values from prior years. b.d.l. = below detection limit.
Sampling Location Parameter 2024 Value
(Range of Prior Values)
Prior Years Measured
(# of Measurements)
001 Alkalinity (CaCO3) 290 (265–350) 2017–2022 (5)
001 Calcium (Ca) 38 (50–66) 2017–2022 (5)
001 Chloride (Cl) 41 (14–32) 2017–2022 (5)
001 Magnesium (Mg) b.d.l. (24–70) 2017–2022 (5)
001 Potassium (K) 4.6 (3.1–35.0) 2017–2022 (5)
001 Sulphate (SO4) 5 (0–8) 2017–2022 (5)

Literature Cited

Author Information

Bryn Callie 1

Annika Munson 1

Cheryl McIntyre 1 ORCID ID Logo https://orcid.org/0000-0001-7554-7586

Andy Hubbard 1 ORCID ID Logo https://orcid.org/0000-0002-4223-7730

Edited by Tani Hubbard 2 ORCID ID Logo https://orcid.org/0009-0009-8777-4773

1 National Park Service
Sonoran Desert Inventory and Monitoring Network
12661 E. Broadway Blvd.
Tucson, Arizona

2 Northern Rockies Conservation Cooperative and National Park Service
12661 E. Broadway Blvd.
Tucson, Arizona

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